Indiana Soil and Landscape Evaluation Manual Version 1.0
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Nichols Arboretum: Soil Types
Nichols Arboretum: Soil Types Not Present in Arboretum Boyer Sandy Loam 0-6% Slopes Fox Sandy Loam 6-12% Slopes Miami Loam 2-6% Slopes Miami Loam 6-12% Slopes Miami Loam 12-18% Slopes Miami Loam 18-25% Slopes Miami Loam 25-35% Slopes Sloan Silt Loam, Wet Water Wasepi Sandy Loam 0-4% Slopes Mary Hejna : September 2012 0 0.125 0.25 Miles Data from NRCS Soil Survey t Soil Series Descriptions BOYER SERIES The Boyer series consists of very deep, well drained soils formed in USE AND VEGETATION sandy and loamy drift underlain by sand or gravelly sand outwash at Soils are cultivated in most areas. Principal crops are corn, small depths of 51 to 102 cm (20 to 40 inches). grain, soybeans, field beans, and alfalfa hay. A few areas remain in GEOGRAPHIC SETTING permanent pasture or forest. The dominant forest trees are oaks, hickories, and maples. Boyer soils are on outwash plains, valley trains, kames, beach ridges, river terraces, lake terraces, deltas, and moraines of Wisconsinan age. TYPICAL PEDON The slope gradients are dominantly 0 to 12 percent, but range from 0 Boyer loamy sand, on a 4 percent slope in a cultivated field. (Colors to 50 percent. Boyer soils formed in sandy and loamy drift underlain are for moist soil unless otherwise stated.) by sand or gravelly sand outwash at depths of 51 to 102 cm (20 to 40 inches). Quartz is the dominant mineral in the 3C horizon, which Ap--0 to 18 cm (7 inches); dark grayish brown (10YR 4/2) loamy contains, in addition, varying amounts of material from igneous and sand, light brownish gray (10YR 6/2) dry; weak fine granular metamorphic rocks, limestone, and dolomite. -
Peat and Peatland Resources of Southeastern Ontario
THESE TERMS GOVERN YOUR USE OF THIS DOCUMENT Your use of this Ontario Geological Survey document (the “Content”) is governed by the terms set out on this page (“Terms of Use”). By downloading this Content, you (the “User”) have accepted, and have agreed to be bound by, the Terms of Use. Content: This Content is offered by the Province of Ontario’s Ministry of Northern Development and Mines (MNDM) as a public service, on an “as-is” basis. Recommendations and statements of opinion expressed in the Content are those of the author or authors and are not to be construed as statement of government policy. You are solely responsible for your use of the Content. You should not rely on the Content for legal advice nor as authoritative in your particular circumstances. Users should verify the accuracy and applicability of any Content before acting on it. MNDM does not guarantee, or make any warranty express or implied, that the Content is current, accurate, complete or reliable. MNDM is not responsible for any damage however caused, which results, directly or indirectly, from your use of the Content. MNDM assumes no legal liability or responsibility for the Content whatsoever. Links to Other Web Sites: This Content may contain links, to Web sites that are not operated by MNDM. Linked Web sites may not be available in French. MNDM neither endorses nor assumes any responsibility for the safety, accuracy or availability of linked Web sites or the information contained on them. The linked Web sites, their operation and content are the responsibility of the person or entity for which they were created or maintained (the “Owner”). -
Northern Fen Communitynorthern Abstract Fen, Page 1
Northern Fen CommunityNorthern Abstract Fen, Page 1 Community Range Prevalent or likely prevalent Infrequent or likely infrequent Absent or likely absent Photo by Joshua G. Cohen Overview: Northern fen is a sedge- and rush-dominated 8,000 years. Expansion of peatlands likely occurred wetland occurring on neutral to moderately alkaline following climatic cooling, approximately 5,000 years saturated peat and/or marl influenced by groundwater ago (Heinselman 1970, Boelter and Verry 1977, Riley rich in calcium and magnesium carbonates. The 1989). community occurs north of the climatic tension zone and is found primarily where calcareous bedrock Several other natural peatland communities also underlies a thin mantle of glacial drift on flat areas or occur in Michigan and can be distinguished from shallow depressions of glacial outwash and glacial minerotrophic (nutrient-rich) northern fens, based on lakeplains and also in kettle depressions on pitted comparisons of nutrient levels, flora, canopy closure, outwash and moraines. distribution, landscape context, and groundwater influence (Kost et al. 2007). Northern fen is dominated Global and State Rank: G3G5/S3 by sedges, rushes, and grasses (Mitsch and Gosselink 2000). Additional open wetlands occurring on organic Range: Northern fen is a peatland type of glaciated soils include coastal fen, poor fen, prairie fen, bog, landscapes of the northern Great Lakes region, ranging intermittent wetland, and northern wet meadow. Bogs, from Michigan west to Minnesota and northward peat-covered wetlands raised above the surrounding into central Canada (Ontario, Manitoba, and Quebec) groundwater by an accumulation of peat, receive inputs (Gignac et al. 2000, Faber-Langendoen 2001, Amon of nutrients and water primarily from precipitation et al. -
Field Indicators of Hydric Soils
United States Department of Field Indicators of Agriculture Natural Resources Hydric Soils in the Conservation Service United States In cooperation with A Guide for Identifying and Delineating the National Technical Committee for Hydric Soils Hydric Soils, Version 8.2, 2018 Field Indicators of Hydric Soils in the United States A Guide for Identifying and Delineating Hydric Soils Version 8.2, 2018 (Including revisions to versions 8.0 and 8.1) United States Department of Agriculture, Natural Resources Conservation Service, in cooperation with the National Technical Committee for Hydric Soils Edited by L.M. Vasilas, Soil Scientist, NRCS, Washington, DC; G.W. Hurt, Soil Scientist, University of Florida, Gainesville, FL; and J.F. Berkowitz, Soil Scientist, USACE, Vicksburg, MS ii In accordance with Federal civil rights law and U.S. Department of Agriculture (USDA) civil rights regulations and policies, the USDA, its Agencies, offices, and employees, and institutions participating in or administering USDA programs are prohibited from discriminating based on race, color, national origin, religion, sex, gender identity (including gender expression), sexual orientation, disability, age, marital status, family/parental status, income derived from a public assistance program, political beliefs, or reprisal or retaliation for prior civil rights activity, in any program or activity conducted or funded by USDA (not all bases apply to all programs). Remedies and complaint filing deadlines vary by program or incident. Persons with disabilities who require alternative means of communication for program information (e.g., Braille, large print, audiotape, American Sign Language, etc.) should contact the responsible Agency or USDA’s TARGET Center at (202) 720-2600 (voice and TTY) or contact USDA through the Federal Relay Service at (800) 877-8339. -
Soil Survey of Walworth County, Wisconsin
Issued February 1971 . SOIL SURVEY . .W alworthCounty I Wisconsin UNITED STATES DEPARTMENT OF AGRICULTURE Soil Conservation Service In cooperation with -- .. UNIVERSITY OF WISCONSIN Wisconsin Geological and Natural History Survey Soils Department, and Wisconsin Agricultural Experiment Station Major fieldwork for this soil survey was done in the period 1959-64. Soil names and descriptions were approved in 1966. Unless otherwise indicated, statements in this publication refer- to conditions in the county in 1966. This survey was made cooperatively by the Soil Conservation Service and the Wisconsin Geological and Natural History Survey, Soils Department, and the Wisconsin Agricultural Experiment Station, University of Wisconsin. It is part of the technical assistance furnished to the Walworth County Soil and Water Conservation District. The fieldwork that is the basis for this soil survey was partly financed. by the Southeastern Wisconsin Regional Planning Commission; by a joint planning grant from the State Highway Commission of Wisconsin; by the U.S. Department of Commerce, Bureau of Public Roads; and by the Department of Housing and Urban Development under the provisions of the Federal Aid to Highways legislation and section 701 of the Housing Act of 1954, as amended. Either enlarged or reduced copies of the soil map in this publication can be made by commercial photographers, or they can be purchased on individual order from the Cartographic Division, Soil Conservation Service, U.S. Department of Agriculture, Washington, D.C. 20250. HOW TO USE THIS SOIL SURVEY HIS SOIL SURVEY contains informa- an oved.ay over the soil map an? ?olo!,ed to Ttion that can be applied in managing farms sh?w ?(:nls that have ,bhe sal!le hm~tatIOn or . -
Part 629 – Glossary of Landform and Geologic Terms
Title 430 – National Soil Survey Handbook Part 629 – Glossary of Landform and Geologic Terms Subpart A – General Information 629.0 Definition and Purpose This glossary provides the NCSS soil survey program, soil scientists, and natural resource specialists with landform, geologic, and related terms and their definitions to— (1) Improve soil landscape description with a standard, single source landform and geologic glossary. (2) Enhance geomorphic content and clarity of soil map unit descriptions by use of accurate, defined terms. (3) Establish consistent geomorphic term usage in soil science and the National Cooperative Soil Survey (NCSS). (4) Provide standard geomorphic definitions for databases and soil survey technical publications. (5) Train soil scientists and related professionals in soils as landscape and geomorphic entities. 629.1 Responsibilities This glossary serves as the official NCSS reference for landform, geologic, and related terms. The staff of the National Soil Survey Center, located in Lincoln, NE, is responsible for maintaining and updating this glossary. Soil Science Division staff and NCSS participants are encouraged to propose additions and changes to the glossary for use in pedon descriptions, soil map unit descriptions, and soil survey publications. The Glossary of Geology (GG, 2005) serves as a major source for many glossary terms. The American Geologic Institute (AGI) granted the USDA Natural Resources Conservation Service (formerly the Soil Conservation Service) permission (in letters dated September 11, 1985, and September 22, 1993) to use existing definitions. Sources of, and modifications to, original definitions are explained immediately below. 629.2 Definitions A. Reference Codes Sources from which definitions were taken, whole or in part, are identified by a code (e.g., GG) following each definition. -
The Beginning of a Masterpiece? Cont
FRIDAY, 27 JULY 2018 KEW OUT, CRACKSMAN IN KING GEORGE THE BEGINNING OF In a surprise twist to the tale of Saturday=s G1 King George VI A MASTERPIECE? and Queen Elizabeth S. at Ascot, Aidan O=Brien ruled out the G1 Grand Prix de Paris winner Kew Gardens (Ire) (Galileo {Ire}) after he scoped dirty before Thursday=s confirmation stage. Ballydoyle are supervising the wellbeing of the string due to the disappointing effort of Magic Wand (Ire) (Galileo {Ire}) in Saturday=s G1 Irish Oaks, after which she was found to have had a dirty nose. AOur horses are just going through a little bit of a stage--a little bit of a change--and the odd one is not scoping right at the moment,@ he explained. AWe=ve seen it with the filly in the Oaks and we just have to be careful.@ The removal of Kew Gardens means that Ryan Moore is on last year=s G1 Qipco British Champions Fillies & Mares S. heroine Hydrangea (Ire) (Galileo {Ire}) and the sole 3-year-old in the line-up will be the stable=s G1 Irish Derby runner-up Rostropovich (Ire) (Frankel {GB}). Cont. p5 Galileo=s Anthony Van Dyck takes the Tyros S. | Racing Post IN TDN AMERICA TODAY Despite having to navigate troubled waters as a bug infects PHOENIX ‘DREAMING’ BIG AT THE SPA parts of the Ballydoyle armada, Anthony Van Dyck (Ire) (Galileo Phoenix Thoroughbreds, off to a flyer at Saratoga with an {Ire}) was a faithful steer for Ryan Moore as he handed Aidan opening day ‘TDN Rising Star’, is primed for a big summer at the O=Brien a 12th win in resounding fashion in the G3 Japan Racing upstate oval. -
Compressibility Behavior of Tropical Peat Reinforced with Cement Columns
American Journal of Applied Sciences 4 (10): 786-791, 2007 ISSN 1546-9239 © 2007 Science Publications Compressibility Behavior of Tropical Peat Reinforced with Cement Columns 1Youventharan Duraisamy, 2Bujang B.K. Huat and 2Azlan A. Aziz 1University Malaysia Pahang, Malaysia 2University Putra Malaysia, Serdang, Selangor, Malaysia Abstract : This paper presents the compressibility of tropical peat reinforced with cylin- drical cement columns. When a cement column is installed vertically in peat, its compres- sibility is reduced because of the hardened skeleton matrix formed by cement particles bonding with adjacent soil particles in the presence of pore water. The effects of the ce- ment column diameter on the compressibility have been investigated in this study. The results indicated that compressibility index Cc and Cα decreased with increasing diameter of the cement column. Specimens with 45 mm (area ratio = 0.09) diameter and 60 mm (area ratio = 0.16) diameter of single cement column were cured for 7, 14 and 28 days, after which they were subjected to Rowe Cell Consolidation test. Results are also pre- sented from test conducted on groups of cement columns using four (area ratio = 0.04) and nine (area ratio = 0.09) columns of 15 mm diameter each to investigate the influence of number of cement columns on compressibility of peat soil. Based on the results ob- tained, it shows that cement columns can successfully reduce the compressibility of tropi- cal peat. Keywords: Cement columns, deep soil mixing, organic soil, peat soil, Rowe Cell consol- idation. INTRODUCTION Experimental Design and Laboratory Work: The main objective of this research is to find out the effect of Peat represents the extreme form of soft soil. -
Ujoftni^ Second with I Beth Stakes—And Established Ably Play
C-2 THE EVENING STAR FLYING SCUD ADDED Hugh Wiley Wins Waihington, 0. C., WtrfwWar, Hormbtr 19, 1951 Davis Heads In Toronto Event -- (AP).— JWfM'w’l "*•)*<' x « TORONTO. Nov. 19 \ \ at T3I, *-¦ V//. S*• 7 Field Dozen ¦ wUHBim -PwtL. Back American and German riders Field dominated an international Hurdles horse jumping event at the For Pimlico Futurity Royal Agricultural Winter Fair last night, easily displacing \ / By JOSEPH B, KELLY Farm's Rico Tesio and Cam- Canada, Mexico WF:. Pilot. The riders from Gaines SUr Ruins Idltor bridge Stable's top In places. Star and Cuba for yesterday that Qlenn Davis, Ohio State’s su- announcement Hugh Wiley of Towson, Md., BALTIMORE. Nov. 19.—The ride Pine /N »^?^v.\.^gWIB^PB!PB^EBBBBfcA 3* ? >jL/ ¦&* per track star, will bead a field prospective for Saturday’s Eddie Arcaro would riding Nautical for the United i*x? V field Oak Farm’s Derrick of the world's beet hurdlers in $l7O, 000-plus Pimlico Puturity advanced States, raced over a 12-obstacle Star Games January 24 at today the stock of that colt, who fin- in The is back to 12 after a recent Rem- course without a fault 66.2 the Armory. couple and an ished third in the seconds for first place. He was of withdrawals sen Stakes, beaten a head by Davis, Olympic champion in addition. the only one of 15 riders to hurdles and join Rico Tesio. Derrick is a eon 345-yard the 488-meter low The latest to the fortune the, cover the course with- holder of records in that of Oil Capitol, who won knocking jump. -
Floristic Quality Assessment Report
FLORISTIC QUALITY ASSESSMENT IN INDIANA: THE CONCEPT, USE, AND DEVELOPMENT OF COEFFICIENTS OF CONSERVATISM Tulip poplar (Liriodendron tulipifera) the State tree of Indiana June 2004 Final Report for ARN A305-4-53 EPA Wetland Program Development Grant CD975586-01 Prepared by: Paul E. Rothrock, Ph.D. Taylor University Upland, IN 46989-1001 Introduction Since the early nineteenth century the Indiana landscape has undergone a massive transformation (Jackson 1997). In the pre-settlement period, Indiana was an almost unbroken blanket of forests, prairies, and wetlands. Much of the land was cleared, plowed, or drained for lumber, the raising of crops, and a range of urban and industrial activities. Indiana’s native biota is now restricted to relatively small and often isolated tracts across the State. This fragmentation and reduction of the State’s biological diversity has challenged Hoosiers to look carefully at how to monitor further changes within our remnant natural communities and how to effectively conserve and even restore many of these valuable places within our State. To meet this monitoring, conservation, and restoration challenge, one needs to develop a variety of appropriate analytical tools. Ideally these techniques should be simple to learn and apply, give consistent results between different observers, and be repeatable. Floristic Assessment, which includes metrics such as the Floristic Quality Index (FQI) and Mean C values, has gained wide acceptance among environmental scientists and decision-makers, land stewards, and restoration ecologists in Indiana’s neighboring states and regions: Illinois (Taft et al. 1997), Michigan (Herman et al. 1996), Missouri (Ladd 1996), and Wisconsin (Bernthal 2003) as well as northern Ohio (Andreas 1993) and southern Ontario (Oldham et al. -
Race and (Stakes) Record A.P
Entered Stud in 2015 TRITAP gr/ro, 2009 Dosage (6-5-10-1-0); DI: 2.67; CD: 0.73 See gray pages—Bold Ruler RACE AND (STAKES) RECORD A.P. Indy, 1989 Seattle Slew, by Bold Reasoning Age Starts 1st 2nd 3rd Earned 11s, SW, $2,979,815 Pulpit, 1994 1,184 f, 163 SW, 2.89 AEI Weekend Surprise, by Secretariat 2 3 0 2 0 $20,200 6s, SW, $728,200 3 4 2 1 0 $101,736 919 f, 79 SW, 1.85 AEI Preach, 1989 Mr. Prospector, by Raise a Native Tapit, gr/ro, 2001 15s, SW, $304,656 4 2 0 1(1) 0 $34,000 14 f, 12 r, 12 w, 1 SW Narrate, by Honest Pleasure Totals 9 2 4(1) 0 $155,936 6s, SW, $557,300 866 f, 70 SW, 2.33 AEI Unbridled, 1987 Fappiano, by Mr. Prospector Won At 3 7.45 AWD 24s, SW, $4,489,475 An allowance race at CD ($52,000, 9.5f in 1:58.12, Tap Your Heels, 1996 566 f, 49 SW, 2.65 AEI Gana Facil, by Le Fabuleux 9s, SW, $47,275 NTR, dftg. Suns Out Guns Out, Shun, Charlie’s the 10 f, 6 r, 3 w, 1 SW Ruby Slippers, 1982 Nijinsky II, by Northern Dancer Man, Kid Sidney, Starforce, Chalybeate Springs). 14s, wnr, $83,760 A maiden special weight race at Sar ($80,000, 7f in 13 f, 13 r, 10 w, 2 SW Moon Glitter, by In Reality 1:22.56, dftg. Cape Glory, Joking, D’tiger, In Seattle Slew, 1974 Bold Reasoning, by Boldnesian Speight Ofitall, Chief Gaga, Dattts Happy, Guilt Trip, 17s, SW, $1,208,726 Avarice, Starter, Grand Rapids). -
Calcareous Fens in Southeast Alaska
United States Department of Agriculture Calcareous Fens in Southeast Forest Service Pacifi c Northwest Alaska Research Station 1 Research Note Michael H. McClellan, Terry Brock, and James F. Baichtal PNW-RN-536 February 2003 Abstract Calcareous fens have not been identifi ed previously in southeast Alaska. A limited survey in southeast Alaska identifi ed several wetlands that appear to be calcare- ous fens. These sites were located in low-elevation discharge zones that are below recharge zones in carbonate highlands and talus foot-slopes. Two of six surveyed sites partly met the Minnesota Department of Natural Resources water chemistry criteria for calcareous fens, with pH values of 6.7 to 7.4 and calcium concentrations of 41.8 to 51.4 mg/L but fall short with regard to specifi c conductivity (315 to 380 μS/cm). Alkalinity was not determined. The vegetation was predominately herbaceous, with abundant Sitka sedge (Carex aquatilis) and scattered shrubs such as Barclay’s willow (Salix barclayi) and redosier dogwood (Cornus sericea ssp. sericea). The taxa found in these fens have been reported at other sites in southeast Alaska, although many were at the southern limits of their known ranges. The soils were Histosols composed of 0.6 to greater than 1 m of sedge peat. We found no evidence of calcium carbonate precipitates (marl or tufa) in the soil. Keywords: Alaska (southeast), fens, calcareous fens, wetlands, peatlands, karst. Introduction Calcareous fens, a subtype of extremely rich fen, are important because of their rarity, their distinctive water chemistry, and because they frequently harbor rare or endangered plants (Calcareous Fen Technical Committee 1994).