To Assess the Response of Organo-Mineral Soils to Changes
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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. -
General Soil Map of Ireland, 1969 Survey of Some Midland Sub-Peat Mineral Soils (With Bord Na Móna), 1971 — M
SOIL SURVEY PUBLICATIONS 1962-1979 County Surveys Soils of Co. Wexford, 1964* — M. J. Gardiner and P. Ryan Soils of Co. Limerick, 1966 — T. F. Finch and P. Ryan Soils of Co. Carlow, 1967 — M. J. Conry and P. Ryan Soils of Co. Kildare, 1970 — M. J. Conry, R. F. Hammond and T. O’Shea Soils of Co. Clare, 1971 — T. F. Finch, E. Culleton and S. Diamond Soils of Co. Westmeath, 1977 — T. F. Finch and M. J. Gardiner Soils of West Cork, (part of Resource Survey) 1963 — M. J. Conry, P. Ryan and J. Lee Soils of West Donegal, (part of Resource Survey) 1969 — M. Walsh, M. Ryan and S van de Schaaf Soils of Co. Leitrim, (part of Resource Survey) 1973 — M. Walsh An Foras Talúntais Farms Grange, Co. Meath, 1962 — M. J. Gardiner Kinsealy, Co. Dublin, 1963 — M. J. Gardiner Creagh, Co. Mayo, 1963 — M. J. Gardiner Herbertstown, Co. Limerick, 1964 — T. F. Finch Drumboylan, Co. Roscommon, 1968 — G. Jaritz and J. Lee Ballintubber, Co. Roscommon, 1969 — M. Ryan and J. Lee Ballinamore, Co. Leitrim, 1969 — T. F. Finch and J. Lee Clonroche, Co. Wexford, 1970 — T. F. Finch and M. J. Gardiner Mullinahone, Co. Tipperary, 1970 — M. J. Conry Ballygagin, Co. Waterford, 1972 — T. F. Finch and M. J. Gardiner Department of Agriculture Farms Clonakilty, Co. Cork, 1964* — J. Lee and M. J. Conry Ballyhaise, Co. Cavan, 1965* — M. Ryan and J. Lee Athenry, Co. Galway, 1965* — S. Diamond, M. Ryan and M. J. Gardiner Other Farms Kells Ingram, Co. Louth, 1964* — M. J. Gardiner Multyfarnham Agricultural College, Co. -
The Soils of Ireland by PIERCE RYAN, B.Agr.Sc., M.Sc
46 Irish Forestry driven ploughs, rotovators and seed sowers and chemical sprayers and dusters~al1 new to the scene. The Society has served its members well during those years of rapid change and development. It has by means of lectures, field trips and study tours kept members up-to-date with developments. The Society has welcomed and introduced new ideas ·and new techniques. The elected officers have given splendid service to the adv.ancement of forestry in general and the Society in particular. As to the future, I hope and pray and confidently expect that the next twenty-one years will be at least as fruitful for our Society and for Irish forestry as the period under review. The Soils of Ireland By PIERCE RYAN, B.Agr.Sc., M.Sc. , Head, National Soil Survey, .o.n fOR<\S "C<\ltl1nc<\s . Soil Formation SOIL formation is the process by which geological parent materials subjected to the action of natural forces and living organisms are transformed over tirrie into soils. In the course of the transformation various chemical, physical and biological changes take place so that the end-product, the soil, is a completely different natural body from the parent material. The nature of the parent materials and the environ mental conditions involved are largely responsible for the character of the resultant soil. Five major genetic factors namely, parent material, climate, relief, vegetation and time are usually associated with soil form ing processes and man's influence in modifying these natural processes cannot be discounted. The interaction of these factors and the relative impact of each, determine the nature and intensity of the processes by which the inert parent material is developed into a dynamic soil and the character of that soil. -
FAO-UNESCO Soil Map of the World, 1:5000000 Vol. 1. Legend
FAO-Unesco Soilmap of the world Volume I Legend FAO-Unesco Soil map of the world 1: 5 000 000 Volume I Legend FAO-Unesco Soil map of the world Volume I Legend Volume II North America Volume III Mexico and Central America Volume IV South America Volume V Europe Volume VI Africa Volume VII South Asia Volutne VIII North and Central Asia Volume IX Southeast Asia Volume X Australasia FOOD AND AGRICULTURE ORGANIZATION OF THE UNITED NATIONS NHCO UNILLD NATIONS EDUCATIONAL, SCIENTIFIC AND CULTURAL ORGANIZATION FAO-Unesco Soilmap of the world 1: 5 000 000 Volume I Legend Prepared by the Food and Agriculture Organization of the United Nations Unesco-Paris 1974 Printed by Tipolitografia F. Failli, Rome for the Food and Agriculture Organization of the United Nations and the United Nations Educational, Scientific and Cultural Organization Published in 1974 by the United Nations Educational, Scientific and Cultural Organization Place de Fontenoy, 75700 Paris (I) FAO/Unesco 1974 Printed in Italy ISBN 92 - 3- 101125 - 1 PREFACE The project for a joint FAo/Unesco Soil Map of the The present volume is the first of a set of ten which, World was undertaken following a recommendation with maps, make up the complete publication of of the International Society of Soil Science.It is the Soil Map of the World.This first volume re- the first attempt to prepare, on the basis of interna- cords introductory information and presents the defi- tional cooperation, a soil map covering all the conti- nitions of th.e elements of the legend which is used nents of the world in a uniform legend, thus enabling uniformly throughout the publication.Each of the the correlation of soii units and the comparison of nine following volumescontainsanexplanatory soils on a global scale.The project, which started text and soil maps covering one of the main regions in 1961, fills a gap in present knowledge of soils and of the world. -
Classifying Soil Classifyingagriculture and FO Odsoil DEVELOPMENT AUTHORITY
AGRICULTURE AND FOOD DEVELOPMENT AUTHORITY Classifying Soil ClassifyingAGRICULTURE AND FO ODSoil DEVELOPMENT AUTHORITY What is soil? to an engineer, it is a surface upon which houses and roads are built and the source of raw material. It also Blanket Peat When rock is exposed to a new environment – following lava flow, protects many of the archeological resources that are Lithosol Podzol sediment uplift, retreat of glaciers – soil begins to form. Physical and preserved in Ireland. The characteristics of a soil and how chemical weathering changes the rock, as do the actions of living they may be modified need to be known. In agriculture, one Brown Podzolic organisms. A soil eventually forms, which changes over time, as a result must know the type, quantity and quality of food that can be Groundwater AGRICULTURE AND FOOD DEVELOPMENT AUTHORITY of the rock type on which it is developed, the climate, the vegetation that Basin Peat produced on that soil. For habitat restoration, the suitability Brown Earth grows upon the soil, the organisms that lives in the soil and the topography of the soil for the original species should be known. Gley Luvisol (slope and aspect) on which the soil is found. Soil, air and water are three Builders need to know whether the land might subside or Alluvium Surface Water major factors affecting life on Earth. All three factors are strongly dependent be easily flooded. Gley Rendzina Teagasc is Ireland’s agricultural and food development upon each other. For example, soil cleans much of the water that passes authority supporting science based innovation in the agri-food through it to the groundwater and soil can act as a source or sink of carbon If the different types of soil can be classified in an efficient SANDSTONE and repeatable way, then soil characteristics are more sector and the wider bioeconomy. -
Potential Contribution of Soil Diversity and Abundance Metrics To
Potential contribution of soil diversity and abundance metrics to ANGOR UNIVERSITY identifying high nature value farmland (HNV) Jones, David Geoderma DOI: 10.1016/j.geoderma.2017.05.049 PRIFYSGOL BANGOR / B Published: 01/11/2017 Peer reviewed version Cyswllt i'r cyhoeddiad / Link to publication Dyfyniad o'r fersiwn a gyhoeddwyd / Citation for published version (APA): Jones, D. (2017). Potential contribution of soil diversity and abundance metrics to identifying high nature value farmland (HNV). Geoderma, 305, 417-432. https://doi.org/10.1016/j.geoderma.2017.05.049 Hawliau Cyffredinol / General rights Copyright and moral rights for the publications made accessible in the public portal are retained by the authors and/or other copyright owners and it is a condition of accessing publications that users recognise and abide by the legal requirements associated with these rights. • Users may download and print one copy of any publication from the public portal for the purpose of private study or research. • You may not further distribute the material or use it for any profit-making activity or commercial gain • You may freely distribute the URL identifying the publication in the public portal ? Take down policy If you believe that this document breaches copyright please contact us providing details, and we will remove access to the work immediately and investigate your claim. 09. Oct. 2020 Potential contribution of soil diversity and abundance metrics to identifying high nature value farmland (HNV) Maxwell, D.1, Robinson D.A.2, Thomas, A.2, Jackson, B.1, Maskell L.3, Jones, D.L.4, Emmett B.A.2 1 Victoria University of Wellington, Wellington, New Zealand 2 Centre for Ecology and Hydrology, Bangor, UK 3 Centre for Ecology and Hydrology, Lancaster, UK 4 School of Environment, Natural Resources and Geography, Bangor University, UK Abstract Identifying and halting the decline of High Nature Value farmland (HNV) is seen as essential to the EU meeting its 2020 biodiversity targets. -
Potential Contribution of Soil Diversity and Abundance Metrics To
Potential contribution of soil diversity and abundance metrics to ANGOR UNIVERSITY identifying high nature value farmland (HNV) Jones, David Geoderma DOI: 10.1016/j.geoderma.2017.05.049 PRIFYSGOL BANGOR / B Published: 01/11/2017 Peer reviewed version Cyswllt i'r cyhoeddiad / Link to publication Dyfyniad o'r fersiwn a gyhoeddwyd / Citation for published version (APA): Jones, D. (2017). Potential contribution of soil diversity and abundance metrics to identifying high nature value farmland (HNV). Geoderma, 305, 417-432. https://doi.org/10.1016/j.geoderma.2017.05.049 Hawliau Cyffredinol / General rights Copyright and moral rights for the publications made accessible in the public portal are retained by the authors and/or other copyright owners and it is a condition of accessing publications that users recognise and abide by the legal requirements associated with these rights. • Users may download and print one copy of any publication from the public portal for the purpose of private study or research. • You may not further distribute the material or use it for any profit-making activity or commercial gain • You may freely distribute the URL identifying the publication in the public portal ? Take down policy If you believe that this document breaches copyright please contact us providing details, and we will remove access to the work immediately and investigate your claim. 05. Oct. 2021 Potential contribution of soil diversity and abundance metrics to identifying high nature value farmland (HNV) Maxwell, D.1, Robinson D.A.2, Thomas, A.2, Jackson, B.1, Maskell L.3, Jones, D.L.4, Emmett B.A.2 1 Victoria University of Wellington, Wellington, New Zealand 2 Centre for Ecology and Hydrology, Bangor, UK 3 Centre for Ecology and Hydrology, Lancaster, UK 4 School of Environment, Natural Resources and Geography, Bangor University, UK Abstract Identifying and halting the decline of High Nature Value farmland (HNV) is seen as essential to the EU meeting its 2020 biodiversity targets. -
(2006) World Reference Base for Soil Resources
A0510E-Cover-A4-Pant 4725 [ConvePage 1 30-05-2006 12:03:10 ISSN 0532-0488 WORLD SOIL 103 RESOURCES 103 REPORTS WORLD SOIL RESOURCES REPORTS 103 World reference base W orld reference base for soil resources 2006 for soil resources 2006 A framework for international classification, World reference base correlation and communication for soil resources 2006 A framework for international classification, correlation and communication This publication is a revised and updated version of World Soil Resources Reports No. 84, a technical manual for soil C scientists and correlators, designed to facilitate the – A framework for international classification, correlation and communication M exchange of information and experience related to soil Y resources, their use and management. The document CM provides a framework for international soil classification and MY an agreed common scientific language to enhance communication across disciplines using soil information. It CY contains definitions and diagnostic criteria to recognize soil CMY horizons, properties and materials and gives rules and K guidelines for classifying and subdividing soil reference groups. ISBN 92-5-105511-4 ISSN 0532-0488 F 9 7 8 9 2 5 1 0 5 5 1 1 3 AO TC/M/A0510E/1/05.06/5200 International Union of Soil Sciences Cover photograph: Ferralsol (Ghana), Cryosol (Russian Federation), Solonetz (Hungary), Podzol (Austria), Phaeozem (United States of America), Lixisol (United Republic of Tanzania), Luvisol (Hungary). Compiled by Erika Micheli. Copies of FAO publications can be requested -
Podzols and Podzolization in Temperate Regions ISM Monograph 1 .>-• .....•• F
Podzols and podzolization in temperate regions ISM Monograph 1 .>-• .....•• f \:. Î / - ••* **«.- r ,-* 't 1 ISM Monograph 1 Podzols and podzolization in temperate regions D.L. Mokma1 and P. Buurman2 CENTRALE LANDBOUWCATALOGUS 0000 0006 7161 1 Department of Crop and Soil Sciences, Michigan State University, East Lansing, Michigan 2 Department of Soil Science and Geology, Agricultural University, Wageningen, The Netherlands International Soil Museum - Wageningen - The Netherlands bN •'. K'ijH CIP-gegevens Mokma,D.L . Podzols andpodzolizatio n intemperat e regions/D.L .Mokm aan dP .Buurman . Wageningen: International SoilMuseum . - 111.- (ISMmonograph ;1 ) Metlit .opg . ISBN90-6672-011- 5 SISO631. 2UD C631. 4 Trefw.:Bodemkunde . Correctcitation : Mokma,D.L . andP .Buurma n (1982). Podzolsan dpodzolizatio n intemperat eregions . ISMmonograp h1 ,Int .Soi lMuseum ,Wageningen ,12 6pp . ISBN90-6672-011- 5 Foreword This is the first of an envisaged serieso f ISMMonograph st ob epu blishedb yth e International SoilMuseu m inadditio nt oth eserie sappearin g under the name 'SoilMonolit h Papers'.Whil e a Soil MonolithPape rdeal s specifically with a soil unit of theFAO-Unesc o SoilLegend ,base do non e representative example inth e ISMsoi lmonolit hcollection ,th ene wserie s isope nfo ra wide rrang eo fsubject si nsoi lscience .I nparticula r itma y describe the results of studies in soil genesis and classification,soi l analysisan dlan devaluatio no fa majo rgrou po fsoils .Th egenera l aimi st o strengthenth estat eo fknowledg eo nth eworld' s soilresources ,fo rapplica tioni nth efiel do flan dmanagemen tan dagro-technolog ytransfer . The presentpape r isth eresul to fa comparativ estud yo nth echarac teristics,genesi san danalysi so fa majo rgrou po fsimila rsoils ,th epod zols,wit hth eai mt odefin eclassificatio n criteriao funiversa lvalidity . -
Soil Groups and Their Suitability to Forestry
Great Soil Groups and their suitability to forestry • Acid brown earth • Brown earth (high base) • Brown podzolic • Grey brown podzolic • Podzol • Peaty podzol • Gley • Peaty gley • Rendzina • Lithosol • Peat Toddy Radford Ian Short AcidAcid brown brown earth earth • Well drained mineral soil • Good soil physical properties • Very productive soil • Formed from various acidic parent materials • Highly suitable to broadleaf and conifer production Fairly uniform soil profile throughout with little leaching of minerals BrownBrown earth earth (high base) • Well drained mineral soil • Possess desirable soil physical characteristics • Formed from lime-rich, calcareous parent materials • Little leaching or translocation of elements in the soil profile • High pH may limit use range for certain tree species BrownBrown podzolicpodzolic Reddish / brown colour indicates accumulation of leached iron • Well drained, acid mineral soil • Derived from sandstone / shale / granite parent material • Rolling lowland • Highly suitable for broadleaves and conifers GreyGrey brown brown podzolicpodzolic Has a soil horizon of clay accumulation • Well drained, deep fertile soil • Parent material mainly limestone • Desirable soil physical properties • Highly suitable to broadleaf and conifer PodzolPodzol Horizon of leached minerals • Well drained acid mineral soil • Subject to intense leaching of minerals • Have a distinct leached soil horizon • Located mainly on hill-land areas • Mainly suitable to conifer species PeatyPeaty podzolpodzol • Very acid soil, located -
Major Soils of the World
the united nations educational, scientific international centre for theoretical physics international atomic energy agency H4.SMR/1304-5 "COLLEGE ON SOIL PHYSICS11 12 March - 6 April 2001 Major Soils of the World O. Spaargaren International Soil Reference and Information Centre Wageninen, The Netherlands These notes are for internal distribution only strada costiera, I I - 34014 trieste Italy - tel. +39 04022401 I I fax +39 040224163 - [email protected] - www.ictp.trieste.it INTRODUCTION This lecture note describes the thirty Reference Soil Groups in terms, which are readily understood. The significance of each Reference Soil Group important features are highlighted such as: a short history, connotation, international soil correlation, geographical distribution, the landscapes in which it occurs and its salient morphological features. The chemical and physical properties of the soils are summarized as well as consequences for land use and management. Spatial and temporal linkages form an important element in the description of the WRB soil units. These linkages refer to vertical and lateral successions of soil horizons, associations of soils related to the position in the landscape, and the evolution of soil horizons and soils over time. Placing soils in their geographical and regional context facilitates formulation of appropriate soil classes at a high level of generalization. It also demonstrates the continuity of the soil cover and illustrates the reasons for separating the classes. The thirty reference groups are arranged