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SOIL PROFILE DESCRIPTIONS ______ Soil Profile: a Vertical Section of the Soil Extending Through All Its Horizons and Into ______The Parent Material

SOIL PROFILE DESCRIPTIONS ______ Soil Profile: a Vertical Section of the Soil Extending Through All Its Horizons and Into ______The Parent Material

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TITLE 5 ______EVALUATOR ______CERTIFICATION TRAINING ______SOIL HORIZONS AND LAYERS ______Prepared for: Commonwealth of Massachusetts Department of Environmental Protection By L.A. Spokas, PhD, Stockbridge School of Agriculture University of Massachusetts Amherst Presented by: New England Interstate Water Pollution Control Commission

______SOIL PROFILE DESCRIPTIONS ______ Soil Profile: A vertical section of the soil extending through all its horizons and into ______the parent material.  Soil Horizon: A layer of soil, approximately ______parallel to the surface, having distinct ______characteristics produced by soil-forming processes. ______ Soil Layer: A layer in the soil deposited by geologic forces (e.g., wind, water, ice) and not related to a soil-forming process.

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______SOIL HORIZON AND LAYER DESIGNATIONS ______ Three kinds of symbols are used in various combinations to designate soil horizons and ______layers: CAPITAL LETTER, lower-case ______letters, and Arabic numerals (1,2,3…) ______ Master Horizons and Layers: ______O,A,E,B,C, and R are symbols that designate major breaks in the soil and are base symbols to which other characters may be added to describe the soil in more detail.

______A ______Bw ______

C

______SOIL HORIZON AND LAYER DESIGNATIONS ______

 Subordinate Distinctions: ______Lower-case letters are used as suffixes to designate ______specific kinds of master horizons and layers. Ap, plowed A horizon ______Bh, B horizon with an accumulation of Bhs, B horizon with an accumulation of organic matter ______and “sesquioxides” ( and aluminium) Bw, weathered B horizon ______Bs, B horizon with only sesquioxides Cd, dense C horizon (usually till) Cg, “gleyed” C horizon – typically in wetlands

______SOIL HORIZON AND LAYER DESIGNATIONS ______ Vertical Subdivision: Two or ______more horizons or layers designated by a single ______C combination of letters which needs to be subdivided. ______C2  Arabic numerals are used, ______C3 and generally follow all letters. Within a C-Layer, for example, ______C4 successive C-layers should be designated as C1, C2, C3, etc. C5

______SOIL HORIZON AND LAYER DESIGNATIONS ______ Vertical Subdivision: Two or ______more horizons or layers designated by a single ______combination of letters which needs to be subdivided. ______C  Arabic numerals are used, ______and generally follow all letters. Within a C-Layer, for example, ______successive C-layers should be designated as C1, C2, C3, etc. C2

______SOIL HORIZON AND LAYER DESIGNATIONS ______When lithological ______discontinuities occur in a profile, Arabic numerals ______are placed in front of all letters starting at the first discontinuity. ______For example sequence A, Bw, C, 2C indicates that ______the 2C horizon has formed in a parent material different from the C.

______ Horizons followed by the letter “b” are buried ______horizons  By definition of Title 5 - ______all material above an “A” horizon is fill, and Fill ______must be removed ______

Ab

______MASTER HORIZONS -O ______O Layer with predominantly ______organic matter ______

______O-HORIZON ______ O-horizons are layers dominated by organic matter. ______ Greater than 20-30% organic matter by weight ______ Dark, nearly black or black, color (note: colors can be misleading and should only ______be used when other field criteria are observed). ______ Weak strength, greasy feel, light weight when dry, high fiber content.  Typically a surface horizon; if buried, often indicates disturbance.

SUBORDINATE DISTINCTIONS ______OF O-HORIZONS: ______ Oi - Slightly decomposed organic ______material: fibric ______ Oe - Organic material of intermediate ______decomposition: hemic ______ Oa - Highly decomposed organic material: sapric

______A-HORIZON ______The A-horizon is commonly referred to as the , and typically ranges ______from 8-20 cm in thickness. It is a ______mineral horizon that formed at the ______surface or below an O-horizon, and is characterized by an accumulation of ______humified organic matter intimately mixed with the mineral fraction.

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A-HORIZON ______

 Mineral soil material ______ Mixture of well decomposed organic ______matter and mineral ______material.  Surface mineral horizon. ______ Typically dark in color – ______characteristically darker than underlying horizons due to a relatively high organic matter content.

______A-HORIZON ______Suborinate Distinctions of A-horizon: Ap- Plowing or other disturbance. ______This symbol is used to indicate disturbance of the surface layer by ______cultivation. ______

______E-HORIZON ______The E-horizon is a mineral horizon in the upper part of the ______soil, typically underlying an O or an A-horizon. ______ It is a light-colored, leached horizon often associated with ______woodland areas. ______ E-horizons range from not being present in the soil to thicknesses of about 10 – 20 cm.

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E-Horizon Field Criteria: ______ Commonly near the surface, below an O or A- ______horizon and above a B-horizon  Generally lighter in color than overlying organic ______and/or A-horizons and underlying B-horizon ______

Formation: Weak organic acids strip coatings ______from grains, and material is leached down ______into the . Light color is due to natural color of the dominant quartz sand grains.

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______B-HORIZON ______Commonly referred to as subsoil.  Zone of accumulation within the soil. ______ Well-drained typically have bright ______orange-brown or red colors which fade with depth. ______ Accumulation of iron, , organic matter. ______ Horizon generally extends about 45 to 90 cm below the soil surface.

______B-HORIZON ______Subordinate Distinction of B-horizon: ______

 Bw- Development of color and/or structure. This symbol is ______very common in New England. ______ Bhs or Bs -Illuvial accumulation of sesquioxides and organic matter. ______ Bt- Illuvial accumulation of clay, often forming coatings on ped faces, in pores, or on bridges between sand-sized ______grains.

 Bg- strong gleying, indicating prolonged periods of saturation.

______B-HORIZON ______

______C-LAYER ______ C-layers are commonly referred to as the substratum. They are layers, excluding , ______that are little affected by soil forming processes. They are unweathered geologic materials. ______ Field Criteria: Little affected by soil forming factors. ______Lack of profile development. Lack color development.

______C-LAYER ______Subordinate Distinctions:  Cd- dense, ______unconsolidated . ______ Cr - weathered or soft bedrock. ______ Cg - strong gleying, indicating prolonged periods of saturation.

______R-LAYER ______R-layers are hard bedrock (ledge)  Cannot be excavated with a backhoe unless ______fractured. Blasting is often needed to ______remove this material.  May be difficult to differentiate from the ______overlaying soil material and boulders and ______depth to bedrock.

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