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69 69

of of

or or

led led

of of

or or

and and

and and

ester ester

both both

1992, 1992,

forest

of of

should should

pro­

forests

is is

or or

1982, 1982,

number number

1985). 1985).

involve involve

sinks sinks

of of

have have

influ­

supplied supplied

pools pools

and and

indicate indicate

a a

1985, 1985,

nitrogen nitrogen

al. al. is is

numerous numerous

(soluble (soluble

U.S. U.S.

Mitchell Mitchell

result result

Wiklander Wiklander

and and

(Mitchell (Mitchell

increased increased

Zhang Zhang

may may

sulfur

et et

Zech Zech

magnesium

Harrison Harrison

largest largest

a a

in in

weathering

cases cases

reactant. reactant.

sulfate

with with

physico-chemi­

major major

studies studies

constituents constituents

Henderson Henderson

a a

Studies Studies

ecosystems

the the

Soils

as as

Europe

and and

Sulfur Sulfur

the the

and and

(C-bonded (C-bonded

Sparks Sparks

and and

1985, 1985,

1993, 1993,

(Rechcigl (Rechcigl

the the

(Ca), (Ca),

sulfate sulfate

in in

as as

1995 1995

The The

sites, sites,

sulfate sulfate

some some

forests forests

either either

including including

Eastern Eastern

and and

when when

sources sources

up up

1). 1).

1996 1996

of of

sur­

over over

and and

al. al.

total total

of of

and and

These These

, nutrient,

sulfur sulfur soils, soils,

in in

in in

resulted resulted

(Johnson (Johnson

deter­

in in

and and

and and

1986). 1986).

interacts interacts

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et et

and and

May May

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sulfur sulfur

Surface Surface

(fig. (fig.

Zucker Zucker

Mitchell Mitchell

(Foster (Foster

May May

directly directly

(K), (K),

occur occur

production. production.

al. al.

1989). 1989).

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has has

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calcium

form form

total total

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help help

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, carbon,

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cycling cycling

Concern Concern

Canada, ,

sulfur sulfur

cycling cycling

elements, elements,

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(P), (P),

transformations, transformations,

limiting limiting

quantified quantified

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4 4

Rechcigl Rechcigl

to to

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1987, 1987,

1986, 1986,

studied studied

soils soils

nutrient nutrient

et et

problem. problem.

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organic organic

may may

by by

date. date.

of of

sulfur sulfur

soils' soils'

habitat habitat

Watwood Watwood

MOFEP MOFEP

in in

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1993 1993

potassium

ecosystem

1977, 1977,

sulfur sulfur

important important

al. al.

mobility mobility

total total

al. al.

and and

U.S., U.S.,

by by

forest forest

understanding understanding

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sulfur sulfur

this this

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were were

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et et

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sulfur sulfur

1992, 1992,

potassium potassium

1992). 1992).

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1985, 1985,

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However, However,

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precipitation, precipitation,

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forest forest

Mitchell Mitchell

of of

organic organic

essential essential

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August August

Jr.

in in

indicated indicated

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organic organic

better better

Loon Loon

compared compared

phosphorus

interactions interactions

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Lindberg Lindberg

acidic acidic studies studies

added added

cal cal

(Johnson (Johnson

input input

sulfur sulfur

to to

1992, 1992,

to to

1978), 1978),

precipitation precipitation

consideration consideration Lindberg Lindberg

Studies Studies

portion portion

soils soils 1978). 1978).

adsorbed) adsorbed)

that that

sulfur sulfur

Van Van

from from

sulfate; sulfate;

(Mg), (Mg),

(N), (N),

encing encing

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Sulfur Sulfur

Transformations Transformations

carbon carbon

Spratt, Spratt,

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1,4 1,4

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Stolp Stolp

were were

in in

sulfur. sulfur.

in in

is is

1983). 1983).

ofMOFEP ofMOFEP

of of

with with

critical critical

neces­ with with

soil soil

dioxide dioxide

back­

all all

forests forests

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the the

cycles cycles

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carbon carbon

Hemy Hemy

the~ the~

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sulfur sulfur

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mineralization mineralization

pools pools

MOFEP MOFEP

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1977, 1977,

capable capable

possess possess

Kirk Kirk

1988). 1988).

degradative degradative

play play observed observed

essential essential

Sulfur Sulfur

extensive extensive

primary primary

microorgan­

Tennessee Tennessee

other other

in in

keeps keeps

form form

organic organic

up up

both both

al. al.

carbon, carbon,

and and

becoming becoming

and and

carbon carbon

involved involved

are are

soils soils

of of

to to

37403-2598. 37403-2598.

are are

lead lead

and and

presence presence

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measured measured

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et et

complex complex

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Stolp Stolp

associated associated

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splitting splitting

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and and

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watersheds watersheds

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species species

Element Element

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from from

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TN TN

lignocellulose lignocellulose

that that

of of

fungi fungi

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contribute contribute

makes makes

(Tien (Tien

concentrations concentrations

sulfur sulfur

of of

their their

on on

differences differences

part part

Surface Surface

transformations transformations

1993, 1993,

relation relation

from from

cycling cycling

lignocellulose lignocellulose

data, data,

Carbon Carbon

soil. soil.

Biological Biological

and and

in in

system system

going. going.

energy energy

recycle recycle

University University

1996. 1996.

fungal fungal

decomposing decomposing

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plots plots

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of of (Crawford (Crawford

the the

of of

agents agents

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lignin lignin

mechanisms mechanisms

the the

parameters parameters

microorganisms microorganisms

to to

the the

large large

Carbon Carbon

possessing possessing

capable capable

soils soils

their their

in in

elements elements

the the

literally literally

atmosphere

of of

greatest greatest

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and and

in in

for for

May May

Bartha Bartha

producers producers

this this

Soil Soil

are are

help help

magnesium. magnesium.

mine mine

and and

sulfur, sulfur, sulfate,

baseline baseline

to to

Most Most

and and

included included

with with

Chattanooga, Chattanooga,

face face

the the

Abstract.-Carbon Abstract.-Carbon

bacteria

the the

dependent dependent

carbon carbon

fungi fungi

elements elements

role role

these these

ecosystem. ecosystem.

within within

and and

to to

forest. forest.

providing providing

is is

Aspects Aspects

cellulose cellulose

in in

carbon carbon

oxidizing oxidizing

Professor Professor

provide provide

that that

decomposition decomposition

and and

it it

of of

and and

the the

ecosystems. ecosystems.

bacterial bacterial

Other Other

Sciences, Sciences,

the the

primary primary

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transformation transformation

major major

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soils soils

floor floor

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critical critical

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of of

responsible responsible

to to

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webs, webs,

) )

sulfur, sulfur,

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2

Associate Associate

1988). 1988).

1

Chattanooga, Chattanooga,

mental mental

abilities. abilities.

depolymerization depolymerization Certain Certain

(C0

forest forest producing producing

bacteria bacteria

linkages linkages

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Thus, Thus,

lignocellulose. lignocellulose.

forest forest these these

sary sary

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nutrient nutrient

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sulfur sulfur

retention retention

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compounds compounds

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alization alization trant, trant, via via

into into

sulfur sulfur

soil soil

or or

exchange exchange

forest forest

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Figure Figure

1986). 1986).

70 70

microbial microbial

possibly possibly

soil soil

abiotic abiotic

availability availability

microorganisms, microorganisms,

a a

accumulate accumulate

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ecosystem. ecosystem.

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variety variety

soils soils

organic organic

loss loss

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microorganisms microorganisms

I.-Forest I.-Forest

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cations cations

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nutrient nutrient

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1980, 1980,

origin origin

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soils soils

sulfur sulfur

(McLaren (McLaren

(1993) (1993)

of of

added added

organic organic

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where where

mineral

organic organic

found found

forest forest

LEACHING LEACHING

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sulfur sulfur

ATMOSPHERE ATMOSPHERE

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Wiklander Wiklander

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cations cations

compounds compounds

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ca+

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cation cation

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soils soils

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soil. soil.

play play

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sulfur sulfur

cycling. cycling.

potential potential

soils, soils,

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2

et et

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plants

cations cations

positively positively

Mg+

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exchange exchange

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1978). 1978).

with with

fraction fraction

sulfur sulfur

critical critical

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1985), 1985),

2

compounds. compounds.

(Strickland (Strickland

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mineralized mineralized

Forest Forest

be be

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important important

forest forest

either either

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charged charged

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released released

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microbial microbial

K+). K+).

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sulfur sulfur

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role role

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loss loss

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organic organic

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soils soils

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ADSORPTION ADSORPTION

DESORPTION DESORPTION

et et

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4 4

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2

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Solution Solution

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PPT PPT

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K+ K+

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was was

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whole-tree whole-tree

horizon horizon

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soil. soil.

far far

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cation cation served served

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EX})erimental EX})erimental

post-harvest) post-harvest)

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tems tems

adsorbed adsorbed

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spodsols spodsols

4 4

preliminary preliminary

2

and and

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(1989) (1989)

as as

t t

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result result

anthropogenic anthropogenic

change change

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is is

that that

organic organic

reduction reduction

leaching leaching

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Mg

has has

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from from

soils soils

in in

organic organic

Oa Oa

was was

sulfate sulfate

made made

2

MICROBIAL MICROBIAL

MO, MO,

lower lower

the the

ACTIVITIES ACTIVITIES

+ +

harvesting harvesting

of of

soil soil

harvesting harvesting

on on

were were

to to

observed observed

Mitchell, Mitchell,

of of

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effect effect

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Deer Deer

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at at

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sulfur sulfur

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sulfur sulfur

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organic organic

horizons. horizons.

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timber. timber.

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ORGANIC ORGANIC

the the

SULFUR SULFUR

increase increase

were were

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______

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Hampshire Hampshire

Hubbard Hubbard

cycling cycling

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et et

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SOIL SOIL

potential potential

exchangeable exchangeable

(ca. (ca.

forest forest

Mitchell Mitchell

in in

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1989). 1989).

in in

of of

clear­

horizons horizons

Brook Brook

the the

no no

in in

2 2

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1992 1992

from from

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harvest harvest

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____J ____J

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for for

et et

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71 71

& &

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were were

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of of

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were were

pro­

be be

with with

17 17

follow­

site site

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all all

perma­

date. date.

1995 1995

aspect aspect

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helped helped

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1993 1993

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1994 1994

a a

plots plots

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replicate replicate

1996 1996

used used

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ensure ensure

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predictable, predictable,

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September September

different different

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1993 1993

Soil Soil

of of

had had

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10, 10,

plots plots

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to to

experimentally experimentally

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1997). 1997).

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9 9

management) management)

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sites sites

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Control Control

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1994 1994

site. site.

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table table

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subset subset

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et et

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1996, 1996, much much

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plots plots

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Because Because

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(18.C). (18.C).

necessary necessary

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22 22

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1995, 1995,

parentheses]: parentheses]:

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sampled). sampled).

enough enough

year year

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1996 1996

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year. year.

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carefully carefully

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Brookshire Brookshire

three three

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1994 1994

3, 3,

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cutting cutting

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locations locations

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parameters parameters

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16, 16,

1995 1995

possible possible

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from from

on on

2 2

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to to

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collected collected

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7 7

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MOFEP MOFEP

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15 15

1993 1993

sites sites

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low low

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18, 18,

(5.C), (5.C),

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chosen chosen

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in in

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At At

a a

+) +)

2

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Project Project

compli­

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report report

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numbers numbers

the the

Deer Deer

below below

or or

signifi­

and and

due due

of of

soil soil

and and

in in

followed followed

practices practices

long-term long-term

component component

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previously previously

in in

in in

years years

The The

microbial microbial

may may

may may

K+ K+

was was

to to

by by

fall fall

treatments. treatments.

This This

3 3

(Lundgren (Lundgren

microbial microbial

in in

non-manipula­

transforma­

activities activities

and and

this this

study study

post post

forested forested

sample sample

that that

that that

debris debris

undisturbed undisturbed

mineralization mineralization

(e.g., (e.g.,

years years

development development

study study

populations populations

in in

soil soil

constituents constituents

study study

Ecosystem Ecosystem

and and

1995). 1995).

harvest, harvest,

concentrations concentrations

Collection Collection

the the

METHODS METHODS

large-scale large-scale

10 10

practices practices

nearly nearly

observed observed

harvest harvest

1997). 1997).

the the

processing processing

in in

sulfur sulfur

the the

total total

available available

the the

years years

decline decline

other other

of of

this this

to to

activities activities

in in the the

uneven-aged, uneven-aged,

2 2

al. al.

apparently apparently

to to

and and

bacterial bacterial

management management

this this

in in

8 8

sulfur sulfur

production. production.

instrumental instrumental

AND AND

cations cations

transformations transformations

post post

Fritze Fritze

Forest Forest

decaying decaying

for for

et et

timber timber

short-term short-term

experimental experimental

of of

keep keep

sulfur sulfur

or or

led led

be be

soil soil

activity activity

generated generated

these these

involving involving

and and

3 3

to to

by by

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preliminary preliminary

and and

Sites Sites

or or

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marked marked

relationships relationships

relationships relationships

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the the

forest forest

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OBJECTIVES OBJECTIVES

microbial microbial

lignocellulose lignocellulose

present present

findings findings

years years

from from

sulfur sulfur

materials materials

in in

sulfur sulfur

to to

Ozark Ozark

soils soils

to to

depleted, depleted,

of of

Studies Studies

that that

uneven-aged, uneven-aged,

2 2

data data

the the

management management

2 2

any any

materials materials

the the

nutrient nutrient

even-aged, even-aged,

need need

the the

soil soil

soil soil

selection selection

soils. soils.

of of

and and

project project

carbon carbon

of of

objectives objectives

bacterial bacterial

(Brookshire (Brookshire

MATERIALS MATERIALS

approximately approximately

Sample Sample

and and

Once Once

the the

appears appears

result result

organic organic

organic organic

site site

of of

forest forest

1997). 1997).

stimulated stimulated

determine determine

soil soil

determine determine

assess assess

determine determine

a a

Hence, Hence,

Missouri Missouri

Pietikainen Pietikainen

by by

organic organic

clearcut clearcut

indicated indicated

reductions reductions

A-horizon A-horizon

necessary necessary

major major

results results

carbon carbon

and and

soils. soils.

as as

on on

tive tive effects effects

tions tions

even-aged, even-aged, lignocellulose lignocellulose

manipulative manipulative between between

between between

MOFEP MOFEP

To To

To To

To To

To To

first first

the the

labile labile

1. 1.

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4. 4.

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1982, 1982,

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are: are:

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soil soil

ofMOFEP. ofMOFEP.

soils. soils.

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microorganisms microorganisms

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approximately approximately

labile labile

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pattem pattem

harvest. harvest.

material material

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microorganisms microorganisms

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ELT ELT

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plot plot

3 3 4 4

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1 1

Table Table

72 72

As As

Ecologicallandtype Ecologicallandtype

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17. 17.

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C - C

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collected collected

of of

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center center

are are

9 9

8 8 9 9 6 6

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5 5

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7 7

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7 7

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Dennis Dennis

1 1

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located located

26 26

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70 70

55 55

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65 65 42 42

* *

21 21

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21 21

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31 31

40 40

16 16

post): post):

18 18

16 16

15 15

14 14

14 14

3 3

9 9

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sampling sampling

the the

indicates indicates

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in in

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stand stand

stand stand

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study study

classification, classification,

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about about

carbon carbon

1 1

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and and

positions positions

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14

are are

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4 4

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located located

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and and

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plots plots

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ELT ELT

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as as

marked marked

in in

indicated indicated

estimated estimated

70 70

soils. soils.

also also

classification classification

stand stand

A, A,

feet; feet;

ultisol ultisol

ultisol ultisol

ultisol ultisol

ultisol ultisol

ultisol ultisol

alfisol alfisol

ultisol ultisol

ultisol ultisol

alfisol alfisol

alfisol alfisol alfisol alfisol

alfisol alfisol

alfisol alfisol

ultisol ultisol

alfisol alfisol

ultisol ultisol

ultisol ultisol alfisol alfisol

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the the

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transformation transformation

338. 338.

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Dennis Dennis

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determined determined

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center center

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17 17

17 17

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17* 17*

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same same

ridge ridge

site site

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3 3

5, 5, on on

73 73

the the

the the

or or

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not not

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on on

soil soil

placed placed

were were

the the

re­

then then

deter­

are are

of of

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Mis­

con­

1993 1993

for for

vegeta­

at at sterile sterile

removed removed

adminis­

to to

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on on

and and

from from

horizon horizon

15 15

1994 1994

litter

and and

bag. bag.

in in

was was

soils soils

was was

the the

in in

soils soils

2 2

A A

transformation transformation

d.b.h. d.b.h.

and and

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ca. ca.

summed summed

2. 2.

Details Details

Cape Cape

cooler cooler

included included

cm

soil soil

woody woody

with with

taken taken

B-horizon B-horizon

the the

oak oak

August August

em em

of of

a a

A-horizon A-horizon

avoiding avoiding

MOFEP MOFEP

plot plot

in in

sulfur sulfur

study study

placed placed

found found

4 4

horizon, horizon,

Southeast Southeast

sample sample

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soil soil

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100 100

laboratory laboratory

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table table

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plots plots

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into into

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A A

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and and

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spatula spatula

removing removing

September September

B-horizon B-horizon

distribution distribution

1997). 1997).

this this

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ca. ca.

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to to

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in in

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stored stored

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from from

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Number Number

alba) alba)

carbon carbon

taken taken

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et et

total total

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Finally, Finally,

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placed placed

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white white

area area

and and

soil soil

watershed watershed

plots plots

plots plots

darker darker

laboratory laboratory

to to

samples samples

and and

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presented presented

1994), 1994),

organic-rich organic-rich

The The

taken taken

the the

trowel, trowel,

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sampled sampled

collected collected

All All

a a

the the

1996). 1996).

used used

data data

spatula. spatula.

with with

and and

horizon horizon

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litter, litter,

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bag. bag.

of of

University University

in in

soil soil

to to bags, bags,

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for for

the the

B B

of of

in in

3 3

3 3

3 3

3 3

3 3

3 3

3 3

3 3

3 3

much much

data data

down down

cut cut

layer, layer,

27 27

May May

were were

June June

plots plots

Plots Plots

Number Number

soil, soil,

soils. soils.

small small

MOFEP MOFEP

MOFEP MOFEP

(Brookshire (Brookshire

using using

trip trip

The The

sharp sharp

the the

oak oak

a a

floor floor

(1997). (1997).

sampled sampled

only only

State State

the the

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on on

sample sample

sample sample

of of

the the

litter litter

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al. al.

a a

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trators trators

tion tion

methodology methodology

yield yield

mined mined

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Girardeau Girardeau

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4.3 4.3

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7.0 7.0

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5.6 5.6

7.6 7.6

11.1 11.1

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near near

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12 12

h. h.

were were

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site site

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2 2

September September

b. b. of of

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Current Current

Three Three

were were

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Tennessee Tennessee

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each each

figures figures

Number Number

Creek, Creek,

13 13

18 18

36.1 36.1

30 30

42.3 42.3

58 58

20.3 20.3

51.7 51.7

46 46

46 46

of of

1.5 1.5

samples samples

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chromatography. chromatography.

white white

the the

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> >

streams streams

1996 1996

acetate acetate

collected collected

habitat. habitat.

--

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running running

indicated indicated

There There

located located

Mill Mill

on on

surface surface

9, 9,

ion ion

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sample sample

and and

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from from

from from

1995 1995

refer refer

oaks oaks

following following

1995, 1995,

three three

1997). 1997).

samples samples

between between

Mean Mean

until until

habitats. habitats.

frozen frozen

one one

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the the

site site

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located located

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MOFEP MOFEP

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aspect aspect

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24, 24,

ice ice

University University

al. al.

and and

9), 9),

using using

white white

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May May

cellulose cellulose

Creek Creek

of of

one one

March March

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water water

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slope, slope,

& &

et et

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3

water water

please please

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on on

were were

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east east

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Cave. Cave.

collected collected

collected collected

watershed. watershed.

and and

23 23

(UTC) (UTC)

plots plots

plots plots

·c), ·c),

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temperatures temperatures

·c). ·c). concave concave

7 7

watershed watershed

plots, plots,

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sites. sites.

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plots plots

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hours). hours).

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Rodgers Rodgers

May May

0.45-)-lm 0.45-)-lm

placed placed

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Bend. Bend.

soil soil

locations locations

-and -and

1 1

5 5

All27 All27 8 8

6 6

9 9

3 3

7 7

4 4

2 2

6 6

Site Site

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stream stream

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MOFEP MOFEP

Bankers Bankers

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Brookshire Brookshire

beginning beginning

north north

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1995 1995

study. study.

S0

1996 1996

Owls Owls

site site

in in

and and

Table Table

5 5

collection collection Chattanooga Chattanooga

(within (within

for for

For For

site site

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7 7

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Waring Waring

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lignin lignin

Published Published

also also

analysis analysis

litter litter

pestle, pestle,

weight weight For For

weighed weighed

tent tent

ca. ca.

negate negate

although although

treated treated

are are

able able

below); below);

74 74

mine mine

frozen frozen moisture moisture

lignocellulose lignocellulose

1985, 1985,

determined, determined,

sulfate sulfate

incorporation; incorporation;

Mg+ Mg+

and and

ture ture

passing passing

extractable extractable

sieve. sieve.

into into

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MOFEP MOFEP

figure figure

September September

each each

aliquots aliquots

collected collected

collected collected

each each

of of

sites sites

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a1. a1.

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1 1

presented presented

the the

other other

and and

used used

throughout throughout

determination determination

four four

base base

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followed followed

week. week.

and and

from from

were were

1977, 1977,

plot plot

the the

of of

distribution distribution

at at

or or

Crawford Crawford

2. 2.

The The at at

was was

dried dried

changes changes

as as

samples samples

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the the

exactly exactly

watershed watershed

the the

the the

plots plots

the the

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cellulose cellulose

of of were were

K+); K+);

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fractions: fractions:

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replicates replicates

soil soil

Unwanted Unwanted

lost. lost.

from from

from from

B-hortzon B-hortzon

for for

From From

before before

content content

recognizable recognizable

the the

techniques techniques

any any

processed processed

the the

sieved sieved

samples samples

Hackett Hackett

obtained obtained

1994, 1994,

sulfate; sulfate;

81 81

The The

soils soils

laboratory, laboratory,

the the

again, again,

a a

below). below).

then then

elemental elemental

processed processed

total total

were were

(Benner (Benner

mineralization. mineralization.

species species

on on

collected collected

stored stored

third third

the the

and and

the the

of of

Mter Mter

of of

individual individual

three three

as as

until until

August August

due due

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were were

dried dried

the the

litter litter

continuing continuing

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through through

the the

14

samples samples

samples samples

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dried dried

throughout throughout

watershed watershed

MOFEP MOFEP

sulfur sulfur

samples, samples,

gram gram

pooled pooled

a a

C-Labeled C-Labeled

of of

and and

were were

a a

et et

one one

soils soils

for for

root root

total total

ground ground

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3 3

to to

Crawford Crawford

the the

replicate replicate

further further

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fourth fourth

at at

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years years

soils soils

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below). below).

a1. a1.

measure measure

litter litter

determine determine

from from

analysis. analysis.

percent percent

1993 1993

5'C 5'C

then then

the the

according according

at at

for for

percent percent

specifically specifically

be be

a1. a1.

material, material,

dry dry

not not

were were

content content

sulfur sulfur

replicate replicate

1977). 1977).

of of

a a

using using

then then

collected collected

60'C 60'C

were were

plots plots

were were

B-hortzon B-hortzon

radiolabeled, radiolabeled,

measurement measurement

soils soils

to to

2-mm 2-mm

and, and, A-horizon A-horizon

with with

1984, 1984,

in in

of of

woody woody

processing processing

in in

were were

weight weight

MOFEP MOFEP

mixed. mixed.

used used

until until

for for

sample sample

soil soil

plot plot

The The

Lignocellulose Lignocellulose

the the

1976, 1976,

measure measure

dried dried

sampling. sampling.

a a

Note: Note:

sealed sealed

moisture moisture

chopped chopped

moisture moisture

until until nearest nearest

measurement, measurement,

then then

35

and and

moisture moisture

equal equal

mortar mortar

used used

percent percent

within within

and and

sample sample

White White

and and

Beginning Beginning

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removed removed

Benner Benner

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rocks, rocks,

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June June

samples, samples,

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samples samples

plant plant

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basis basis

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label label

at at

Crawford Crawford

Watershed Watershed

all all

the the

site site

all all

subdivided subdivided

collection collection

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extract­

soils soils

weight weight

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to to

soils soils

weight weight

60 60

constant constant

oak oak

14

samples samples

(see (see

3 3

and and

plot plot

data data

1994, 1994,

deter­

up up

mois­

chart chart

pro­

based based

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were were

8 8

the the

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SMSU, SMSU,

14

immediately immediately

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10 10

Analysis Analysis

Figure Figure

C-precursor C-precursor

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14

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July July

either either

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Nuclear, Nuclear,

14

plants plants

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1993. 1993.

leaves leaves

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throughout throughout

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cutting cutting

1977). 1977).

sterile sterile

ends ends

C-cellulose" C-cellulose"

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3 3

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tillation tillation

35

35

as as

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Extratons Extratons

of of

1977). 1977).

leaves leaves

water water

plants plants

to to

remainder remainder

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1 1

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Uptake Uptake

hours. hours.

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Liquid Liquid

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below). below).

syrtnge syrtnge

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plant plant

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1977). 1977).

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1985). 1985).

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72 72

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through through

NJ), NJ),

water water

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counting counting

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weights weights

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placed. placed. removed removed

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31.4 31.4

Finally, Finally,

·c ·c

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free free

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Crawford Crawford

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14

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24 24

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14

solution solution

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lignocellulosic lignocellulosic

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amounts amounts

ran ran

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clear). clear).

vartable vartable

1985, 1985,

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ensure ensure

previously previously

beaker, beaker,

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outside outside

stoppers stoppers

stoppers stoppers connected connected

tubing tubing

cosm). cosm).

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cellulose cellulose

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Mineralization Mineralization

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were were scintillation scintillation

matertal matertal

NaOH NaOH

beled beled

project, project,

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ing ing

Swedesboro, Swedesboro,

Schoniger Schoniger cellulose cellulose

ered ered 1984, 1984,

matertal) matertal)

cellulose." cellulose."

total total

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removed removed

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washed washed extracted extracted

fluid fluid

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conducted conducted

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lanine lanine

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The The matertal matertal

ground ground To To

~~M@W~W------­

76 76

in in

mineralization mineralization

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in in

g g

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hours hours

tions. tions.

completion completion top top remainder remainder perature, perature,

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tubes. tubes.

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sulfur sulfur

of of

technique technique

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Incorporation Incorporation

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(1988). (1988).

the the grounds grounds

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tion tion

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soil soil

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of of

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NaOH NaOH

December December

of of

samples samples

containing containing

rate rate

35

sieved sieved

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mineralization mineralization

found found

-8o·c -8o·c

over over

8-Sulfate 8-Sulfate

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3 3

this this

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in in

technique technique

in in

the the

35

directly directly

The The

pools pools

soil soil

each each

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soil soil

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rate rate

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2

minimize minimize

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May May

the the

1993, 1993,

glass

lost lost

sampling sampling

samples samples

of of

of of

35

1985). 1985).

into into

were were

for for

was was

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soil. soil.

procedure procedure

added added

Maximal Maximal

Incorporation Incorporation

S0

were were

aerobic aerobic

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35

of of

total total

incubator incubator

monitored monitored

Experiments Experiments

35

for for

course course

incubation). incubation).

of of

S-sulfate S-sulfate

the the

due due

from from

to to

technique technique

4

1996, 1996,

August August

Sulfur Sulfur

for for

S-sulfate, S-sulfate,

throughout throughout

Watwood Watwood

The The

12-ml 12-ml used used

change change

were were

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porosity porosity

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duration duration

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arrest arrest

recovered recovered

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incubated incubated

Samplings Samplings

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time time

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potential potential

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dates), dates),

soil soil

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rates rates

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mineralization. mineralization.

rates rates

breakage) breakage)

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Mineralization Mineralization

change change

pmols pmols

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15 15

in in

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Glass Glass

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amount amount

percent percent

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Approximately Approximately

of of

25 25

watershed watershed

Experiments Experiments

the the

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incubation. incubation.

December December

liquid liquid

further further

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In In

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lignin lignin

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sulfate) sulfate)

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organic organic

Fitzgerald Fitzgerald

centrifuge centrifuge

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further further

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filter filter

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experiment experiment

while while

(back­

Of Of

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periods periods

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modification modification

incubations. incubations.

for for

filter filter

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50 50

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by by

of of

incuba­

soil soil

were were

to to

scintilla­

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made made

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of of

of of

the the collect collect

first first

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48 48

the the

at at

placed placed

trans­

tem­

1 1

)lm), )lm),

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sticks sticks

ca. ca.

produce produce

water water

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was was not not

to to

sulfur sulfur

soil soil

were were

ml ml

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1993), 1993),

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35

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fied fied

tions). tions).

tions tions

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horizon horizon

incubation. incubation. 35

mineralization. mineralization.

incubations incubations

to to

35

tubes tubes

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Organic Organic present present

technique technique

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counting. counting.

Schoniger Schoniger

flask flask

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all all

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cation cation

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1986). 1986).

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0.3-ml 0.3-ml

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followed followed

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desiccated desiccated

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total total

of of

liquid liquid

35

each each

mixture), mixture),

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centrifuge centrifuge

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activity activity

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sulfur sulfur

Radiolabeled Radiolabeled

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below below

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35

then then

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combustion combustion

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sulfur sulfur

S0

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Separate Separate

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Spratt Spratt

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dH

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4 4

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35

times times

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MOFEP MOFEP

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Morgan Morgan

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of of

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soil. soil.

10 10

liquid liquid

of of

soils, soils,

radiolabeled radiolabeled

minutes). minutes).

remaining remaining

was was

soil soil

dried dried

distributed distributed

times times dH

up up

organic organic

time time

freezing freezing

at at

dH

a a

and and

72 72

in in

cc), cc),

(3.0 (3.0

dH

to to

and and

watershed watershed

following following

soils soils

mg mg

vo~ex vo~ex

soils soils

on on

subdivided subdivided

sulfur sulfur

salt salt

the the incubated incubated

the the

experiments experiments

which which

2

sites. sites.

of of

2

the the

to to

the the

to to

of of

hours. hours.

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washes washes

initiate initiate

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2

at at

determined determined

immediately immediately

followed followed

1 g g 1

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designated designated

scintillation scintillation

using using

the the

these these

of of

ml ml

soil soil

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(see (see

1990). 1990).

for for

the the

2 2

wash. wash.

mix mix

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centrifuge centrifuge

was was

wash, wash,

mixture mixture

were were

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combustion combustion

The The

or or

soil soil

collected collected

total total

weeks. weeks.

the the

sulfur sulfur

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at at

centrifuge centrifuge

dH

mixer, mixer,

was was

1\venty 1\venty

the the

date date

point point

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salt salt

et et

below), below),

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the the

in in

field field

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quanti­

The The

first first

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extrac­

among among

2

extrac­

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and and

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gener­

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soils, soils,

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of of

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were were

160 160

up up

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2o·c 2o·c and and

with with

by by

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t

was was

0

to to

35

, , S S

77 77

by by

A A

as as

as as

the the

the the

of of

were were

all all

in in

were were

was was

on on

Soil Soil

and and

the the

for for

quanti­

vial. vial.

all all

0 0

soil soil 35

to to

from from used used

determi­

These These

the the

a a

2

soluble soluble

for for

number, number,

using using

deter­

differ­

counter. counter.

total total

samples samples

exactly exactly

1994. 1994.

in in

by by

samples samples

additional additional

of of

dates dates

which which

Care Care

samples samples

liquid liquid

dH

from from

curves curves

the the

radionu­

S S

reactions reactions

"H" "H" counters. counters.

NaOH NaOH

was was

soils soils

Pools Pools

35

1993 1993

determined determined

the the

and and

quench quench

only only

samples samples

one one

were were

using using

mg) mg)

analyses analyses

the the

water water

necessary necessary

used used

centrifuga­

September September

For For

June June

period, period,

into into

of of

C C

quantified quantified

the the

counting. counting.

1409 1409

both both

the the

, acids,

counter counter

of of

S S

of of

moisture moisture

30 30

14

washes). washes).

the the

sample sample

was was

dates. dates.

Counting Counting

instrument instrument

followed followed

35

scintillation scintillation

scintillation scintillation

quench quench

only only extracted extracted

was was

used used

0 0

for for

Sulfur Sulfur this this

made made

determined determined

sulfur sulfur

from from

obtained obtained

cocktail cocktail

2

until until

also also

a a

horizon horizon

August August

(ca. (ca.

scintillation scintillation

external external

of of hydrolytic hydrolytic

pools pools

1994, 1994,

and and

collect collect

quench. quench.

B-

but but

to to

dH

fractions fractions

other other

Wallac Wallac

The The

between between

XR) XR)

sulfur sulfur

(Beckman's (Beckman's

This This

flask, flask,

scintillation scintillation

organic organic

was was

C C

TA TA

Wallac Wallac

adsorbed adsorbed

percent percent

a a total total

After After

liquid liquid

sample sample

were were

to to

Finally, Finally,

fll fll

S, S,

1993 1993

were were

which which

14

the the

all all

From From

colors colors

specific specific

35

Quenching Quenching

and and

correction). correction).

same same

scintillation scintillation

color color

using using

TA TA

the the

scintillation scintillation

aliquot aliquot

the the

Gold Gold

these these

total total

on on

added added

the the

5000 5000

soils. soils.

were were

processed processed

and and

1996 1996

mixing mixing

comparability comparability

1995 1995

using using

Scintillation Scintillation

counterparts; counterparts;

for for

in in

on on

dark dark

an an

the the

for for

sulfate sulfate

of of

scintillation scintillation sulfate sulfate

(2-300 (2-300

litter litter

different different

LS LS

sampled. sampled.

added added

August August

September September

each each

rinsing, rinsing,

5000 5000

extracted extracted

of of

also also

liquid liquid

Schoniger Schoniger to to

dates. dates.

below). below).

counter. counter.

1994, 1994,

and and

quench quench

techniques techniques

May May

the the

on on

plots plots

the the

May May

Ultima Ultima

samples, samples,

on on

a a

in in

to to

no no

stick stick

centrifuged centrifuged

experiments experiments

sulfur sulfur

for for

LS LS

all all

the the

dried dried

of of

ensure ensure

Determination Determination

of of

soils soils

collected collected

Liquid Liquid

from from

in in

(see (see

significant significant

temperature. temperature.

samples samples

were were

present present

and and

using using

on on

to to

washed washed

due due

C C

rinse, rinse, until until

S S

with with

quantified quantified

filter filter

treated treated

adsorbed adsorbed

was was

total total

quantified quantified

were were

accounted accounted

Wallac Wallac

14

radiolabeled radiolabeled

35

Beckman Beckman

above above

0 0

2

room room

(initially (initially

fication fication

nation) nation) combustion combustion

carbon carbon performed performed

September September

and and

horizon horizon

Soil Soil

watershed watershed

soils, soils,

caused caused because because

soils soils

the the

prepared prepared

extraction extraction

and and

(Packard-

clides clides

monitoring monitoring

1994 1994

quantified quantified

biodegradable biodegradable

was was

also also taken taken

March March scintillation scintillation

Beginning Beginning

the the

counter counter

Quantification Quantification

Beckman Beckman

were were

the the

The The tions. tions.

dH

their their ence ence

mined mined

samples samples

soils soils

finally finally

were were

at at

washes washes The The

of of

in in

2N 2N

15 15

the the

soils soils

was was

filter filter

of of

soils soils

HCl HCl

1M 1M

to to

For For

of of

(2,000 (2,000

were were

was was

with with

wash, wash,

mixing mixing

any any

period period

, ,

base base

After After

bottom bottom

five five

also also

were were

vial vial

the the

water water 4

was was

deter­

more more

collec­

washed washed

fll fll

filter filter

scintilla­

6N 6N

rinses). rinses).

the the

the the

dates dates

The The

between between

soil soil

trans­

Fitzgerald Fitzgerald

a a

extraction. extraction.

soils soils

Soil Soil

used used

the the

carefully carefully

of of

water water

adsorbed adsorbed

of of

the the

in in with with

each each

this this

collected collected and and

one one but, but,

the the

(121·c, (121·c,

was was

300 300

each), each),

were were

soils soils

then then

through through

in in

Fractions Fractions

1993 1993

the the

fll fll

in in

strong strong

in in

N~SO N~SO

in in

was was

the the

0 0

and and

solutions solutions

of of

water water

samples, samples,

washes washes

incorporated incorporated

was was

soil soil

2 0), 0),

was was

temperature temperature

base base

of of

remained remained

2

removing removing

vial. vial.

the the

and and

sample sample

soils, soils,

salts salts

extraction extraction

and and

period. period.

centrifuged centrifuged

1M 1M

300 300

incubation. incubation.

The The

dH

pools, pools,

dates dates

the the

minutes) minutes)

dH

to to

the the

with with

pooled pooled

Sulfur Sulfur

of of

Between Between

fraction fraction

1993 1993

salts salts

S-sulfate S-sulfate

samples samples

supernatant supernatant

of of

that that

washes washes

the the

soil/rinse soil/rinse

fll fll

filtrate filtrate

These These

10 10

HCl HCl

extraction extraction

the the

present present 35

present present

autoclave autoclave

stick stick

strong strong

centrifugation. centrifugation.

stick, stick,

cooling, cooling,

were were

other other

fll fll

of of

vial. vial.

addition addition

recovered recovered

with with

on on

December December

1993, 1993,

fraction fraction

g, g,

a a

of of

without without

was was

(Watwood (Watwood

Soil Soil

the the

Cl). Cl).

and and

the the

each each

an an the the

with with

sulfate sulfate

added added

radiolabel radiolabel

times times

12-hour 12-hour

4

all all

/high acid/high

x x

sample sample

(200 (200

soil soil

the the

by by

in in

filter filter

a a

filter filter

washes, washes,

(200 (200

in in

soluble soluble

After After

and and

supernatant supernatant

scintillation scintillation

incubation incubation

each each

NH

on on

during during

six six

before before

and and

the the

S S

and and

above above

pipet pipet

sulfur sulfur

tubes tubes

filtrate filtrate

by by

35

December December

radiolabel radiolabel

washes). washes).

the the

with with

S-sulfate S-sulfate

a a

of of

successive successive

other other

the the

collect collect

radiolabel radiolabel

the the

1M 1M

sequential sequential

amount amount

(2,000 (2,000

strong strong

fraction fraction

each each

35

(as (as

washes washes

0 0

with with

of of

water water

extraction extraction

2

water water

sticks sticks

December December

a a

to to

all all

Ll Ll

placed placed

the the

S-sulfate S-sulfate

The The

adsorbed adsorbed

used, used,

.. ..

and and

to to J J scintillation scintillation

by by

hours. hours.

mixed mixed

extraction extraction

followed followed

August August

involved involved

labeled labeled

the the

the the

35

were were

and and

dH

washed washed

a a

the the

The The

three three

sticks sticks

a a

using using

surfaces surfaces the the

on on

collected collected

, ,

organic organic

20 20

pipet pipet

acid acid

of of

and and

4

successively successively

followed followed

fll fll

sulfur sulfur

during during

minutes), minutes),

filter filter

and and

For For

to to

centrifugation, centrifugation,

were were

to to

by by

were were

using using

centrifuge centrifuge

was was

washed washed

than than

P0

soil soil

for for

wash. wash.

added added

the the

in in

via via

10 10

2

(2-200 (2-200

the the

vial. vial.

filter filter

fate fate

August August soil. soil.

Recovery Recovery

the the

quantify quantify

g, g,

(2-300 (2-300

NaOH, NaOH,

added added

extraction extraction

sticks sticks

centrifuged centrifuged

PSI) PSI)

For For

hydrolysis hydrolysis

made made

Determination Determination

was was

into into

August August

tion tion

before before

time time

samples samples

ferred ferred

NaH the the

salt salt

stick stick

x x were were

the the

following following

onto onto

determine determine

Sequential Sequential

collected collected

the the

thoroughly thoroughly centrifugation, centrifugation,

collected collected

1988). 1988). rinses rinses

soluble soluble

represented represented

washed washed

each each tion tion

of of

centrifugation centrifugation

samples, samples,

soils soils

soluble soluble

mined mined

organic organic

to to

determined determined The The

• •

~ ~

August August

vortex vortex

The The

Adsorbed Adsorbed

the the

analyzed analyzed

acetate acetate

Five Five

peated peated determined determined supematant supematant

fuge fuge

Sulfur Sulfur (2,000 (2,000

repeated repeated

7.0. 7.0.

minute. minute.

mine mine and and

filtered filtered

The The the the

quantified quantified

phate phate and and

was was

soil soil

the the

August August

adsorbed adsorbed ml ml

from from

dH

filter, filter, Total Total

ferred ferred IlOOB IlOOB sulfate sulfate

collected collected

analyzed analyzed

sieving. sieving. bustion bustion

rection. rection.

January January

determined determined

sulfur, sulfur,

traceable traceable

graph graph

flask, flask, to to

CNS CNS

mg) mg)

analyzer analyzer

78 78

standardize standardize

2

of of

M(Q)lFJElP M(Q)lFJElP

mixing/ mixing/

0 0

soil soil

soil soil

remaining remaining

exchangeable exchangeable

Fitzgerald Fitzgerald

water water

adsorbed adsorbed

grams grams

of of

shaken shaken

tube tube

The The

2000 2000

the the

adsorbed adsorbed

20 20

washes), washes),

carbon carbon

I I

using using

solution solution

to to mixer, mixer,

x x

(Spratt (Spratt

= =

the the

atomic atomic

twice; twice;

soil soil

pool. pool.

and and

extraction extraction

was was

ml ml

was was

I993 I993

1993 1993

technique technique

g). g).

Total Total

Approximately Approximately

mM mM

To To

The The

was was

soil soil

two two

forK+ forK+ a a

tube tube

and and

1995, 1995,

on on

sulfate sulfate

along along

Sulfate)). Sulfate)).

soil soil

using using

soluble soluble

dried dried

by by

of of

filter filter

of of

samples samples

centrifugation centrifugation

for for

collected collected

validate validate

using using

The The

calculated calculated

resuspended resuspended

for for

a a

the the

collected. collected.

------

totaled totaled

to to

N~HPO N~HPO

times, times,

phosphate phosphate

dH

and and

and and

The The

Exchangeable Exchangeable

to to

available available

I5 I5

dried dried

used used

combusting combusting

standard standard

sulfate sulfate

and and

Shimadzu Shimadzu

was was

Sulfur Sulfur

adsorption adsorption

on on

was was

the the

I988). I988).

all all and and

sulfate. sulfate.

and and

a a

June June

with with

I5 I5

September September

funnel funnel

2

CNS CNS

soils. soils.

supernatant supernatant

ml ml

ion ion

0 0

pool pool

Leco Leco

centrifuged centrifuged

sulfur sulfur

soil soil

the the

bases bases

the the

procedure procedure

samples samples

sulfate sulfate

Morgan Morgan

for for

instrument, instrument,

thoroughly thoroughly

minutes. minutes.

was was

to to

pooled pooled

soil soil

the the

was was

Mg+

and and

collected collected

the the

chromatography chromatography

approximately approximately

5 5

4 4

in in

-

2000. 2000.

concentrations concentrations

filter filter

I994 I994

determine determine

was was

was was

soil soil

the the

Organic Organic

was was

CNS CNS

ml ml

(Water (Water

Sulfamethazine Sulfamethazine

by by

for for

fitted fitted

This This

final final

2 2

was was

was was

added, added,

a a

0.4 0.4

Both Both

Schoniger Schoniger

the the

were were

solution solution

the the

K+ K+

using using

HIC-6A HIC-6A

vial. vial.

spectrophotometer spectrophotometer

pool pool

and and

of of

analysis analysis

fraction fraction

procedure procedure

difference difference

an an

rinsed rinsed

use use

determined determined

and and

using using

1990). 1990).

in in

added added

samples. samples.

and and

2000 2000

1994 1994

g g

placed placed

used used

final final

total3 total3

supematant supematant

volume volume

Bases Bases

IN IN

The The

with with

(Simard (Simard

the the

aliquot aliquot

was was

of of

over over

the the

for for

Soluble Soluble quantified quantified

then then

mixed mixed

in in

on on

sulfur sulfur

This This used used

a a

and and

and and

Mg+

NH

soil soil

the the

Perkin-Elmer Perkin-Elmer

ion ion

was was

were were

these these

water water

volume volume

an an

elemental elemental

I I

filtrate filtrate

(two (two

funnel. funnel.

for for

to to

this this

collected collected

a a

0 0

the the

frozen frozen

Beginning Beginning

of of

flask flask

4

in in

ml ml

shaken shaken

2 2

3 3

the the

0Ac, 0Ac,

an an

0.45-J.Uil 0.45-J.Uil

was was

process process

minutes minutes

the the

extracted extracted

soluble soluble

ammonium ammonium

to to

(Organic (Organic

chromato­

was was

were were

were were

drift drift

(ca. (ca.

using using

total total For For

ml. ml.

present present

then then

(Watwood (Watwood

I993). I993).

a a

Sulfate Sulfate

period period

project. project.

I-ml I-ml

for for

also also

of of

was was

NIS­

deter­

soils soils

mixture mixture

soluble soluble

centri­

funnel; funnel;

com­

in in

was was

trans­

phos­

pH pH

of of

200 200

after after

was was

re­

The The

cor- the the

One One

the the

for for

a a

and and

used used

was was

was was

for for

in in

+ +

in in

I I

Figure Figure

were were

A-horizon A-horizon

spring spring ably ably

Samples Samples

compared compared

were were

horizon horizon

sample sample

Trends Trends

cluded cluded MOFEP MOFEP

variate variate

contains contains For For

Overall, Overall,

using using

Relationships Relationships

Varian Varian

possibili1y possibili1y

prepared prepared samples samples (alpha=O.lO) (alpha=O.lO)

photometer. photometer.

exchangeable exchangeable

-

-

1-

0 0

-e"' -e"'

-

-

0 0

ca ca

ca ca

E E

0~ 0~

E E £:-20 £:-20

0 0

C) C)

per per

carbon, carbon,

1 1

2 2

different. different.

obsetved obsetved

evident evident

through through

of of

a a

4.-MOFEP 4.-MOFEP

(fig. (fig.

in in

site, site,

Spectr Spectr

repeated-measures repeated-measures

dates dates

in in

Pearson Pearson

soil soil

plots plots

the the

the the

from from

collected collected

only only

10 10

25 25

15 15

in in

30 30

35 35

these these

with with

soils. soils. the the

May-93 May-93

of of 0 0

5 5

4, 4,

August August

largest largest

total total

3 3

line line

IN IN

for for

using using

Atomic Atomic

errors errors

9 9

was was

p

presented presented

Statistical Statistical

three three

years years

data data

bases bases

AAlO AAlO

September September among among

in in

Consideration Consideration

samples samples

represent represent

NH

analyses. analyses.

• •

both both

The The

correlation correlation

represents represents

seasonal seasonal

carbon carbon

MOFEPPlots MOFEPPlots

from from

in in

plots, plots,

4

1993 1993

were were RESULTS RESULTS

SYSTA'f® SYSTA'f®

differences differences

Jan-94 Jan-94

0Ac, 0Ac,

seasons seasons

due due

of of

6 6

atomic atomic

were were

the the

adsorption adsorption

data data

variables variables

carbon carbon

appendix appendix

pre-treatment pre-treatment

7 7

9 9

6 6

here, here,

collected collected

to to

A-horizon A-horizon

determined determined

to to

late late

over over

pH pH

mean mean

to to

Methods Methods

quantified quantified

I994 I994

set set

The The

comparisons. comparisons.

May May

matrix matrix

analysis analysis

mean mean

adsorption adsorption

32 32

Oct-94 Oct-94

analysis. analysis.

and and

5.03 5.03

7.0 7.0

summer summer

and and

9 9

1 1

all all

for for

of of

Date Date seasonal seasonal

range range

in in

were were

Jlmol Jlmol

values values

to to

1996, 1996,

I), I),

total total

standards standards

to to

plots plots

was was

~ ~

the the

in in

total total

of of

sulfur sulfur

(SPSS, (SPSS,

May May

effects. effects.

soils soils

were were

reduce reduce

of of

the the

aU aU

Jun-95 Jun-95

by by

examined examined

using using

C/g C/g

third third

in in

study study

not not

carbon carbon

I I

9 9

numbers numbers

of of

and and

variance variance

early early

carbon carbon

I996, I996,

27 27

spectro­

trends trends

-

a a

early early

notice­

pools pools

3 3

total total

Inc.). Inc.).

dry. dry.

in­

multi­

2 2

plots. plots.

plots plots

year year

the the

a a

were were

on on

fall, fall,

in in

Feb-96 Feb-96 in in A-horizon soils by or treatment indicated 70 no substantial differences. 60 9 Total sulfur in MOFEP plot A-horizon soils also exhibited marked yearly trends over the 2 years analyzed (pt,0~ 8 a. I. 20 l ~.."C Figure. 5.-MOFEP plots, A-horizon soils- total :Eg» sulfur, August 1993 to May 1996; numbers 1 ::::JO 15 through 9 represent mean values of three WE plots per site; line represents mean of all 27 uc: 10 plots. ·--r:::: ca Organic sulfur in MOFEP plot A-horizon soils I.C) 5 was also found to change year to year (p

Organic sulfur production rates for A-horizon then stabilized, with a total of 51 percent of the soils over all dates and plots ranged from 1 to added labeled plant material mineralized over 39 nmol/ g dxy I d. Over the 2 years considered, the 5-week incubation. The lignin moiety of the organic sulfur production exhibited some radiolabeled plant material produced a similar seasonality (p=O.ll4, appendix 4), but no other time course of mineralization; however, there differences in the data were evident. was a notable lag period before the onset of 14 exponential C0 2 release (fig. 8-B). Comparison The presence of white oak on MOFEP plots used of cellulose and lignin mineralization indicates for the soil carbon and sulfur transformation that the cellulose moiety is much more labile, study was determined by summing all white being mineralized approximately twice as fast as oaks> 1.5 in. in diameter (table 2). Some the lignin moiety (1.8 to 2.5 times faster, as differences (p=O.l13, appendix 5) in the num­ calculated for all soils tested from August 1993 bers of white oak present on the plots sampled to June 1994). were detected when compared by block. No differences were obsetved in numbers of white Maximum rates of white oak cellulose mineral­ oaks on the plots in comparisons by treatment. ization, calculated from the exponential portion Plots in blocks 1 and 2 had similar mean num­ of time course experiments, exhibited seasonal bers ofwhite oak trees present (47.8 and 40.2, differences across the pre-treatment period. respectively), while plots in block 3, on average, The overall range of cellulose mineralization had many fewer white oaks (20.3). calculated for all plots and dates was from 0.02 to 1.18 mgCig dxyld (fig. 9-A). Substantial Lignocellulose was mineralized in the micro­ differences (p

900 - 350 ·--0 '6 (J) 800 (J) 300 -Cl) 700 -0 '6 'i5 250 ::E 600 ::E ,w500 ,w200 G) a.. ~ G) 400 > ~ 150 0 300 0 (,) (,) G) G) 100 a: 200 A a: ::E 100 ::E 50 8 a. a. c 0 c 0 0 150 300 450 600 750 900 0 150 300 450 600 750 900 Incubation Time (h) Incubation Time (h)

Figure 8.-MOFEP plots, A-horizon soils- lignocellulose mineralization time course, August 1993, 32"C; mean values for aU plots +I- 1 SE, n=9; note differences in vertical scale; A) cellulose mineralization, B) lignin mineralization. 80

-

2

4 4

of of

in in

81 81

SO SO

(fig. (fig.

to to

con­

the the

2 2

great­

1-1mol/g 1-1mol/g

Feb-96 Feb-96

soils, soils,

treat­

across across

ex­

9). 9).

35 35

in in

2 2

summer. summer.

Mg+

vicinity vicinity

76 76

the the

trends. trends.

other other

summer summer

water water

A-horizon A-horizon

to to

1993 1993

moisture moisture

observed observed

SO/-

large large

sample sample

soil soil

of of

lignin lignin

to to

A-horizon A-horizon

Mg+

7 7

block block

the the

comparisons comparisons

seasonal seasonal

late late

represents represents

the the

for for

future future

had had

Jun-95 Jun-95

late late

IPrr®~~~~fima~:~ IPrr®~~~~fima~:~

soil soil

B) B)

12 12

in in

by by

in in

were were

or or

soil soil

K+ K+

A-horizon A-horizon

1995, 1995,

the the

appendix appendix

line line

fall fall

from from

surface surface

winter winter

over over

August August

dates, dates,

seasonal seasonal

Date Date

differences differences

in in

while while

of of

from from

exhibited exhibited

or or

, ,

Oct-94 Oct-94

A-horizon A-horizon

late late

2

block block

8 8

site, site,

no no

exhibited exhibited

and and

greatest greatest

little little

streams streams

in in

OO

sampled sampled

in in

fall fall

detected detected

MOFEP MOFEP

ranged ranged

also also

Mg+

driest driest

per per

(p<0.01, (p<0.01,

A-horizon A-horizon

concentrations concentrations

differences differences

for for

in in

The The

were were

ranged ranged

of of

only only

September September -

either either

exhibited exhibited

plots plots

late late

K+, K+,

2 2

Jan-94 Jan-94

2

mineralization, mineralization,

the the

for for 4 4

were were

exchangeable exchangeable

dates dates

no no

treatment. treatment.

in in

3). 3).

plots plots

2 2

by by

~ ~

all all

9 9

on on

moisture moisture

Mg+

of of

SO SO

also also

mineralization, mineralization,

by by

lowest lowest

collected collected

dates dates

the the

There There

varied varied

Mg+

were were

For For

differences differences

concentrations concentrations

while while

0 0

May-93 May-93

soil soil

three three

(table (table

differences differences

0.4 0.4

had had

0.3 0.3

0.2 0.2

0.1 0.1

and and

plots plots

cellulose cellulose

soils soils

water water

d:ry. d:ry.

of of

from from

0.35 0.35

0.25 0.25 Variation Variation

0.15 0.15

0.05 0.05

soils soils

concentrations concentrations

g g

A) A)

measured measured

Some Some

compared compared

measured measured

lowest lowest

10-A). 10-A).

exchangeable exchangeable

K+ K+

E E

concentrations concentrations

plots plots

data data

c::: c::: 0 0

ca, ca,

CO'-

~C) ~C)

'-"C '-"C

values values

C) C)

c:::-

;:~ ;:~

~~ ~~

·-() ·-()

::iC) ::iC)

10-B). 10-B).

.5 .5

:::; :::; lignocellulose lignocellulose

centrations centrations

MOFEP MOFEP

(p=0.062), (p=0.062),

dates; dates;

Stream Stream

were were

d:ry. d:ry.

comparisons comparisons

of of

changeable changeable

was was

all all

variation variation

seasonal seasonal The The

samples samples

est est

like like soils soils

Exchangeable Exchangeable

A-horizon A-horizon

horizon horizon

(fig. (fig.

concentration concentration

1-1mol/ 1-1mol/

ment. ment.

soil soil

scale; scale;

oak oak

or or

mean mean

or or

vertical vertical

fall fall

dates dates

0.018, 0.018,

white white plots plots

that that

7 7

9 9

g g

~ ~

2 2

also also

8 8

white white

the the

in in

plots plots

of of

mgC/g mgC/g

lowest lowest

(compare (compare

lignin lignin

lignin lignin

soils soils

the the

summer summer

the the

late late

mineral­

plots plots

and and

all all

sampled. sampled.

Feb-96 Feb-96

correlation correlation

rates rates

or or

represent represent

sampled. sampled.

in in

the the

treatment treatment

for for

on on

cellulose cellulose

soil soil

cellulose cellulose

soils-

0.37 0.37

late late

the the

9 9

for for

at at

concentrations concentrations

dates dates

of of

lignin lignin

to to

in in

between between

and and

on on

oak oak

numbers numbers

differences differences

period period

all all

differences differences

dates dates

of of

differences differences

Jun-95 Jun-95

(r=0.012 (r=0.012

future future

A-horizon A-horizon

Pearson Pearson

present present

on on

cellulose cellulose

0.01 0.01

fall, fall, rates rates

mineralization mineralization

the the

occurred occurred

the the

the the

through through

a a

highest highest

A-horizon A-horizon

white white

note note

A-horizon A-horizon

1 1

and and

differences differences

rates rates

Date Date

the the

present present

oak oak

late late

of of of of

from from over over

trees trees

mineralized mineralized

plots plots

Oct-94 Oct-94

the the

with with

over over

soils soils

measured measured

seasonal seasonal

seasonal seasonal

A A

MOFEP MOFEP

correlation correlation

in in

detected detected

using using

Lignin Lignin

8) 8)

7) 7)

mineralization mineralization

plots, plots,

all all

plots; plots;

block block

than than

in in

oak oak

was was

white white

rates rates

Lowest Lowest

were were

was was

by by

for for

nwnbers nwnbers

K+ K+

basis, basis,

of of

of of

ranged ranged

Jan-94 Jan-94

made made

diameter diameter

9-B). 9-B).

n=27). n=27).

noticeable noticeable

lignin lignin

B). B).

all27 all27

lower lower

white white

detected detected

2 2

9 9

A-horizon A-horizon

lignin lignin

9-

in. in.

of of

noticeable noticeable

no no

noticeable noticeable

of of

significant significant

appendix appendix

and and

appendix appendix

of of

1996; 1996;

rates rates

Comparisons Comparisons

were were

dates dates

for for

annual annual

9.-MOFEP 9.-MOFEP

(fig (fig

1.5 1.5

mineralization mineralization

oak oak

1 1

0 0

No No

May-93 May-93

. .

were were

much much

all all

9-A 9-A

the the

d d

> >

rates rates

1.2 1.2

08 08

0.6 0.6

0.4 0.4

0.2 0.2

an an

mineralization. mineralization.

mean mean

May May

I I

K+ K+

>., >.,

E E

(p=0.05, (p=0.05,

concentrations concentrations

of of

On On

Exchangeable Exchangeable exhibited exhibited

mineralization mineralization

(J (J

studied studied number number

and and test. test.

respectively, respectively,

sampled. sampled. oak oak

lignin lignin

(p<0.05, (p<0.05, Comparisons Comparisons

d:ry d:ry

mineralization mineralization

indicated indicated

ization ization exhibited exhibited

over over

mineralization mineralization

figs. figs.

winter. winter.

were were

Figure Figure The The

White White

c::: c:::

~- 0 0

c::: c:::

CI)"C CI)"C

CG CG ::::s ::::s

CI)C) CI)C)

~ ~

......

......

=~ =~

:i~ :i~

·-

G) G)

-

-- 0 0 ------

~M©WEW------

80 2 5 3 3 ij 8 30 A 70 1 N 9 9 + C) 60 3 8 :E- 2 a (1)~50 9 jl"C mg40 ao ce 30 .s:::_cu:::i. 2 2 7 2 CJ 20 @! 7 >< 9 LIJ 7 5 10 I)! 0 +----+---+---+----+--' 0 May-93 Jan-94 Oct-94 Jun-95 Feb-96 May-93 Jan-94 Oct-94 Jun-95 Feb-96 Date Date Figure 10.-MOFEP plots, A-horizon soils -exchangeable potassium and magnesium, August 1993 to May 1996; numbers 1 through 9 represent mean values of three plots per site, line represents mean of all 27 plots; A) potassium, B) magnesiwn.

sample dates (fig. 11). Sulfate concentrations pared by season. Sample site aspect and slope from all collection sites over all dates ranged location resulted in little difference in the B­ from 12 to 57 11M. horizon total carbon. From March to May 1996, the largest change in total carbon for litter, A-, Watershed Plots and B-horizon soils was measured for A-horizon soils collected from south and west aspect plots. The watershed plots, located in MOFEP sites 1, high in the landscape (figs. 12-A and 12-B). 3, and 4, represent a subsample of the larger The change in total carbon for these soils from carbon and sulfur study of MOFEP, including March to May was an increase of nearly 30 sample plots with both south and west aspect percent (from 18 to 23 !lmol/g chy). and north and east aspect, as well as plots positioned both high and low on the slopes. If A closer look at total carbon in A-horizon soils we consider data from two dates (March and from south and west aspect watershed plots May 1996). total carbon in watershed plots was high in the landscape indicated these soils greatest in forest floor litter on the winter followed the same basic pattem for total carbon sampling date (mean values across south and observed in A-horizon soils from the MOFEP west and east and west aspects, and both plots (see fig. 4). The highest concentrations of landscape positions were approximately 40 total carbon in these watershed A-horizon soils 11mol/ g chy), and somewhat lower in the spring (up to 30 !lmol/g chy) were measured in the (mean values ranging from 37 to 39 !lffiOl/ g dry, early fall; the lowest concentrations were ob­ figs. 12-A and 12-B, p<0.01, appendix 10). served in the winter (as low as 20 f.lmol/g dry, Total carbon in litter from watershed plots fig. 13). The only possible difference in A­ exhibited no noticeable differences when com­ horizon soil total carbon for watershed plots pared by aspect or slope position. In March (p=0.145, appendix 12). occurred when the data 1996, A-horizon soil total carbon ranged from were compared by season. Comparison of the 18 to 24 11mol/ g chy; the largest difference data by aspect or slope position indicated between the total carbon in litter and A-horizon minimal differences in the A-horizon soil total soil was found for samples from south and west carbon. aspect sites, high in the landscape. Total carbon in B-horizon soils exhibited noticeable Lignocellulose mineralization in A-horizon soils differences (p=0.086, appendix 11) when com- of watersheds also followed the general trends 82

------··--·------

M©IFltiP • 45 45 40 40 35 35 s::- o>- s::- 30 .a"""... 30 o>- , .a""""-'ti CfS~25 25 00 00CfS~ CGE20 20 oE CGE t-- 15 t--oE 15 10 10 5 5 0 0 S& S& N& N& S& S& N& N& W- W- E- E- W- W- E- E- HI LO HI LO HI LO HI LO Landscape Location Landscape Location

Figure 12.-Watershed plots, litter, A- and B-horizon soils- total carbon, March and May 1996; S& W=southwest aspect, N&E=northeast aspect, HI=near top of slope, W=near bottom of slope; mean values+/- 1 SE, n=9; A) March 1996, B) May 1996.

obsenred for A-horizon soil from MOFEP plots over the period May 1995 to May 1996 (see fig. 30 -r------. 9-A). Noticeable differences in cellulose miner­ alization were obsenred for A-horizon soils comparing May 1995 and March 1996; May 25 1996 had the highest rates (fig. 14-A, p=0.024, appendix 13). The rates of cellulose mineraliza­ s>:20 tion in May 1995 and March 1996 ranged from .c""' 0.2 to 0.3 mgC/g d:ry/d for A-horizon soils from I.., all watershed plots. No notable differences in ~g 15 rates of cellulose mineralization were detected _o in comparisons of site aspect or slope location. SE • S&W-HI ~.s10 D S&W-LO White oak lignin mineralization in A-horizon --A--N&E-HI soils from watershed plots, as obsenred for MOFEP plots (see figs. 9-A and 9-B), was much ---X-- -N&E-LO 5 lower than cellulose mineralization for all dates and sample locations. The differences in rates 0+----r----~--~--~ of lignin and cellulose mineralization for water­ Apr-95 Aug-95 Nov-95 Feb-96 May-96 shed A-horizon soils ranged from 2.5- to 12.5- fold, with lignin mineralization always lower Date th211 cellulose mineralization (fig. 14-B). For all dates and plots, rates of lignin mineralization ranged from 0.02 to 0.08 mgC/g dry/d. Rates of lignin mineralization in A-horizon soils were Figure 13.-Watershedplots, A-horizon soils­ marginally greater in May 95 than March 96 total carbon, May 1995 to May 1996; S&W= (p=0.159, appendix 14). No differences in lignin southwest aspect, N&E=northeast aspect, mineralization for watershed plots were ob­ HI=near top of slope, W=near bottom of senred when compared by site aspect or slope slope; mean values +I- 1 SE, n=9. location. 84

85 85

in in

the the

2 2

15). 15).

to to

soils soils

17). 17).

May-96 May-96

fig. fig.

plots plots

bottom bottom

plots) plots)

6). 6).

con­

fall fall

have have

basic basic sulfur sulfur

fall, fall,

soils soils

data­

over over

also also

mea­

all all

March March

(see (see

sulfur sulfur

1995 1995

year year

to to

sulfur sulfur

fig. fig.

total total

A-horizon A-horizon

late late

on on

aspect aspect

total total

early early

same same

indicated indicated

the the

a a

in in

Feb-96 Feb-96

soils soils

plots plots

appendix appendix

The The

3-year 3-year

soil soil

total total

May May

appendix appendix

A-horizon A-horizon

(see (see

MOFEP MOFEP

tend tend

of of

plots plots

mineralization, mineralization,

total total

(highest (highest

in in

of of

W=near W=near

the the

in in

plots plots

west west

in in

A-horizon A-horizon

year year

for for

the the

approximately approximately

soil soil

S&W-LO S&W-LO

S&W-HI S&W-HI

1 1

differences differences

-N&E-LO -N&E-LO

plots plots

of of

for for

include include

trend trend

horizon horizon

Date Date

and and

found found

aspect aspect

slope, slope,

Nov-95 Nov-95

to to

(p<0.01, (p<0.01,

May May

MOFEP MOFEP

with with

percent percent

the the

• •

B-

cellulose cellulose

0 0

p=0.069, p=0.069,

aspect aspect

of of

watershed watershed

A-horizon A-horizon

not not

(p=0.022). (p=0.022).

in in

followed followed

(loss (loss

changes changes

50 50

A) A)

---X--

--.--N&E-HI --.--N&E-HI

same same

of of

aspect aspect

same same

16, 16,

plots plots

top top

south south

1996 1996

the the

sulfur sulfur

from from

plots plots

concentrations concentrations

did did

east east

A-horizon A-horizon

mineralization, mineralization,

concentrations concentrations

observed observed

May May

Aug-95 Aug-95

the the

the the

for for

(fig. (fig.

west west

concentrations concentrations

the the

scale; scale;

although although

May May

study study

from from

and and

total total

by by

8 8

of of

percent). percent).

sulfur sulfur

of of

sulfur sulfur

that that

to to

of of

significant significant

landscape landscape

HI=near HI=near

and and

35 35

higher higher

the the

however, however,

...------: ...------:

dates dates

substantial substantial

pattern pattern

watershed watershed

0-1----+-----+-----+-----1 0-1----+-----+-----+-----1

sulfur sulfur

evident evident

plots plots

Apr-95 Apr-95

watershed watershed

north north

to to

collection. collection.

the the

dry). dry).

total total

vertical vertical

concentrations concentrations

0.1 0.1

in in

approximately approximately

0.2 0.2

were were

g g

of of

in in

do do

21 21

for for March March

sampled, sampled,

in in

lignocellulose lignocellulose

south south

organic organic

not not

aspect, aspect,

indicates indicates

watersheds watersheds

oak oak

seasonal seasonal

MOFEP MOFEP Organic Organic

high high

of of

sample sample

sampled, sampled,

sured sured The The

5) 5)

lowest lowest

year year centrations centrations

data data

Comparison Comparison

base base

sampling sampling was was

somewhat somewhat

than than

sulfur sulfur

that that

J..lmOl/ J..lmOl/

concentration concentration

Extending Extending

losing losing

from from

exhibited exhibited

from from

white white

of of

on on

differences differences

for for

the the

in in

soils soils

and and

and and

west west

sulfur sulfur

42 42

dates dates

dry dry

May-96 May-96

T T

soils soils

com­

had had

note note

I I

total total

usually usually

f f

detected detected

N&E=northeast N&E=northeast

total total

f f

soils-

to to

,' ,'

g g

I I

, ,

sulfur sulfur

the the

f f

approxi­

cases, cases,

and and

north north

I I

either either

or or

both both

1 1

l l

measured measured

slightly slightly

total total

of of

aspects aspects

1 1

' '

~~~ ~~~

south south

both both

27 27

sample sample

dates. dates.

had had

was was

n=9; n=9;

sites sites

in in

all all

(increases (increases

in in

on on

were were

had had

sulfur sulfur

A-horizon A-horizon

differences differences

total total

on on J..lmolj J..lmolj

by by

from from

noticeable noticeable

Feb-96 Feb-96

In In

very very

litter litter

aspect, aspect,

1996, 1996,

both both

south south

5 5

SE, SE,

17) 17)

from from

15) 15)

Substantial Substantial

both both

sulfur sulfur

while while

B-horizon B-horizon

plots plots

than than

Litter Litter

soils soils

1 1

A-horizon A-horizon

soil soil

16). 16).

sites sites

total total

to to

soils, soils,

had had

for for

aspect aspect

had had

in in

on on

1-

2 2

May May

of of

both both

sulfur sulfur

either either

+ +

total total

notable notable

15-B). 15-B).

S&W-LO S&W-LO

S&W-HI S&W-HI

soils, soils,

soils soils

ranging ranging

Date Date

dry dry

-N&E-LO -N&E-LO

1996 1996

Nov-95 Nov-95

In In

positions positions

dates. dates.

plots, plots,

east east

in in

soils soils

of of

soils soils

ranging ranging

g g

aspect aspect

from from concentrations concentrations

total total

from from

appendix appendix

appendix appendix

and and

• •

D D

sampled. sampled.

1996 1996 two two

watershed watershed

appendix appendix

and and

B-horizon B-horizon

soils, soils,

values values

samples samples

W=southwest W=southwest

than than

---X--

1996. 1996.

--.--N&E-HI --.--N&E-HI

March March

J..tmOl/ J..tmOl/

west west

of of

litter litter

same same

Soils Soils all all

indicated indicated

Aug-95 Aug-95

the the

orB-horizon orB-horizon

15-A 15-A

the the

S& S&

A-horizon A-horizon

dates dates

4 7 7 4

of of

ranging ranging

landscape landscape

A-horizon A-horizon

A A north north

mean mean

mineralization. mineralization.

in in

A-

A-horizon A-horizon

on on

for for

and and

concentrations concentrations

March March

lower lower

(p<0.01, (p<0.01,

the the

with with

concentrations concentrations

to to

(p=0.022, (p=0.022,

date date

the the

(p<0.01, (p<0.01,

March March

or or

(figs. (figs.

1996; 1996;

soil, soil,

concentration concentration

and and

-.------: -.------:

dates. dates.

dry dry

and and

in in

31 31

0~----r---~-----+----~ 0~----r---~-----+----~

14.-Watershed 14.-Watershed

in in

concentrations concentrations

Apr-95 Apr-95

with with

1 1

lignin lignin

g g

slope; slope;

sulfur sulfur

south south

aspect aspect

orB-horizon orB-horizon

much much

sulfur sulfur

0.4 0.4

aspect aspect

0.6 0.6

0.8 0.8

data data

1.2 1.2

different different

litter, litter,

of of

B) B)

May May

samples samples

comparisons comparisons

compared compared

pared pared

increases increases

sulfur sulfur

east east

essentially essentially

aspect, aspect,

increased increased

sample sample

for for west west

highest highest

J..tmOl/ J..tmOl/

Comparison Comparison

this this

from from

collection collection

sulfur sulfur

differences differences

the the

in in

horizon horizon

all all

studied studied

total total

analyzed analyzed mately mately

were were

litter litter

greater greater

Figure Figure Total Total

CJ)~ CJ)~

'S"C 'S"C

1-.,:; 1-.,:; c;o c;o

_ _

oE oE

......

::::~>-

• •

......

-o -o

-

!e !e

en~ en~

="C ="C

::I ::I

......

o::::t o::::t ......

::I~ ::I~

~ ~

-

_ _

Figure Figure

p=0.019, p=0.019,

86 86

soils soils

steadily steadily plots plots

Figure Figure

30 30

50 50

40 40

60 60 20 20

10 10

Apr-95 Apr-95

0+-----~----~------+-----~ 0+-----~----~------+-----~

of of

S& S&

aspect, aspect,

OO©IFJEJP OO©IFJEJP

total total

20 20

30 30 40 40

50 50

10 10

60 60

S& S&

mean mean

···················································································· ····················································································

0 0

from from

were were

slope; slope;

W=southwest W=southwest

W=southwest W=southwest

16.-Watershedplots, 16.-Watershedplots,

15.-Watershed 15.-Watershed

through through

sulfur, sulfur,

appendix appendix

values values

Aug-95 Aug-95

south south

S& S&

W-

greatest greatest

HI=near HI=near

HI HI

mean mean

Landscape Landscape

May May

--A--N&E-HI --A--N&E-HI

---X--

·······H······S&W-LO ·······H······S&W-LO

and and

+I-

the the

values values

• •

in in

Nov-95 Nov-95

18). 18).

top top

Date Date

1995 1995

S& S&

LO LO

W-

aspect, aspect,

1 1

aspect, aspect,

next next

west west

the the

-N&E-LO -N&E-LO

SE, SE,

S&W-HI S&W-HI

of of

plots, plots,

A-horizon A-horizon

+I-

to to

slope, slope,

spring spring

early early

aspect aspect

n=9; n=9;

Location Location

May May

N&E=northeast N&E=northeast

N&E=northeast N&E=northeast

Feb-96 Feb-96

A-horizon A-horizon

1 1

litter, litter,

N& N&

HI HI

-E- E-

SE, SE,

A) A)

fall fall

W=near W=near

(fig. (fig.

1996; 1996;

watershed watershed

March March

A-

soils soils

n=9. n=9.

and and

17, 17,

and and

May-96 May-96

soils­

......

N& N&

LO LO

declined declined

A A

from from

1996, 1996,

bottom bottom

B-horizon B-horizon

aspect, aspect,

B) B)

May May

Figure Figure

landscape landscape

sulfur sulfur

J.liT"oll J.liT"oll

south south

'S"C 'S"C

en~ en~ c;o c;o

_ _

~~ ~~

HI=near HI=near

3

soils-

-;: -;:

HI=near HI=near

......

organic organic

slope; slope;

southwest southwest

1996. 1996.

g g

50 50

60~------: 60~------:

60 60

50 50

30 30 4o 4o

and and

20 20

10 10

10 10

over over

17.-

Apr-95 Apr-95

total total

0~----+-----+-----~----~ 0~----+-----+-----~----~

0 0

dry). dry).

top top

mean mean

had had

west west

sulfur, sulfur,

the the

top top Watershed Watershed

sulfur, sulfur,

of of

S& S&

Soils Soils

W-

HI HI

aspect, aspect,

a a

sample sample

slope, slope,

of of

values values

aspect aspect

Aug-95 Aug-95

slight slight

Landscape Landscape

May May

slope, slope,

March March

from from

---X-- ·······H······S&W-LO ·······H······S&W-LO

--A--N&E-HI --A--N&E-HI

W=near W=near

N&E=northeast N&E=northeast

+I-

1995 1995

• •

plots, plots,

plots plots

period period

increase increase

S& S&

W-

LO LO

W=near W=near

both both

Nov-95 Nov-95

and and

Date Date

1 1

-N&E-LO -N&E-LO

S&W-HI S&W-HI

SE, SE,

to to

located located

A A

slope slope

(from (from

May May

-horizon -horizon

May May

bottom bottom

Location Location

in in

n=9. n=9.

N& N&

E-

HI HI

bottom bottom

Feb-96 Feb-96

organic organic

1996; 1996;

locations locations

1996; 1996;

33 33

low low

aspect, aspect,

of of

soils soils

up up

in in

slope; slope;

of of

S& S&

to to N& N&

LO LO

E-

the the

May-96 May-96

-

in in

38 38 W= W=

K+ K+

. .

87 87

to to

and and

May May

west west

in in

n=9 n=9

22 22

to to

or or

22). 22).

aspect aspect

nmol/ nmol/

May May

con­

water­

greater greater

and and

and and

west west

soils­

10-A 10-A

pattern pattern

Potas­

SE, SE,

than than

through through

of of

east east

W=near W=near

date. date.

1 1

observed observed

and and May-96 May-96

(from (from

from from

1,300 1,300

March March

compared compared

and and

while while

N&E=north­

aspect, aspect,

to to

appreciably appreciably

figs. figs.

differences differences

A-horizon A-horizon

concentra­

fall fall

percent, percent,

dry. dry.

sites sites

south south

March March

+I-

and and

2 2

exchangeable exchangeable

appendix appendix

in in

were were

slope, slope,

soils soils

not not

34 34

of of

from from

(see (see

late late

seasonal seasonal

March March

date date

A-horizon A-horizon

date, date,

Mg+

south south

of of

20-A). 20-A).

20). 20).

percent percent

some some

from from

Date Date

K+ K+

aspect, aspect,

(increases (increases

north north

aspect aspect

values values

by by

J.lmol/g J.lmol/g

13 13

for for

p>0.2, p>0.2,

top top

were were

higher higher

in in

from from

plots plots

(fig. (fig.

of of

from from

same same

landscape, landscape,

plots, plots,

soils soils

30 30

data data

east east

between between

approximately approximately

21) 21)

A-horizon A-horizon

mean mean

the the

the the was was

to to

plots plots

20-B, 20-B,

soils soils

about about

2 2

appendix appendix

indicated indicated

dates dates

mineralization, mineralization,

to to

in in

lowest lowest

Mar-96 Mar-96

Comparison Comparison

and and

on on

change change

22 22

1996 1996

HI=near HI=near

MOFEP MOFEP

concentrations concentrations

by by

compared compared

approximately approximately

increased increased

Mg+

(fig. (fig.

exchangeable exchangeable

K+ K+

up up

slope; slope;

soils soils

the the

low low

for for

A-horizon A-horizon

were were

sulfur sulfur

dry). dry).

from from

followed followed

of of

north north

only only

was was

soil soil

increased increased

appendix appendix

sample sample

S&W=southwest S&W=southwest

when when

p=O.l04, p=O.l04,

March March

aspect, aspect,

watershed watershed

A-horizon A-horizon

For For

Highest Highest

plots plots 19.-Watershed 19.-Watershed

plots plots

but but

location location

in in

in in

also also

plots plots

from from

fourfold, fourfold,

1996 1996

the the

1996; 1996;

bottom bottom

east east

organic organic

B). B).

J.lmol/g J.lmol/g

spring spring

observed observed

A-horizon A-horizon

dry/d. dry/d.

1996, 1996,

10-

soils soils

slope slope

(p=O.l37, (p=O.l37,

Exchangeable Exchangeable

tions tions

different different

plots plots

25 25

sium sium

in in

May May

increasing increasing

shed shed

aspect aspect

centrations centrations

on on

Exchangeable Exchangeable

as as

A-horizon A-horizon

than than

winter. winter.

g g

mineralization mineralization

aspect aspect

with with Figure Figure

41 41

in in

rate rate

for for

n=9. n=9.

May May

to to

in in

(fig. (fig.

rates rates

to to

ob­

winter, winter,

but but

the the

produc­

on on

soils­

MOFEP MOFEP

d d

May May

30 30

SE, SE,

sulfur sulfur

ranged ranged

I I

horizon horizon

from from

watershed watershed

W=near W=near

supported supported

May-96 May-96

1 1

in in

in in

the the

differences differences

A-

A-horizon A-horizon

A-horizon A-horizon

N&E=north­

all all

dry dry

1995 1995

trend trend

measured measured

1996, 1996,

(from (from

based based

highest highest

sulfur sulfur

+I-

g g

measured measured

in in

consistently consistently

winter, winter,

rates rates

for for

for for

declining declining

measured measured

plots plots

slope, slope,

For For

S&W-HI S&W-HI

ranged ranged

organic organic

-N&E-LO -N&E-LO

May May

A-horizon A-horizon

during during

were were

The The of of

late late

Feb-96 Feb-96

notable notable

that that

of of

had had

aspect, aspect,

collected collected

was was

nmol/ nmol/

March March

values values

• •

sulfur sulfur

sulfur sulfur

18). 18).

sulfur sulfur

d. d.

production production

top top

organic organic

percent percent

plots plots

seasonal seasonal

I I

observed observed

In In

plots, plots,

rate rate

spring. spring.

······H·······S&W-LO ······H·······S&W-LO

with with

--.l--N&E-HI --.l--N&E-HI

---X--

than than

of of

sites sites

300 300

34 34

plots plots

(fig. (fig.

dry dry

the the

production production

watershed watershed

19) 19)

mean mean

to to

through through

the the

declining declining

g g

Date Date

late late

Nov-95 Nov-95

sulfur sulfur

samples samples

production, production,

rate rate

organic organic

organic organic

organic organic

mineralization mineralization

production production

1996. 1996.

lower lower

date date

dates, dates,

HI=near HI=near

fall fall

from from

150 150

of of

of of

about about

aspect aspect

of of

for for

the the

sulfur sulfur

watershed watershed

rates rates

slope; slope;

The The

by by

W=southwest W=southwest

1996, 1996,

nmol/ nmol/

in in

May May

sulfur sulfur

of of

all all

sulfur sulfur

watershed watershed

samples. samples.

east east

sulfur sulfur

organic organic

early early

S& S&

soils soils

much much

appendix appendix

7). 7).

55 55

Aug-95 Aug-95

supporting supporting

aspect, aspect,

sample sample

with with

May May

dry) dry)

lB.-Watershed lB.-Watershed

and and

to to

for for

organic organic

and and

g g

was was

(fig. (fig.

from from

In In

from from

3 3

increased increased

1995 1995

from from

the the

measured measured

fall, fall,

1996; 1996;

bottom bottom

east east

organic organic

production production

organic organic

organic organic

0+-----+-----t-----+--~ 0+-----+-----t-----+--~

19). 19).

Apr-95 Apr-95

approximately approximately

of of

soils soils

soils soils

March March

Mineralization Mineralization

1996 1996

Figure Figure

70 70

60 60

served served

of of

plots plots May May

tion tion

(p=0.020, (p=0.020,

plots, plots, J.lmol/ J.lmol/

late late

from from

10 10

soils soils

40 40

comparisons comparisons basically basically

over over

then then

30 30

concentrations concentrations

the the

north north

A-horizon A-horizon

"-

c c

e e

o:!2 o:!2

_, _,

"->'o "->'o

:::JC) :::JC)

uc uc

as as

E> E>

u u

. .

-5-50 -5-50

il. il.

;=s ;=s

cne cne

'2-20 '2-20 0 0 ------

~ • OO< () 15 w 10 • S&W-HI w>< • S&W-HI D S&W-LO 10 D S&W-LO 5 _...,.__N&E-HI --A--N&E-HI ---X-- -N&E-LO 5 ---X-- -N&E-LO 0+------r------r-----,_----~ 0 Apr-95 Aug-95 Nov-95 Feb-96 May-96 Apr-95 Aug-95 Nov-95 Feb-96 May-96 Date Date

Figure 20.-Watershedplots, A-horizon soils- exchangeable potassiwn and magnesiwn, May 1995 to May 1996; S& W=southwest aspect, N&E=northeast aspect, HI=near top of slope, W=near bottom of slope; mean values +I- 1 SE, n=9; A) potnssiwn, B) magnesium

soils from south and west aspect sites. Com­ this report may be due to changes in soil mois­ parison of the watershed exchangeable Mg+2 ture content over the year. Moisture levels can data with that from the MOFEP plots (see fig. have pronounced effects on the activity of 10-B) indicates some differences in the two microorganisms (Atlas and Bartha 1993), and if datasets. For example, between March and May the parameter being tested is the result (either 1996, Mg+2 A-horizon soils declined somewhat direct or indirect) of some microbial activity, for MOFEP plots, but increased for watershed then it should be expected to differ by soil plots. moisture content. Whatever the difference detected in the pre-treatment dataset, having a DISCUSSION baseline of the parameter of interest, and knowing something of the natural variation over The pre-treatment portion of this study has several seasons occurring in that parameter sexved a vital role in helping to establish should help in comparing data collected after baseline data that will be used to determine if the experimental treatment. changes in the parameters measured after treatment might be due to the treatment. In looking at the data sets presented in this Natural variation in forest ecosystems is great; report, we found that soil total carbon varied however, if any trends in data sets can be from the litter layer down through the A and B determined prior to an experimental treatment, horizons. This would be expected, because the then a higher level of certainty of the treatment primacy source of carbon to the surface soils effect should be obtained. In the pre-treatment would be litter fall. As soil microorganisms carbon and sulfur transformation data pre­ decompose this litter, labile components of the , sented here, the data have been compared by litter will be released as C0 2 leaving behind season, replicate grouping of sites (block), site more refractile compounds to become part of aspect, and slope location (high or low). In the soil humus (Atlas and Bartha 1993). For many cases very noticeable differences (p<0;01) MOFEP soils, the major accumulation of organic in the pre-treatment data exist when compared carbon appears to be found in the A-horizon by season. This fmding reflects the variability soils, at least in a comparison of A-horizon soils that might be expected of biological processes with B-horizon soils from no deeper than ap­ over different seasons. In many cases differ­ proximately 15 em. The A-horizon soil total ences detected in the parameters measured in carbon was also found to differ by sample date.

88

in in

of of

89 89

a a

to to leaf leaf

that that

trees trees

of of

in in

that that

good good

any any the the

plots plots

after after

non­

is is

(one (one

har­

carbon carbon

a a

the the

The The

and and

the the

soil soil

tree tree

these these

carbon carbon

of of

1978). 1978).

harvest. harvest.

plots, plots,

offer offer

or or

micro­

on on

sulfur sulfur

due due

carbon carbon from from

for for

bacterial bacterial

A-horizon A-horizon

after after

At At

be be

soils soils

in in

on on

Fritze Fritze

comes. comes.

Although Although

of of

have have

where where

after after

plots plots

years years

percent percent

of of

Forest Forest

lignocellu­

lignocellu­

may may

1957, 1957,

which which

after after

Because Because

litter litter

Forest Forest

soil soil suggests suggests

least least

MOFEP MOFEP

evidence evidence

microorgan­

also also

10 10

and and

generally generally

of of

25 25

non-leached non-leached

labile labile

dcy). dcy).

altered. altered.

vegetation vegetation

matter matter

years years

potential potential MOFEP MOFEP

may may

increase increase

in in

at at

oak oak

carbon carbon

based based

plots plots

all all

principal principal

dcy, dcy,

study study

average average

to to

dominant dominant

growth growth

discriminate discriminate

2 2

here here

these these

1982). 1982).

as as

State State

to to

represent represent

mean mean

the the

transformations transformations

for for

from from

to to

estimation estimation

years years

a a

8 8

State State

was was

may may

Henderson Henderson in in

rate rate

the the

for for

to to

A-horizon A-horizon

to to

the the

2 2

woody-debris woody-debris

finding finding

the the

the the

not not

roots

in in

or or

processes processes

first first

in in

white white

to to

Run Run

greatly greatly

of of

the the

J.lmol/g J.lmol/g

organic organic

of of

and and

3 3

years years

Run Run

or or

soils soils

lignocellulose lignocellulose

affect affect

Reisenauer Reisenauer grand grand

treatment. treatment.

plots plots

J.lmol/g J.lmol/g

sulfur sulfur

suggestive suggestive

sources sources

of of

found found

decrease decrease

which which

removing removing

be be

carbon carbon

the the

used used

of of

This This

limiting limiting

to to

Pietikainen Pietikainen

than than

microbial microbial

a a

is is

of of

microbial microbial

one one

presented presented reduced reduced

the the

litter litter

approximate approximate

Deer Deer

2 2

is is

by by

(16.9 (16.9

also also

The The

and and

(Lundgren (Lundgren

changes changes

Finland Finland

be be

Deer Deer

for for

27.6 27.6

study, study,

will will

decaying decaying

by by

determined determined

been been

rates rates

in in

calculated calculated

an an

in in

total total

of of

observed observed

microbial microbial

labile labile

measured measured

leaf leaf

MOFEP MOFEP

(Shriner (Shriner

rates. rates.

provision provision

MOFEP MOFEP

there there

from from

not not

activity. activity.

against against

microorganisms, microorganisms,

study study

soils soils

may may

the the

soil soil

greater greater

soils soils

sampled, do do sampled,

of of

this this

was was

has has

of of

which which

made. made.

that that

in in

greatly greatly

soil soil

future future

sources. sources. soil soil

subsequent subsequent

reduced reduced

1986). 1986).

the the

soils soils

in in

(Jordan (Jordan

soil soil

the the

be be

depleted depleted

sulfur, sulfur,

Hence, Hence,

woody-debris woody-debris

of of

experimental experimental

biomass biomass

be be

in in

in in

in in

measured measured

in in

followed followed

forests forests

sites sites

U.S. U.S.

lignocellulose lignocellulose

contribution contribution

from from

plots plots

these these

1997). 1997).

on on

from from

than than

to to

should should

observed observed

dates, dates,

inputs inputs

as as

sulfur sulfur

inputs inputs

are are

baseline baseline

in in

soils soils

will will

previous previous

may may

mineralization mineralization

energy energy

total total

mineralization mineralization

ecosystem ecosystem

metabolic metabolic

specifically specifically

harvested, harvested,

all all

a a

In In

concentrations concentrations sulfur sulfur

the the

considerably considerably

soil soil

leached leached

Stevenson Stevenson

on on

U.S. U.S.

A-horizon A-horizon

higher higher

soils, soils, changes changes

(Spratt (Spratt

good good decaying decaying

harvest. harvest.

lose lose

vest vest

resulted resulted

lower lower

Total Total

transformations transformations

sources sources not not

roots roots

Clearcutting Clearcutting

(1995) (1995)

biomass biomass

clearcut clearcut harvest, harvest,

bacterial bacterial

decrease decrease

and and

clearcut clearcut

isms isms source source

lower lower

species species

are are

litter litter

reduced reduced

following following

indicator indicator

Lignocellulose Lignocellulose

species species

mineralization mineralization

lose lose

bial bial

MOFEP MOFEP

between between

Therefore, Therefore,

A-horizon A-horizon

the the

al. al.

this this

that that

and and

such such

in in

may may

et et

made made

plots plots

the the

be be

lignin lignin

an an

soils. soils.

spe­

which which

ligno­ emis­

the the

to to

stud­

oak oak

miner­

soil soil

cellu­

white white

2 2

with with

lignocel­

between between

working working

predis­

to to

to to

similar similar

in in

or or

the the

to to

species. species.

soil soil

of of

the the

microor­

for for

of of

was was

forests. forests.

availabil­

cellulose cellulose

one one

oak oak

differences differences

south south C0

Crawford Crawford

plots plots

different different

substantial substantial

mineraliza­

to to

address address

microbial microbial

the the

soils, soils,

in in

14

to to

white white

primary primary of of

Finally, Finally,

vecy vecy

Benner Benner

in in

of of

mineralization mineralization

is is

might might activities activities

To To

of of

the the

rates rates

indicating indicating

of of

that that

required required

by by

soil soil

species species

differences differences

possibly possibly

C-lignocellulose C-lignocellulose

A-horizon A-horizon

parameters parameters

white white

Ozark Ozark

detected detected

correlate correlate

1976, 1976,

lignin lignin

14

activity activity

monitor monitor

cellulose cellulose

these these

on on

ecologists ecologists

were were

number number

critical critical

to to

in in

microorganisms microorganisms

MOFEP MOFEP

are are

floor floor

1984, 1984,

to to

rate rate

particular particular

carbon carbon

species species

occur occur

preferred preferred

determined determined

or or

limitations limitations

to to

in in

studies studies

and and

mineralization mineralization

used used

1993). 1993).

of of

equipment equipment

a a

1977). 1977).

plant plant

by by

of of

the the

were were

are are

al. al.

these these

with with

C-lignocellulose C-lignocellulose

courses courses

due due

here here

monitor monitor

the the

lignocellulose lignocellulose

to to

possible possible

another. another.

either either

this this

they they

14

found found

microbial microbial

forest forest

was was

microorganisms microorganisms

al. al.

et et

indications indications

in in

physical physical

forest forest

is is

to to

be be

A-horizon A-horizon

other other

of of

from from

temperature. temperature.

Crawford Crawford

from from

with with

et et

microbial microbial

lignin, lignin,

It's It's

chosen chosen

to to

oak oak

lignocellulose lignocellulose

the the

soil soil

of of

and and

Time Time

used used

Due Due

oak oak

expected expected

Bartha Bartha

nutrient nutrient

species species

the the

radiolabeled radiolabeled

cellulose cellulose

with with

for for

activities activities

since since

processes processes

of of

sources sources

of of

here here

may may

nutrients nutrients

and and

and and

soil soil

be be

of of

due due

was was

exist exist

amended amended

on on

present present

and and

(Benner (Benner

decomposers decomposers

tree tree

diameter diameter

mineralization mineralization

white white

correlations correlations

lignocellulose lignocellulose

to to

absence absence

White White

be be

using using

plots. plots.

Hackett Hackett

future future

decomposers decomposers

Therefore, Therefore,

rates rates

used used

surface surface

of of

major major

mineralization mineralization

in. in.

number number

activity? activity?

the the

rates rates

soils soils

compared compared

activity. activity.

measure measure

metabolism

or or

No No

might might

of of

decomposing decomposing

soils soils assay assay

trees trees

found found

obtained obtained

in in

oak oak

if if

(Atlas (Atlas

microbial microbial

the the

microbial microbial

experience, experience,

may may

essential essential

the the

lignocellulose lignocellulose

moisture moisture

structures structures

microcosms microcosms

Crawford Crawford

in in

of of

oak oak

soils. soils.

ecosystem, ecosystem,

variations variations

1977, 1977,

A-horizon A-horizon

>1.5 >1.5

known known

the the

of of

consultation consultation

aspect aspect

from from

were were

over over lignocellulose

of of

lignin lignin

to to

choice choice

means means

dominant dominant

of of

and and

MOFEP. MOFEP.

the the

soil soil

those those

the the

al. al.

white white

turn turn

studied. studied.

1985, 1985,

question, question,

cies cies

tion tion

studied studied oaks oaks

determined determined

presence presence

soil soil

cellulose cellulose

white white

lose, lose,

Hence, Hence,

species species pose pose

metabolic metabolic

in in

similar similar

adequate adequate Is Is

et et

and and forest forest

sion sion

found found to to

alization alization

in in

ity ity

microbial microbial

after after

ies ies

the the

on on

One One

west west

lulose lulose

microbial microbial

lignocellulose lignocellulose

producers. producers.

ganisms ganisms

producers. producers.

activities activities

foreshadow foreshadow

changes changes The The as as

larger larger

recycle recycle

in in

rates rates

The The These These

• •

""' ""'

The The

sulfur sulfur

horizon horizon

the the

other other

fraction fraction

sulfur sulfur

soils. soils.

Strickland Strickland

35

organic organic

principally principally

of of

large large

et et the the

sites sites

measured, measured,

finding finding

predominant predominant

Organic Organic

by by

sulfur sulfur

90 90

Sulfur Sulfur

forest forest

there there

are are

ally ally

during during

A-horizon A-horizon

of of

1986, 1986,

greatest greatest

researchers researchers

1992), 1992),

those those

has has appears appears

total total

content content

sulfur. sulfur.

have have

Deer Deer good good

total total

MOFEP MOFEP

One One trol trol

not not

90 90

sulfur sulfur

1985). 1985).

cant cant

the the

S-sulfate S-sulfate

root root

a1.. a1..

total total

organic organic

to to

:OO

organic organic

fall fall

reported reported

methodology methodology

State State

part part

have have

soils. soils.

to to

potential potential

around around

reduction reduction

sulfur sulfur

sulfur sulfur

seasonal seasonal

been been

Run Run

baseline baseline

1983, 1983,

99 99

soils soils

is is

used used

Strickland Strickland

It It

soils soils

utilizes utilizes

production production

over over

indicating indicating

in in

of of

release. release.

do do

the the

must must

is is

Since Since

sulfur sulfur

sulfur sulfur

soils soils

Dry Dry

in in

the the

of of

is is

block block

sulfur sulfur

loss loss

to to

percent percent

of of

these these

slightly slightly

MOFEP MOFEP

in in

Forests Forests

with with

soils. soils.

soil soil

The The

possible possible

some some

short-term short-term

found found

amended amended

added added

et et

but but

sulfur. sulfur.

incorporated incorporated

wetter wetter

occur occur

MOFEP, MOFEP,

all all

in in

(David (David

sulfur sulfur

McLaren McLaren

analyzed analyzed

possibility possibility of of

combustion combustion

have have

keeping keeping

here. here.

the the

may may

be be

------

of of

al. al.

form form

MOFEP MOFEP

an an

this this

when when

concern concern

to to

dates dates

also also

or or

the the

total total

increases increases

the the

lack lack

of of

it it

soils soils

(54 (54

sulfur sulfur

due due

1986). 1986).

soils soils

world world

obsetve obsetve

of of

may may

treatment, treatment,

and and

to to

used used

extraction extraction

higher higher

for for

that that

plant plant

to to

A-horizon A-horizon soils

not not

be be

included included

sampling sampling

presented presented

found found

magnitude magnitude

et et

study, study,

of of

method method

Organic Organic

represents represents

percent, percent,

that that

the the

sulfur, sulfur,

underestimate underestimate

of of

MOFEP MOFEP

clearcutting clearcutting

analyzing analyzing

when when

and and

with with

to to

with with

aquic aquic

somewhat somewhat

a1.. a1..

et et

sulfur sulfur

in in

obsetved obsetved

Fitzgerald Fitzgerald

(Amaral (Amaral

soils soils

be be

organic organic

incubations, incubations,

substantial substantial

on on

that that

here here

in in

(Mitchell (Mitchell

litter litter

A-horizon A-horizon

origin origin

a1.. a1..

Microbially Microbially

different different

the the

1982, 1982,

into into

total total

techniques, techniques,

in in

in in

sites sites

inferred inferred

any any

drying, drying,

require require

this this

comparing comparing

findings findings

compared compared

1985, 1985,

when when

or or

used used

are are

in in

sulfur sulfur

this this

MOFEP MOFEP

samples samples

periods periods

in in

to to

rates rates

of of

p

A-horizon A-horizon

should should

here here

drop drop

the the

changes changes

udic udic

sulfur sulfur

was was

obsetved obsetved

MOFEP), MOFEP),

isotope

sampled. sampled.

sulfur sulfur

Wieder Wieder

et et

a a

quantify quantify

most most

dried dried

soluble soluble

mostly mostly

substantial substantial

underestimated. underestimated.

compound compound

major major

and and

1984, 1984,

to to

led led

a1.. a1..

organic organic

compared compared

Schindler Schindler

laboratories laboratories

however, however,

was was

dried dried

that that

for for

soil soil

of of

or or

made made

1) 1)

not not

differences differences

from from

soils. soils.

total total

quantify quantify

similar similar

A-horizon A-horizon

produced produced

may may

provide provide

1989). 1989).

forest forest

values values

organic organic

and and

in in

to to

collected collected

some some

Zhang Zhang

forest forest

with with

is is

similar similar

MOFEP MOFEP

dominated dominated

total total

(Fitzgerald (Fitzgerald

et et

xeric, xeric,

directly directly

the the

in in

and and

portion portion

soils soils

a a

the the

in in

soils soils

the the

on on

organic organic

diverse diverse

up up

sulfur sulfur

a1.. a1..

This This

actu­

moist moist

signifi­

sulfur sulfur

soil soil

Other Other

the the

con­

very very

soils. soils.

form form

plots plots

total total

to to

loss loss

in in

soil soil

The The

et et

than than

from from

by by

a a

was was

the the

and and

to to

in in

a1.. a1..

of of

greater greater

whole-tree whole-tree

finding finding

soils soils

Experimental Experimental

ho:izon ho:izon

much much

Brook Brook

ha.-vest, ha.-vest,

A-horizon A-horizon

State State

though though

transformations transformations

term term different different clearcut clearcut

control control

clearcut clearcut

hatvesting, hatvesting,

reductions reductions

mostly mostly

Run Run

organic organic

sampling. sampling.

hatvest, hatvest,

differences differences

higher higher

comes comes

annual annual

treatment treatment

that that

production production

Rates Rates horizon horizon

wid! wid!

porting porting

those those

play play

of of

sured sured

Strickland Strickland the the

this this

the the

Microbial Microbial

a1.. a1..

amino amino

of of

fraction fraction

substantial substantial

organic organic

organic organic

adsorbed adsorbed

1986, 1986,

1982, 1982,

soluble soluble

organic organic

1984, 1984,

soil. soil.

methodology methodology

soluble soluble

maintenance maintenance

State State

a a

down down

rates rates

(<10 (<10

Forest Forest

thinner thinner

soils, soils,

of of

Fitzgerald Fitzgerald

Spratt Spratt

for for

study study

role role

from from

than than

acids) acids)

organic organic

for for suggests suggests

sites. sites.

no no

contribution contribution

sulfur sulfur

microbial microbial

total total

soils soils

sulfur sulfur

sulfur sulfur

is is

the the

sites sites

either either

may may

organic organic

conclusion conclusion

Abundant Abundant

Watwood Watwood

MOFEP MOFEP

production production

sulfate sulfate

years). years).

soils soils

organic organic

soils soils

Forest Forest

sulfur sulfur

of of

mention mention

the the

hatvesting hatvesting

quantified. quantified.

the the

Mitchell Mitchell

in in

in in

et et

(p

where where

over over

suggesting suggesting

litter litter

fraction fraction

rates rates

clearcut clearcut

organic organic

had had

of of

sulfur sulfur

lignocellulose lignocellulose

for for

negatively negatively

are are

1997, 1997,

a1.. a1..

the the

in in

litter litter

Forest Forest

In In

than than

are are

clearcut clearcut

steep steep

compounds compounds

(Strickland (Strickland

2 2

sulfur) sulfur)

any any

at at

over over

Deer Deer

the the

in in

two two

sulfur sulfur

that that

addition, addition,

to to

1986). 1986).

et et

much much

in in

used used

present present

before before

fall. fall.

formation formation

(Spratt (Spratt

involvement involvement

1) 1)

of of

soils soils

the the

In In

no no

of of

great, great,

sulfur sulfur

A-horizon A-horizon

et et

fall, fall,

a1.. a1..

3 3

changes changes

soils soils

was was

et et

was was

Strick Strick

forest forest

evidence evidence

in in

same same

in in

microbial microbial

many many

sulfur. sulfur.

of of

slopes slopes

of of

in in

organic organic

sampling sampling

a a

Missouri Missouri

significant significant

or or

erosion erosion

al. al.

of of

Run Run

levels levels

in in

al. al.

were were

The The

1983, 1983,

previous previous

here here

total total

other other

If If

their their

was was

that that

organic organic

mineralization mineralization

New New

sites sites

thinner thinner

as as

affect affect

8 8

made made

organic organic

the the

found found

the the

at at

of of

1993). 1993).

appreciable appreciable

(e.g., (e.g.,

(1989) (1989)

1997), 1997),

in in

to to

soils soils

period. period.

A-horizon A-horizon

et et

and and

years years

a a

State State

implications implications

have have

control control

mineralization mineralization

least least

may may

found found

would would

found found

microorganisms microorganisms

of of

sulfur sulfur

found found

organic organic

MOFEP MOFEP

Hampshire. Hampshire.

However, However,

result result

in in

study study

Hubbard Hubbard

than than

forest forest

Schindler Schindler

sulfur sulfur

a1.. a1..

10 10

is is

of of

soils soils

A-

in in

organic organic

this this

sites sites

in in

sulfur-containing sulfur-containing

dates dates

2 2

litter litter

Fitzgerald Fitzgerald

sulfur sulfur

(David (David

litter litter

available available

years years

the the

study study

substantial substantial

1982, 1982,

came came

sulfur sulfur

horizon horizon

Forest Forest

not not

change change

have have

years years

requires requires

in in

the the

the the

the the

to to for for

This This

not not

in in

of of

(again, (again,

from from

of of

sites. sites.

compound compound

soil soil

the the

in in

A-horizon A-horizon

in in

sulfur sulfur

layers layers

soils, soils,

made made

were were

soils soils

Hubbard Hubbard

correlate correlate

layers layers

whole-tree whole-tree

production production

these these

quantities quantities

timber timber

soils soils

been been

control control

prior prior

that that

soluble soluble

to to

Brook Brook

MOFEP MOFEP

of of

Swank Swank

in in

Deer Deer

et et

detect detect

sulfur sulfur

after after

mea­

et et

short short

total total

were were

suggests suggests

that that

Deer Deer

in in

soil soil

a a

sulfur sulfur

A­ al. al.

sup­

Al­

This This

the the

a1.. a1..

1984, 1984,

of of

much much

then then

in in

up up

after after

pre­

to to

than than

Run Run

all all

et et

a a in in

2 2

91 91

in in

soils soils

they they

data data

the the

From From

and and

has has

sulfur sulfur

the the

part­

soil soil

sulfur sulfur

retain retain

of of

rela­

pos­

from from

any any

sulfur sulfur

oc­

clearcut clearcut

short­

in in

(Spratt (Spratt

These These

status status

the the

corre­

we we

in in

40 40

will will

both both

and and

of of

as as

clearcut clearcut

with with

in in

these these organic organic

exchange exchange

were were

question. question.

will will

Com Com

and and

the the

forest forest

from from

represent represent

these these

2 2

by by

any any

precipita­ soils soils

(1997) (1997)

treatments, treatments,

research. research.

winter winter

sulfur sulfur

mineraliza­

of of

in in

have have

from from

soils soils

organic organic

organic organic

conducted conducted were were

baseline baseline

ion ion

bases bases

mineralization mineralization

soils, soils,

hanrest. hanrest.

this this

that that

have have

were were

(K+ (K+

Mg+

study study

from from

drained, drained,

they they

project project

of of

soil soil

with with

substantially substantially

nutrtent nutrtent

from from

changes changes

Ozark Ozark

Because Because

level level

soil soil

the the

hanrest hanrest

percent). percent).

soils soils

Goals Goals

the the

with with

sites, sites,

changes changes

2 2

Spratt Spratt

in in

sampling, sampling,

deficit deficit

to to

evident. evident.

and and

that that Duling Duling

identification identification

bases bases

collected collected

indicate indicate

ongoing ongoing

of of

ecosystem, ecosystem,

well well

this this

loss loss

70 70

clearcutting. clearcutting.

a a

the the

might might

1997). 1997).

to to

were were

sulfur, sulfur,

Mg+

A-horizon A-horizon

K+ K+

sulfur sulfur

answer answer

be be

with with

disturbance disturbance

after after

of of

2 2

of of

further further

on on

to to

A-horizon A-horizon

of of

to to

to to

controls controls

to to

large large

A-horizon A-horizon

1992). 1992).

because because

in in

plots plots

help help

supplied supplied

were were

surface surface

expertmental expertmental

were were

in in

control control

months) months)

they they

1993). 1993).

for for

soil soil

lignocellulose lignocellulose

Mg+

40 40

Missourt Missourt

and and

forest forest

related related

result result

prtor prtor

help help

correlate correlate

data data

status. status.

changes changes

exchangeable exchangeable

lead lead

lignocellulose lignocellulose

soon soon

A-horizon A-horizon

lead lead

of of

a a

with with

goals goals

very very

focus focus

limit limit

forest forest

(Spratt (Spratt

the the

al. al.

will will

K+ K+

that that

by by

here here

should should

result result

organic organic

to to

organic organic

transformations transformations the the

the the

in in

or or

and and

2 2

and and

as as

with with

for for

Forest Forest

a a

as as

of of

need need

study study

of of

et et

Forest Forest

may may

the the

of of

to to

years years

that that

K+ K+

exchangeable exchangeable

samples samples

cation cation

data data

might might

order order

as as

Mg+

(Johnson (Johnson

Post-treatment Post-treatment

might might

concentrate concentrate

keep keep

be be

study study

10 10

The The

soils soils

this this

plots plots

in in

nutrtent nutrtent

adequately adequately

A-horizon A-horizon

sulfur sulfur

shown shown

here here

State State

loss loss

processes, processes,

State State

occur occur

minimal minimal

between between

levels levels

long-term long-term

to to

result result

the the

evidence evidence

to to

relationship relationship

in in

and and

that that

compared compared

for for

know know

of of

a a

soils soils

soils soils

soils soils

including including

a a

previously previously

the the

1997, 1997,

help help

8 8

post-treatment post-treatment

These These

goals goals

concentrations concentrations

ecosystem, ecosystem,

compared compared

Watwood Watwood

(on (on

Run Run

with with

Run Run

been been

may may

in in

as as

nutrtents nutrtents

any any

nutrtent nutrtent

to to

pre-treatment pre-treatment

or or

of of

the the

3 3

there there

curred curred

sites, sites,

transformations transformations

studies studies

Deer Deer already already

that that

sible. sible.

transformations transformations

sprtng sprtng

term term

ecosystem ecosystem tion tion

and and transformations transformations

watershed watershed potential potential

continue continue

and and

presented presented

of of son son

1997, 1997, microbial microbial

These These

The The

ecosystem ecosystem

tionships tionships

adequate adequate nutrtents? nutrtents?

tion tion

matter, matter,

Is Is

horizon horizon

exchangeable exchangeable

percent, percent,

lated lated sulfur sulfur

reduced reduced

to to

provided provided reductions reductions

Deer Deer surface surface

sites sites

selected selected

have have

surface surface

changes changes nutrtents. nutrtents.

sampled sampled

vital vital

of of

in in

the the

in in

As As

of of

soils soils

as as

of of

A A

B B

of of

Little Little

them them

that that

this this

soil soil

was was

organic organic

organic organic

for­

on on

power. power.

(Spratt (Spratt

soils soils

Deer Deer

be­

alfisols alfisols

the the

mecha­

soil soil

bases bases MOFEP MOFEP

to to

lower lower

result result

play play

have have

have have of of

horizons horizons

soil soil

a a

post­

and and

K+ K+

atmo­

a a

Other Other

in in of of

K K

loss, loss,

in in

soils soils

in in

soils soils

character­

Alfisols Alfisols

1992). 1992).

range range

A-horizon A-horizon

soil soil

deciduous deciduous

and and

of of

forest forest

A A

prtmazy prtmazy

of of

sulfur, sulfur,

and and

be be

other other

As As

1982). 1982).

may may

effect effect

of of

retention retention

these these

and and

the the

al. al.

to to

classified classified

Band Band

exchangeable exchangeable

A-horizon A-horizon

of of

One One

, ,

This This

source source

concentrations concentrations

retention. retention.

2

of of

suggested suggested

wide wide

A-horizon A-horizon

mineral mineral

total total

of of

et et

from from

potential potential

sulfur sulfur

A-horizon A-horizon bases. bases.

result result

a a

loss loss

bases. bases.

from from

differentiate differentiate

the the

must must

A-horizon A-horizon

1980, 1980,

that that

obsenred obsenred

on on

cations, cations,

source source

clearcut clearcut

Mg+

clearcutting clearcutting

were were

K-supplying K-supplying

from from

relationship relationship

compounds compounds

layers, layers,

between between

of of

comparing comparing

on on

A-horizon A-horizon

in in

, ,

base base

of of

availability availability Both Both

exchangeable exchangeable

2

the the

negative negative

(the (the

in in

mineral. mineral.

cation cation

study. study.

al. al.

lower lower

here, here, 1978). 1978).

(1993) (1993)

power power

higher higher

available available

a a

By By

the the

loss loss

weathered, weathered,

charactertstic charactertstic

helps helps

the the

data data

cations cations

base base

organic organic

after after

et et

Ca+

in in

litter litter

study study

noted noted

is is

these these

al. al.

the the

the the

(Ragsdale (Ragsdale

of of

with with

ecosystems. ecosystems.

limited limited

evidence evidence

of of

a a

placed placed

aspect aspect

et et

of of

soil soil

that that predominant predominant

have have

ecosystem ecosystem

sulfur, sulfur,

horizons horizons

process) process)

pr'.unartly pr'.unartly

ecosystem-wide ecosystem-wide

play play

indicating indicating

much much

soils soils noted noted

this this

concentrations concentrations

nutrtent nutrtent

sulfur sulfur

role role

that that

ultisols. ultisols.

highly highly

1986). 1986).

loss loss

exchangeable exchangeable

than than

A A

Missourt Missourt

on on

exchangeable exchangeable

their their

utilizes utilizes

good good

K K

the the

Another Another

in in

to to

presented presented

been been

those those

or or

baseline baseline

elucidated. elucidated.

nutrtent nutrtent

adsorption adsorption

be be

accumulate accumulate

to to

of of

soils soils

and and

forests forests

reduced reduced al. al.

Johnson Johnson the the

demarcations demarcations

of of

they they

is is

is is

exchangeable exchangeable

forms forms

have have

might might

the the

forest forest

the the

in in

of of

K-supplying K-supplying

lower lower

to to

be be

comes comes

to to

leaching leaching

is is

et et

Forest Forest

data data

the the

has has

organic organic

correlated correlated

(Hausenbuiller (Hausenbuiller

contain contain

in in

Watwood Watwood

organic organic

soils, soils,

in in

important important plots, plots,

U.S. U.S.

role role

deposition, deposition,

with with

the the

(e.g., (e.g.,

sulfur sulfur

sulfur sulfur

level level

these these

from from

of of

alfisols alfisols

fractions fractions Loss Loss

sulfate sulfate

by by

may may

There There

tend tend

tend tend

ecosystems ecosystems leading leading

sampled sampled

to to

ultisols. ultisols.

higher higher

with with

of of

distinct distinct

State State

ultisols ultisols

soluble soluble

the the

horizons horizons

limited limited

vegetation vegetation

retention retention

these these

their their

eastem eastem

trees trees

MOFEP MOFEP

sphertc sphertc

the the

base base

and and

In In

than than the the

and and producers producers

horizons horizons

istic istic

have have

is is

either either

sulfur sulfur 1997) 1997)

types types

Soils Soils

ecosystems ecosystems positively positively

production production

soils. soils.

ecosystem ecosystem

and and study study

very very

cations cations

soil soil

emphasis emphasis physico-chemical physico-chemical

ecosystem ecosystem tween tween

organic organic

the the

(Schindler (Schindler

researchers researchers

Run Run

soils. soils.

sulfur sulfur

organic organic treatment treatment

nisms nisms

sites, sites,

especially especially

plots plots

coupled coupled

ested ested

resulted resulted

Another Another

generally generally obsenred obsenred ~ ~M©W~W------

As a result of the study in Deer Run State Dr. Ron Popham at SMSU and Dr. Mark Bzyant Forest, this project will concentrate on several at UTC were vezy helpful with the use of these things after harvest in the MOFEP plots. First, AA's. The statistical analyses could not have the status of microbial organic sulfur produc­ been performed without the expert help of Ms. tion and the pools of organic sulfur in A-horizon A. K. Spratt and the assistance of Mr. Steve soils will be carefully monitored after harvest. Sheriff. This work was supported by grants The pilot study indicated substantial changes in from the Missouri Department of Conservation these aspects of soil sulfur cycling. Future and the U.S. Department of Agriculture, Na­ research will attempt to determine the relative tional Research Initiative Competitive Grants importance of microbial vs. plant derived or­ Program. ganic sulfur to the soil sulfur pool. Because litter drop from clearcut managed sites should LITERATURE CITED be noticeably less than from control plots, the role microorganisms play in the production of Amaral, J.A.; Hesslein, R.H.; Rudd, J.W.M.; Fox, soil organic sulfur may gain importance. Moni­ D.E. 1989. Loss of total sulfur and changes toring soil organic sulfur mineralization will also in sulfur isotope ratios due to dzying of be of great importance after harvest. If the lacustrine sediments. Limnology and Ocean­ balance between organic sulfur production ography. 34: 1351-1358. (both microbial and plant) and mineralization is shifted towards mineralization, then the poten­ Atlas, R.M.; Bartha, R. 1993. Microbial . tial for nutrient loss (e.g., K+ and Mg+2) similar Fundamentals and applications. 3d ed. to that observed in the pilot study may exist. Redwood City, CA: Benjamin/Cummings Publ. Co. 563 p. Lignocellulose mineralization is expected to increase in the short-term following harvest Benner, R.; Maccubbin, A.E.; Hodson, R.E. (Lundgren 1982, Pietikainen and Fritze 1995), 1984. Preparation, characterization, and but later diminish along with litter fall. As with microbial degradation of specifically radiola­ the sulfur study, short-term changes in ligno­ beled [I4C] Lignocelluloses from marine and cellulose mineralization should be evident freshwater macrophytes. Applied and Envi­ during the 1997 study of watershed plots. ronmental Microbiology. 47: 381-389. Information from the lignocellulose mineraliza­ tion study will be helpful as an indicator of Benner, R.; Moran, M.A.; Hodson, R.E. 1985. microbial activity in these soils, and to some Effects of pH and plant source on lignocellu­ degree will be related to carbon cycling in these lose biodegradation rates in two soils. Any correlations between lignocellulose ecosystems, the Okefenokee Swamp and a mineralization and sulfur transformations in Georgia salt marsh. Limnology and Ocean­ these soils after harvest will be noted. ography. 30: 489-499.

ACKNOWLEDGMENTS Brookshire, B.L.; Jensen, R.; Dey, D.C. 1997. The Missouri Ozark Forest Ecosystem The assistance of Mr. Randy Jensen and the Project: past, present, and future. In: MOFEP staff at Ellington was greatly appreci­ Brookshire, Brian L.; Shifley, Stephen R., ated throughout this work. Their help with eds. Proceedings of the Missouri Ozark enumerations of white oak on the sample plots Forest Ecosystem Project symposium: an used here is also appreciated. The help of the experimental approach to landscape re­ faculty and staff of the Biology Department at search; 1997 June 3-5; St. Louis, MO. Gen. SMSU was critical to completion of this work. Tech. Rep. NC-193. St. Paul, MN: U.S. This work could not have been completed Department of Agriculture, Forest Service, without the technical assistance of Mr. Kong North Central Forest Experiment Station: 1- Lee, Mr. Douglas Abner, Mr. Michael Geile, Mr. 25. John Mills, Ms. Debra Long, Ms. Staci Van Winkle, Ms. Melissa Eslinger, and Ms. Jennifer Crawford, D.L.; Crawford, R.L. 1976. Microbial Pulliam. The use of atomic absorption (AA) degradation of lignocellulose: the Lignin spectrophotometers both from the Chemistiy component. Applied and Environmental Department at SMSU and from the Chemistiy Microbiology. 31: 714-717. Department at UTC was greatly appreciated.

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3-

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and and

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Forest Forest

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nutrient nutrient

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Forest Forest

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Relation­

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Rechcigl, J.E.; Sparks, E.L. 1985. Effect of acid Swank, W.T.; Fitzgerald, J.W.; Ash, J.T. 1984. rain on the soil environment: a review. Microbial transformation of sulfate in forest Communications in Soil Science and Plant soils. Science. 223: 182-184. Analysis. 16: 653-680. Tien, M.; Kirk, T.K. 1983. Lignin-degrading Schindler, S.C.; Mitchell, M.J.; Scott, T.J.; from the hymenomycete Fuller, R.D.; Drtscoll, C.T. 1986. Incorpora­ Phanerochaete chrysosporiwn bonds. Sci­ tion of 35S-sulfate into inorganic and organic ence. 221: 661-663. constituents of two forest soils. Soil Science Society of Amertca Journal. 50: 457-462. Ulrich, B.; Mayer, R.; Kahanna, R.K. 1980. Chemical changes due to acid precipitation Shrtner, D.S.; Henderson, G.S. 1978. Sulfur in a loess-dertved soil in central Europe. Soil distribution and cycling in a deciduous Science. 130: 193-199. forest watershed. Joumal of Environmental Quality. 7: 392-397. Van Loon, G.W.; Hay, G.W.; Goh, R. 1987. Analysis of sulfur-containing components of Simard, R.R. 1993. Ammonium acetate-extract­ a soil treated with simulated . able elements. In: Carter, M.R., ed. Soil Water, Air and Soil Pollution. 34: 233-240. sampling and methods of analysis. Boca Raton, FL: Canadian Society of Soil Science. Watwood, M.E.; Fitzgerald, J.W. 1988. Sulfur Lewis Publishers: 39-42. transformations in forest litter and soil: results of laboratory and field incubations. Spratt, H.G., Jr. 1997. Microbial sulfur trans­ Soil Science Society of Amertca Joumal. 52: formations in A-horizon soils of a Missourt 1478-1483. Ozark Forest managed for timber production by clear-cutting. Soil Biology and Biochem­ Watwood, M.E.; Sommer, A.S.; Fitzgerald, J.W. istry (in press). 1993. Biological sulfur retention in surface soils as a predictor of ecosystem sensitivity Spratt, H.G., Jr.; Morgan, M.D. 1990. Sulfur to acidic precipitation. Soil Science fl'rends cycling in a cedar-dominated, freshwater in Agrtcultural Science). 1: 103-111. wetland. Limnology and Oceanography. 35: 1586-1593. Wieder, R.K.; Lang, G.E.; Granus, V.A. 1985. An evaluation of wet chemical methods for Stevenson, F.J. 1986. Cycles of soil carbon, quantifying sulfur fractions in freshwater nitrogen, phosphorous, sulfur, micronutri­ wetland peat. Limnology and Oceanography. ents. New York, NY: John Wiley and Sons. 30: 1109-1114. 94 380 p. Wiklander, L. 1978. Interaction between cations Zucker, A.; Zech, W. 1985. Sulfur status of four and anions influencing adsorption and uncultivated soil profiles in northern Ba­ leaching. In: Hutchinson, T.C.; Havas, M., varia. Geoderma. 36: 229-240. eds. Effects of acid precipitation on terres­ trial ecosystems. New York, NY: Plenum Press: 239-254.

APPENDIXES

Appendix 1.-ANOVA table, total carbon in MOFEP A-horizon soils (August 1993 to May 1996).

Source DF MS F p

Between site effects Block 2 1.040 0.007 0.993 Treatment 2 60.612 0.400 0.694 Error A (Block*Treatment) 4 151.410

F NumDF DenDF p

Within sitet effects Year 92.68 1 4 0.001 Year*Treatment 0.446 1 2 4 0.668 Season 16.36F 3 2 0.058 Season*Treatment 0.8142 6 6 0.596 Year* Season 6.00)2 3 2 0.146 Year* Season *Treatment 0.2432 6 6 0.945

1 Systat® outputs analysis for year, with only 1 DF, in the univariate ANOVA table. F-value from univariate tables. 2 Pillai's Trace F.

Appendix 2.-ANOVA table, total sulfur in MOFEP A-horizon soils (August 93 to May 96)

Source DF MS F p

Between site effects Block 2 51.006 0.130 0.882 Treatment 2 291.512 0.741 0.532 Error A (Block*Treatment) 4 393.380

F NumDF DenDF p

Within site effects Year 61.640 1 4 0.001 Year*Treatment 0.755 1 2 4 0.527 Season 4.96F 3 2 0.172 Season *Treatment 0.8262 6 6 0.589 Year*Season 26.5182 3 2 0.037 Year*Season*Treatment 0.2972 6 6 0.917

1 Systat® outputs analysis for year, with only 1 DF, in the univariate ANOVA table. F-value from univariate tables. 2 Pillai's Trace F.

95 + Ul

Source DF MS F p

Between site effects Block 2 46.328 0.120 0.890 Treatment 2 260.543 0.675 0.559 Error A (Block*Treatment) 4 386.223

F NumDF DenDF p

Within site effects Year 66.632 1 1 4 0.001 Year*Treatment 0.6401 2 4 0.574 Season 3.7782 3 2 0.216 Season*Treatment 0.9452 6 6 0.527 Year*Season 13.8322 3 2 0.068 Year*Season*Treatment 0.3382 6 6 0.894

1 Systat® outputs analysis for year, with only 1 DF, in the univariate ANOVA table. F-value from univariate tables. 2 Pillai's Trace F.

Appendix 4.-ANOVA table, organic sulfur production in MOFEP A-horizon soils (August 1993 to May 1996)

Source DF MS F p

Between site effects Block 2 9.745 0.582 0.600 Treatment 2 28.013 1.672 0.297 Error A (Block*Treatment) 4 16.755

F NumDF DenDF p

Within site effects Year 2.085 1 1 4 0.222 Year*Treatme:lit 0.8071 2 4 0.508 Season 7.9172 3 2 0.114 Season*Treamentt 0.3632 6 6 0.879 Year*Season 35.0862 3 2 0.020 Year*Season*Treatment 2.2352 6 6 0.175

1 Systat® outputs analysis for year, with only 1 DF, in the univariate ANOVA table. F-value from univariate tables. 2 Pillai's Trace F.

Appendix 5.-ANOVA table, white oak enumeration (> 1.5 in. diam.), MOFEP plots

Source DF :viS F p

Block 2 606.827 3.959 0.113 Treatment 2 138.531 0.904 0.474 Error A (Block*Treatment) 4 153.272

96 Appendix 6.-ANOVA table, white oak cellulose mineralization, MOFEP A-horizon soils (August 1993 to May 1996)

Source DF MS F p

Between site effects Block 2 0.029 6.254 0.059 Treatment 2 0.000 0.041 0.960 Error A (Block*Treatment) 4 0.005

F NumDF DenDF p

Within site effects Year 1.335 1 1 4 0.312 Year*Treatment 0.494 1 2 4 0.646 Season 502.7762 3 2 0.002 Season*Treatment 1.1872 6 6 0.420 Year* Season 9.2192 3 2 0.099 Year* Season *Treatment 0.9122 6 6 0.543

1 Systat® outputs analysis for year, with only 1 DF, in the univariate ANOVA table. F-value from univariate tables. 2 Pillai's Trace F.

Appendix 7.-ANOVA table, white oak lignin mineralization, MOFEP A-horizon soils (August 1993 to May 1996)

Source DF MS F p

Between site effects Block 2 0.001 0.697 0.550 Treatment 2 0.000 0.298 0.757 Error A (Block*Treatment) 4 0.001

F NumDF DenDF p

Within site effects Year 19.0091 1 4 0.012 Year*Treatment 0.734 1 2 4 0.535 Season 34.3002 3 2 0.028 Season *Treatment 0.6872 6 6 0.670 Year* Season 46.3162 3 2 0.021 Year* Season *Treatment 0.9442 6 6 0.527

1 Systat® outputs analysis for year, with only 1 DF, in the univariate ANOVA table. F-value from univariate tables. 2 Pillai's Trace F.

97 /~ ~M@W~W------

Appendix 8.-ANOVA table, exchangeable potassium, MOFEP A-horizon soils (August 93 to May 96)

Source DF MS F p

Between site effects Block 2 15.583 0.315 0.747 Treatment 2 187.124 3.777 0.120 Error A (Block*Treatment) 4 49.549

F NumDF DenDF p

Within site effects Year 60.624I 1 4 0.001 Year*Treatment 0.446I 2 4 0.668 Season 19.21F 3 2 0.050 Season*Treatment 0.7162 6 6 0.652 Year* Season 0.7322 3 2 0.621 Year*Season*Treatment 0.88F 6 6 0.559

I Systat® outputs analysis for year, with only 1 DF, in the univariate ANOVA table. F-value from univariate tables. 2 Pillai's Trace F.

Appendix 9.-ANOVA table, exchangeable magnesium, MOFEPA-horizon soils (August 1993 to May 1996)

Source DF MS F p

Between site effects Block 2 2023293 6.009 0.062 Treatment 2 3.111 0.009 0.991 Error A (Block*Treatment) 4 336.724

F NumDF DenDF p

Within site effects Year 1.045I 1 4 0.365 Year*Treatment 0.275I 2 4 0.773 Season 345.5182 3 2 0.003 Season*Treamentt 1.0192 6 6 0.491 Year* Season 7.0652 3 2 0.127 Year*Season*Treatment 2.0832 6 6 0.197

I Systat® outputs analysis for year, with only 1 DF, in the univariate ANOVA table. F-value from univariate tables. 2 Pillai's Trace F.

98

99 99

p p

p p

0.137 0.137

0.303 0.303

0.721 0.721

0.642 0.642

0.051 0.051

0.562 0.562

0.414 0.414

0.247 0.247

0.056 0.056

0.221 0.221

p p

p p

0.246 0.246

0.750 0.750

0.265 0.265

0.086 0.086

0.125 0.125

0.000 0.000

0.016 0.016

0.858 0.858

96) 96)

May May

F F

F F

1.632 1.632

3.448 3.448

0.146 0.146

0.293 0.293

6.824 6.824

1.837 1.837

0.831 0.831

6.476 6.476

3.094 3.094

0.667 0.667

and and

4 4

4 4

4 4

4 4

4 4

4 4

4 4

4 4

1996) 1996) May

DenDF DenDF

(March (March

DenDF DenDF

and and

plots plots

1.695 1.695

0.857 0.857

0.405 0.405

0.119 0.119

0.248 0.248

0.036 0.036

MS MS

1.080 1.080

0.111 0.111 0.167 0.167

0.139 0.139

0.306 0.306

3.342 3.342

MS MS

(March (March

watershed watershed plots plots

NumDF NumDF

NumDF NumDF

of of

soils soils

1 1

4 4

watershed watershed

2 2

2 2

DF DF

1 1

4 4

2 2

2 2

DF DF

of of

B-horizon B-horizon

litter litter

1.840 1.840

1.680 1.680

0.116 0.116

5.138 5.138

3.748 3.748

0.036 0.036

in in

in in

15.958 15.958

413.279 413.279

carbon carbon

carbon carbon

total total

total total

tables. tables.

tables. tables.

table, table,

table, table,

(Rep*ELT) (Rep*ELT)

(Rep*Slope+Rep*Slope*ELT)) (Rep*Slope+Rep*Slope*ELT))

(Rep*Slope+Rep*Slope*ELT)) (Rep*Slope+Rep*Slope*ELT))

(Rep*ELT) (Rep*ELT)

*ELT*Slope *ELT*Slope

univariate univariate

B B

univariate univariate

A A

B B

A A

effects effects

effects effects

effects effects

effects effects

0.-ANOVA 0.-ANOVA

11.-ANOVA 11.-ANOVA

1 1

from from

from from

site site

Season Season

Season*Slope Season*Slope

Season*ELT Season*ELT

Season Season

site site

Error Error

Slope Slope Error Error Source Source

ELT*Slope ELT*Slope

ELT ELT

Rep Rep

Season*ELT*Slope Season*ELT*Slope

Season*Slope Season*Slope

Season Season

Season*ELT Season*ELT

Slope Slope Error Error

ELT*Slope ELT*Slope

ELT ELT

Rep Rep

Source Source

Error Error

site site

site site

F-value F-value

F-value F-value

1 1

Within Within

1 1 Between Between

Appendix Appendix

Within Within

Between Between Appendix Appendix

• •

......

, ,

Within Within

1 1 Between Between

Appendix Appendix

Within Within

1 1 Between Between

Appendix Appendix

100 100

F-value F-value

F-value F-value

McrDlFJEIP McrDlFJEIP

May May

site site

site site

Error Error

ELT*Slope ELT*Slope

Season*ELT*Slope Season*ELT*Slope

Season* Season*

Season*ELT Season*ELT

Error Error

ELT ELT

Rep Rep

Slope Slope

Season Season

Source Source

Season Season

Rep Rep

Season*ELT*Slope Season*ELT*Slope

Season*Slope Season*Slope

Season*ELT Season*ELT

Error Error

ELT*Slope ELT*Slope

Error Error

ELT ELT

Source Source

Slope Slope

site site

from from

1996) 1996)

site site

from from

13.-ANOVA 13.-ANOVA

12.-ANOVA 12.-ANOVA

effects effects

effects effects

effects effects

effects effects

A A

B B

univariate univariate

A A

B B

univariate univariate

------

(Rep*Slope+Rep*Slope*ELT)) (Rep*Slope+Rep*Slope*ELT))

(Rep*ELT) (Rep*ELT)

Slope Slope

(Rep*Slope+Rep*Slope*ELT)) (Rep*Slope+Rep*Slope*ELT))

(Rep*ELT) (Rep*ELT)

------

table, table,

table, table,

tables. tables.

tables. tables.

white white

total total

carbon carbon

oak oak

cellulose cellulose

12.618 12.618

inA-horizon inA-horizon

0.937 0.937

3.014 3.014

3.726 3.726

3.438 3.438

2.741 2.741

6.068 6.068

2.633 2.633

mineralization mineralization

4 4

2 2

2 2

DF DF

1 1

1 1

1 1

4 4

2 2

2 2

DF DF

1 1

1 1

soils soils

of of

NumDF NumDF

NumDF NumDF

watershed watershed

in in

3 3

3 3

3 3

3 3

A-horizon A-horizon

100.595 100.595

48.538 48.538

30.300 30.300

30.608 30.608

0.042 0.042

0.042 0.042

0.081 0.081

0.033 0.033

0.128 0.128

0.058 0.058

MS MS

MS MS

3.700 3.700

0.473 0.473

plots plots

soils soils

DenDF DenDF

DenDF DenDF

(May (May

4 4

4 4

4 4

4 4

2 2

2 2

2 2

2 2

of of

watershed watershed

1995 1995

3.879 3.879

0.792 0.792

1.015 1.015

1.948 1.948

1.398 1.398

0.122 0.122

0.016 0.016

3.320 3.320

0.304 0.304

1.602 1.602

F F

F F

to to

May May

plots plots

0.388 0.388

0.158 0.158

0.126 0.126

0.024 0.024

0.145 0.145

0.279 0.279

0.287 0.287

0.233 0.233

1996) 1996)

p p

p p

(May (May

0.371 0.371

0.235 0.235

0.513 0.513

0.188 0.188

0.346 0.346

0.308 0.308

0.744 0.744

0.907 0.907

0.141 0.141

0.637 0.637

199 199

p p

p p

5 5 to to

101 101

May May

to to

p p

p p

0.107 0.107

0.926 0.926

0.023 0.023

0.805 0.805

0.415 0.415

0.239 0.239

0.521 0.521

0.491 0.491

0.534 0.534

0.512 0.512

1995 1995

p p

p p

(May (May

0.284 0.284

0.002 0.002

0.542 0.542

0.145 0.145

0.325 0.325

0.328 0.328

0.472 0.472

0.159 0.159

1996) 1996)

plots plots

May May

F F

F F

1.910 1.910

0.494 0.494

0.855 0.855

0.556 0.556

0.794 0.794

1.105 1.105

4.303 4.303

0.070 0.070

0.011 0.011

11.182 11.182

and and

4 4

4 4

4 4

4 4

watershed watershed

4 4

4 4

4 4 4 4

DenDF DenDF

DenDF DenDF

of of

(March (March

e-03 e-03

e-03 e-03

e-03 e-03

e-03 e-03

e-03 e-03

plots plots

1.363 1.363

0.317 0.317

0.004 0.004

0.022 0.022

0.350 0.350

3.541 3.541

MS MS

0.001 0.001

0.378 0.378

0.765 0.765

0.654 0.654

0.364 0.364

0.607 0.607

MS MS

soils soils A-horizon

watershed watershed

NumDF NumDF

NumDF NumDF

in in

of of

soils soils

1 1

4 4

2 2

2 2

DF DF

1 1

4 4

2 2

2 2

DF DF

mineralization mineralization

1.256 1.256

1.238 1.238

B-horizon B-horizon

0.629 0.629

2.979 2.979

1.532 1.532

0.444 0.444

3.272 3.272

54.672 54.672

in in

lignin lignin

oak oak

sulfur sulfur

total total

white white

tables. tables.

tables. tables.

table, table,

table, table,

(Rep*Slope+Rep*Slope*ELT)) (Rep*Slope+Rep*Slope*ELT))

(Rep*ELT) (Rep*ELT)

(Rep*Slope+Rep*Slope*ELT)) (Rep*Slope+Rep*Slope*ELT))

(Rep*ELT) (Rep*ELT)

univariate univariate

B B

univariate univariate

A A

B B

A A

effects effects

effects effects

effects effects

effects effects

15.-ANOVA 15.-ANOVA

14.-ANOVA 14.-ANOVA

from from

from from

site site

Season*ELT Season*ELT

Season*ELT*Slope Season*ELT*Slope

Season*Slope Season*Slope

Season Season

Slope Slope

Error Error

ELT*Slope ELT*Slope

Error Error

Rep Rep

site site

ELT ELT

Source Source

Season*ELT*Slope Season*ELT*Slope

Season*Slope Season*Slope

Season*ELT Season*ELT

Season Season

Slope Slope

ELT*Slope ELT*Slope

Error Error Source Source

Error Error

ELT ELT

Rep Rep

site site

site site

1996) 1996)

F-value F-value

F-value F-value

1 1

Within Within

Between Between

1 1

Appendix Appendix

Within Within

Between Between Appendix Appendix

~M@W~W------

~ ~

Within Within

Appendix Appendix

Between Between

1 1

Within Within

1 1

Appendix Appendix

Between Between

102 102

F-value F-value

F-value F-value

site site

site site

Error Error

Rep Rep

ELT*Slope ELT*Slope

Season*ELT Season*ELT

Season Season

Error Error

Season*ELT*Slope Season*ELT*Slope

Season*Slope Season*Slope

EU EU

Slope Slope

Source Source

Season Season

Season*ELT*Slope Season*ELT*Slope

Error Error

Rep Rep

Season*S1ope Season*S1ope

Season*ELT Season*ELT

ELT*Slope ELT*Slope

Error Error

ELT ELT

Slope Slope

Source Source

site site

from from

site site from from

17.-ANOVA 17.-ANOVA

16.-ANOVA 16.-ANOVA

effects effects

effects effects

effects effects

effects effects

A A

B B

univariate univariate

A A

B B

univariate univariate

(Rep*Slope+Rep*Slope*ELT)) (Rep*Slope+Rep*Slope*ELT))

(Rep*ELT) (Rep*ELT)

(Rep*Slope+Rep*Slope*ELT)) (Rep*Slope+Rep*Slope*ELT))

(Rep*ELT) (Rep*ELT)

-

table, table,

table, table,

tables. tables.

tables. tables.

total total

total total

sulfUr sulfUr

sulfUr sulfUr

inA-horizon inA-horizon

in in

39.599 39.599

0.000 0.000

0.004 0.004

0.008 0.008

44.283 44.283

17.424 17.424

12.281 12.281

13.628 13.628

litter litter

of of

watershed watershed

4 4

2 2

2 2

DF DF

1 1

1 1

1 1

4 4

DF DF

2 2

2 2

1 1

1 1

1 1

soils soils

of of

NumDF NumDF

NumDF NumDF

watershed watershed

plots plots

3 3

3 3

3 3

3 3

1 1

1 1

1 1

(March (March

449.342 449.342

517.272 517.272

151.028 151.028

166.023 166.023

46.124 46.124

77.449 77.449

32.575 32.575

14.862 14.862

22.135 22.135

MS MS

0.218 0.218

0.304 0.304

MS MS

3.163 3.163

plots plots

and and

(May (May

DenDF DenDF

DenDF DenDF

May May

2 2

2 2

2 2

2 2

4 4

4 4

4 4

4 4

1995 1995

96) 96)

0.868 0.868

0.021 0.021

0.147 0.147

3.425 3.425

1.099 1.099

2.192 2.192

5.211 5.211

0.015 0.015

3.104 3.104

0.009 0.009

to to

F F

F F

May May

0.055 0.055

1996) 1996)

0.076 0.076

0.022 0.022

0.069 0.069

0.992 0.992

0.954 0.954

0.003 0.003

0.931 0.931

p p

p p

0.450 0.450

0.416 0.416

0.892 0.892

0.721 0.721

0.136 0.136

0.909 0.909

0.153 0.153

0.228 0.228

0.933 0.933

0.077 0.077

p p p p Appendix 18.-ANOVA table, organic sulfur in A-horizon soils of watershed plots (May 1995 to May 1996)

Source DF MS F p

Between site effects Rep 2 140.957 0.990 0.448 ELT 507.906 1.039 0.415 Error A (Rep*ELT) 2 488.813 3.432 0.136 Slope 22.469 0.158 0.712 ELT*Slope 0.424 0.003 0.959 Error B (Rep*Slope+Rep*Slope*ELT)) 4 142.440

pt NumDF DenDF p

Within site effects Season 51.247 3 2 0.019 Season*ELT 9.943 3 2 0.093 Season*Slope 3.189 3 2 0.248 Season*ELT*Slope 14.791 3 2 0.064

1 F-value from univariate tables.

Appendix 19.-ANOVA table, organic sulfur production in A-horizon soils of watershed plots (May 1995 to May 1996)

Source DF MS F p

Between site effects Rep 2 802.524 3.238 0.146 ELT 1 5.197 0.024 0.891 Error A (Rep*ELT) 2 215.256 0.869 0.486 Slope 25.568 0.103 0.764 ELT*Slope 49.916 0.201 0.677 Error B (Rep*Slope+Rep*Slope*ELT)) 4 247.842

pt NumDF DenDF p

Within site effects Season 50.038 3 2 0.020 Season*ELT 18.122 3 2 0.053 Season*Slope 1.132 3 2 0.501 Season*ELT*Slope 1.527 3 2 0.419

1 F-value from univariate tables.

103 •

Appendix

Between

Between

Appendix Within

Within

1

1

104

F-value

F-value

~«DlFIElP

1996,

site

site

Rep

EIT Error

Rep ELT*Slope Error

Slope

Source

ELT Season Error Season*ELT Season*Slope ELT*Slope Season*ELT*Slope Error

Slope

Source

Season Season*ELT

Season*Slope Season*ELT*Slope

site

site

from

from

20.-ANOVA

21.-ANOVA

oe data note:

effects

effects

effects

effects

A

A

B

B

univariate

univariate

------­

(Rep*ELT)

(Rep*Slope+Rep*Slope*ELT))

(Rep*ELT)

(Rep*Slope+Rep*Slope*ELT))

were

table,

table,

tables.

tables.

log

organic

exchangeable

transformed

sulfor

before

potassium

4.396

0.116

6.467

0.418 0.854 0.435

1.358

1.789

mineralization

analysis)

DF

2 DF 2

2

4

2

4

1

1 1

1

1 1

inA-horizon

in

NumDF

NumDF

A-horizon

3

3 3 3

1 1 1 1

soils

78.118

21.653

44.639 70.757 27.946

MS

MS 0.019 0.091 0.013 0.008 0.005 0.009

0.710

of

soils

watershed

of

DenDF

DenDF

watershed

4 4 4 4

2 2 2 2

plots

2.029

7.000

0.838 0.485 0.564 0.631 0.010 0.395

1.417

1.104

F

F

plots

(May

(March

0.104 0.309 0.751 0.252

1995

0.137

0.761 0.579 0.752

p

p

to

and

May

0.246 0.118 0.343 0.412 0.494

0.415 0.558 0.578 0.925 0.564

p

p

May

1996)

105 105

1996) 1996)

p p

May May

0.770 0.770

0.337 0.337

0.098 0.098

0.201 0.201

0.912 0.912

to to

p p

1995 1995

0.628 0.628

0.138 0.138

0.385 0.385

0.227 0.227

(May (May

F F

1.190 1.190

0.098 0.098

0.094 0.094

4.392 4.392

3.522 3.522

plots plots

2 2

2 2

2 2

2 2

DenDF DenDF

watershed watershed

of of

6.722 6.722

6.962 6.962

MS MS

84.748 84.748

71.233 71.233

soils soils

312.877 312.877

1101.826 1101.826

3 3

3 3

3 3

3 3

NumDF NumDF

A-horizon A-horizon

in in

1 1

4 4

2 2

2 2

DF DF

1.740 1.740

0.715 0.715

6.401 6.401

3.556 3.556

magnesium magnesium

exchangeable exchangeable

tables. tables.

table, table,

(Rep*Slope+Rep*Slope*ELT)) (Rep*Slope+Rep*Slope*ELT))

(Rep*ELT) (Rep*ELT)

univariate univariate

B B

A A

effects effects

effects effects

22.-ANOVA 22.-ANOVA

from from

site site

Season Season

Season*ELT*Slope Season*ELT*Slope

Season*Slope Season*Slope

Season*ELT Season*ELT

Slope Slope

Error Error

ELT*Slope ELT*Slope

Error Error

Rep Rep

ELT ELT

Source Source

site site

F-value F-value

1 1

Within Within

Between Between Appendix Appendix