Polygenetic Oxisols on Tertiary Surfaces, Minas Gerais, Brazil
Total Page:16
File Type:pdf, Size:1020Kb
Load more
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. -
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. -
Murphey Et Al. 2019 Best Practices in Mitigation Paleontology
PROCEEDINGS of the San Diego Society of Natural History Founded 1874 Number 47 1 May 2019 BEST PRACTICES IN MITIGATION PALEONTOLOGY By Paul C. Murphey Paleo Solutions, 2785 Speer Boulevard, Suite 1, Denver, CO 80211, U.S.A.; [email protected]; Department of Paleontology, San Diego Natural History Museum, 1788 El Prado, San Diego, CA 92101, U.S.A.; [email protected] Department of Earth Sciences, Denver Museum of Nature and Science, 2001 Colorado Boulevard, Denver, CO 80201, U.S.A. Georgia E. Knauss SWCA Environmental Consultants, 1892 S. Sheridan Avenue, Sheridan, WY 82801 U.S.A.; [email protected] Lanny H. Fisk PaleoResource Consultants, 550 High Street, Suite 108, Auburn, CA 95603, U.S.A. (deceased) Thomas A. Deméré Department of Paleontology, San Diego Natural History Museum, 1788 El Prado, San Diego, CA 92101, U.S.A.; [email protected] Robert E. Reynolds Department of Paleontology, San Diego Natural History Museum, 1788 El Prado, San Diego, CA 92101, U.S.A.; [email protected] For correspondence, write to: Paul C. Murphey, Paleo Solutions, 4614 Lonespur Ct. Oceanside, CA 92056 Email: [email protected] [email protected] bpmp-19-01-fm Page 2 PDF Created: 2019-4-12: 9:20:AM 2 Paul C. Murphey, Georgia E. Knauss, Lanny H. Fisk, Thomas A. Deméré, and Robert E. Reynolds TABLE OF CONTENTS Abstract . 4 Introduction . 4 History and Scientific Contributions . 5 History of Mitigation Paleontology in the United States . 5 Methods Best Practice Categories . 7 1. Qualifications. 7 Confusion between Resource Disciplines . 7 Professional Geologists as Mitigation Paleontologists. 8 Mitigation Paleontologist Categories . -
Paleoenvironmental Constraints from Paleosol-Loess Sequences: Evaluating Clumped (∆47) Isotopic Records in Biogenic and Pedogenic Carbonate
Paleoenvironmental constraints from paleosol-loess sequences: evaluating clumped (∆47) isotopic records in biogenic and pedogenic carbonate Katharine Huntington, Department of Earth and Space Sciences The project goal was to advance understanding of how the geochemistry of biogenic and pedogenic (formed in soil) carbonates record surface environmental temperatures and soil water compositions relevant to the interpretation of proxy records in Quaternary loess-paleosol sequences and cultural layers. Reconstructing Quaternary paleoenvironments is important for a broad range of paleoclimate, geology, biology, anthropology and archaeology studies. The geochemistry of carbonate minerals formed at and near the Earth surface can provide quantitative environmental constraints including the δ18O values of water, δ13C-based information about vegetation, and most recently, estimates of Earth-surface temperatures from clumped isotope (∆47) thermometry. Early efforts to develop clumped isotope thermometry in modern-Holocene soils raise many 18 questions about how to interpret not only ∆47 temperatures but also conventional δ O and δ13C values in soil and loess carbonates. We conducted a study of biogenic, pedogenic, and geogenic carbonates of different types from two Quaternary paleosol-loess deposits, the Nussloch (Rhine Valley, SW Germany) and Palouse (eastern Washington state) loess-paleosol sequences. Carbonate δ18O, δ13C 14 and ∆47 analyses were conducted in the University of Washington IsoLab as well as C dating of carbonates to determine their age and pedogenic vs. geogenic nature. In the 18 13 Nussloch, the δ O, δ C and Δ47 data for multiple carbonate types revealed the effects of geogenic carbonate input, pedogenesis and environmental factors on the isotopic variations, and showed that geogenic “bulk loess” carbonates that are poor environmental proxies can still provide important context for interpreting the isotopic signature of pedogenic and biogenic carbonates (Zamanian et al., in revision). -
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. -
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. -
Anatomy of a Sub-Cambrian Paleosol in Wisconsin
Anatomy of a Sub-Cambrian Paleosol in Wisconsin: Mass Fluxes of Chemical Weathering and Climatic Conditions in North America during Formation of the Cambrian Great Unconformity L. Gordon Medaris Jr.,1,* Steven G. Driese,2 Gary E. Stinchcomb,3 John H. Fournelle,1 Seungyeol Lee,1,4 Huifang Xu,1,4 Lyndsay DiPietro,2 Phillip Gopon,5 and Esther K. Stewart6 1. Department of Geoscience, University of Wisconsin, Madison, Wisconsin 53706, USA; 2. Department of Geosciences, Terrestrial Paleoclimatology Research Group, Baylor University, Waco, Texas 76798, USA; 3. Department of Geosciences and Watershed Studies Institute, Murray State University, Murray, Kentucky 42071, USA; 4. NASA Astrobiology Institute, University of Wisconsin, Madison, Wisconsin 53706, USA; 5. Department of Earth Sciences, University of Oxford, South Parks Road, Oxford OX1 3AN, United Kingdom; 6. Wisconsin Geological and Natural History Survey, Madison, Wisconsin 53705, USA ABSTRACT A paleosol beneath the Upper Cambrian Mount Simon Sandstone in Wisconsin provides an opportunity to evaluate the characteristics of Cambrian weathering in a subtropical climate, having been located at 207S paleolatitude 500 My ago. The 285-cm-thick paleosol resulted from advanced chemical weathering of a gabbroic protolith, recording a total mass loss of 50%. Weathering of hornblende and plagioclase produced a pedogenic assemblage of quartz, chlorite, kaolinite, goethite, and, in the lowest part of the profile, siderite. Despite the paucity of quartz in the protolith and 40% removal of SiO2 from the profile, quartz constitutes 11%–23% of the pedogenic mineral assemblage. Like many other Precambrian and Cambrian paleosols in the Lake Superior region, the paleosol experienced potassium metasomatism, now con- taining 10%–25% mixed-layer illite-vermiculite and 5%–44% potassium feldspar. -
Redalyc.CONTAMINATION POTENTIAL of SPECIFIC IONS IN
Revista Caatinga ISSN: 0100-316X [email protected] Universidade Federal Rural do Semi- Árido Brasil PAIVA DE OLIVEIRA, ANDLER MILTON; MEDEIROS REBOUÇAS, CEZAR AUGUSTO; DA SILVA DIAS, NILDO; CRUZ PORTELA, JEANE; ARAÚJO DINIZ, ADRIANA CONTAMINATION POTENTIAL OF SPECIFIC IONS IN SOIL TREATED WITH REJECT BRINE FROM DESALINATION PLANTS Revista Caatinga, vol. 29, núm. 3, julio-septiembre, 2016, pp. 569-577 Universidade Federal Rural do Semi-Árido Mossoró, Brasil Available in: http://www.redalyc.org/articulo.oa?id=237146823005 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 Universidade Federal Rural do Semi-Árido ISSN 0100-316X (impresso) Pró-Reitoria de Pesquisa e Pós-Graduação ISSN 1983-2125 (online) http://periodicos.ufersa.edu.br/index.php/sistema CONTAMINATION POTENTIAL OF SPECIFIC IONS IN SOIL TREATED WITH REJECT BRINE FROM DESALINATION PLANTS1 ANDLER MILTON PAIVA DE OLIVEIRA2, CEZAR AUGUSTO MEDEIROS REBOUÇAS2, NILDO DA SILVA DIAS2*, JEANE CRUZ PORTELA2, ADRIANA ARAÚJO DINIZ2 ABSTRACT - Percolation columns constructed in the Laboratory can predict the degree of contamination in soil due to reject brine disposal and can be a tool for reducing environmental impacts. This study aim to evaluate the mobilization of ions in reject brine from desalination process by reverse osmosis. The mobilization of the contaminant ions in the saline waste was studied in glass percolation columns, which were filled with soil of contrasting textures (eutrophic CAMBISOL, typic dystrophic Red OXISOL, ENTISOL Quartzipsamment). -
Parameters Related to the Identification of Paleosols in the Geologic Record
6206) V96 nd. K3-776 UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY Parameters Related to the Identification of Paleosols in the Geologic Record by Robert A. Miller and Wayne R. Sigleo 601ijiLv!h7"'104 \ir: a A.4.1 Ni() V 071983 44 Open-File Report $3-776 This report is preliminary and has not been reviewed for conformity with U.S. Gelogical Survey editorial standards. CONTENTS Page Introduction 1 Color 2 Biogenic Properties 2 Soil Structure 3 Clay Minerals and Sesquioxides 4 Concretions 4 Summary 5 References Cited 6 FIGURES Figure 1. Pedologic profile of a soil (after Ruhe, 1965) 1 Figure 2. General description of soil structure 3 ii Parameters Related to the Identification of Paleosols in the Geologic Record by Robert A. Miller and Wayne R. Sigleo Introduction Paleosols or fossil soils occur in most geologic environments, and where consistent recognition is possible, they can provide important evidence to interpret and correlate local and regional stratigraphic successions (North American Code of Stratigraphic Nomenclature, 1983). A paleosol, whether buried, exhumed, or relict, may indicate a hiatus in deposition, and may be the only record of a certain time interval. Studies of paleosols, especially in conjunction with paleobotanical and geochemical research, are particularly useful in deciphering paleoenvironments, climates, and landscape evolution. The study of modern soils or pedology provides the basic framework to understand and interpret fossil soils (Fitzpatrick, 1971; Oilier, 1969). Although there is no simple definition for a modeorn soil; most soils include all of the material which differs from underlying rock or parent material through weathering, and is capable of supporting vegetation. -
Berino Paleosol, Late Pleistocene Argillic Soil Development on the Mescalero Sand Sheet in New Mexico
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by UNL | Libraries University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Earth and Atmospheric Sciences, Department Papers in the Earth and Atmospheric Sciences of 2012 Berino Paleosol, Late Pleistocene Argillic Soil Development on the Mescalero Sand Sheet in New Mexico Stephen A. Hall Red Rock Geological Enterprises, Santa Fe, NM, [email protected] Ronald J. Goble University of Nebraska-Lincoln, [email protected] Follow this and additional works at: https://digitalcommons.unl.edu/geosciencefacpub Part of the Earth Sciences Commons Hall, Stephen A. and Goble, Ronald J., "Berino Paleosol, Late Pleistocene Argillic Soil Development on the Mescalero Sand Sheet in New Mexico" (2012). Papers in the Earth and Atmospheric Sciences. 325. https://digitalcommons.unl.edu/geosciencefacpub/325 This Article is brought to you for free and open access by the Earth and Atmospheric Sciences, Department of at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in Papers in the Earth and Atmospheric Sciences by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. Berino Paleosol, Late Pleistocene Argillic Soil Development on the Mescalero Sand Sheet in New Mexico Stephen A. Hall1,* and Ronald J. Goble2 1. Red Rock Geological Enterprises, 3 Cagua Road, Santa Fe, New Mexico 87508, U.S.A.; 2. Department of Earth and Atmospheric Sciences, 214 Bessey Hall, University of Nebraska, Lincoln, Nebraska 68588, U.S.A. ABSTRACT The Berino paleosol is the first record of a directly dated Aridisol in the American Southwest where paleoclimatic conditions during the time of pedogenesis can be estimated. -
One Year Residual Effect of Sewage Sludge Biochar As a Soil Amendment for Maize in a Brazilian Oxisol
sustainability Article One Year Residual Effect of Sewage Sludge Biochar as a Soil Amendment for Maize in a Brazilian Oxisol Joisman Fachini 1 , Thais Rodrigues Coser 1 , Alyson Silva de Araujo 1 , Ailton Teixeira do Vale 2, Keiji Jindo 3 and Cícero Célio de Figueiredo 1,* 1 Faculty of Agronomy and Veterinary Medicine, University of Brasilia, Brasília 70910970, Brazil; [email protected] (J.F.); [email protected] (T.R.C.); [email protected] (A.S.d.A.) 2 Department of Forestry Engineering, University of Brasilia, Brasília 70910970, Brazil; [email protected] 3 Agrosystems Research, Wageningen University & Research, P.O. Box 16, 6700 AA Wageningen, The Netherlands; [email protected] * Correspondence: [email protected]; Tel.: +55-61-3107-7564 Abstract: The thermochemical transformation of sewage sludge (SS) to biochar (SSB) allows exploring the advantages of SS and reduces possible environmental risks associated with its use. Recent studies have shown that SSB is nutrient-rich and may replace mineral fertilizers. However, there are still some questions to be answered about the residual effect of SSB on soil nutrient availability. In addition, most of the previous studies were conducted in pots or soil incubations. Therefore, the residual effect of SSB on soil properties in field conditions remains unclear. This study shows the results of nutrient availability and uptake as well as maize yield the third cropping of a three-year consecutive corn cropping system. The following treatments were compared: (1) control: without mineral fertilizer and biochar; (2) NPK: with mineral fertilizer; (3) SSB300: with biochar produced at ◦ ◦ 300 C; (4) SSB300+NPK; (5) SSB500: with biochar produced at 500 C; and (6) SSB500+NPK. -
Global Soil Change
GLOBAL SOIL CHANGE Report of an International lnstitute for Applied System Analysis, International Society of Soil Science, United Nations Environmental Programme Task Force on the Role of Soil in Global Change Editors: R. W. ARNOLD, I. SZABOLCS, V. 0. TARGULIAN International lnstitute for Applied Systems Analysis Laxenburg, Austria 1990 CONTENTS FtXd ........................................................ 7 Prefaae ........................................................ 9 Editorial Preface ............................................... 11 Q=@=I In- ...................................... 15 Chapter 11 Pedospkre ....................................... 21 Chapter I11 Soil axe.r of t.h?Wrld ........................... 31 Chapterm Types of Soil Prooesses and Changes ............... 41 Chapter v Pdleosols in the ca-ltext of Envirmm?ntal Changes .......................................... 63 Chaptern An-c Effects cm Soils .................... 69 Chapter VII EUture Changes of tk Pedospkre .................. 87 Chapter VIII Spatial Soil Databases ard kdeling ............... 91 mpter IX amclusions and &amendations ................... lo3 FOREWORD The International Institute for Applied Systems, is a non-governmental, interdisciplinary research organization founded in 1972. Arrang its mst relevant abjectives are "the initiation and supprt of individual and col- lakorative research on problems associated with environmental chanqe, and thereby to assist scientific camunities throughout the world in tackling such problems". One mans to this goal