Chapter 3 Chapter 3 Learning Objectives

Total Page:16

File Type:pdf, Size:1020Kb

Chapter 3 Chapter 3 Learning Objectives Chapter 3 Learning Objectives Chapter 3 • Describe the current USDA soil classification system • List the six categories of classification in Soil Soil Taxonomy Taxonomy • Describe the major characteristics, the general degree of weathering and soil development, and the worldwide distribution and uses of the 12 soil orders • List key features of a particular soil and its environment given the soil name (e.g., Hapludalf) Diagnostic Subsurface Horizons Diagnostic Subsurface Horizons • 18 of them – Albic: light-colored elluvial horizon (leached) – Cambic: weakly developed horizon, some color • Six we will focus on (and the assoc. genetic change label): – Spodic: illuvial horizon with accumulations of O.M. – Argillic: subsurface accumulations of silicate clays – Albic (E) -Argg(illic (Bt) – CliCalcic: accumu ltilation o f car bona tes, o ften as – Cambic (Bw) - Fragic (Bx) white, chalk-like nodules – Spodic (Bhs) - Calcic (Bk) – Fragipan: cemented, dense, brittle pan Light colored horizon Albic Argillic Weakly developed horizon Cambic No significant accumulation silicate clays Unweathered Accumulation of Acid weathering, material organic matter Fe, Al oxides Spodic Calcic Fragipan Modified from full version of Figure 3.3 in textbook (page 62). 1 Levels of Description Levels of Description • Order Most general • Order – One name, all end in “-sol” There are 12. Differentiated by presence or absence of • Suborder diagnostic horizons or features that reflect • Great group soil-forming processes. EXAMPLE: ENTISOL • Subgroup • Suborder • Family • Great group • Subgroup •Series •Family Most specific •Series Levels of Description Levels of Description • Order – One name, all end in “-sol” There are 12 . • Order – One name, all end in “-sol” There are 12 . • Suborder – One name, last 2-3 letters • Suborder –properties (e.g., climate info) AND order indicates the soil order. Tells something • Great group – 3 pieces of info. Last 2-3 letters about properties important to genesis and tell the order, includes suborder info, and plant growth (e.g., climate info) Example: adds info about the horizons (e.g., sandy, Aquent clay ey, hard… ) EampleExample: Psammaquent • Great group • Subgroup • Subgroup •Family •Family •Series •Series Levels of Description Levels of Description • Order – One name, all end in “-sol” There are 12 . • Order – One name, all end in “-sol” There are 12 . • Suborder –properties (e.g., climate info) AND which • Suborder – Tells something about properties (e.g., Order climate) • Great group – 3 parts, adds info about the horizons • Great group – 3 parts, adds info about the horizons • Subgroup – TWO words. All info from above plus whether it is “typical” or shares • Subgroup – TWO words. properties with another soil type. Example: • Family – name includes about 5-6 words! Mollic Psammaquent Adds physical and chemical properties that •Family affect growth of plants •Series •Series 2 Soil Taxonomy Levels of Description • Order – One name, all end in “-sol” There are 12 . Order • Suborder – Tells something about properties (e.g., climate) • Great group – 3 parts, adds info about the horizons • Subgroup – TWO words. •Family – name includes about 5-6 words! • Series – Often referred to by a single name that doesn’t tell you anything unless you already know it well. 12 Soil Orders Fig 3.5 3 Soil Orders Soil Order “Formative Characteristics, Entisols element” location, etc. Entisol -ent Absence of distinct pedogenic horizons; climate & PM key Inceptisol -ept Gelisol -el Histosol -ist Andisol -and Aridisol -id Entisols Soil Orders • Sandy, young soils Soil “Formativ Characteristics, location, etc. Order e • Plainfield loamy sand: element” Typic Udipsamment Entisol -ent Absence of distinct pedogenic horizons; climate & PM key Inceptisol -ept Weak development, nothing exciting. There is a “B” horizon Gelisol -el Histosol -ist Andisol -and Aridisol -id Inceptisol: few horizons, inception Soil Orders of B (Bw) Soil “Form. el” Characteristics, location, etc. Order Entisol -ent Absence of pedogenic horizons Inceptisol -ept Weak development Gelisol -el Permafrost, freeze-thaw fea tures (13% o f so ils worldwide!) Lithic Eutrudept - northern Histosol -ist Michigan Andisol -and Aridisol -id 4 Gelisols: permafrost Gelisols • cryoturbation Soil Orders Gelisols Soil “Form el” Characteristics, location, etc. Order Entisol -ent Absence of distinct pedogenic horizons Inceptisol -ept Weak development GlilGelisol -el PftfPermafrost, freeze-thaw Histosol -ist Very high OM in upper 80 cm (peats), wet Andisol -and Aridisol -id Histosols: organic soils Histosols • Wetland delineation 5 Soil Orders Andisols Soil “Form el” Characteristics, location, etc. Order Entisol -ent Absence of horizons Inceptisol -ept Weak development Gelisol -el Permafrost, freeze-thaw Histosol -ist Very high OM, wet Andisol -and Volcanic soils, Al-humus complexes, mild temp, fairly moist Aridisol -id Soil Orders Andisols Soil Ending Characteristics, etc. Order Entisol -ent Absence of distinct pedogenic horizons Inceptisol -ept Weak development Gelisol -el Permafrost, freeze-thaw Histosol -ist Very high OM, wet Andisol -and Volcanic soils Aridisol -id No avail. H2O when plants growing – the largest group of soils on Earth! Aridisols: dry soils Aridisols • 12% globally •9% US 6 Soil Orders Vertisol: swelling and cracking Soil Order “Formative Characteristics, clays element” location, etc. Vertisol -ert Swelling clays, high BS, dry-wet Mollisol -oll Ultisol -ult Alfisol -alf Spodosol -od Oxisol -ox Vertisols Soil Orders Vertisols Soil Ending Characteristics, location, etc. Order Vertisol -ert Swelling clays, high BS Mollisol -oll Dark, thick epipedon, grasslands, some dry period, high BS Ultisol -ult Alfisol -alf Spodosol -od Oxisol -ox 7 Mollisol: dark, grassland, high base sat. • Loess: silt Mollisols • 22% of US • Very productive Plate 8 Mollisols -- a Typic Hapludoll from central Iowa. Mollic epipedon to 1.8 ft. Scale in feet. Soil Orders Ultisols Soil Ending Characteristics, etc. Order Vertisol -ert Swelling clays, high BS Mollisol -oll Dark, thick, grasslands Ultisol -ult Wet subtroppp,gyical or tropical, highly acidic, high in clay, Fe and Al oxides, productive if add fertilizers Alfisol -alf Spodosol -od Oxisol -ox Soil Orders Ultisols: Bt w/ low bases Soil Ending Characteristics, etc. Order • More Vertisol -ert Swelling clays, high BS leached than Mollisol -oll Dark, thick, grasslands Alfisols Ultisol -ult subtropp,ical, acidic, ,g high in clay, y,, Fe, Al • Less fertile Alfisol -alf Moist, forested, mildly acidic, translocation of clays, moderate-high BS Spodosol -od Oxisol -ox 8 Alifsols Alfisols: Bt, ochric epipedon Soil Orders Soil Endin Characteristics, etc. Spodosols Order g Vertisol -ert Swelling clays, high BS Mollisol -oll Dark, thick, grasslands Ultisol -ult Moist & warm, acidic, high in clay, oxides Alfisol -alf Moist, forested, clays Spodosol -od Translocation of humus and Al, Fe, cool, wet, sandy, coniferous forest Oxisol -ox Spodosol: Bs, Bh or Bhs, albic Spodosols horizon • Northern Wis – Orthods: typical of central concept of Spodosols 9 Soil Orders Soil Ending Characteristics, etc. Oxisols Order Vertisol -ert Swelling clays, high BS Mollisol -oll Dark, thick, grasslands Ultisol -ult Moist & warm, acidic . Alfisol -alf Moist, forested, clays Spodosol -od cool, wet, sandy, acidic . Oxisol -ox Extreme weathering, tropical forest, Fe, Al oxides, old, stable PM Oxisols • Tropical • Highly weathered Development and soil orders Development of the soil orders Bk ice Bo 10 The SUPER SIMPLIFIED guide to soil orders The SUPER SIMPLIFIED guide (cont.) 1. If no subsurface horizons Æ Entisol 6. If on volcanic material Æ Andisol 2. If aridic moisture regime and NOT and 7. If TONS of clay, with shrink-swell features Entisol Æ Aridisol (“slickensides,” large cracks when dry) Æ 3. If mollic epipedon Æ Mollisol Vertisols 4. If histic epppipedon Æ Histosol 8. If spodic horizon (Bh, Bs) Æ Spodosols 5. If permafrost Æ Gelisol 9. If oxic horizon (Bo) Æ Oxisols The SUPER SIMPLIFIED guide (cont.) 10.If umbric epipedon (low BS), argillic horizon, subtropical location Æ Ultisol 11.If ochric epipedon (sometimes umbric), argillic horizon, often an albic horizon, and a cool, moist climate Æ Alfisol 12.If oc hr ic ep ipe don an d NOT an En tiso l or Aridisol, often a cambic horizon Æ Inceptisol Soil Taxonomy Suborder 11 Suborders • Often described based on climatic information • Name of the suborder tells what order the soil belongs to PLUS one other feature of the soil (usually climate, except for Aridisols…) Soil Moisture Regimes Soil Temperature Regimes o COLD • Aquic – saturated for extended periods WET • Pergelic - < 0 C • Udic – not dry for more than 90 days • Cryic – 0-8, cold summer • Frigid – 0-8, warm summer • Ustic – dry 90-180 days •Mesic –8-15 • Xeric – dry summer, moist winter • Thermic – 15-22 • Hyperthermic - >22 • Aridic – moist <90 days HOT • Torric (not a real moisture regime but used in • Iso-(frigid, mesic, thermic, hyperthermic): small difference between summer and winter names like one. dry + hot ) DRY Suborders Suborders (cont.) • Often described based on climatic information Also differentiated based on key features – Aqu - wet •Fluv: fluvial, from a river – Ud - moist –Ust -dry • Psamm: sandy – Xer – moist winter, dry summer • Alb: albic horizon (()E) – leached – Torr – hot and dry • Arg: argillic horizon (Bt) – clayey –Cry –very cold – Hist – histic epipedon • Orth: “other” or “true to the definition” • Example: Aqualf (note capitalization) 12 Examples
Recommended publications
  • Engineering Behavior and Classification of Lateritic Soils in Relation to Soil Genesis Erdil Riza Tuncer Iowa State University
    Iowa State University Capstones, Theses and Retrospective Theses and Dissertations Dissertations 1976 Engineering behavior and classification of lateritic soils in relation to soil genesis Erdil Riza Tuncer Iowa State University Follow this and additional works at: https://lib.dr.iastate.edu/rtd Part of the Civil Engineering Commons Recommended Citation Tuncer, Erdil Riza, "Engineering behavior and classification of lateritic soils in relation to soil genesis " (1976). Retrospective Theses and Dissertations. 5712. https://lib.dr.iastate.edu/rtd/5712 This Dissertation is brought to you for free and open access by the Iowa State University Capstones, Theses and Dissertations at Iowa State University Digital Repository. It has been accepted for inclusion in Retrospective Theses and Dissertations by an authorized administrator of Iowa State University Digital Repository. For more information, please contact [email protected]. INFORMATION TO USERS This material was produced from a microfilm copy of the original document. While the most advanced technological means to photograph and reproduce this document have been used, the quality is heavily dependent upon the quality of the original submitted. The following explanation of techniques is provided to help you understand markings or patterns which may appear on this reproduction. 1. The sign or "target" for pages apparently lacking from the document photographed is "Missing Page(s)". If it was possible to obtain the missing page(s) or section, they are spliced into the film along with adjacent pages. This may have necessitated cutting thru an image and duplicating adjacent pages to insure you complete continuity. 2. When an image on the film is obliterated with a large round black mark, it is an indication that the photographer suspected that the copy may have moved during exposure and thus cause a blurred image.
    [Show full text]
  • 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]
  • Stabilization and Destabilization of Soil Organic Matter: Mechanisms and Controls
    13F7H GEODERLIA ELSEVIER Geoderma 74 (1996) 65-105 • Stabilization and destabilization of soil organic matter: mechanisms and controls Phillip Sollins, Peter Homann, Bruce A. Caldwell Department of Forest Science Oregon State University Corvallis, OR 97331, USA Receed 1 December 1993; revised 26 July 1995; accepted 3 April 1996 Abstract We present a conceptual model of the processes by which plant leaf and root litter is transformed to soil organic C and CO 2. Stabilization of a portion of the litter C yields material that resists further transformation; destabilization yields material that is more susceptible to microbial respiration. Stability of the organic C is viewed as resulting from three general sets of characteristics. Recalcitrance comprises, molecular-level characteristics of organic substances, including elemental composition, presence of functional groups, and molecular conformation, that influence their degradation by microbes and enzymes. Interactions refers to the inter-molecular interactions between organics and either inorganic substances or other organic substances that alter the rate of degradation of those organics or synthesis of new organics. Accessibility refers to the location of organic substances with respect to microbes and enzymes. Mechanisms by which these three characteristics change through time are reviewed along with controls on those mechanisms. This review suggests that the following changes in the study of soil organic matter dynamics would speed progress: (1) increased effort to incorporate results
    [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]
  • Subsurface Stratigraphy and Genesis of Pre-Wisconsin Paleosols in Whitebreast Creek Watershed, South-Central Iowa
    Iowa State University Capstones, Theses and Retrospective Theses and Dissertations Dissertations 1995 Subsurface stratigraphy and genesis of pre- Wisconsin paleosols in Whitebreast Creek Watershed, south-central Iowa Amir Hossein Charkhabi Iowa State University Follow this and additional works at: https://lib.dr.iastate.edu/rtd Part of the Agricultural Science Commons, Agriculture Commons, Agronomy and Crop Sciences Commons, Geology Commons, and the Mineral Physics Commons Recommended Citation Charkhabi, Amir Hossein, "Subsurface stratigraphy and genesis of pre-Wisconsin paleosols in Whitebreast Creek Watershed, south- central Iowa " (1995). Retrospective Theses and Dissertations. 10887. https://lib.dr.iastate.edu/rtd/10887 This Dissertation is brought to you for free and open access by the Iowa State University Capstones, Theses and Dissertations at Iowa State University Digital Repository. It has been accepted for inclusion in Retrospective Theses and Dissertations by an authorized administrator of Iowa State University Digital Repository. For more information, please contact [email protected]. INFORMATION TO USERS This manuscript has been reproduced from the microfihn master. UMI filmc the text directly from the original or copy submitted. Thus, some thesis and dissertation copies are in ^pewriter face, while others may be from any type of computer printer. The qnalify of this reprodnction is dependent upon the quality of the copy submitted. Broken or indistinct print, colored or poor quality illustrations and photographs, print bleedthrough, substandard margins, and inqjroper aligmnent can adversefy affect reproduction. In the unlikely event that the author did not send UMI a complete manuscript and there are missing pages, these will be noted. Also, if unauthorized copyright material had to be removed, a note will indicate the deletion.
    [Show full text]
  • The Hidden Ecological Resource of Andic Soils in Mountain Ecosystems: Evidence from Italy
    Solid Earth, 9, 63–74, 2018 https://doi.org/10.5194/se-9-63-2018 © Author(s) 2018. This work is distributed under the Creative Commons Attribution 4.0 License. The hidden ecological resource of andic soils in mountain ecosystems: evidence from Italy Fabio Terribile1,2, Michela Iamarino1, Giuliano Langella1, Piero Manna2,3, Florindo Antonio Mileti1, Simona Vingiani1,2, and Angelo Basile2,3 1Department of Agricultural Sciences, University of Naples Federico II, Via Università 100, 80055 Portici (Naples), Italy 2CRISP, Interdepartmental Research Centre on the Earth Critical Zone, University of Naples Federico II, Via Università 100, 80055 Portici (Naples), Italy 3Institute for Mediterranean Agricultural and Forestry Systems, National Research Council of Italy, Via Patacca 85, 80056 Ercolano (Naples), Italy Correspondence: Fabio Terribile ([email protected]) Received: 9 June 2017 – Discussion started: 9 August 2017 Revised: 1 November 2017 – Accepted: 20 November 2017 – Published: 31 January 2018 Abstract. Andic soils have unique morphological, physical, 1 Introduction and chemical properties that induce both considerable soil fertility and great vulnerability to land degradation. More- Andic soils (i.e. soils with evident andosolization process) over, they are the most striking mineral soils in terms of are known to have a unique set of morphological, physi- large organic C storage and long C residence time. This is cal, and chemical soil properties. Andosolization (Ugolini especially related to the presence of poorly crystalline clay et al., 1988; Shoji et al., 1993) is a major soil-forming pro- minerals and metal–humus complexes. Recognition of andic cess regardless of whether these soils meet or do not meet soils is then very important.
    [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]
  • 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.
    [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]