Soils Classified (USDA System)

Total Page:16

File Type:pdf, Size:1020Kb

Soils Classified (USDA System) Soils Classified (USDA System) 1. Terminology a. class: A group of individuals that are similar in selected properties. b. category: A group of classes. c. hierarchical system: A system having a number of categories differing in level of generalization, such that each class within a category is also a subclass of a class within any higher category. 2. Categories of the USDA System Order (12 total), ex. Spodosol Suborder, ex., Aquod Great Group, ex., Alaquod Subgroup, ex., Aeric Alaquod Family, ex., sandy, siliceous, hyperthermic, Aeric Alaquod Series, ex., Myakka Syllables used to designate classes 1 Formative elements for Orders are as follows: Alfisols - alf Inceptisols - ept Andisols – and Mollisols - oll Aridisols – id Oxisols - ox Entisols – ent Spodosols - od Gelisol – el Ultisols - ult Histosols – ist Vertisols - ert Useful formative elements at suborder level are: Aqu - Frequently saturated to surface or near surface. Fluv - Evidence of stratification from flooding. Fibr - High amount of undecomposed organic matter. Hem - High amount of organic matter, moderately decomposed. Sapr - High amount of highly-decomposed organic matter. Ud - HidlibHumid climate, but so il not too wet. Ust - Intermediate rainfall, soil not too wet. Xer - Dry climate, soil not too wet. Torr - Hot, dry climate; soil not too wet. Orth - Nothing extreme or distinctive. Umbr - Umbric (dark, thick, low-base surface horizon). 3. Diagnostic Horizons a. Examples of Diagnostic Surface Horizons (Epipedons) Histic: high organic C content (generally > 12%) Mollic: soft,,, dark, thick, high base saturation Umbric: soft, dark, thick, low base saturation Ochric: Essentially a default 2 b. Examples of Diagnostic Subsurface Horizons (Epipedons) Albic: light-colored due to loss (eluviation) of components Argillic: zone of clay accumulation via translocation Spodic: zone of preciitation of organo-metal components chemically translocated from another zone Salic: zone of soluble salt accumulation Sulfuric: low pH, yellow mottles from Fe sulfate minerals 4. Soil Orders that occur in Florida Histosols - Dominated by organic soil material Spodosols - Have Spodic. May have Argillic Mollisol - Have Mollic & BS ≥ 50%. May have Argillic Alfisols - Have argillic and BS ≥ 35% in lower part Ultisol - Have argillic and BS < 35% in lower part Inceptisol - Have Umbric or Histic (in some cases Mollic) Entisol - Default. Absence of most diagnostic horizons to 2 m 5. Categories & Nomenclature Examples Credit Wade Hurt for this a subsequent slides Examples of Entisol Great Groups • Suborder • Great Groups Aquents Cryaquents - cold (Wet Entisols) Fluvaquents - floodplain Hydraquents - water Psammaquents - sand Epiaquents - perched 3 Examples of Entisol Great Groups • Suborder • Great Groups Fluvents Torrifluvents - torrid (Floodplain (hot and dry) soils) Tropofluvents - tropical (dhid)(warm and humid) Udifluvents - humid (not dry in most years) Ustifluvents - semi-arid (between Udic-Aridic) Xerofluvents - semi-arid (Mediterranean climate) Examples of Entisol Great Groups • Suborder • Great Groups Psamments Cryopsamments (Sandy Soils) Quartzipsamments - Quartz Torripsamments Udipsamments Ustipsamments Xeropsamments Examples of Subgroups 4 3 2 1 Typic Fluvaquents 4 1 2 Typical Entisols with aquic moisture regimes 3 that occur on floodplains. 1. Order 3. Great Group 2. Suborder 4. Subgroup (typical concept of Fluvaquents 4 Examples of Subgroups 4 3 2 1 Mollic Fluvaquents 1 2 EntisolsEntisols wwithith aquaquicic mmoistureoisture rregimesegimes tthathat 3 occur on floodplains & have thick, 4 dark surface layers. 1. Order 3. Great Group 2. Suborder 4. Subgroup (intergrading toward a Mollisol) Examples of Subgroups 4 3 2 1 Aeric Fluvaquents 1 3 2 Entisols on floodplains with aquic moisture regimes that are not so wet. They are better 4 aerated in the “upper” part of the soil profile. 1. Order 3. Great Group 2. Suborder 4. Subgroup (intergrading toward a more aerated subgroup) “Sidebar”:Aquic Soil Moisture Regimes • Typic subgroup of an aquic suborder: • Typic ____aqu____ – wettest • AiAericsubfbgroup of an aquic suborder: • Aeric ____aqu____ – better aerated • Aquic subgroup: • Aquic ___________ –driest From Mausbach 1992 5 Nature of Number Differentiating Category of Taxa Characteristics Family Many The Family name consists of a series of descriptive terms that modify the subgroup name. Note: Family name adds no knowledge to understanding of wet soils. Nature of Number Differentiating Category of Taxa Characteristics Series 17,000+ May have virtually the full range of properties permitted in a family, but range is restricted in one or more properties . Note: since the series name adds no knowledge to our understanding of wet soils it the series level of soil classification will not be discussed. 7. Practice Typic Haplosaprists 6 Typic Haplosaprists • What does the taxonomic classification mean? • Is it likely, not likely, or maybe hydric? – Histosol dominated by sapric material (wet). – Likely to be hydric. Large areas of this soil converted to crop land in south Florida. Aquic Paleudalfs Aquic Paleudalfs • What does the taxonomic classification mean? • Is it likely, not likely, or maybe hydric? – Alfisol with aquic conditions moderately deep in profile. – Likely to be nonhydric. Has water table in E horizon for brief periods during high rainfall. In an aquic subgroup. 7 Aquic Quartzipsamments Aquic Quartzipsamments • What does the taxonomic classification mean? • Is it likely, not likely, or maybe hydric? – Entisol that is sandy, dominated by quartz sand, with aquic conditions moderately deep in profile. – Likely to be a nonhydric soil. In an aquic subgroup. Seasonal high water table at about 24 inches. Typic Argiaquolls 8 Typic Argiaquolls • What does the taxonomic classification mean? • Is it likely, not likely, or maybe hydric? – Mollisol with aquic conditions near surface and accumulation of clay in subsoil. – Likely to be hydric. Hydric soils commonly classify in an aquic suborder; “argi” is “double whammy” (will explain). Aeric Alaquods Aeric Alaquods • What does the taxonomic classification mean? • Is it likely, not likely, or maybe hydric? – Spodosol with aquic conditions near surface; not quite as wet as “typic” subgroups. – Maybe hydric. Typical Spodosol on flatwoods. In an aquic suborder. 9 Class as Likely Hydric, Maybe Hydric, or Likely Non-Hydric • Typic Haplosaprists Terric Haplosaprists • Lithic Cryofolists Aquic Paleudalfs •Aquic Glossudalfs Typic Aq uisalids • Aquic Quartzipsamments Typic Humaquepts • Typic Argiaquolls Argiaquic Argialbolls • Aeric Calciaquolls Aeric Alaquods • Typic Umbraquults Chromic Epiaquerts Answers According to Hurt • Likely Hydric – Typic Haplosaprists Terric Haplosaprists – Typic Humaquepts Typic Umbraquults – Typic Argiaquolls Typic Aquisalids – Chromic Epiaquerts Argiaquic Argialbolls • Maybe Hydric – Aeric Calciaquolls Aeric Alaquods • Likely Nonhydric – Aquic Glossudalfs Aquic Paleudalfs – Aquic Quartzipsamments Lithic Cryofolists Summary • Likely Hydric: Soils in the Albolls Suborder or soils with a formative element at the Suborder level of soil classification (Aqu, Fibr, Hist, and Sapr.), unless they have the formative element aeri at the suborder level & soils in the following Great Groups Aquisalids, Historthels, and Histoturbels. • MbMaybe HdiHydric: So ils w ith a ftiformative elttthSbdlement at the Suborder level of soil classification (Aqu, Fibr, Hist, and Sapr.) and the formative element aeri at the suborder level & soils on flood plains such as Aquic Dystrochrepts, Aquic Eutrochrepts, & Aquic Udifluvents. • Likely Nonhydric: Soils with all other classifications including aqu at the Subgroup level of soil classification with some exceptions (note the three example given above). 10.
Recommended publications
  • Topic: Soil Classification
    Programme: M.Sc.(Environmental Science) Course: Soil Science Semester: IV Code: MSESC4007E04 Topic: Soil Classification Prof. Umesh Kumar Singh Department of Environmental Science School of Earth, Environmental and Biological Sciences Central University of South Bihar, Gaya Note: These materials are only for classroom teaching purpose at Central University of South Bihar. All the data/figures/materials are taken from several research articles/e-books/text books including Wikipedia and other online resources. 1 • Pedology: The origin of the soil , its classification, and its description are examined in pedology (pedon-soil or earth in greek). Pedology is the study of the soil as a natural body and does not focus primarily on the soil’s immediate practical use. A pedologist studies, examines, and classifies soils as they occur in their natural environment. • Edaphology (concerned with the influence of soils on living things, particularly plants ) is the study of soil from the stand point of higher plants. Edaphologist considers the various properties of soil in relation to plant production. • Soil Profile: specific series of layers of soil called soil horizons from soil surface down to the unaltered parent material. 2 • By area Soil – can be small or few hectares. • Smallest representative unit – k.a. Pedon • Polypedon • Bordered by its side by the vertical section of soil …the soil profile. • Soil profile – characterize the pedon. So it defines the soil. • Horizon tell- soil properties- colour, texture, structure, permeability, drainage, bio-activity etc. • 6 groups of horizons k.a. master horizons. O,A,E,B,C &R. 3 Soil Sampling and Mapping Units 4 Typical soil profile 5 O • OM deposits (decomposed, partially decomposed) • Lie above mineral horizon • Histic epipedon (Histos Gr.
    [Show full text]
  • Soils Section
    Soils Section 2003 Florida Envirothon Study Sections Soil Key Points SOIL KEY POINTS • Recognize soil as an important dynamic resource. • Describe basic soil properties and soil formation factors. • Understand soil drainage classes and know how wetlands are defined. • Determine basic soil properties and limitations, such as mottling and permeability by observing a soil pit or soil profile. • Identify types of soil erosion and discuss methods for reducing erosion. • Use soil information, including a soil survey, in land use planning discussions. • Discuss how soil is a factor in, or is impacted by, nonpoint and point source pollution. Florida’s State Soil Florida has the largest total acreage of sandy, siliceous, hyperthermic Aeric Haplaquods in the nation. This is commonly called Myakka fine sand. It does not occur anywhere else in the United States. There are more than 1.5 million acres of Myakka fine sand in Florida. On May 22, 1989, Governor Bob Martinez signed Senate Bill 525 into law making Myakka fine sand Florida’s official state soil. iii Florida Envirothon Study Packet — Soils Section iv Contents CONTENTS INTRODUCTION .........................................................................................................................1 WHAT IS SOIL AND HOW IS SOIL FORMED? .....................................................................3 SOIL CHARACTERISTICS..........................................................................................................7 Texture......................................................................................................................................7
    [Show full text]
  • The Impact of White Pine (Pinus Strobus) on a Mollisol After Seven Decades of Soil Development
    Journal of the Iowa Academy of Science: JIAS Volume 111 Number 3-4 Article 4 2004 The Impact of White Pine (Pinus strobus) on a Mollisol After Seven Decades of Soil Development Irina Kovda Institute of Geography, Moscow Eric C. Brevik Iowa State University Thomas E. Fenton Moscow State University Maria Gerasimova Valdosta State University Let us know how access to this document benefits ouy Copyright © Copyright 2005 by the Iowa Academy of Science, Inc. Follow this and additional works at: https://scholarworks.uni.edu/jias Part of the Anthropology Commons, Life Sciences Commons, Physical Sciences and Mathematics Commons, and the Science and Mathematics Education Commons Recommended Citation Kovda, Irina; Brevik, Eric C.; Fenton, Thomas E.; and Gerasimova, Maria (2004) "The Impact of White Pine (Pinus strobus) on a Mollisol After Seven Decades of Soil Development," Journal of the Iowa Academy of Science: JIAS, 111(3-4), 58-66. Available at: https://scholarworks.uni.edu/jias/vol111/iss3/4 This Research is brought to you for free and open access by the Iowa Academy of Science at UNI ScholarWorks. It has been accepted for inclusion in Journal of the Iowa Academy of Science: JIAS by an authorized editor of UNI ScholarWorks. For more information, please contact [email protected]. Jour. Iowa Acad. Sci. 111(3,4):58-66, 2004 The Impact of White Pine (Pinus strobus) on a Mollisol After Seven Decades of Soil Development IRINA KOVDA1, ERIC C. BREVIK2A, THOMAS E. FENTON2, and MARIA GERASIMOVA3 1 Institute of Geography, Staromonetny 29, Moscow, 109017,
    [Show full text]
  • Determining Carbon Stocks in Cryosols Using the Northern and Mid Latitudes Soil Database
    Permafrost, Phillips, Springman & Arenson (eds) © 2003 Swets & Zeitlinger, Lisse, ISBN 90 5809 582 7 Determining carbon stocks in Cryosols using the Northern and Mid Latitudes Soil Database C. Tarnocai Agriculture and Agri-Food Canada, Ottawa, Ontario, Canada J. Kimble USDA-NRCS-NSSC, Lincoln, Nebraska, USA G. Broll Institute of Landscape Ecology, University of Muenster, Muenster, Germany ABSTRACT: The distribution of Cryosols and their carbon content and mass in the northern circumpolar area were estimated by using the Northern and Mid Latitudes Soil Database (NMLSD). Using this database, it was estimated that, in the Northern Hemisphere, Cryosols cover approximately 7769 ϫ 103 km2 and contain approxi- mately 119 Gt (surface, 0–30 cm) and 268 Gt (total, 0–100 cm) of soil organic carbon. The 268 Gt organic carbon is approximately 16% of the world’s soil organic carbon. Organic Cryosols were found to have the highest soil organic carbon mass at both depth ranges while Static Cryosols had the lowest. The accuracy of these carbon val- ues is variable and depends on the information available for the area. Since these soils contain a significant por- tion of the Earth’s soil organic carbon and will probably be the soils most affected by climate warming, new data is required so that more accurate estimates of their carbon budget can be made. 1 INTRODUCTION which is in Arc/Info format, the Soils of Northern and Mid Latitudes (Tarnocai et al. 2002a) and Northern Soils are the largest source of organic carbon in ter- Circumpolar Soils (Tarnocai et al. 2002b) maps were restrial ecosystems.
    [Show full text]
  • World Reference Base for Soil Resources 2014 International Soil Classification System for Naming Soils and Creating Legends for Soil Maps
    ISSN 0532-0488 WORLD SOIL RESOURCES REPORTS 106 World reference base for soil resources 2014 International soil classification system for naming soils and creating legends for soil maps Update 2015 Cover photographs (left to right): Ekranic Technosol – Austria (©Erika Michéli) Reductaquic Cryosol – Russia (©Maria Gerasimova) Ferralic Nitisol – Australia (©Ben Harms) Pellic Vertisol – Bulgaria (©Erika Michéli) Albic Podzol – Czech Republic (©Erika Michéli) Hypercalcic Kastanozem – Mexico (©Carlos Cruz Gaistardo) Stagnic Luvisol – South Africa (©Márta Fuchs) Copies of FAO publications can be requested from: SALES AND MARKETING GROUP Information Division Food and Agriculture Organization of the United Nations Viale delle Terme di Caracalla 00100 Rome, Italy E-mail: [email protected] Fax: (+39) 06 57053360 Web site: http://www.fao.org WORLD SOIL World reference base RESOURCES REPORTS for soil resources 2014 106 International soil classification system for naming soils and creating legends for soil maps Update 2015 FOOD AND AGRICULTURE ORGANIZATION OF THE UNITED NATIONS Rome, 2015 The designations employed and the presentation of material in this information product do not imply the expression of any opinion whatsoever on the part of the Food and Agriculture Organization of the United Nations (FAO) concerning the legal or development status of any country, territory, city or area or of its authorities, or concerning the delimitation of its frontiers or boundaries. The mention of specific companies or products of manufacturers, whether or not these have been patented, does not imply that these have been endorsed or recommended by FAO in preference to others of a similar nature that are not mentioned. The views expressed in this information product are those of the author(s) and do not necessarily reflect the views or policies of FAO.
    [Show full text]
  • Phosphorus Adsorption of Some Brazilian Soils in Relations to Selected Soil Properties
    Open Journal of Soil Science, 2015, 5, 101-109 Published Online May 2015 in SciRes. http://www.scirp.org/journal/ojss http://dx.doi.org/10.4236/ojss.2015.55010 Phosphorus Adsorption of Some Brazilian Soils in Relations to Selected Soil Properties Valdinar Ferreira Melo1*, Sandra Cátia Pereira Uchôa1, Zachary N. Senwo2*, Ronilson José Pedroso Amorim3 1Department of Soil and Agricultural Engineering, Federal University of Roraima, Boa Vista, Brazil 2Department of Biological & Environmental Sciences, Alabama A&M University, Huntsville, USA 3Agronomy, Federal University of Roraima, Boa Vista, Brazil Email: *[email protected], *[email protected] Received 3 April 2015; accepted 17 May 2015; published 20 May 2015 Copyright © 2015 by authors and Scientific Research Publishing Inc. This work is licensed under the Creative Commons Attribution International License (CC BY). http://creativecommons.org/licenses/by/4.0/ Abstract A major nutritional problem to crops grown in highly weathered Brazilian soils is phosphorus (P) deficiencies linked to their low availability and the capacity of the soils to fix P in insoluble forms. Our studies examined factors that might influence P behavior in soils of the Amazon region. This study was conducted to evaluate the maximum phosphate adsorption capacity (MPAC) of the soils developed from mafic rocks (diabase), their parent materials and other factors resulting in the formation of eutrophic soils having A chernozemic horizon associated with Red Nitosols (Alfisol) and Red Latosols (Oxisol) of the Amazonian environment. The MPAC was determined in triplicates as a function of the remnant P values. The different concentrations used to determine the MPAC allowed maximum adsorption values to be reached for all soils.
    [Show full text]
  • Diagnostic Horizons
    Exam III Wednesday, November 7th Study Guide Posted Tomorrow Review Session in Class on Monday the 4th Soil Taxonomy and Classification Diagnostic Horizons Epipedons Subsurface Mollic Albic Umbric Kandic Ochric Histic Argillic Melanic Spodic Plaggen Anthropic Oxic 1 Surface Horizons: Mollic- thick, dark colored, high %B.S., structure Umbric – same, but lower B.S. Ochric – pale, low O.M., thin Histic – High O.M., thick, wet, dark Sub-Surface Horizons: Argillic – illuvial accum. of clay (high activity) Kandic – accum. of clay (low activity) Spodic – Illuvial O.M. accumulation (Al and/or Fe) Oxic – highly weathered, kaolinite, Fe and Al oxides Albic – light colored, elluvial, low reactivity Elluviation and Illuviation Elluviation (E horizon) Organic matter Clays A A E E Bh horizon Bt horizon Bh Bt Spodic horizon Argillic horizon 2 Soil Taxonomy Diagnostic Epipedons Diagnostic Subsurface horizons Moisture Regimes Temperature Regimes Age Texture Depth Soil Taxonomy Soil forming processes, presence or Order Absence of major diagnostic horizons 12 Similar genesis Suborder 63 Grasslands – thick, dark Great group 250 epipedons High %B.S. Sub group 1400 Family 8000 Series 19,000 Soil Orders Entisols Histosols Inceptisols Andisols Gelisols Alfisols Mollisols Ultisols Spodosols Aridisols Vertisols Oxisols 3 Soil Orders Entisol Ent- Recent Histosol Hist- Histic (organic) Inceptisol Incept- Inception Alfisol Alf- Nonsense Ultisol Ult- Ultimate Spodosol Spod- Spodos (wood ash) Mollisol Moll- Mollis (soft) Oxisol Ox- oxide Andisol And- Ando (black) Gelisol
    [Show full text]
  • Sustaining the Pedosphere: Establishing a Framework for Management, Utilzation and Restoration of Soils in Cultured Systems
    Sustaining the Pedosphere: Establishing A Framework for Management, Utilzation and Restoration of Soils in Cultured Systems Eugene F. Kelly Colorado State University Outline •Introduction - Its our Problems – Life in the Fastlane - Ecological Nexus of Food-Water-Energy - Defining the Pedosphere •Framework for Management, Utilization & Restoration - Pedology and Critical Zone Science - Pedology Research Establishing the Range & Variability in Soils - Models for assessing human dimensions in ecosystems •Studies of Regional Importance Systems Approach - System Models for Agricultural Research - Soil Water - The Master Variable - Water Quality, Soil Management and Conservation Strategies •Concluding Remarks and Questions Living in a Sustainable Age or Life in the Fast Lane What do we know ? • There are key drivers across the planet that are forcing us to think and live differently. • The drivers are influencing our supplies of food, energy and water. • Science has helped us identify these drivers and our challenge is to come up with solutions Change has been most rapid over the last 50 years ! • In last 50 years we doubled population • World economy saw 7x increase • Food consumption increased 3x • Water consumption increased 3x • Fuel utilization increased 4x • More change over this period then all human history combined – we are at the inflection point in human history. • Planetary scale resources going away What are the major changes that we might be able to adjust ? • Land Use Change - the world is smaller • Food footprint is larger (40% of land used for Agriculture) • Water Use – 70% for food • Running out of atmosphere – used as as disposal for fossil fuels and other contaminants The Perfect Storm Increased Demand 50% by 2030 Energy Climate Change Demand up Demand up 50% by 2030 30% by 2030 Food Water 2D View of Pedosphere Hierarchal scales involving soil solid-phase components that combine to form horizons, profiles, local and regional landscapes, and the global pedosphere.
    [Show full text]
  • Impact of Tillage on Physical Characteristics in a Mollisol of Northeast China
    Plant Soil Environ. Vol. 60, 2014, No. 7: 309–313 Impact of tillage on physical characteristics in a Mollisol of Northeast China X.W. Chen, A.Z. Liang, S.X. Jia, X.P. Zhang, S.C. Wei Key Laboratory of Mollisols Agroecology, Northeast Institute of Geography and Agroecology, Chinese Academy of Sciences, Changchun, P.R. China ABSTRACT Soil management is aimed at the maintenance of optimal soil physical quality for crop production. In order to ex- plore the effects of tillage practices on soil physical properties, a study was conducted to compare the effects of no tillage (NT), moldboard plow (MP) and ridge tillage (RT) on soil bulk density (BD), soil penetration resistance (SPR), soil water content (SWC), soil macroporosity (MAC) and soil air-filled porosity (AFP) in Northeast China. Results showed that both NT and RT led to significant BD increment than MP at 0–20 cm (P < 0.05). Compared with MP, NT and RT increased SPR at the depths of 2.5–17.5 cm (P < 0.05). SWC of 0–10 cm layer was significantly higher in NT and RT than MP soils (P < 0.05). NT showed a significantly lower MAC than MP and RT at 0–20 cm soil depths (P < 0.05). All AFP values were above the limit of 0.10 cm3/cm3 under all tillage treatments. RT im- proved the soil physical quality as evidenced by decreased BD and SPR, and increased SWC, MAC and AFP relative to NT. Keywords: soil bulk density; soil penetration resistance; soil water content; soil macroporosity; soil air-filled porosity Soil physical properties can influence the avail- factor is soil air-filled porosity (AFP), an important ability and uptake of water, oxygen and nutrients criterion for soil aeration which is commonly used for plant growth (Filho et al.
    [Show full text]
  • Geology As a Georegional Influence on Quercus Fagaceae Distribution
    GEOLOGY AS A GEOREGIONAL INFLUENCE ON Quercus FAGACEAE DISTRIBUTION IN DENTON AND COKE COUNTIES OF CENTRAL AND NORTH CENTRAL TEXAS AND CHOCTAW COUNTY OF SOUTHEASTERN OKLAHOMA, USING GIS AS AN ANALYTICAL TOOL George F. Maxey, B.S., M.S. Dissertation Prepared for the Degree of DOCTOR OF PHILOSOPHY UNIVERSITY OF NORTH TEXAS December 2007 APPROVED: C. Reid Ferring, Major Professor Miguel Avevedo, Committee Member Kenneth Dickson, Committee Member Donald Lyons, Committee Member Paul Hudak, Committee Member and Chair of the Department of Geography Sandra L. Terrell, Dean of the Robert B. Toulouse School of Graduate Studies Maxey, George F. Geology as a Georegional Influence on Quercus Fagaceae Distribution in Denton and Coke Counties of Central and North Central Texas and Choctaw County of Southeastern Oklahoma, Using GIS as an Analytical Tool. Doctor of Philosophy (Environmental Science), December 2007, 198 pp., 30 figures, 24 tables, references, 57 titles. This study elucidates the underlying relationships for the distribution of oak landcover on bedrock and soil orders in two counties in Texas and one in Oklahoma. ESRI’s ArcGis and ArcMap was used to create surface maps for Denton and Coke Counties, Texas and Choctaw County, Oklahoma. Attribute tables generated in GIS were exported into a spreadsheet software program and frequency tables were created for every formation and soil order in the tri-county research area. The results were both a visual and numeric distribution of oaks in the transition area between the eastern hardwood forests and the Great Plains. Oak distributions are changing on this transition area of the South Central Plains.
    [Show full text]
  • Perennial Grain Crop Roots and Nitrogen Management Shape Soil Food Webs T and Soil Carbon Dynamics ∗ Christine D
    Soil Biology and Biochemistry 137 (2019) 107573 Contents lists available at ScienceDirect Soil Biology and Biochemistry journal homepage: www.elsevier.com/locate/soilbio Perennial grain crop roots and nitrogen management shape soil food webs T and soil carbon dynamics ∗ Christine D. Sprungera, , Steven W. Culmana, Ariane L. Peraltab, S. Tianna DuPontc, Jay T. Lennond, Sieglinde S. Snappe a School of Environment and Natural Resources, The Ohio State University, Wooster, OH, 44691, USA b Department of Biology, East Carolina University, Greenville, NC, 27858, USA c Tree Fruit Research and Extension, Washington State University, Wenatchee, WA, 98801, USA d Department of Biology, Indiana University, Bloomington, IN, 47405, USA e Department of Plant, Soil, and Microbial Sciences, Michigan State University, East Lansing, MI, 48824, USA ARTICLE INFO ABSTRACT Keywords: Perennial grain crops may confer greater ecosystem services relative to annual row crop systems due to their Organic matter extensive roots systems and year-round ground cover. However, less is known about the extent to which per- Root biomass ennial grain crops affect food web dynamics and soil carbon (C) cycling over time. Furthermore, manyme- Nematodes chanistic questions remain regarding the influence of root quantity and quality on soil biological communities Bacteria and C cycling function. In this study, we quantified root biomass and quality, bacterial and nematode community Soil food webs structure, and labile soil C pools of perennial intermediate wheatgrass [Thinopyrum intermedium (Host) Buckworth and Dewey] and annual winter wheat (Triticum aes L.) across three nitrogen (N) management systems (Organic, Low inorganic N, High inorganic N). After 4 years, the perennial grain crop had significantly greater root quantity and permanganate oxidizable carbon (POXC) relative to annual wheat.
    [Show full text]
  • Genesis of Mollisols Under Douglas-Fir
    University of Montana ScholarWorks at University of Montana Graduate Student Theses, Dissertations, & Professional Papers Graduate School 1983 Genesis of Mollisols under Douglas-fir Mark E. Bakeman The University of Montana Follow this and additional works at: https://scholarworks.umt.edu/etd Let us know how access to this document benefits ou.y Recommended Citation Bakeman, Mark E., "Genesis of Mollisols under Douglas-fir" (1983). Graduate Student Theses, Dissertations, & Professional Papers. 2434. https://scholarworks.umt.edu/etd/2434 This Thesis is brought to you for free and open access by the Graduate School at ScholarWorks at University of Montana. It has been accepted for inclusion in Graduate Student Theses, Dissertations, & Professional Papers by an authorized administrator of ScholarWorks at University of Montana. For more information, please contact [email protected]. COPYRIGHT ACT OF 1976 THIS IS AN UNPUBLISHED MANUSCRIPT IN WHICH COPYRIGHT SUB­ SISTS, ANY FURTHER REPRINTING OF ITS CONTENTS MUST BE APPROVED BY THE AUTHOR, MANSFIELD LIBRARY UNIVERSITY OF MONTANA DATE : 19 83 THE GENESIS OF MOLLISOLS UNDER DOUGLAS-FIR by MARK E. BAKEMAN B.S., S.U.N.Y. College of Environmental Science and Forestry, Syracuse, 1978 Presented in partial fulfillment of the requirements for the degree of Master of Science UNIVERSITY OF MONTANA 1983 Approved by: Chairman, B6ard of Examiners rh, Graduate Schoor Date UMI Number: EP34103 All rights reserved INFORMATION TO ALL USERS The quality of this reproduction is dependent on the quality of the copy submitted. In the unlikely event that the author did not send a complete manuscript and there are missing pages, these will be noted.
    [Show full text]