Soil CLASSIFICATION a Global Desk Reference
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General Characteristics of Soil| Sample Answer
General Characteristics of Soil| sample answer Q: ‘Examine the general composition and characteristics of any one soil type that you have studied’ (2007 Q17) Latosol- A tropical zonal soil. 3 aspects will be discussed. 1. Composition: Soil is composed of a number of ingredients/components. These components can vary in portion. All soils form as result of the action of several factors. THese factors combine to influence the many processes at work in soil formation eg. Leaching and weathering. These give soil its own characteristics. Soil is composed of number of ingredients and constituents. The components of soil are mixed in different quantities to create different soil types. They are made up of mineral matter, air, water, humus, living organisms. However, climate is the single most important factor in determining what a soil will be like as climate influences vegetation, the rate of weathering and soil, forming processing in an area. The majority of soil is composed of mineral matter. Mineral matter are rock particles from the bedrock and weathered rock. The soil type varies depending on mineral matter. Unconsolidated material eg boulder clay will help form soil more rapidly than solid bedrock as it is partly weathered. Soil is also composed of organic matter. Organic matter includes decaying plants and animals which bacteria and fungi breakdown. Humus is a dark brown jelly-like substance formed from organic matter. Living organisms are also included in ‘organic matter’, earthworms, beetles, fungi, bacteria; they digest organic matter to humus and also mix and create soil. Water is another important component of soil. -
Puerto Rico Oxisols-Highly Weathered,Red Soils of the Tropics
AGENCY FOR INTERNATIONAL DEVELOPML;4 FOR AID USE ONLY WASHINGTON. 0. C. 20523 BiBL;OGRAPHIC INPUT SHEET 16IIA.-C~ i A. PRIMARY l.SUBJECT Agriculture AF22-0000-G339 CLASSI- FCASI- SECONDARY FICATON IS. Soil chemistry and physics--Puerto Rico 2. TITLE AND SUBTITLE Oxisols-highly weathered,red soils of the tropics 3. AUTHOR(S) Beinroth,F.H. 4. DOCUMENT DATE S.NUMBER OF PAGES 8. ARC NUMBER 1973I 5p. ARC 7. REFERENCE ORGANIZATION NAME AND ADDRESS Puerto Rico 8. SUPPLEMENTARY NOTES (Sponcoring Organization, Publiahers, Availability) (InSoils of the southern States and Puerto Rico,ed.by S.W.Buol,p.87-91) 9. ABSTRACT 10. CONTROL NUMBER 11. PRICE OF DOCUMENT PN-RAB-104 12. DESCRIPTORS 13. PROJECT NUMBER Puerto Rico 14. CONTRACT NUMBER CSD-2857 211(d) 15. TYPE OF DOCUMENT AID 590.1 (4-74) Chapter 12 OXISOLS-IIGIILY WEATIIERED, RED SOILS OF TIlE TROPICS F. H. Beinroth Introduction and General Setting of a western spur of the Cordillera Central, there Although the term "laterite" readily springs to ranging in altitude from 200 to 500 m. (600 to mind when the tipic of red tropical soils is raised, 1,500 feet), and consisting of ultrabasic plutonic it is but one of many names that have been pro- rocks (serpentinite) of Early Cretaceous age. For posed to characterize these soils. Latosols, Ferra- the most part this area is strongly dissected and lities, and Terra Roxa are some other of these only in a few places have older erosion surfaces vaguely defined and often synonymously used been preserved. As it is on those remnants where terms. -
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. -
The Fractal Mind of Pedologists (Soil Taxonomists and Soil Surveyors)
Ecological Complexity 6 (2009) 286–293 Contents lists available at ScienceDirect Ecological Complexity journal homepage: www.elsevier.com/locate/ecocom The fractal mind of pedologists (soil taxonomists and soil surveyors) J.J. Iba´n˜ez a,d,*, R.W. Arnold b,1,2, R.J. Ahrens c a Centro de Investigaciones Sobre Desertificacio´n, CIDE (CSIC-UV, Valencia, Spain b USDA, Natural Resources Conservation Service, Washington, DC, USA c National Soil Survey Center, USDA-NRCS, Lincoln, NE, USA d E.P.S. A´rea de Edafologı´ayQuı´mica Agrı´cola, Universidad de Burgos, Spain ARTICLE INFO ABSTRACT Article history: There has been little work in science dealing with the organizational, political and scientific layering of Available online 24 June 2009 database structures as well as classifications and surveys of natural resources. There is disagreement among scientists whether taxonomies are invented (human-made constructs) or are discovered Keywords: (‘‘natural’’ structures) independent of the discipline involved. We believe it would be helpful to study the Soil survey practices nature of taxonomies from different points of view in order to examine questions such as; are there Soil taxonomies common features in all taxonomic systems?, are the systems neutral?, and how are classifications and Power laws data collection (surveys) linked? It is generally accepted that much institutional work on soil Fractals classification systems was nationally biased, especially in terms of practical land management. Mental constructs Information processing Recent studies show that the USDA soil taxonomy has the same mathematical structure as some biological ones that conform to physical laws that dictate and optimize information flow in user friendly retrieval systems. -
Effects of Afforestation on Soil Structure Formation in Two Climatic Regions Of
JOURNAL OF FOREST SCIENCE, 61, 2015 (5): 225–234 doi: 10.17221/6/2015-JFS Eff ects of aff orestation on soil structure formation in two climatic regions of the Czech Republic V. Podrázský1, O. Holubík2, J. Vopravil2, T. Khel2, W.K. Moser3, H. Prknová1 1Faculty of Forestry and Wood Sciences, Czech University of Life Sciences Prague, Prague, Czech Republic 2Research Institute for Soil and Water Conservation, Department of Soil Science and Soil Conservation, Prague-Zbraslav, Czech Republic 3U.S. Department of Agriculture, Forest Service, Rocky Mountain Research Station, Flagstaff, Arizona, USA ABSTRACT: The aim of this study was to determine the effect of agricultural land afforestation on soil characteristics. Two sites in two regions of the Czech Republic were evaluated, at lower as well as higher submountain elevations: in the regions of the Orlické hory Mts. and Kostelec nad Černými lesy, afforested, arable and pasture lands were com- pared for basic chemical and physical characteristics. It was determined: pH, CEC, exchangeable nutrients, SOC, bulk density, volume density, porosity (differentiated by pore size), water conductivity and soil aggregate stability. This study demonstrated the important influence of previous land use upon soil characteristics. The characteristics of the arable horizon can persist for many years; in forests, the mineral horizons (15–30 cm) can persist within 15–30 years after afforestation. Afforestation, which caused an increase in soil porosity by decreasing reduced bulk density and increasing capillary and gravitational pores (increasing the water-holding capacity and soil air capacity), is important for maintaining the soil stability. The positive effect on infiltration and retention capacity resulted not only from the presence of a forest overstorey, but also from the presence of permanent grass cover of pasture land. -
Conversations in Soil Taxonomy (Original Tr,.&Nscr|F't~Ons of Taped Conversations)
CONVERSATIONS IN SOIL TAXONOMY (ORIGINAL TR,.&NSCR|F'T~ONS OF TAPED CONVERSATIONS) by Guy D Smith Compiled by an editorial committee a, 'I~,e Agronomy Departmen: of Cornell University for the So~i Management Support St.:vice USD/ - Sf~ Ithaca, New York .~996 7 ¸ ~" "-2 2. z- . = .C .%- Addendum to: THE GUY SM|TH INTERVIEWS: RATIONALE FOR CONCEPTS tr~ SOIL TAXONOMY by Guy O. Smith Edited by T.P,~. Forbes Reviewed by N. Ahmad J. Comerma H. Eswaran K. Flach T.R. Forbes B. Hajek W. Johnson J. McClelland F.T. MiJqer J. Nichols J. Rourl,:e R. Rust A. Van Wambeke J. W~y S'~d Management Support Services Soil Conservation Service LL $. Dep~,rtment of Agriculture New York State Co!le,ge of Agriculture and Life Sciences Corneil University Department of Agronomy 1986 SM:~S Technical Monograph No. i I .1 o - "f Ib!e of Contents Preface ii Interview by Mike L. Leanly 1 Interview by J. Witty & R. Guthrie 37 Interview at the Agronomy Department at Corneil University 48 Interview at the Agronomy bepartn'e.'.zt at University of Minneso,m 149 Interview by H. E.qwaran 312 Lecture Given at the University of the West Indies 322 Interview at the Agronomy Department at Texas A & M University 328 Interviews b3: Coplar~ar staff & J. Comerma, Venezuela 441 #rrr Preface Many papers have been published explaining the rationale for properties and class limits used in Soil T<:txonomy, a system of .soil classificalion for making and interpreting soil surveys (U.S. Department of Agrical~.ure, 1975) before and since its publication. -
National Cooperative Soil Survey Newsletter
ational February 2013 ooperative Issue 62 N oil C urvey SS Newsletter In This Issue— 2013 National Cooperative Soil Survey Conference 2013 National Cooperative Soil Survey Conference ....................................................1 he biennial National Cooperative Soil and Site Suitability for Viticulture in the TSoil Survey (NCSS) Conference United States .................................................2 will be held June 16 to 21, 2013, at New Edition of Field Book ....................................6 Annapolis, Maryland. The conference Pedoderm and Pattern Class Workshops at will be hosted by the University of the Jornada ....................................................7 Maryland at College Park and supported Korean Soil Scientists Visit the National Soil by the Natural Resources Conservation Survey Center ................................................7 Service, the U.S. Forest Service, the Haiti Pilot Soil Survey Capacity Building Mid-Atlantic Association of Professional Initiative ..........................................................8 Soil Scientists, the Soil Science Society Map Unit Descriptions Available in Spanish of America, and the National Association on Web Soil Survey .....................................12 of Consulting Soil Scientists. NRCS Where the Sun Always Shines: Mojave personnel supporting the conference National Preserve ........................................13 include soil survey staff from Raleigh, Global Soil Week .................................................15 North Carolina; Morgantown, -
Ph, SOIL ACIDITY, and PLANT GROWTH 67 Numbers, the Danish Biochemist S
pH, SOIL ACIDITY, AND PLANT GROWTH 67 numbers, the Danish biochemist S. P. L. Sorenson devised a system called pH for expressing the acidity or alka- pH, Soil Acidity, linity of solutions. The pH scale goes from o to 14. At pH 7, the midpoint of the scale, there and Plant Growth are equal numbers of hydrogen and hydroxyl ions, and the solution is neu- W. H. Allaway tral. pH values below 7 indicate an acid solution, where there are more hydro- When crop plants do not grow gen ions than hydroxyl ions, with the well, one of the first questions acidity (or hydrogen ion concentra- tion) increasing as the pH values get the soil scientist usually asks smaller. is, ''What is the pH of the soil?'' pH values above 7 denote alkaline solutions, with the concentration of or, 'Is the soil acid, neutral, hydroxyl ions increasing as the pH or alkaline?'' values get larger. The pH scale is based on logarithms The reason for these questions lies in of the concentration of the hydrogen the fact that the pH, or degree of and hydroxyl ions. This means that a acidity of the soil, often is a symptom solution of pH 5 has 10 times the hy- of some disorder in the chemical con- drogen ion concentration of a solution dition of the soil as it relates to plant of pH 6. A solution of pH 4 has 10 nutrition. times more hydrogen ions than one of A measurement of soil acidity or pH 5 and 10 times 10, or 100 times, alkalinity is like a doctor's measure- the hydrogen ion concentration of a ment of a patient's temperature. -
Redalyc.STRUCTURAL QUALITY of POLYACRYLAMIDE-TREATED
Revista Brasileira de Ciência do Solo ISSN: 0100-0683 [email protected] Sociedade Brasileira de Ciência do Solo Brasil Vandeval Maranhão de Melo, Diego; Gomes de Almeida, Brivaldo; Rodrigues de Souza, Edivan; Santos Silva, Laércio; Jacomine, Paulo Klinger Tito STRUCTURAL QUALITY OF POLYACRYLAMIDE-TREATED COHESIVE SOILS IN THE COASTAL TABLELANDS OF PERNAMBUCO Revista Brasileira de Ciência do Solo, vol. 38, núm. 2, 2014, pp. 476-485 Sociedade Brasileira de Ciência do Solo Viçosa, Brasil Available in: http://www.redalyc.org/articulo.oa?id=180231134011 How to cite Complete issue Scientific Information System More information about this article Network of Scientific Journals from Latin America, the Caribbean, Spain and Portugal Journal's homepage in redalyc.org Non-profit academic project, developed under the open access initiative 476 Diego Vandeval Maranhão de Melo et al. STRUCTURAL QUALITY OF POLYACRYLAMIDE-TREATED COHESIVE SOILS IN THE COASTAL TABLELANDS OF PERNAMBUCO(1) Diego Vandeval Maranhão de Melo(2), Brivaldo Gomes de Almeida(3), Edivan Rodrigues de Souza(3), Laércio Santos Silva(4) & Paulo Klinger Tito Jacomine(5) SUMMARY Water-soluble polymers are characterized as effective flocculating agents due to their molecular features. Their application to soils with horizons with structural problems, e.g, a cohesive character, contributes to improvements in the physical quality and thus to the agricultural suitability of such soils. The purpose of this study was to evaluate the structural quality of soils with cohesive horizons of coastal tablelands in the State of Pernambuco treated with polyacrylamide (PAM) as chemical soil conditioner. To this end, three horizons (one cohesive and two non- cohesive) of a Yellow Argisol (Ultisol) were evaluated and to compare cohesive horizons, the horizon of a Yellow Latosol (Oxisol) was selected. -
The Comparative Effects of Calcium Carbonate and of Calcium Silicate on the Yield of Sudan Grass Grown in a Ferruginous Latosol and a Hydrol Humic Latosol
TECHNICAL BULLETIN No. 53 JUNE 1963 The Comparative Effects of Calcium Carbonate and of Calcium Silicate on the Yield of Sudan Grass Grown in a Ferruginous Latosol and a Hydrol Humic Latosol N. H. MONTEITH and G. DONALD SHERMAN HAWAII AGRICULTURAL EXPERIMENT STATION, UNIVERSITY OF HAWAII The Comparative Effects of Calcium Carbonate and of Calcium Silicate on the Yield of Sudan Grass Grown in a Ferruginous Latosol and a Hydrol Humic Latosol N. H. MONTEITH and G. DONALD SHERMAN UNIVERSITY OF HAWAII COLLEGE OF TROPICAL AGRICULTURE HAWAII AGRICULTURAL EXPERIMENT STATION HONOLULU, H AWAII J UNE 1963 T ECIINICAL B ULLETIN No. 53 ACKNOWLEDGMENT The authors gra tcfully acknow ledge the assistance of the staff of th e Experiment Station of the H awaii an Sugar Planters' Association in pro viding greenhouse, photographic, and laboratory facilities, and for advice on sta tistical and analytical methods. Research funds on this proj ect were pro vid ed by the Hawaiian Sugar Planters' Association Experiment Station under a coope rative research agreemcnt with the Department of Agronomy and Soil Science. Funds and materials we re also provided by the Tenn essee Valley Authority, Contract No. TV21132A. THE AUTHORS N. H. MONTEITH was In structor in Agricultur e, University of Hawaii, 1961-1962. DR. G. DONALD SHERMAN, Associate Director of the Hawaii Agricultural Experiment Station, is Senior Soil Scientist at the Hawaii Agricultural Ex periment Station and Senior Professor of Soil Science, University of Hawaii. CONTENTS PAGE INTRODUcrION 5 LITERAT UHE REVIEW 5 Effect of Calcium Carbonate on Phosphorus Availability 5 Effect of Calcium Carbonate on Other Factors 7 Effect of Calcium Silicate on Phosphorus Availability 8 Effect of Calcium Silicate on Other Factors 8 EXPEmMENTAL PROCEDUHES 9 Soils . -
Standardised Soil Profile Data to Support Global Mapping
Earth Syst. Sci. Data, 12, 299–320, 2020 https://doi.org/10.5194/essd-12-299-2020 © Author(s) 2020. This work is distributed under the Creative Commons Attribution 4.0 License. Standardised soil profile data to support global mapping and modelling (WoSIS snapshot 2019) Niels H. Batjes, Eloi Ribeiro, and Ad van Oostrum ISRIC – World Soil Information, Wageningen, 6708 PB, the Netherlands Correspondence: Niels H. Batjes ([email protected]) Received: 6 September 2019 – Discussion started: 16 September 2019 Revised: 17 December 2019 – Accepted: 9 January 2020 – Published: 10 February 2020 Abstract. The World Soil Information Service (WoSIS) provides quality-assessed and standardised soil profile data to support digital soil mapping and environmental applications at broadscale levels. Since the release of the first “WoSIS snapshot”, in July 2016, many new soil data were shared with us, registered in the ISRIC data repos- itory and subsequently standardised in accordance with the licences specified by the data providers. Soil profile data managed in WoSIS were contributed by a wide range of data providers; therefore, special attention was paid to measures for soil data quality and the standardisation of soil property definitions, soil property values (and units of measurement) and soil analytical method descriptions. We presently consider the following soil chemi- cal properties: organic carbon, total carbon, total carbonate equivalent, total nitrogen, phosphorus (extractable P, total P and P retention), soil pH, cation exchange capacity and electrical conductivity. We also consider the fol- lowing physical properties: soil texture (sand, silt, and clay), bulk density, coarse fragments and water retention. Both of these sets of properties are grouped according to analytical procedures that are operationally comparable. -
19Th World Congress of Soil Science Working Group 1.1 the WRB
19th World Congress of Soil Science Working Group 1.1 The WRB evolution Soil Solutions for a Changing World, Brisbane, Australia 1 – 6 August 2010 Table of Contents Page Table of Contents ii 1 Diversity and classification problems of sandy soils in subboreal 1 zone (Central Europe, Poland) 2 Finding a way through the maze – WRB classification with 5 descriptive soil data 3 Guidelines for constructing small-scale map legends using the 9 World Reference Base for Soil Resources 4 On the origin of Planosols – the process of ferrolysis revisited 13 5 Orphans in soil classification: Musing on Palaeosols in the 17 World Reference Base system 6 Pedometrics application for correlation of Hungarian soil types 21 with WRB 7 The classification of Leptosols in the World Reference Base for 25 Soil Resources 8 The World Reference Base for Soils (WRB) and Soil 28 Taxonomy: an initial appraisal of their application to the soils of the Northern Rivers of New South Wales 9 A short guide to the soils of South Africa, their distribution and 32 correlation with World Reference Base soil groups ii Diversity and classification problems of sandy soils in subboreal zone (Central Europe, Poland) Michał Jankowski Faculty of Biology and Earth Sciences, Nicolaus Copernicus University, Toruń, Poland, Email [email protected] Abstract The aim of this study was to present some examples of sandy soils and to discuss their position in soil systematics. 8 profiles represent: 4 soils widely distributed in postglacial landscapes of Poland (Central Europe), typical for different geomorphological conditions and vegetation habitats (according to regional soil classification: Arenosol, Podzolic soil, Rusty soil and Mucky soil) and 4 soils having unusual features (Gleyic Podzol and Rusty soil developed in a CaCO 3-rich substratum and two profiles of red-colored Ochre soils).