Guidelines for Soil Description
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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. -
Changes in Soil Properties in a Fluvisol (Calcaric) Amended with Coal Fly Ash A
Changes in soil properties in a fluvisol (calcaric) amended with coal fly ash A. Riehl, F. Elsass, J. Duplay, F. Huber, M. Trautmann To cite this version: A. Riehl, F. Elsass, J. Duplay, F. Huber, M. Trautmann. Changes in soil properties in a fluvisol (calcaric) amended with coal fly ash. Geoderma, Elsevier, 2010, 155 (1-2), pp.67-74. 10.1016/j.geoderma.2009.11.025. halsde-00546980 HAL Id: halsde-00546980 https://hal.archives-ouvertes.fr/halsde-00546980 Submitted on 30 May 2020 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Geoderma 155 (2010) 67–74 Contents lists available at ScienceDirect Geoderma journal homepage: www.elsevier.com/locate/geoderma Changes in soil properties in a fluvisol (calcaric) amended with coal fly ash A. Riehl a, F. Elsass b, J. Duplay a,⁎, F. Huber a, M. Trautmann c a Laboratoire d'Hydrologie et de Géochimie de Strasbourg, UMR 7517 CNRS, 1 rue Blessig 67084 Strasbourg Cedex, France b Institut National de Recherche Agronomique, route de Saint-Cyr 78026Versailles, France c UMS 830 UDS/CNRS, Laboratoire d'Analyses des Sols et des Formations Superficielles, 3 rue de l'Argonne 67083 Strasbourg Cedex, France article info abstract Article history: Fluidized bed combustion ash (FBC) is a by-product from coal-fired power stations used for many decades in Received 25 March 2009 concrete, cement and brick manufacturing and more recently for trace metal immobilization and pesticide Received in revised form 17 November 2009 retention in soils. -
Soil Properties, and Soil Organic Carbon Stocks of Tropical Andosol Under Different Land Uses
Open Journal of Soil Science, 2013, 3, 153-162 153 http://dx.doi.org/10.4236/ojss.2013.33018 Published Online July 2013 (http://www.scirp.org/journal/ojss) Soil Properties, and Soil Organic Carbon Stocks of Tropical Andosol under Different Land Uses Girma Abera*, Endalkachew Wolde-Meskel School of Plant and Horticultural Sciences, Hawassa University, Hawassa, Ethiopia. Email: *girmajibat2006 @yahoo.com Received December 21st, 2012; revised April 21st, 2013; accepted April 29th, 2013 Copyright © 2013 Girma Abera, Endalkachew Wolde-Meskel. This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited. ABSTRACT Land use effect of tropical Andosol, with two from crop lands (Site 1 and Site 2) and one from Agroforestry coffee plantation (Site 3) was explored under laboratory conditions to understand their physical, chemical and biological prop- erties and soil organic carbon (SOC) stocks from the rift valley of Ethiopia. Site 3 that acquired less cultivation than others exhibited better aggregate size fraction (AF, 55%), higher aggregate stability (AS, 91%), and greater active mi- crobial biomass (AMB), reflecting better soil structure development. Comparatively, higher total carbon (TC), organic carbon (OC) and total nitrogen (TN) concentrations were recorded in bulk soils and microaggregate fractions of Site 2 and Site 3 than in intensively cultivated Site 1. As expected, microaggregate fractions displayed greater OC and TN than bulk soils across all land uses. Site 1 revealed higher metabolic quotient (qCO2) and lower SOC stock (2.1 Mg·ha−1), suggesting microbial stress, while micro nutrients deficiencies were observed with the alkaline soil (Site 2). -
Effect of Soil Chiseling on Soil Structure and Root Growth for a Clayey Soil Under No-Tillage
Geoderma 259–260 (2015) 149–155 Contents lists available at ScienceDirect Geoderma journal homepage: www.elsevier.com/locate/geoderma Effect of soil chiseling on soil structure and root growth for a clayey soil under no-tillage Márcio Renato Nunes a,⁎, José Eloir Denardin b, Eloy Antônio Pauletto c, Antônio Faganello b, Luiz Fernando Spinelli Pinto c a University of São Paulo, “Luiz de Queiroz” College of Agriculture, Avenida Pádua Dias, 11, CEP 13418-900 Piracicaba, São Paulo, Brazil b Embrapa Trigo, Rodovia BR 285, km. 294, P.O. Box 451, CEP 99001-970 Passo Fundo, Rio Grande do Sul, Brazil c Federal University of Pelotas, Department of Soil Science, Campus Universitário s/n, P.O. Box 354, 96010-900 Pelotas, Rio Grande do Sul, Brazil article info abstract Article history: Soil chiseling under no-tillage (NT) promotes root growth in depth. This practice, however, might affect soil ag- Received 11 November 2014 gregation. This study evaluated the chiseling effects on the aggregation of a Ferralic Nitisol (Rhodic), under NT, in Received in revised form 2 June 2015 humid subtropical climate region. The treatments carried out consisted of the time that soil was kept under NT Accepted 3 June 2015 after chiseling: continuous NT for 24 months after chiseling in September 2009; continuous NT for 18 months Available online xxxx after chiseling in March 2010; continuous NT for 12 months after chiseling in September 2010; continuous NT for 6 months after chiseling in March 2011; NT in newly chiseling soil in September 2011; continuous NT without Keywords: Soil physical attributes chiseling (control). -
Fate of Organic Carbon in Paddy Soils – Results of Alisol and Andosol Incubation with 13C Marker
Geophysical Research Abstracts Vol. 18, EGU2016-17404, 2016 EGU General Assembly 2016 © Author(s) 2016. CC Attribution 3.0 License. Fate of organic carbon in paddy soils – results of Alisol and Andosol incubation with 13C marker Pauline Winkler (1), Chiara Cerli (2), Sabine Fiedler (3), Susanne Woche (4), Sri Rahayu Utami (5), Reinhold Jahn (1), Karsten Kalbitz (6), and Klaus Kaiser (1) (1) Soil Science, Martin Luther University Halle-Wittenberg, Germany, (2) Earth Surface Science, Institute for Biodiversity and Ecosystem Dynamics, University of Amsterdam, The Netherlands, (3) Soil Science, Johannes Gutenberg University Mainz, Germany, (4) Soil Science, Leibniz University Hannover, Germany, (5) Faculty of Agriculture, Brawijaya University, Malang, Indonesia, (6) Soil Science & Site Ecology, TU Dresden, Germany For a better understanding of organic carbon (OC) decomposition in paddy soils an incubation experiment was performed. Two soil types with contrasting mineralogy (Alisol and Andosol) were exposed to 8 anoxic–oxic cycles over 1 year. Soils received rice straw marked with 13C (228 at the beginning of each cycle. A second set of samples without straw addition was used as control. Headspacesh of the incubation vessels were regularly analysed for CO2 and CH4. In soil solutions, redox potential, pH, dissolved organic C (DOC), and Fe2+ were measured after each anoxic and each oxic phase. Soils were fractionated by density at the end of the experiment and the different fractions were isotopically analysed. Samples of genuine paddy soils that developed from the test soils were used as reference. During anoxic cycles, soils receiving rice straw released large amounts of CO2 and CH4, indicating strong micro- bial activity. -
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 -
Stability of Superparamagnetic Minerals in Soils and Rocks 0.5Ex
Stability of superparamagnetic minerals in soils and rocks Can frequency-dependent susceptibility be used as a proxy for climate in the past? Jan Igel1, Holger Preetz1;2 & Christian Rolf1 1Leibniz Institute for Applied Geophysics, Hannover, Germany Leibniz Institute for 2OFD Niedersachsen, Federal Competence Center for Soil and Applied Geophysics Groundwater Protection / UXO Clearance, Hannover, Germany Motivation Results & Interpretation I Frequency-dependent (FD) magnetic susceptibility is a property of I Samples treated with oxygen free water and samples treated superparamagnetic (SP) minerals. The presence of these minerals with sodium sulphide (shown here) show similar results. in soils and sediments is commonly attributed to neoformation Magnetic susceptibility during weathering and pedogenesis. 55000 Warm and humid conditions give rise to neoformation of SP mi- 50000 I Rocks: after dithionite 45000 reduction experiment Tuff nerals and thus frequency-dependent susceptibility is often used as treatment Tephra palaeoclimate proxy in sediment stratigraphy. Rhyolite SI] 40000 6 − I SP minerals can also be of lithogenic origin and occur in magmatic [10 Soils: LF rocks and volcanic ashes. However, a lithogenic origin is commonly κ ≈ Luvisol Humous loess 10000 Laterite neglected in palaeoclimatic studies. Terra Rossa I Pedogenic SP minerals are assumed to be less stable than lithoge- 5000 nic SP minerals. 0 0 50 100 150 200 250 time [days] Materials I No decrease of κLF or ∆κ in reducing environment ! SP minerals stable regardless of their origin (lith./ped.) A number of 7 samples with high I Some soils show increase of κLF and ∆κ during reduction content of SP minerals were in- ! neoformation of SP minerals due to bacterial activity vestigated. -
Fiji)Iji) Uusingsing Tthehe UUSLESLE Mmodelodel Andand a GISGIS
COMPONENT 1A - Project 1A4 Integrated Coastal Management - GERSA Project Spatial Approach - Remote Sensing September 2008 TECHNICAL REPORT MMappingapping PotentialPotential EErosionrosion RRisksisks iinn NNorthorth VVitiiti LLevuevu (FFiji)iji) uusingsing tthehe UUSLESLE MModelodel andand a GISGIS AAuthor:uthor: JJuliaulia PPRINTEMPSRINTEMPS Photo : Julia PRINTEMPS The CRISP programme is implemented as part of the policy developed by the Secretariat of the Pacifi c Regional Environment Programme for a contribution to conservation and sustainable development of coral reefs in the Pacifi c. he Initiative for the Protection and Management of Coral Reefs in the Pacifi c T (CRISP), sponsored by France and prepared by the French Development Agency (AFD) as part of an inter-ministerial project from 2002 onwards, aims to develop a vision for the future of these unique eco-systems and the communities that depend on them and to introduce strategies and projects to conserve their biodiversity, while developing the economic and environmental services that they provide both locally and globally. Also, it is designed as a factor for integration between developed countries (Australia, New Zealand, Japan and USA), French overseas territories and Pacifi c Island developing countries. The CRISP Programme comprises three major components, which are: Component 1A: Integrated Coastal Management and Watershed Management - 1A1: Marine biodiversity conservation planning - 1A2: Marine Protected Areas (MPAs) - 1A3: Institutional strengthening and networking - -
DOGAMI MP-20, Investigations of Nickel in Oregon
0 C\1 a: w a.. <( a.. en ::::> 0 w z <( __j __j w () en � INVESTIGATIONS OF NICKEL IN OREGON STATE OF OREGON DEPARTMENT OF GEOL.OGY AND MINERAL. IN OUSTRIES DONAL.D .A HUL.L. STATE GEOLOGIST 1978 STATE OF OREGON DEPARTMENT OF GEOLOGY AND MINERAL INDUSTRIES 1069 State Office Building, Portland, Oregon 97201 MISCELLANEOUS PAPER 20 INVESTIGATIONS OF NICKEL IN OREGON Len Ramp, Resident Geologist Grants Pass Field Office Oregon Department of Geology and Mineral Industries Conducted in conformance with ORS 516.030 . •. 5 1978 GOVERNING BOARD Leeanne MacColl, Chairperson, Portland Talent Robert W. Doty STATE GEOLOGIST John Schwabe Portland Donald A. Hull CONTENTS INTRODUCTION -- - ---- -- -- --- Purpose and Scope of this Report Acknowledgments U.S. Nickel Industry GEOLOGY OF LATERITE DEPOSITS - -- - 3 Previous Work - - - - --- 3 Ultramafic Rocks - ----- --- 3 Composition - - -------- - 3 Distribution ------ - - - 3 Structure - 3 Geochemistry of Nickel ---- 4 Chemical Weathering of Peridotite - - 4 The soi I profile ------- 5 M i nero I ogy -- - ----- 5 Prospecting Guides and Techniques- - 6 OTHER TYPES OF NICKEL DEPOSITS - - 7 Nickel Sulfide Deposits- - - - - - 7 Deposits in Oregon 7 Other areas --- 8 Prospecting techniques 8 Silica-Carbonate Deposits - -- 8 DISTRIBUTION OF LATERITE DEPOSITS - ------ 9 Nickel Mountain Deposits - - ------ --------- 9 Location --------------- --- 9 Geology - ------- ----- 11 Ore deposits ----------- - -- 11 Soil mineralogy - ------- 12 Structure --- ---- ---- 13 Mining and metallurgy ------------ ---- 13 Production- -
Sorption and Desorption of Vanadate, Arsenate and Chromate by Two Volcanic Soils of Equatorial Africa
Article Sorption and Desorption of Vanadate, Arsenate and Chromate by Two Volcanic Soils of Equatorial Africa Sara Gonzalez-Rodriguez 1 and Maria Luisa Fernandez-Marcos 1,2,* 1 Department of Soil Science and Agricultural Chemistry, Universidad de Santiago de Compostela, 27002 Lugo, Spain; [email protected] 2 Institute of Agricultural Biodiversity and Rural Development, University of Santiago de Compostela, 27002 Lugo, Spain * Correspondence: [email protected] Abstract: Sorption of oxyanions by soils and mineral surfaces is of interest due to their role as nutrients or pollutants. Volcanic soils are variable charge soils, rich in active forms of aluminum and iron, and capable of sorbing anions. Sorption and desorption of vanadate, arsenate, and chromate by two African andosols was studied in laboratory experiments. Sorption isotherms were determined by equilibrating at 293 K soil samples with oxyanion solutions of concentrations between 0 and 100 mg L−1 V, As, or Cr, equivalent to 0−2.0 mmol V L−1, 0−1.3 mmol As L−1, and −1 0−1.9 mmol Cr L , in NaNO3; V, As, or Cr were determined by ICP-mass spectrometry in the equilibrium solution. After sorption, the soil samples were equilibrated with 0.02 M NaNO3 to study desorption. The isotherms were adjusted to mathematical models. After desorption with NaNO3, desorption experiments were carried out with a 1 mM phosphate. The sorption of vanadate and arsenate was greater than 90% of the amount added, while the chromate sorption was much lower (19–97%). The sorption by the Silandic Andosol is attributed to non-crystalline Fe and Al, while in Citation: Gonzalez-Rodriguez, S.; the Vitric Andosol, crystalline iron species play a relevant role. -
The Soil Map of the Flemish Region Converted to the 3 Edition of the World Reference Base for Soil Resources
Ontwikkelen en toepassen van een methodiek voor de vertaling van de Belgische bodemclassificatie van de kustpolders naar het internationale WRB systeem en generaliseren van de WRB-bodemkaart voor gans Vlaanderen naar het 1 : 250 000 schaalniveau The soil map of the Flemish region converted to the 3 rd edition of the World Reference Base for soil resources Stefaan Dondeyne, Laura Vanierschot, Roger Langohr Eric Van Ranst and Jozef Deckers Oct. 2014 Opdracht van de Vlaamse Overheid Bestek nr. BOD/STUD/2013/01 Contents Contents............................................................................................................................................................3 Acknowledgement ...........................................................................................................................................5 Abstract............................................................................................................................................................7 Samenvatting ...................................................................................................................................................9 1. Background and objectives.......................................................................................................................11 2. The soil map of Belgium............................................................................................................................12 2.1 The soil survey project..........................................................................................................................12 -
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.