FAO-UNESCO Soil Map of the World, 1:5000000 Vol. 1. Legend
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NRCS Keys to Soil Taxonomy
United States Department of Agriculture Keys to Soil Taxonomy Ninth Edition, 2003 Keys to Soil Taxonomy By Soil Survey Staff United States Department of Agriculture Natural Resources Conservation Service Ninth Edition, 2003 The United States Department of Agriculture (USDA) prohibits discrimination in all its programs and activities on the basis of race, color, national origin, gender, religion, age, disability, political beliefs, sexual orientation, and marital or family status. (Not all prohibited bases apply to all programs.) Persons with disabilities who require alternative means for communication of program information (Braille, large print, audiotape, etc.) should contact USDA’s TARGET Center at 202-720-2600 (voice and TDD). To file a complaint of discrimination, write USDA, Director, Office of Civil Rights, Room 326W, Whitten Building, 14th and Independence Avenue, SW, Washington, DC 20250-9410, or call 202-720-5964 (voice and TDD). USDA is an equal opportunity provider and employer. Cover: A natric horizon with columnar structure in a Natrudoll from Argentina. 5 Table of Contents Foreword .................................................................................................................................... 7 Chapter 1: The Soils That We Classify.................................................................................. 9 Chapter 2: Differentiae for Mineral Soils and Organic Soils ............................................... 11 Chapter 3: Horizons and Characteristics Diagnostic for the Higher Categories ................. -
Soil Taxonomy" in Particular ,
1. CONTROL NUMBER 2. SUBECT CLASSIFICATION (695) BIBLIOGRAPItlC DATA SHEET IN-AAJ-558 AF26-0000-0000 3. TITLE ANt) SUBTITLE (240) Experimental designs for predicting crop productivity with environmental and economic inputs for al rotcchnology transfer 4. PERSON.\I. AUTHORS (10P) Silva, J. A. 5. CORPORATE AUTHORS (101) Hawaii Univ. College of Tropical Agriculture 6. IDOCUMEN2< DATE (110)7. NUMBER OF PAGES (120) 8.ARC NUMBER [7 1981 13n631.5.S586b __ 9. R FRENCE ORGANIZATION (130) Hawaii 10. SUPI'PLEMENTARY NOTES (500) (In Departmental paper 49) 11. ABSTRACT (950) 12. DESCRIPTORS (920) 13. PROJECT NUMBER (150) Agricultural production Agricultural technology 931582C00 Technology transferi!Techoloy tansferYieldY e d14. CONTRACT NO.(I It)) 15. CONTRACT Soil fertility Experimentation TYPE (140) Tropics Productivity AID/ta-C-1108 Forecasting 16. TYPE OF DOCUMENT (160) AM 590-7 (10-79) Departmental Paper 49 Experimental Designs for Predicting Crop Productivity with Environmental and Economic Inputs for Agrotechnology Transfer Edited by James A. Silva ...... ,..,... *** .......... ....* ...... .... .. 00400O 00€€€€*00 .. ...* Y Y*b***S4....... ~~~.eeeeeoeeeeeU ........ o .. *.4.............*e............ :0 ooee............. ........... ....... nae of T c.e Haw i. ns..ut. CollegeofTrpclgr.cut a UnversityoHa B....EMAR.SO University of Hawaiio~ee BENCHMAR SO I Le~eSPoJECTU/ADCotac o.t-C1 14.. C4 '4 t 10 wte IA:A 77 d E/ Adt , I 26Esi ',. ,~ )~'I *3-! * Ire ~ -I ~ 0 1 N Koel4 'I M M Experimental Designs for Predicting Crop Productivity with Environmental and Economic Inputs for Agrotechnology Transfer Edited by James A. Silva Benchmark Soils Project UH/AiD Contract No. to-C-1108 The Author James A. Silva is Soil Scientist and Principal Investigator, Benchmark Soils Project/Hawaii, Department of Agronomy and Soil Science, College of Tropical Agriculture and Human Resources, University of Hawaii, Honolulu. -
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. -
Terra Rossa in the Mediterranean Region: Parent Materials, Composition and Origin
Geologia Croatica 56/1 83–100 23 Figs. 6 Tabs. ZAGREB 2003 Terra Rossa in the Mediterranean Region: Parent Materials, Composition and Origin Goran DURN Key words: Terra rossa, Parent materials, Composi- relict soil formed during the Tertiary and/or hot and humid periods of the Quaternary. However, some recent investigation in the Atlantic tion, Origin, Mediterranean region. coastal region of Morocco (BRONGER & SEDOV, 2002) show that at least some terra rossa previously referred to as polygenetic relict soils should be regarded as Vetusols. In some isolated karst terrain, terra Abstract rossa may have formed exclusively from the insoluble residue of lime- In the past, the term “terra rossa” became quite a common indication stone and dolomite but much more often it comprises a span of parent for all limestone derived red soils in the Mediterranean region. Today, materials including, for example, aaeolian dust, volcanic material or in some classification systems based on the Mediterranean climate as sedimentary clastic rocks which were derived on carbonate terrain via the major soil differentiating criterion, the term terra rossa is used as a different transport mechanisms. BOERO & SCHWERTMANN (1989) name for the soil subclass “Modal Fersiallitic Red soil” when situated concluded that it is of little relevance for the process of rubification on limestones (DUCHAUFOUR, 1982). However, several national whether the primary Fe sources are autochthonous or allochthonous as soil classifications (e.g. Croatian, Italian, Israeli) retained the term long as the general pedoenvironment remains essentially suitable for “terra rossa” for the hard limestone derived red soils. The nature and the formation of terra rossa. -
Good Practices for the Preparation of Digital Soil Maps
UNIVERSIDAD DE COSTA RICA CENTRO DE INVESTIGACIONES AGRONÓMICAS FACULTAD DE CIENCIAS AGROALIMENTARIAS GOOD PRACTICES FOR THE PREPARATION OF DIGITAL SOIL MAPS Resilience and comprehensive risk management in agriculture Inter-american Institute for Cooperation on Agriculture University of Costa Rica Agricultural Research Center UNIVERSIDAD DE COSTA RICA CENTRO DE INVESTIGACIONES AGRONÓMICAS FACULTAD DE CIENCIAS AGROALIMENTARIAS GOOD PRACTICES FOR THE PREPARATION OF DIGITAL SOIL MAPS Resilience and comprehensive risk management in agriculture Inter-american Institute for Cooperation on Agriculture University of Costa Rica Agricultural Research Center GOOD PRACTICES FOR THE PREPARATION OF DIGITAL SOIL MAPS Inter-American institute for Cooperation on Agriculture (IICA), 2016 Good practices for the preparation of digital soil maps by IICA is licensed under a Creative Commons Attribution-ShareAlike 3.0 IGO (CC-BY-SA 3.0 IGO) (http://creativecommons.org/licenses/by-sa/3.0/igo/) Based on a work at www.iica.int IICA encourages the fair use of this document. Proper citation is requested. This publication is also available in electronic (PDF) format from the Institute’s Web site: http://www.iica. int Content Editorial coordination: Rafael Mata Chinchilla, Dangelo Sandoval Chacón, Jonathan Castro Chinchilla, Foreword .................................................... 5 Christian Solís Salazar Editing in Spanish: Máximo Araya Acronyms .................................................... 6 Layout: Sergio Orellana Caballero Introduction .................................................. 7 Translation into English: Christina Feenny Cover design: Sergio Orellana Caballero Good practices for the preparation of digital soil maps................. 9 Printing: Sergio Orellana Caballero Glossary .................................................... 15 Bibliography ................................................. 18 Good practices for the preparation of digital soil maps / IICA, CIA – San Jose, C.R.: IICA, 2016 00 p.; 00 cm X 00 cm ISBN: 978-92-9248-652-5 1. -
A New Era of Digital Soil Mapping Across Forested Landscapes 14 Chuck Bulmera,*, David Pare´ B, Grant M
CHAPTER A new era of digital soil mapping across forested landscapes 14 Chuck Bulmera,*, David Pare´ b, Grant M. Domkec aBC Ministry Forests Lands Natural Resource Operations Rural Development, Vernon, BC, Canada, bNatural Resources Canada, Canadian Forest Service, Laurentian Forestry Centre, Quebec, QC, Canada, cNorthern Research Station, USDA Forest Service, St. Paul, MN, United States *Corresponding author ABSTRACT Soil maps provide essential information for forest management, and a recent transformation of the map making process through digital soil mapping (DSM) is providing much improved soil information compared to what was available through traditional mapping methods. The improvements include higher resolution soil data for greater mapping extents, and incorporating a wide range of environmental factors to predict soil classes and attributes, along with a better understanding of mapping uncertainties. In this chapter, we provide a brief introduction to the concepts and methods underlying the digital soil map, outline the current state of DSM as it relates to forestry and global change, and provide some examples of how DSM can be applied to evaluate soil changes in response to multiple stressors. Throughout the chapter, we highlight the immense potential of DSM, but also describe some of the challenges that need to be overcome to truly realize this potential. Those challenges include finding ways to provide additional field data to train models and validate results, developing a group of highly skilled people with combined abilities in computational science and pedology, as well as the ongoing need to encourage communi- cation between the DSM community, land managers and decision makers whose work we believe can benefit from the new information provided by DSM. -
Pedometric Mapping of Key Topsoil and Subsoil Attributes Using Proximal and Remote Sensing in Midwest Brazil
UNIVERSIDADE DE BRASÍLIA FACULDADE DE AGRONOMIA E MEDICINA VETERINÁRIA PROGRAMA DE PÓS-GRADUAÇÃO EM AGRONOMIA PEDOMETRIC MAPPING OF KEY TOPSOIL AND SUBSOIL ATTRIBUTES USING PROXIMAL AND REMOTE SENSING IN MIDWEST BRAZIL RAÚL ROBERTO POPPIEL TESE DE DOUTORADO EM AGRONOMIA BRASÍLIA/DF MARÇO/2020 UNIVERSIDADE DE BRASÍLIA FACULDADE DE AGRONOMIA E MEDICINA VETERINÁRIA PROGRAMA DE PÓS-GRADUAÇÃO EM AGRONOMIA PEDOMETRIC MAPPING OF KEY TOPSOIL AND SUBSOIL ATTRIBUTES USING PROXIMAL AND REMOTE SENSING IN MIDWEST BRAZIL RAÚL ROBERTO POPPIEL ORIENTADOR: Profa. Dra. MARILUSA PINTO COELHO LACERDA CO-ORIENTADOR: Prof. Titular JOSÉ ALEXANDRE MELO DEMATTÊ TESE DE DOUTORADO EM AGRONOMIA BRASÍLIA/DF MARÇO/2020 ii iii REFERÊNCIA BIBLIOGRÁFICA POPPIEL, R. R. Pedometric mapping of key topsoil and subsoil attributes using proximal and remote sensing in Midwest Brazil. Faculdade de Agronomia e Medicina Veterinária, Universidade de Brasília- Brasília, 2019; 105p. (Tese de Doutorado em Agronomia). CESSÃO DE DIREITOS NOME DO AUTOR: Raúl Roberto Poppiel TÍTULO DA TESE DE DOUTORADO: Pedometric mapping of key topsoil and subsoil attributes using proximal and remote sensing in Midwest Brazil. GRAU: Doutor ANO: 2020 É concedida à Universidade de Brasília permissão para reproduzir cópias desta tese de doutorado e para emprestar e vender tais cópias somente para propósitos acadêmicos e científicos. O autor reserva outros direitos de publicação e nenhuma parte desta tese de doutorado pode ser reproduzida sem autorização do autor. ________________________________________________ Raúl Roberto Poppiel CPF: 703.559.901-05 Email: [email protected] Poppiel, Raúl Roberto Pedometric mapping of key topsoil and subsoil attributes using proximal and remote sensing in Midwest Brazil/ Raúl Roberto Poppiel. -- Brasília, 2020. -
Soils of County Clare
Copyright of Teagasc, The Agriculture and Food Development Authority Soil Survey Bulletin No. 23 Soils of County Clare by T. F. Finch (Report compiled by T. F, Finch, E. Culleton and S. Diamond) National Soil Survey of Ireland An Foras Taluntais (THE AGRICULTURAL INSTITUTE) Published by An Foras Taluntais, 33 Merrion Road, Dublin 4 Price: £1.50 June, 1971 PREFACE This publication, Soil Survey Bulletin No. 23, presents the findings of the Soil Survey of County Clare. It is one of a series of county soil surveys being carried out by the National Soil Survey of An Foras Taluntais (The Agricultural Institute) for the purpose of providing basic information which can be used in optimum land-use planning. The field mapping was carried out at a scale of 1:10,560 (6 in. = 1 mile; 15 cm = 1.6 km) but the detail mapped on the field sheets is not shown on the published soil map at the scale of 1:126,720 (} in. 1 mile: 1.25 cm = 1.6 km) due to scale limitation. Copies of the field maps are available for consultation in the Soil Survey Office at Johnstown Castle, Wexford. Mr. T. F. Finch was responsible for the operation of this survey; he commenced work in the county in 1965 and completed the field investigations in 1968. Technical assistance was provided from time to time by Mr. P. Feeney, Mr. T. O'Shea and Mr. T. Martin. Mr. S. Diamond gave assistance and advice in soil correlation, classification and land-use interpretation, and Mr. R. F. -
Characteristics and Formation of So-Called Red-Yellow Podzolic Soils in the Humid Tropics (Sarawak-Malaysia)
Characteristics and Formation of so-called Red-Yellow Podzolic Soils in the Humid Tropics (Sarawak-Malaysia) J.P, Andriesse Characteristics and Formation of so-called Red-Yellw Podzolic Soils in the Humid Tropics (Sarawak-Malaysia) This thesis will also be published as Communication nr. 66 of the Royal Tropical Institute, Amsterdam Characteristics and Formation of so-called Red^ellow Podzolic Soils in the Humid Tropics (Sarawak-Malaysia) Proefschrift ter verkrijging van de graad van doctor in de Wiskunde en Natuur- wetenschappen aan de Rijksuniversiteit te Utrecht, op gezag van de Rector Magnificus Prof. Dr. Sj. Groenman, volgens besluit van het College van Dekanen in het openbaar te verdedigen op 8 decem- ber 1975 des namiddags te 4.15 uur door Jacobus Pieter Andriesse geboren op 28 maart 1929 te Middelburg Scanned from original by ISRIC - World Soil Information, as ICSU World Data Centre for Soils. The purpose is to make a safe depository for endangered documents and to make the accrued information available for consultation, following Fair Use' Guidelines. Every effort is taken to respect Copyright of the materials within the archives where the identification of the .Copyright holder is clear and, where feasible, to contact the originators. For questions please contact [email protected] indicating the item reference number concerned. Promotores: Prof.Dr.Ir. L.J. Pons, Landbouwhogeschool, Wageningen Prof.Dr. R.D. Schuiling Dit proefschrift kwam in zijn volledigheid tot stand onder leiding van Prof.Dr.Ir. F.A. van Baren f Preface Sarawak - a geography of life 'Extensive, almost inaccessible swamps, stretching along the coast, must be passed to reach the hills which in their monotonous repetition of heights and valleys wear down the traveller, but from where the lofty mountains beyond beckon to carry on' I dedicate this thesis to the memory of my late parents who through their efforts enabled me to receive the basic education which opened the door for my professional career, but who through their premature decease could not witness the results of their labour. -
Bacterial Diversity in Soils of Different Hungarian Karst Areas
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Repository of the Academy's Library Acta Microbiologica et Immunologica Hungarica 65 (4), pp. 439–458 (2018) DOI: 10.1556/030.65.2018.002 First published online February 23, 2018 BACTERIAL DIVERSITY IN SOILS OF DIFFERENT HUNGARIAN KARST AREAS 1,2 2 1 3 MONIKA´ KNÁB ,TIBOR SZILI-KOVÁCS ,KÁROLY MÁRIALIGETI ,JÁNOS MOGA´ and ANDREA K. BORSODI1* 1Department of Microbiology, ELTE Eötvös Loránd University, Budapest, Hungary 2Centre for Agricultural Research, Institute for Soil Sciences and Agricultural Chemistry, Hungarian Academy of Sciences, Budapest, Hungary 3Department of Physical Geography, ELTE Eötvös Loránd University, Budapest, Hungary (Received: 5 June 2017; accepted: 21 November 2017) Karst areas have great environmental importance as sources of subsurface water and often maintain very sensitive ecosystems. In recent years, increasing number of microbiological studies focused on the bacterial communities of karst soils. In this study, diversity examinations on two distinct Hungarian karst areas, Aggtelek and Tapolca, were performed using parallel cultivation and molecular cloning methods. The phylogenetic affiliation of bacterial strains and molecular clones was determined based on their 16S rRNA gene sequences. Bacterial isolates were identified as members of the phyla Actinobacteria, Firmicutes, Proteobacteria, and Bacteroidetes. Besides the taxa identified by cultivation, members of the phyla Chloroflexi, Cyanobacteria, Acidobacteria, Verrucomicrobia, and Gemmatimona- detes were detected by the cloning. The difference in the composition of soil bacterial communities was related to geographic locations and soil types. Both the highest and the lowest bacterial diversities were detected in samples from Aggtelek National Park, characterized by Leptic Luvisol and Rendzic Leptosol soil types. -
Rendzina) on Littoral Plains and Hilly Areas, 2- Hydromorphic Black Soil
Genesis and Evolution of Black Soil in the Eastern Mediterranean Hussam HAG HUSEIN, Bernhard Lucke, Wahib Sahwan, and Rupert Bäumler EGU 2020 1 Soil fertility degradation in the Middle East…myth or reality? The environmental history of the Middle East is not an issue of a fertile land becoming desert. Most of it is desert and it always has been. The precious rain from the Mediterranean falls for 100 km or so from the coast, creating some fertile areas, as isolated islands that were not desert and they still are not. www.google.com However, whatever the definition is used, there is quite a lot of desert impact in the equation (evaporation, aeolian dust). The Eastern Mediterranean Located in the eastern corner of the Mediterranean Sea Submitted to Mediterranean climate condition with meld wet winter and hot dry summer The soil is red Mediterranean (terra rossa) with red color and poor of organic carbon and high of carbonates www.google.com 3 Black Soil in the Eastern Mediterranean The occurrence of such soil is occasionally in Mediterranean because of the climate condition with xeric moisture and thermic temperature soil regimes, which is not favorited for forming and developing such kind of soil However, it is still occurring at a less extending in different climatic zones from xeric to aridic and called SAWDA’A Their current occurrence rise many questions about the conditions of formation and type of paleoclimate that prevailed Theories on their formation in the Mediterranean region are not in general agreement The black soil was studied at five bio-climate areas according to Pluvio- thermic Equation of Emberger (1955): Upper humid Cold, lower sub-humid Fresh and temperate Upper semiarid www.google.com Martials and Methods These areas submitted to meditteranian climate, frish winter, hot dry summer with annual precipitation from 200 to more than 1000 mm The soil moisture regime is xeric and the temperature soil regime is thermic Climax vegetation is -Pinus brutia forest; -maquis mainly Quercus in wet areas. -
Digital Soil Mapping Using Landscape Stratification for Arid Rangelands in the Eastern Great Basin, Central Utah
Utah State University DigitalCommons@USU All Graduate Theses and Dissertations Graduate Studies 5-2015 Digital Soil Mapping Using Landscape Stratification for Arid Rangelands in the Eastern Great Basin, Central Utah Brook B. Fonnesbeck Utah State University Follow this and additional works at: https://digitalcommons.usu.edu/etd Part of the Soil Science Commons Recommended Citation Fonnesbeck, Brook B., "Digital Soil Mapping Using Landscape Stratification for Arid Rangelands in the Eastern Great Basin, Central Utah" (2015). All Graduate Theses and Dissertations. 4525. https://digitalcommons.usu.edu/etd/4525 This Thesis is brought to you for free and open access by the Graduate Studies at DigitalCommons@USU. It has been accepted for inclusion in All Graduate Theses and Dissertations by an authorized administrator of DigitalCommons@USU. For more information, please contact [email protected]. DIGITAL SOIL MAPPING USING LANDSCAPE STRATIFICATION FOR ARID RANGELANDS IN THE EASTERN GREAT BASIN, CENTRAL UTAH by Brook B. Fonnesbeck A thesis submitted in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE in Soil Science Approved: _____________________________ _____________________________ Dr. Janis L. Boettinger Dr. Joel L. Pederson Major Professor Committee Member _____________________________ _____________________________ Dr. R Douglas Ramsey Dr. Mark R. McLellan Committee Member Dean of the School of Graduate Studies UTAH STATE UNIVERSITY Logan, Utah 2015 ii Copyright © Brook B. Fonnesbeck 2015 iii ABSTRACT Digital Soil Mapping Using Landscape Stratification for Arid Rangelands in the Eastern Great Basin, Central Utah by Brook B. Fonnesbeck, Master of Science Utah State University, 2015 Major Professor: Dr. Janis L. Boettinger Department: Plants, Soils and Climate Digital soil mapping typically involves inputs of digital elevation models, remotely sensed imagery, and other spatially explicit digital data as environmental covariates to predict soil classes and attributes over a landscape using statistical models.