Conversations in Soil Taxonomy (Original Tr,.&Nscr|F't~Ons of Taped Conversations)
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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. -
NRCS Keys to Soil Taxonomy
United States Department of Agriculture Keys to Soil Taxonomy Ninth Edition, 2003 Keys to Soil Taxonomy By Soil Survey Staff United States Department of Agriculture Natural Resources Conservation Service Ninth Edition, 2003 The United States Department of Agriculture (USDA) prohibits discrimination in all its programs and activities on the basis of race, color, national origin, gender, religion, age, disability, political beliefs, sexual orientation, and marital or family status. (Not all prohibited bases apply to all programs.) Persons with disabilities who require alternative means for communication of program information (Braille, large print, audiotape, etc.) should contact USDA’s TARGET Center at 202-720-2600 (voice and TDD). To file a complaint of discrimination, write USDA, Director, Office of Civil Rights, Room 326W, Whitten Building, 14th and Independence Avenue, SW, Washington, DC 20250-9410, or call 202-720-5964 (voice and TDD). USDA is an equal opportunity provider and employer. Cover: A natric horizon with columnar structure in a Natrudoll from Argentina. 5 Table of Contents Foreword .................................................................................................................................... 7 Chapter 1: The Soils That We Classify.................................................................................. 9 Chapter 2: Differentiae for Mineral Soils and Organic Soils ............................................... 11 Chapter 3: Horizons and Characteristics Diagnostic for the Higher Categories ................. -
Integrated Evaluation of Petroleum Impacts to Soil
Integrated Evaluation of Petroleum Impacts to Soil Randy Adams, D. Marín, C. Avila, L. de la Cruz, C. Morales, and V. Domínguez Universidad Juárez Autónoma de Tabasco, Villahermosa, Mexico [email protected] 1.00 0.90 0.80 0.70 0.60 R2 = 0.9626 0.50 0.40 1-IAFcorr 0.30 0.20 0.10 0.00 0 1000 2000 3000 4000 5000 6000 7000 8000 9000 10000 Conc. hidrocarburos (mg/Kg) Actual Modelo BACKGROUND U J A T •Clean-up criteria for petroleum contaminated soils developed in US in 60’s and 70’s on drilling cuttings •1% considered OK – no or only slight damage to crops, only lasts one growing season •Bioassays confirmed low toxicity of residual oil •Subsequenty used as a basis for clean-up criteria for hydrocarbons in soils in many countries does not consider kind of hydrocarbons does not consider kind of soil SISTEMATIC EVALUATION U J A T •Selection of light, medium, heavy and extra-heavy crudes •Selection of 5 soil types common in petroleum producing region of SE Mexico •Contamination of soil at different concentrations •Measurement of acute toxicity (Microtox), and subchronic toxicity (28 d earthworm) •Measurement of impacts to soil fertility: water repellency, soil moisure, compaction, complemented with in situ weathering experiments •Measurement of plant growth: pasture, black beans Crude Petroleum Used in Study U J A T 100% 80% 60% Aliphatics Aromatics 40% Polars + Resins Asphaltenes 20% 0% Light Crude Medium Crude Heavy Crude Extra-heavy Crude 37 ºAPI 27 ºAPI 15 ºAPI 3 ºAPI U J A T FAO: FLUVISOL VERTISOL GLEYSOL ARENOSOL ACRISOL USDA: FLUVENT -
Keys to Soil Taxonomy
United States Department of Agriculture Keys to Soil Taxonomy Ninth Edition, 2003 Keys to Soil Taxonomy By Soil Survey Staff United States Department of Agriculture Natural Resources Conservation Service Ninth Edition, 2003 The United States Department of Agriculture (USDA) prohibits discrimination in all its programs and activities on the basis of race, color, national origin, gender, religion, age, disability, political beliefs, sexual orientation, and marital or family status. (Not all prohibited bases apply to all programs.) Persons with disabilities who require alternative means for communication of program information (Braille, large print, audiotape, etc.) should contact USDA’s TARGET Center at 202-720-2600 (voice and TDD). To file a complaint of discrimination, write USDA, Director, Office of Civil Rights, Room 326W, Whitten Building, 14th and Independence Avenue, SW, Washington, DC 20250-9410, or call 202-720-5964 (voice and TDD). USDA is an equal opportunity provider and employer. Cover: A natric horizon with columnar structure in a Natrudoll from Argentina. 5 Table of Contents Foreword .................................................................................................................................... 7 Chapter 1: The Soils That We Classify.................................................................................. 9 Chapter 2: Differentiae for Mineral Soils and Organic Soils ............................................... 11 Chapter 3: Horizons and Characteristics Diagnostic for the Higher Categories ................. -
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 . -
2021 Soils/Land Use Study Resources
2021 NCF Envirothon Soil Test Study Guide Lincoln, Nebraska 2021 NCF-Envirothon Nebraska Soils and Land Use Study Resources Key Topic #1: Physical Properties of Soil and Soil Formation 1. Describe the five soil forming factors, and how they influence soil properties. 2. Explain the defining characteristics of a soil describing how the basic soil forming processes influence affect these characteristics in different types of soil. 3. Identify different types of parent material, their origins, and how they impact the soil that develops from them. 4. Identify and describe soil characteristics (horizon, texture, structure, color). 5. Identify and understand physical features of soil profiles and be able to use this information interpret soil properties and limitations. Study Resources Sample Soil Description Scorecard – University of Nebraska – Lincoln Land Judging Documents, edited by Judy Turk, 2021 (Pages 3-4) Soil Description Field Manual Reference – University of Nebraska – Lincoln Land Judging Documents, edited by Judy Turk, 2021 (Pages 5-17) Correlation of Field Texturing Soils by Feel, Understanding Soil Laboratory Data, and Use of the Soil Textural Triangle – Patrick Cowsert, 2021 (Pages 18-21) Tips for Measuring Percent Slope on Contour Maps – Excerpt from Forest Measurements by Joan DeYoung, 2018 (Pages 22-23) Glossary – Excerpts from Geomorphic Description System version 5.0, 2017, and Field Book for Describing Soils version 3.0, 2012 (Pages 24-27) Study Resources begin on the next page! Contestant Number Sample Soil Description Card Site/Pit Number Host: University of Nebraska – Lincoln Number of Horizons Lower Profile Depth 2021 –Scorecard Nail Depth A. Soil Morphology Part A Score __________ Moist Horizons Boundary Texture Color Redox. -
Effect of Waterlogging on Soil Biochemical Properties and Organic Matter Quality
26 Effect of waterlogging on soil biochemical properties and organic matter quality 27 in different salt marsh systems 28 29 Chiara Ferronatoa, Sara Marinarib, Ornella Franciosoa, Diana Belloc, Carmen Trasar-Cepedac, Livia 30 Vittori Antisaria 31 32 a Dipartimento di Scienze e Tecnologie Agro-Alimentari, Alma Mater Studiorum – Università di 33 Bologna, Via Fanin 44, 40127 Bologna, Italy 34 b Dipartimento per l’ Innovazione dei Sistemi Biologici, Agroalimentari e Forestali, Università della 35 Tuscia, Via S. Camillo de Lellis, 01100 Viterbo, Italy 36 c Departamento de Bioquímica del Suelo, Instituto de Investigaciones Agrobiológicas de Galicia- 37 Consejo Superior de Investigaciones Científicas, Apartado 122, 15780 Santiago de Compostela, 38 Spain 39 40 Abstract 41 This study investigated the effects of hydroperiod on soil organic matter quality in three different salt 42 marshes in the Baiona lagoon (N Italy) representing terrestrial, intertidal and subaqueous ecosystems 43 in the area. The study specifically aimed to gain some insight into how soil waterlogging 44 (hydroperiod) affects the chemical and biological properties of soils as well as the quality and 45 structure of the soil organic matter (SOM). Total contents of selected nutrients, total organic carbon 46 and carbon stable isotope (δC 13) were measured in all soil profiles. The results of these analyses 47 enabled us to define the different origin of the SOM by discriminating between terrestrial and aquatic 48 SOM sources. The findings also show that accumulation of nutrients and SOM is significantly 49 magnified in intertidal systems, in which pedoturbation effects induced by water movements are 50 particularly strong. In addition, DRIFT spectra of humic acids revealed the changes in the main 2 51 functional groups in relation to increased waterlogging, highlighting the lower aromaticity and 52 complexity in subaqueous soils (SASs), which is possibly due to the effect of the soil water saturation 53 on the chemical and biological SOM transformation processes. -
John Day Fossil Beds NM: Geology and Paleoenvironments of the Clarno Unit
John Day Fossil Beds NM: Geology and Paleoenvironments of the Clarno Unit JOHN DAY FOSSIL BEDS Geology and Paleoenvironments of the Clarno Unit John Day Fossil Beds National Monument, Oregon GEOLOGY AND PALEOENVIRONMENTS OF THE CLARNO UNIT John Day Fossil Beds National Monument, Oregon By Erick A. Bestland, PhD Erick Bestland and Associates, 1010 Monroe St., Eugene, OR 97402 Gregory J. Retallack, PhD Department of Geological Sciences University of Oregon Eugene, OR 7403-1272 June 28, 1994 Final Report NPS Contract CX-9000-1-10009 TABLE OF CONTENTS joda/bestland-retallack1/index.htm Last Updated: 21-Aug-2007 http://www.nps.gov/history/history/online_books/joda/bestland-retallack1/index.htm[4/18/2014 12:20:25 PM] John Day Fossil Beds NM: Geology and Paleoenvironments of the Clarno Unit (Table of Contents) JOHN DAY FOSSIL BEDS Geology and Paleoenvironments of the Clarno Unit John Day Fossil Beds National Monument, Oregon TABLE OF CONTENTS COVER ABSTRACT ACKNOWLEDGEMENTS CHAPTER I: INTRODUCTION AND REGIONAL GEOLOGY INTRODUCTION PREVIOUS WORK AND REGIONAL GEOLOGY Basement rocks Clarno Formation John Day Formation CHAPTER II: GEOLOGIC FRAMEWORK INTRODUCTION Stratigraphic nomenclature Radiometric age determinations CLARNO FORMATION LITHOSTRATIGRAPHIC UNITS Lower Clarno Formation units Main section JOHN DAY FORMATION LITHOSTRATIGRAPHIC UNITS Lower Big Basin Member Middle and upper Big Basin Member Turtle Cove Member GEOCHEMISTRY OF LAVA FLOW AND TUFF UNITS Basaltic lava flows Geochemistry of andesitic units Geochemistry of tuffs STRUCTURE OF CLARNO -
Prairie Dog and Burrowing Owl Habitat Analysis Throughout Nebraska: Summary
Prairie Dog and Burrowing Owl Habitat Analysis throughout Nebraska: Summary Rainwater Basin Joint Venture Report. 2012. Andy Bishop1, Laura Achterberg1, Roger Grosse1, Ele Nugent1, and Christopher Jorgensen1,2 1Rainwater Basin Joint Venture, 2550 North Diers Ave, Grand Island, NE 68801 2Nebraska Cooperative Fish and Wildlife Research Unit, 422 Hardin Hall, 3310 Holdrege Street, Lincoln, NE 68583 Introduction For this analysis, we downloaded SSURGO data on a county by Identifying suitable habitat in the landscape for rare and elusive county basis from Soil Data Viewer 5.2 using ArcGIS 9.2. We species can assist wildlife managers in forming conservation merged multiple data layers together into a single shapefile to plans and can even facilitate new discoveries of species provide a statewide coverage. Each polygon in the dataset populations. The following project sought to identify available represented a single SSURGO map unit. We extracted the soil habitat for Burrowing Owls in Nebraska. Burrowing Owls are map unit name and the range site name from the Soil Data considered a Tier 1 at-risk species (i.e., a species globally or Viewer. nationally most at risk of extinction) by the Nebraska Game and Parks Commission (NGPC). We developed a conceptually Burrowing Owls are known to occupy burrows 200 cm below based, spatially explicit habitat suitability index to determine the the soil surface in Washington (Conway et al. 2006) and 69 cm remaining suitable habitat for Burrowing Owls in Nebraska. in Oklahoma (Butts and Lewis 1982). We took the average of Model development was based on a previous modeling exercise these two estimates, establishing burrow preference of 136 cm geared towards identifying suitable habitat for Black-tailed below the soil surface. -
This File Was Created by Scanning the Printed Publication
This file was created by scanning the printed publication. Text errors identified by the software have been corrected; however, some errors may remain. Editors SHARON E. CLARKE is a geographer and GIS analyst, Department of Forest Science, Oregon State University, Corvallis, OR 97331; and SANDRA A. BRYCE is a biogeographer, Dynamac Corporation, Environmental Protection Agency, National Health and Environmental Effects Research Laboratory, Western Ecology Division, Corvallis, OR 97333. This document is a product of cooperative research between the U.S. Department of Agriculture, Forest Service; the Forest Science De- partment, Oregon State University; and the U.S. Environmental Protection Agency. Cover Artwork Cover artwork was designed and produced by John Ivie. Abstract Clarke, Sharon E.; Bryce, Sandra A., eds. 1997. Hierarchical subdivisions of the Columbia Plateau and Blue Mountains ecoregions, Oregon and Washington. Gen. Tech. Rep. PNW-GTR-395. Portland, OR: U.S. Department of Agriculture, Forest Service, Pacific Northwest Research Station. 114 p. This document presents two spatial scales of a hierarchical, ecoregional framework and provides a connection to both larger and smaller scale ecological classifications. The two spatial scales are subregions (1:250,000) and landscape-level ecoregions (1:100,000), or Level IV and Level V ecoregions. Level IV ecoregions were developed by the Environmental Protection Agency because the resolution of national-scale ecoregions provided insufficient detail to meet the needs of state agencies for estab- lishing biocriteria, reference sites, and attainability goals for water-quality regulation. For this project, two ecoregions—the Columbia Plateau and the Blue Mountains— were subdivided into more detailed Level IV ecoregions. -
Custom Soil Resource Report for Miami-Dade County Area, Florida
United States A product of the National Custom Soil Resource Department of Cooperative Soil Survey, Agriculture a joint effort of the United Report for States Department of Agriculture and other Federal agencies, State Miami-Dade Natural agencies including the Resources Agricultural Experiment County Area, Conservation Stations, and local Service participants Florida July 12, 2018 Preface Soil surveys contain information that affects land use planning in survey areas. They highlight soil limitations that affect various land uses and provide information about the properties of the soils in the survey areas. Soil surveys are designed for many different users, including farmers, ranchers, foresters, agronomists, urban planners, community officials, engineers, developers, builders, and home buyers. Also, conservationists, teachers, students, and specialists in recreation, waste disposal, and pollution control can use the surveys to help them understand, protect, or enhance the environment. Various land use regulations of Federal, State, and local governments may impose special restrictions on land use or land treatment. Soil surveys identify soil properties that are used in making various land use or land treatment decisions. The information is intended to help the land users identify and reduce the effects of soil limitations on various land uses. The landowner or user is responsible for identifying and complying with existing laws and regulations. Although soil survey information can be used for general farm, local, and wider area planning, onsite investigation is needed to supplement this information in some cases. Examples include soil quality assessments (http://www.nrcs.usda.gov/wps/ portal/nrcs/main/soils/health/) and certain conservation and engineering applications. For more detailed information, contact your local USDA Service Center (https://offices.sc.egov.usda.gov/locator/app?agency=nrcs) or your NRCS State Soil Scientist (http://www.nrcs.usda.gov/wps/portal/nrcs/detail/soils/contactus/? cid=nrcs142p2_053951). -
On Tropical Soils?
AJCS 13(11):1777-1785 (2019) ISSN:1835-2707 doi: 10.21475/ajcs.19.13.11.p1562 Could 137Cs remediation be accomplished with stable cesium (CsCl) on tropical soils? Riviane Maria Albuquerque Donha1*, Mário Roque2, Antônio Enedi Boaretto2, Antonio Sergio Ferraudo1, Elcio Ferreira Santos2, Fernando Giovannetti Macedo1, Wanderley José Melo13, José Lavres Junior2 1UNESP – São Paulo State University, Postal Code 79560-000, Jaboticabal, SP, Brazil 2USP – University of São Paulo, Center for Nuclear Energy in Agriculture. Postal Code 13416-000, Piraicaba, SP, Brazil 3Brasil University, Postal Code 13690-000, Descalvado, SP, Brazil *Correspondence authorl: [email protected] Abstract Stable cesium can be considered as the best element for desorption of soil radio-cesium. It is considered an element that slightly absorbed by plants, so that the application of high doses to the soil could increase the absorption of 137Cs, which is desired for the remediation of contaminated soils. There is shortage of knowledge on remediation of tropical and subtropical soils contaminated with 137Cs. The aim of this work was to evaluate the use of 133Cs for the remediation of Brazilian tropical and subtropical soils contaminated with 137Cs. In addition, we investigated the Cs uptake by bean plants (Phaseolus vulgaris L.) grown in Cs contaminated soil. The experiment was carried out in pots under greenhouse conditions. Seven soil types were used in the experiment (Oxisol, Udox, Psamment, Ochrept; Aquoll; Udox and Udult), which received the application of four doses of 133Cs (0, 5, 10 and 20 mg/pot in a completely randomized design arranged in a factorial scheme (7 soil types x 4 doses of 133Cs) with three replicates.