DOCSLIB.ORG

THE EUROPEAN SOIL INFORMATION SYSTEM Region and Their Incorporation in the European Soil Information System (EUSIS)

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
THE EUROPEAN SOIL INFORMATION SYSTEM Region and Their Incorporation in the European Soil Information System (EUSIS) 91 World Soil Resources Reports 91 ISSN 0532-0488 This document contains the proceedings of a technical consultation on the soil resources information systems developed in the various countries in the European THE EUROPEAN SOIL INFORMATION SYSTEM region and their incorporation in the European Soil Information System (EUSIS). A summary report of technical discussions, conclusions and recommendations and THE EUROPEAN SOIL individual country reports are included. INFORMATION SYSTEM EUROPEAN SOIL BUREAU EUROPEAN COMMISSION Food and Agriculture Organization O of the United Nations FAO Untitled-1 1 7/17/02, 9:54 AM World Soil Resources Reports 91 THE EUROPEAN SOIL INFORMATION SYSTEM Proceedings of a Technical Consultation Rome, Italy, 2-3 September 1999 Sponsored by FAO and the European Commission FOOD AND AGRICULTURE ORGANIZATION OF THE UNITED NATIONS Rome, 2000 The designations employed and the presentation of the material in this publication do not imply the expression of any opinion whatsoever on the part of the Food and Agriculture Organization of the United Nations concerning the legal status of any country, territory, city or area or of its authorities, or concerning the delimitation of its frontiers or boundaries. ISBN 92-5-104454-6 All rights reserved. Reproduction and dissemination of material in this information product for educational or other non-commercial purposes are authorized without any prior written permission from the copyright holders provided the source is fully acknowledged. Reproduction of material in this information product for resale or other commercial purposes is prohibited without written permission of the copyright holders. Applications for such permission should be addressed to the Chief, Publishing and Multimedia Service, Information Division, FAO, Viale delle Terme di Caracalla, 00100 Rome, Italy or by e-mail to [email protected] © FAO 1999 Preface Soil information has been collected by individual countries for over 100 years, by FAO internationally for nearly 50 years and by the European Union for almost as long. Soil science, soil classification and taxonomy, and information technology have developed enormously over that time. Even more important, the perceived problems for which soil information is an essential knowledge base, and the uses to which it is put, have also changed greatly (and are continually changing). Briefly stated, the original scientific interest in soils and plant growth for commercial crop production has now been joined by numerous concerns of environmental protection, pollution control, carbon sequestration to limit climate change, organic farming and other aspects of multipurpose land use. Thus, the need for an easily accessible and standardized database of soil information at a scale and detail of information adequate for the requirements of the European countries became apparent and has been partially met in past years. The European Soils Bureau, established in 1996, is now able to consolidate the progress made in establishing and using an improved database. Proposals for this technical consultation were established following the 21st FAO Regional Conference for Europe in 1998. Attention was drawn to the actual and potential problems of soil degradation, including erosion in many areas, substantial loss of topsoil and loss of good agricultural land to urbanisation and pollution. There was general agreement on the importance of adequate soil information in the prevention of soil degradation and to facilitate crop forecasting. It was noted that the importance of the issues was recognized in the World Soil Charter of FAO and in the European Soil Charter. The Conference, noting FAO activities in developing a world soil and terrain database (SOTER), accepted a proposal by the EU presidency that it should invite the European Commission to examine the possibility of financing the extension of the existing European Soil Information System (EUSIS) to incorporate information from all countries that are entitled to attend the Conference. Various issues that needed to be addressed were noted. This Technical Consultation, convened to consider the issues related to soils information systems in Europe, was jointly organized by FAO and the European Commission with the technical support of the FAO Land and Water Development Division. Given the technical nature of the consultation, the participants were experts in the field of soil information. They made brief oral statements on the status of soil information in their respective countries (more detailed country reports are included in these proceedings). Success in sharing information to mutual benefit depends primarily on an agreement to interface the mapping, monitoring and research activities of the various national and sub-national soils institutions in Europe. Data must be readily available across borders, though not necessarily cost-free: the vast accumulation of data represents a huge investment of scientific effort and money so the copyright holders may not be willing to have it disseminated freely without any return to them and without their control of how it is used. Secondly, success depends on a willingness to harmonize the concepts underlying mapping scales, procedures and classification and then interpretation for solving problems or operating programmes concerning environmental, agricultural or other policies. iv The purpose of the meeting was not merely to promote the establishment of a European Soil Information System permitting easy inter-European exchange of data and experience, valuable though that is, but also to facilitate its practical use to solve problems both national and continental, and encourage exchange of experience with such activities. An important by-product would be the example to other countries, particularly those in the developing world, on how well-utilized soil information can help to solve national and global problems in a rational and cost-effective manner. Practically all countries in the world today have soil resource databases and soil specialists, due to the long-continued development work of FAO, and other aid agencies, and to the intellectual contributions of scientific institutions such as the IUSS and ISRIC. Reaping the full potential harvest from this past work requires continuing international contributions of ideas and in some cases finance. The exchange of views and the fuller understanding of the needs and potential contributions of each of the countries that resulted from this consultation will facilitate Europe-wide cooperation in the future. The conclusions and recommendations set some priorities for immediate and longer term action. European Soil Information System v Contents SUMMARY REPORT, CONCLUSIONS AND RECOMMENDATIONS 1 Attendance 1 Opening of the Technical Consultation 2 Country Papers 2 Technical Discussions 2 Use of the information 5 Conclusions and Recommendations 5 KEYNOTE PAPERS 7 The Global Soil and Terrain Database and the European Soil Information System 9 The European Soil Information System 19 COUNTRY PAPERS 29 Some aspects of land information in Albaia 31 The status of soil mapping in Austria 35 Rapport sur l’état de l’information sur les sols en Belgique 39 Soil mapping in Bosnia and Herzegovina 43 The status of soil mapping in Cyprus 49 The status of soil mapping in the Czech Republic 61 The status of soil mapping in Finland 67 Knowledge and monitoring of soil resources in France 71 Soil information in Germany: the 1999 position 81 Soil databases and their use in Hungary 87 Advances in soil survey, monitoring and applications in Italy 97 The status of soil mapping in Lithuania 103 The status of soil mapping in the Maltese Islands 107 Information on soil mapping in Poland 111 The status of soil mapping in Romania 115 The status of soil mapping in Slovakia 119 Digital data on soils and environment in Slovenia for establishing a soil information system 123 Rapport national de la Suisse 127 The soil information system of Turkey 133 The status of soil mapping in the United Kingdom 137 ANNEX 1 OPENING ADDRESS 143 ANNEX 2 PROGRAMME 145 ANNEX 3 LIST OF PARTICIPANTS 147 vi Acknowledgements The support of the European Commission and the European Soil Bureau for this meeting hosted by FAO is gratefully acknowledged. Particular thanks are due to J. Meyer Roux and Luca Montanarella for their contributions in the discussions. The technical reports provided by the representatives of the particular countries are highly appreciated (see list of participants, Annex 3). Acknowledgement is also due to M Lindau, FAO Regional Representative for Europe, J. Meyer Roux, Deputy Director, SAI, JRC and H. Wolter, Director of the Land and Water Development Division, FAO, for their support and inspirational opening addresses. The contributions of R. Dudal, Professor Emeritus, W. G. Sombroek and N. Blum, Secretary General of the International Union of Soil Science, who expertly chaired the sessions, are gratefully acknowledged. Special thanks are due to F.O. Nachtergaele (AGLL/FAO) and Ms D. Moro, Regional Office for Europe (FAO) for the organization of the meeting and to M. F. Purnell (FAO Consultant), Ms S. Vrionides (FAO) and Ms C. Smith Redfern (FAO) for the compilation, review and editing of these proceedings. European Soil Information System vii Acronyms AGROTOPO Agrotopographical Database ARIS-unit Agriculture and Regional Information System Unit (EU) B&H Bosnia and Herzegovina CIS Commonwealth of Independent States (Russia) CNRS National Centre for Scientific Research, Universities
Load more

Recommended publications
  • T.C. Selçuk Ünġversġtesġ Fen Bġlġmlerġ Enstġtüsü Tuzlu
    T.C. SELÇUK ÜNĠVERSĠTESĠ FEN BĠLĠMLERĠ ENSTĠTÜSÜ TUZLU TOPRAKLARDA KATALAZ ENZĠMĠNĠN AKTĠVĠTESĠ VE KĠNETĠĞĠ Emine YILDIRIM YÜKSEK LĠSANS TEZĠ TOPRAK BĠLĠMĠ VE BĠTKĠ BESLEME ANABĠLĠM DALI KONYA, 2010 ÖZET YÜKSEK LĠSANS TEZĠ TUZLU TOPRAKLARDA KATALAZ ENZĠMĠNĠN AKTĠVĠTESĠ VE KĠNETĠĞĠ Emine YILDIRIM Selçuk Üniversitesi Fen Bilimleri Enstitüsü Toprak Bilimi ve Bitki Besleme Anabilim Dalı DanıĢman: Yrd. Doç. Dr. Fariz MĠKAĠLSOY 2010, Sayfa: 72 Jüri: Yrd. Doç. Dr. Fariz MĠKAĠLSOY Prof. Dr. Nizamettin ÇĠFTÇĠ Doç. Dr. Refik UYANÖZ Bu araĢtırmada, Tuz gölü çevresi tarım dıĢı arazilerden alınan 3 toprak örneğinde çalıĢılmıĢtır. Gazometrik metod kullanılarak katalaz enziminin aktivitesi tayin edilerek kinetik parametreleri hesaplanmıĢtır. Fiziksel, kimyasal özellikleri ve % tuz oranı farklı toprakların katalaz enzim analizi 20+1 oC laboratuar koĢullarında değiĢik substrat konsantrasyonlarda (% 3, % 6, % 9, % 12, % 15, % 18, %2 1, % 24, % 27, % 30 H2O2) yürütülmüĢtür. Bu analizde ürün olarak açığa çıkan O2‟nin zamana göre değiĢimi (20, 40, 60, 80,….300 sn) kararlı hale gelmesine kadar devam edilmiĢtir. Katalaz enzim aktivitesi (υ) ve kinetik parametreleri (υ0, Vmax ve Km) her toprak için ayrı ayrı yapılmıĢtır. Sonuçlara göre, tuz konsantrasyonu yüksek toprakta katalaz enziminin kinetik parametresi olan Km‟nin değeri yüksek bulunmuĢtur. Vmax değeri ise en düĢük olarak bulunmuĢtur. Ayrıca reaksiyon hızının % 24 substrat konsantrasyonunda artıĢ gösterdiği ve daha sonra değiĢmediği tesbit edildi. Bu metod toprakta katalaz enzim aktivitesinin tesbitinde kullanılabilir. Anahtar Kelimeler: Toprak, enzim aktivitesi, katalaz, kinetik parametreler, tuz i ABSTRACT MASTER THESĠS ACTIVITY AND KINETICS OF CATALASE ENZYME IN SALINE SOILS Emine YILDIRIM Selçuk University Graduate School of Natural and Applied Sciences Department of Soil Science and Plant Nutrition Supervisor: Yrd. Doç.
    [Show full text]
  • Land Suitability Evaluation Using Gis for Vegetable Crops in Kathmandu Valley /Nepal
    LAND SUITABILITY EVALUATION USING GIS FOR VEGETABLE CROPS IN KATHMANDU VALLEY /NEPAL Dissertation zur Erlangung des akademischen Grades Doctor rerum agriculturarum (Dr.rer.agr.) eingereicht an der Landwirtschaftlich-Gärtnerischen Fakultät der Humboldt-Universität zu Berlin von M.Sc. Nabarath Baniya geboren am 01.12.1969 in Kathmandu, Nepal dem Präsident der Humboldt-Universität zu Berlin Prof. Dr. Christoph Markschies Dekan der Landwirtschaftlich-Gärtnerischen Fakultät Prof. Dr. Dr. N.c. Otto Kaufmann Gutachter: Prof. Dr. sc Drs. h. c. Michael H. Böhme Dr. rer. agr. Michael La Rosa Perez Berlin, 13. Oktober 2008 Dedication To my parents, Udaya Bahadur Baniya and Til Kumari Baniya, who would have appreciated seeing it if they were still alive. II ACKNOWLEDGEMENT I wish to express my gratitude to all those who have given me assistance, help and support during the completion of my PhD in Faculty of Agriculture and Horticulture, Institute of Horticultural Sciences, Humboldt University of Berlin. I acknowledge a deep sense of gratitude to Prof. Dr. Michael Böhme my supervisor, who had always spread his helping hands during my PhD study periods, and given me guidance, valuable suggestion, critical comments and kindness during and completion of present work. His innovative research ideas kind patient and effective guidance throughout my work need not to be exaggerated. This thesis would never be accomplished in this shape without his selfless contributions in various aspects. I am very happy to state that I got to learn a lot from his experience in field of horticulture science. I gratefully acknowledge Dr. rer. agr. Michael La Rosa Perez, LGF, WISOLA, for guiding me on analytical aspect of the present dissertation.
    [Show full text]
  • An Introduction SOIL CLASSIFICATION
    Ngogo Mn. Ge:140 @2019 SOIL CLASSIFICATION An Introduction SAUT; Geography Dept Ngogo Mn. Ge:140 @2019 Introduction • Classification of soil is the separation of soil into classes or groups each having similar characteristics and potentially similar behaviour. • The criteria for grouping soils depend on the purposes of classification. • Soil is not uniformly distributed. Properties of soil vary due to several soil forming factors. properties vary very widely. Soil types are many. To identify, understand, and manage soils, soil scientists have developed a set of soil classification or taxonomy systems. SAUT; Geography Dept Ngogo Mn. Ge:140 @2019 Methods of Soil Classification Systems • Systems which use the properties of the soils are called TAXONOMIC SYSTEMS OF CLASSIFICATION. • Systems that employ soil usage are called CAPABILITY CLASSIFICATION. • Though these systems are considered to be subjective or utilitarian system of classification. • International soil classification are primarily for use by soil specialists. SAUT; Geography Dept Ngogo Mn. Ge:140 @2019 Soil Classification Used in the Tropics I. The FAO/UNESCO soil map of the world (FAO/UNESCO, 1977) II. The New Comprehensive Classification System or US Soil Taxonomy Classification (Soil-Survey Staff, 1975) III. The French Classification System (Aubert (1964) SAUT; Geography Dept Ngogo Mn. Ge:140 @2019 FAO Soil Classification System • In 1977 FAO/UNESCO published the first soil map with a uniform classification throughout. • The World Soil Map is not based on any one system, but rather, a collection of national soil maps influenced by US System. • In the FAO system, the soils that occur in a particular region and exhibit a certain relationship to one another are grouped in association or “ major soil Units” SAUT; Geography Dept Ngogo Mn.
    [Show full text]
  • Classification of Soil Magnetic Susceptibility and Prediction of Metal Detector Performance – Case Study of Angola
    Classification of soil magnetic susceptibility and prediction of metal detector performance – case study of Angola Holger Preetz*a, Sven Altfelderb, Volker Henningsb, Jan Igela aLeibniz Institute for Applied Geophysics, Stilleweg 2, D-30655 Hannover, Germany bFederal Institute for Geosciences and Natural Resources, Stilleweg 2, D-30655 Hannover, Germany Abstract Soil magnetic properties can seriously impede the performance of metal detectors used in landmine clearance operations. For a proper planning of clearance operations pre-existing information on soil magnetic susceptibility can be helpful. In this study we briefly introduce a classification system to assess soil magnetic susceptibilities from geoscientific maps. The classification system is based on susceptibility measurements conducted on archived lateritic soil samples from 15 tropical countries. The system is applied to a soil map of Angola, resulting in a map that depicts soil magnetic susceptibilities as a worst case scenario. An additional layer depicting the surveyed mine affected communities in Angola is added to the map, which demonstrates that a large number of those are located in areas where soil is expected to impede metal detector performance severely. Keywords: Angola, soils, soil classification, magnetic susceptibility, metal detector, landmine detection 1. INTRODUCTION Angola is one of more than 75 countries worldwide affected by landmines and/or unexploded ordnance (UXO). Many of these countries are located in the tropics and Angola belongs to the most contaminated places1. The country suffered from a long lasting civil war which began with its independence from Portugal in 1975 and ended in 2002. It is estimated that 500,000 to 1 million landmines remain as a legacy of the armed conflict and still represent a deadly hazard to large parts of the civil population.
    [Show full text]
  • Global Status, Processes and Trends in Soil Erosion
    Status of the World’s Main Report Soil Resources Chapter 6 Global soil status, processes and trends © FAO | Giuseppe Bizzarri © FAO INTERGOVERNMENTAL TECHNICAL PANEL ON SOILS Disclaimer and copyright Recommended citation: FAO and ITPS. 2015. Status of the World’s Soil Resources (SWSR) – Main Report. Food and Agriculture Organization of the United Nations and Intergovernmental Technical Panel on Soils, Rome, Italy 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. ISBN 978-92-5-109004-6 © FAO, 2015 FAO encourages the use, reproduction and dissemination of material in this information product. Except where otherwise indicated, material may be copied, downloaded and printed for private study, research and teaching purposes, or for use in non-commercial products or services, provided that appropriate acknowledgement of FAO as the source and copyright holder is given and that FAO’s endorsement of users’ views, products or services is not implied in any way.
    [Show full text]
  • Construction of an Yucatec Maya Soil Classification and Comparison with the WRB Framework Francisco Bautista1*†, J Alfred Zinck2†
    Bautista and Zinck Journal of Ethnobiology and Ethnomedicine 2010, 6:7 http://www.ethnobiomed.com/content/6/1/7 JOURNAL OF ETHNOBIOLOGY AND ETHNOMEDICINE RESEARCH Open Access Construction of an Yucatec Maya soil classification and comparison with the WRB framework Francisco Bautista1*†, J Alfred Zinck2† Abstract Background: Mayas living in southeast Mexico have used soils for millennia and provide thus a good example for understanding soil-culture relationships and for exploring the ways indigenous people name and classify the soils of their territory. This paper shows an attempt to organize the Maya soil knowledge into a soil classification scheme and compares the latter with the World Reference Base for Soil Resources (WRB). Methods: Several participative soil surveys were carried out in the period 2000-2009 with the help of bilingual Maya-Spanish-speaking farmers. A multilingual soil database was built with 315 soil profile descriptions. Results: On the basis of the diagnostic soil properties and the soil nomenclature used by Maya farmers, a soil classification scheme with a hierarchic, dichotomous and open structure was constructed, organized in groups and qualifiers in a fashion similar to that of the WRB system. Maya soil properties were used at the same categorical levels as similar diagnostic properties are used in the WRB system. Conclusions: The Maya soil classification (MSC) is a natural system based on key properties, such as relief position, rock types, size and quantity of stones, color of topsoil and subsoil, depth, water dynamics, and plant-supporting processes. The MSC addresses the soil properties of surficial and subsurficial horizons, and uses plant communities as qualifier in some cases.
    [Show full text]
  • Experimental and Observational Studies Find Contrasting Responses
    RESEARCH ARTICLE Experimental and observational studies find contrasting responses of soil nutrients to climate change ZY Yuan1,2*†, F Jiao1,2*†, XR Shi1,2, Jordi Sardans3,4, Fernando T Maestre5, Manuel Delgado-Baquerizo5,6, Peter B Reich7,8, Josep Pen˜ uelas3,4 1State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Institute of Soil and Water Conservation, Northwest A&F University, Yangling, China; 2Institute of Soil and Water Conservation, Chinese Academy of Science and Ministry of Water Resource, Yangling, China; 3Global Ecology Unit CREAF-CSIC- UAB, Consejo Superior de Investigaciones Cientı´ficas (CSIC), Bellaterra, Spain; 4CREAF, Cerdanyola del Valle`s, Spain; 5Departamento de Biologı´a y Geologı´a, Fı´sica y Quı´mica Inorga´nica, Universidad Rey Juan Carlos, Mo´stoles, Spain; 6Cooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, Colorado; 7Hawkesbury Institute for the Environment, University of Western Sydney, Penrith, Australia; 8Department of Forest Resources, University of Minnesota, Minnesota, United States Abstract Manipulative experiments and observations along environmental gradients, the two most common approaches to evaluate the impacts of climate change on nutrient cycling, are generally assumed to produce similar results, but this assumption has rarely been tested. We did *For correspondence: zyyuan@ so by conducting a meta-analysis and found that soil nutrients responded differentially to drivers of ms.iswc.ac.cn (ZYY); [email protected]. climate change depending on the approach considered. Soil carbon, nitrogen, and phosphorus ac.cn (FJ) concentrations generally decreased with water addition in manipulative experiments but increased †These authors contributed with annual precipitation along environmental gradients.
    [Show full text]
  • Soil Profile Carbon and Nitrogen in Prairie, Perennial Grass–Legume
    Agriculture, Ecosystems and Environment 181 (2013) 179–187 Contents lists available at ScienceDirect Agriculture, Ecosystems and Environment jo urnal homepage: www.elsevier.com/locate/agee Soil profile carbon and nitrogen in prairie, perennial grass–legume mixture and wheat-fallow production in the central High Plains, USA a,∗ a b Tunsisa T. Hurisso , Jay B. Norton , Urszula Norton a Department of Ecosystem Science and Management, University of Wyoming, 1000 E. University Avenue, Laramie, WY 82071, USA b Department of Plant Sciences, University of Wyoming, 1000 E. University Avenue, Laramie, WY 82071, USA a r t a b i s c l e i n f o t r a c t Article history: Conversion of native prairie land for agricultural production has resulted in significant loss and redis- Received 23 June 2013 tribution of soil organic matter (SOM) in the soil profile ultimately leading to declining soil fertility in Received in revised form a low-productivity semiarid agroecosystem. Improved understanding of such losses can lead to devel- 14 September 2013 opment of sustainable land management practices that maintain soil fertility and enhance soil quality. Accepted 7 October 2013 This study was conducted to determine whether conservation practices impact soil profile carbon (C) and nitrogen (N) accumulation in central High Plains. Soil samples were taken at four-depth increments Keywords: to 1.2 m in July of 2011 from five unfertilized fields under long-term management with varying degrees Prairie sequestration of soil disturbance: (1) historic wheat (Triticum aestivum)-fallow
    [Show full text]
  • A Review of Libyan Soil Databases for Use Within an Ecosystem Services Framework
    Land 2019, 8, 82 1 of 31 Review A Review of Libyan Soil Databases for Use within an Ecosystem Services Framework Hamdi A. Zurqani 1,2, Elena A. Mikhailova 1,*, Christopher J. Post 1, Mark A. Schlautman 3 and Azzeddin R. Elhawej 2 1 Department of Forestry and Environmental Conservation, Clemson University, Clemson, SC 29634, USA; [email protected] (H.A.Z.); [email protected] (C.J.P.) 2 Department of Soil and Water Sciences, University of Tripoli, Tripoli 13538, Libya; [email protected] 3 Department of Environmental Engineering and Earth Sciences, Clemson University, Anderson, SC 29625, USA; [email protected] * Correspondence: [email protected]; Tel.: 864-656-3535 Received: 25 February 2019; Accepted: 15 May 2019; Published: 18 May 2019 Abstract: Ecosystem services (ESs) are increasingly being used by many countries around the world as a framework for addressing the United Nations (UN) Sustainable Development Goals (SDGs). This review article of the usability of Libyan soil databases for ESs and SDGs is the first of its kind for North Africa. The objectives of the article are to: describe the available soil resources of Libya in relation to an ES framework; provide examples of the usability of Libyan soil databases for ES applications (e.g., provisioning, Healthy Eating Plate), and describe some of the typical disservices in the country. Desertification, salinization, and limited freshwater resources are the largest challenges (disservices) for agriculture and future development in Libya. Seawater intrusion in coastal areas due to rising sea levels has resulted in high concentrations of salts in irrigation waters, which can lead to low soil productivity.
    [Show full text]
  • Software for Agroclimatic Data Management
    Software for Agroclimatic Data Management Proceedings of an Expert Group Meeting October 16-20, 2000, Washington D.C., USA Editors Raymond P. Motha M.V.K. Sivakumar Sponsors United States Department of Agriculture Office of the Chief Economist World Agricultural Outlook Board Washington D.C. 20250, USA World Meteorological Organization Agricultural Meteorology Division 7bis, A venue de la Paix 1211 Geneva 2, Switzerland Series WAOB-2001-2 AGM-4 WMO/TD No. 1075 Washington, D.C. 20250 October 2001 Proper citation is requested. Citation: Raymond P. Motha and M.V.K. Sivakumar (Eds.). 2001. Software for Agroclimatic Data Management, Proceedings of an Expert Group Meeting, October 16-20,2000, Washington D.C., USA. Washington D.C., USA: United States Department of Agriculture and Geneva, Switzerland: World Meteorological Organization. Staff Report WAOB-2001-2. 194 pp. About the Editors Raymond P. Motha Chief Meteorologist World Agricultural Outlook Board Mail Stop 3812 United States Department of Agriculture Washington D.C., 20250-3812 USA M.V.K. Sivakumar Chief Agricultural Meteorology Division World Meteorological Organization 1211 Geneva 2, Switzerland The views expressed in these proceedings are those of the authors, not necessarily those of the sponsors. Maps are reproduced as submitted by the authors; they are not intended to show political boundaries and the sponsors hold no responsibility whatsoever in this regard. Table of Contents Foreword.........................................................................................................................................
    [Show full text]
  • Bachelor in Forestry and Natural Environment Engineering Course Information Year 2019-2020
    Bachelor in Forestry and Natural Environment Engineering Course information Year 2019-2020 GENERAL SPECIFICATIONS English name Earth Sciences Spanish name Ciencias del Medio Físico Code Type 606510107 Foundational Time distribution Total In class Out class Working hours 150 60 90 ECTS: 6 Standard group Small groups Computer Classroom Lab Practices classroom 3.5 2.0 0.5 0 Departments Knowledge areas Agroforestry Sciences Environment Technology Year Semester 1st 2nd TEACHING STAFF Name E-Mail Telephone Office Javier Vázquez Piqué [email protected] 959217531 Saltés-19, La Rábida Campus SPECIFIC INFORMATION OF THE COURSE 1. Contents description 1.1. In English: The earth and its components. Earth dinamics. Geomorphology and external geological processes. Minerals and rocks important for soils. Applied metheorology and Climatology. Applied forest soils 1.2. In Spanish La tierra y sus materiales. Dinámica terrestre. Geomorfología y procesos geológicos externos. Minerales y rocas de importancia edafológica. Meteorología y Climatología aplicada. Edafología aplicada y suelos forestales 2. Background 2.1.Situation within the Degree: Earth Sciences is a subject destined to provide the basic knowledge about the soil and the climate of application in subjects that are developed in higher courses of the degree such as "Forest Ecology", "Forestry", "Forest botany, Dendrology" or " Hydrology and Hydrological Forest Restoration "among others 2.2. Recommendations: It is recommended that the students come from the scientific-technological baccalaureate or that they access from the more affinity Higher Level Training Cycles and have studied the subject of "Chemistry and Biochemistry" in the first semester of the course 3. Objectives (as result of teaching): The general objective of the subject is that students acquire basic knowledge about the physical environment that will serve as application for later disciplines of the degree and for the performance of the profession of forest engineer.
    [Show full text]
  • The Soil Texture Wizard: R Functions for Plotting, Classifying, Transforming and Exploring Soil Texture Data
    The soil texture wizard: R functions for plotting, classifying, transforming and exploring soil texture data Julien Moeys March 8, 2012 ● 10 90 20 80 30 m 70 µ 0−2 Cl 40 60 Clay %] [ [ % 50 ] Silt 50 2 − SiCl 50 60 µ SaCl m 40 ClLo SiClLo 70 30 SaClLo 80 20 Lo ● SiLo 90 10 SaLo LoSa Si Sa 90 80 70 60 50 40 30 20 10 [%] Sand 50−2000 µm ● 1 Contents 1 About this document 4 1.1 Whycreating’Thesoiltexturewizard’? . 4 1.2 AboutR................................ 4 1.3 About the author . 4 1.4 CreditsandLicense.......................... 5 2 Introduction: About soil texture, texture triangles and texture classifications 5 2.1 What are soil granulometry and soil texture(s)? . 5 2.2 What are soil texture triangle and classes . 8 3 Installing the package 10 3.1 Installing the package from r-forge . 10 4 Plotting soil texture triangles and classification systems 11 4.1 An empty soil texture triangle . 11 4.2 The USDA soil texture classification . 12 4.3 The FAO soil texture classification (also known as ’European Soil map’, or ’HYPRES’) . 15 4.4 The French ’Aisne’ soil texture classification . 17 4.5 The French ’GEPPA’ soil texture classification . 19 4.6 The German Bodenartendiagramm (B.K. 1994) soil texture clas- sification................................ 21 4.7 The German ’Standortserkundungsanweisung’ (SEA 1974) soil texture classification for forest soils . 23 4.8 The German ’landwirtschaftliche B¨oden’ (TGL 24300-05, 1985) soil texture classification for arable soils . 25 4.9 UK Soil Survey of England and Wales texture classification .
    [Show full text]