Soil degradation and soil surface process intensities on abandoned fields in Mediterranean mountain environments
Identifieur interne : 001947 ( Istex/Corpus ); précédent : 001946; suivant : 001948Soil degradation and soil surface process intensities on abandoned fields in Mediterranean mountain environments
Auteurs : M. Seeger ; J. B. RiesSource :
- Land Degradation & Development [ 1085-3278 ] ; 2008-09.
English descriptors
Abstract
The Pyrenean and Pre‐Pyrenean mountain areas have been intensively used at least since roman times, but nowadays depopulation has lead to widespread land abandonment without a steering land‐management. Vegetation recovery is weak in most abandoned fields. Soil formation and characteristics are conditioned by this fact, and for this, soils show past degradation processes and are mostly predominant factors for continuing land degradation or restoration. Three study areas were set up along a climatic gradient with increasing summer water deficit in the sub‐humid zone between the Central Pyrenees and Pre‐Pyrenees. Soil survey combined with experiments for the determination of infiltration, runoff and erosion were applied for understanding the degradation history and the future development of the soils. All areas are dominated by Entisols, but also Inceptisols and Alfisols are found, and even soils with hydromorphic features. The soils show signs of heavy erosion. The parental material determines the nutrient supply and the general chemical properties. All sites show a weak water storing capacity, as a result of the removal of fine material by erosion and due to the depletion of soil organic matter. In addition, infiltration capacity and runoff generation are high within the studied areas, averaging between 27 and 37 per cent. The driest area studied shows an ongoing trend to degradation, with high erosion rates combined with a high degradations status of the soil. The other areas are characterised by a patchy pattern of soil degradation and regradation processes. Copyright © 2008 John Wiley & Sons, Ltd.
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DOI: 10.1002/ldr.854
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ISTEX:12DD8023E3D138B551FA35BF088201AF8DE9E0C3Le document en format XML
<record><TEI wicri:istexFullTextTei="biblStruct"><teiHeader><fileDesc><titleStmt><title xml:lang="en">Soil degradation and soil surface process intensities on abandoned fields in Mediterranean mountain environments</title><author><name sortKey="Seeger, M" sort="Seeger, M" uniqKey="Seeger M" first="M." last="Seeger">M. Seeger</name><affiliation><mods:affiliation>Department of Physical Geography, University of Trier, D‐54286 Trier, Germany</mods:affiliation></affiliation><affiliation><mods:affiliation>Department of Physical Geography, University of Trier, D‐54286 Trier, Germany.</mods:affiliation></affiliation></author><author><name sortKey="Ries, J B" sort="Ries, J B" uniqKey="Ries J" first="J. B." last="Ries">J. B. Ries</name><affiliation><mods:affiliation>Department of Physical Geography, University of Trier, D‐54286 Trier, Germany</mods:affiliation></affiliation></author></titleStmt><publicationStmt><idno type="wicri:source">ISTEX</idno><idno type="RBID">ISTEX:12DD8023E3D138B551FA35BF088201AF8DE9E0C3</idno><date when="2008" year="2008">2008</date><idno type="doi">10.1002/ldr.854</idno><idno type="url">https://api.istex.fr/document/12DD8023E3D138B551FA35BF088201AF8DE9E0C3/fulltext/pdf</idno><idno type="wicri:Area/Istex/Corpus">001947</idno><idno type="wicri:explorRef" wicri:stream="Istex" wicri:step="Corpus" wicri:corpus="ISTEX">001947</idno></publicationStmt><sourceDesc><biblStruct><analytic><title level="a" type="main" xml:lang="en">Soil degradation and soil surface process intensities on abandoned fields in Mediterranean mountain environments</title><author><name sortKey="Seeger, M" sort="Seeger, M" uniqKey="Seeger M" first="M." last="Seeger">M. Seeger</name><affiliation><mods:affiliation>Department of Physical Geography, University of Trier, D‐54286 Trier, Germany</mods:affiliation></affiliation><affiliation><mods:affiliation>Department of Physical Geography, University of Trier, D‐54286 Trier, Germany.</mods:affiliation></affiliation></author><author><name sortKey="Ries, J B" sort="Ries, J B" uniqKey="Ries J" first="J. B." last="Ries">J. B. Ries</name><affiliation><mods:affiliation>Department of Physical Geography, University of Trier, D‐54286 Trier, Germany</mods:affiliation></affiliation></author></analytic><monogr></monogr><series><title level="j">Land Degradation & Development</title><title level="j" type="abbrev">Land Degrad. Dev.</title><idno type="ISSN">1085-3278</idno><idno type="eISSN">1099-145X</idno><imprint><publisher>John Wiley & Sons, Ltd.</publisher><pubPlace>Chichester, UK</pubPlace><date type="published" when="2008-09">2008-09</date><biblScope unit="volume">19</biblScope><biblScope unit="issue">5</biblScope><biblScope unit="page" from="488">488</biblScope><biblScope unit="page" to="501">501</biblScope></imprint><idno type="ISSN">1085-3278</idno></series><idno type="istex">12DD8023E3D138B551FA35BF088201AF8DE9E0C3</idno><idno type="DOI">10.1002/ldr.854</idno><idno type="ArticleID">LDR854</idno></biblStruct></sourceDesc><seriesStmt><idno type="ISSN">1085-3278</idno></seriesStmt></fileDesc><profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Spain</term><term>abandoned fields</term><term>rainfall simulations</term><term>soil erosion processes</term><term>soils</term></keywords></textClass><langUsage><language ident="en">en</language></langUsage></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">The Pyrenean and Pre‐Pyrenean mountain areas have been intensively used at least since roman times, but nowadays depopulation has lead to widespread land abandonment without a steering land‐management. Vegetation recovery is weak in most abandoned fields. Soil formation and characteristics are conditioned by this fact, and for this, soils show past degradation processes and are mostly predominant factors for continuing land degradation or restoration. Three study areas were set up along a climatic gradient with increasing summer water deficit in the sub‐humid zone between the Central Pyrenees and Pre‐Pyrenees. Soil survey combined with experiments for the determination of infiltration, runoff and erosion were applied for understanding the degradation history and the future development of the soils. All areas are dominated by Entisols, but also Inceptisols and Alfisols are found, and even soils with hydromorphic features. The soils show signs of heavy erosion. The parental material determines the nutrient supply and the general chemical properties. All sites show a weak water storing capacity, as a result of the removal of fine material by erosion and due to the depletion of soil organic matter. In addition, infiltration capacity and runoff generation are high within the studied areas, averaging between 27 and 37 per cent. The driest area studied shows an ongoing trend to degradation, with high erosion rates combined with a high degradations status of the soil. The other areas are characterised by a patchy pattern of soil degradation and regradation processes. Copyright © 2008 John Wiley & Sons, Ltd.</div></front></TEI><istex><corpusName>wiley</corpusName><author><json:item><name>M. Seeger</name><affiliations><json:string>Department of Physical Geography, University of Trier, D‐54286 Trier, Germany</json:string><json:string>Department of Physical Geography, University of Trier, D‐54286 Trier, Germany.</json:string></affiliations></json:item><json:item><name>J. B. Ries</name><affiliations><json:string>Department of Physical Geography, University of Trier, D‐54286 Trier, Germany</json:string></affiliations></json:item></author><subject><json:item><lang><json:string>eng</json:string></lang><value>soils</value></json:item><json:item><lang><json:string>eng</json:string></lang><value>soil erosion processes</value></json:item><json:item><lang><json:string>eng</json:string></lang><value>abandoned fields</value></json:item><json:item><lang><json:string>eng</json:string></lang><value>rainfall simulations</value></json:item><json:item><lang><json:string>eng</json:string></lang><value>Spain</value></json:item></subject><articleId><json:string>LDR854</json:string></articleId><language><json:string>eng</json:string></language><originalGenre><json:string>article</json:string></originalGenre><abstract>The Pyrenean and Pre‐Pyrenean mountain areas have been intensively used at least since roman times, but nowadays depopulation has lead to widespread land abandonment without a steering land‐management. Vegetation recovery is weak in most abandoned fields. Soil formation and characteristics are conditioned by this fact, and for this, soils show past degradation processes and are mostly predominant factors for continuing land degradation or restoration. Three study areas were set up along a climatic gradient with increasing summer water deficit in the sub‐humid zone between the Central Pyrenees and Pre‐Pyrenees. Soil survey combined with experiments for the determination of infiltration, runoff and erosion were applied for understanding the degradation history and the future development of the soils. All areas are dominated by Entisols, but also Inceptisols and Alfisols are found, and even soils with hydromorphic features. The soils show signs of heavy erosion. The parental material determines the nutrient supply and the general chemical properties. All sites show a weak water storing capacity, as a result of the removal of fine material by erosion and due to the depletion of soil organic matter. In addition, infiltration capacity and runoff generation are high within the studied areas, averaging between 27 and 37 per cent. The driest area studied shows an ongoing trend to degradation, with high erosion rates combined with a high degradations status of the soil. The other areas are characterised by a patchy pattern of soil degradation and regradation processes. 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degradation processes: The case of Mwisanga catchment, Kondoa, central Tanzania</title></json:item></refBibs><genre><json:string>article</json:string></genre><host><volume>19</volume><publisherId><json:string>LDR</json:string></publisherId><pages><total>14</total><last>501</last><first>488</first></pages><issn><json:string>1085-3278</json:string></issn><issue>5</issue><subject><json:item><value>Research Article</value></json:item></subject><genre><json:string>journal</json:string></genre><language><json:string>unknown</json:string></language><eissn><json:string>1099-145X</json:string></eissn><title>Land Degradation & Development</title><doi><json:string>10.1002/(ISSN)1099-145X</json:string></doi></host><categories><wos><json:string>science</json:string><json:string>soil science</json:string><json:string>environmental sciences</json:string></wos><scienceMetrix><json:string>applied sciences</json:string><json:string>agriculture, fisheries & forestry</json:string><json:string>agronomy & agriculture</json:string></scienceMetrix></categories><publicationDate>2008</publicationDate><copyrightDate>2008</copyrightDate><doi><json:string>10.1002/ldr.854</json:string></doi><id>12DD8023E3D138B551FA35BF088201AF8DE9E0C3</id><score>1.6108057</score><fulltext><json:item><extension>pdf</extension><original>true</original><mimetype>application/pdf</mimetype><uri>https://api.istex.fr/document/12DD8023E3D138B551FA35BF088201AF8DE9E0C3/fulltext/pdf</uri></json:item><json:item><extension>zip</extension><original>false</original><mimetype>application/zip</mimetype><uri>https://api.istex.fr/document/12DD8023E3D138B551FA35BF088201AF8DE9E0C3/fulltext/zip</uri></json:item><istex:fulltextTEI uri="https://api.istex.fr/document/12DD8023E3D138B551FA35BF088201AF8DE9E0C3/fulltext/tei"><teiHeader><fileDesc><titleStmt><title level="a" type="main" xml:lang="en">Soil degradation and soil surface process intensities on abandoned fields in Mediterranean mountain environments</title></titleStmt><publicationStmt><authority>ISTEX</authority><publisher>John Wiley & Sons, Ltd.</publisher><pubPlace>Chichester, UK</pubPlace><availability><p>Copyright © 2008 John Wiley & Sons, Ltd.</p></availability><date>2008</date></publicationStmt><sourceDesc><biblStruct type="inbook"><analytic><title level="a" type="main" xml:lang="en">Soil degradation and soil surface process intensities on abandoned fields in Mediterranean mountain environments</title><author xml:id="author-1"><persName><forename type="first">M.</forename><surname>Seeger</surname></persName><affiliation>Department of Physical Geography, University of Trier, D‐54286 Trier, Germany</affiliation><affiliation>Department of Physical Geography, University of Trier, D‐54286 Trier, Germany.</affiliation></author><author xml:id="author-2"><persName><forename type="first">J. B.</forename><surname>Ries</surname></persName><affiliation>Department of Physical Geography, University of Trier, D‐54286 Trier, Germany</affiliation></author></analytic><monogr><title level="j">Land Degradation & Development</title><title level="j" type="abbrev">Land Degrad. 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Vegetation recovery is weak in most abandoned fields. Soil formation and characteristics are conditioned by this fact, and for this, soils show past degradation processes and are mostly predominant factors for continuing land degradation or restoration. Three study areas were set up along a climatic gradient with increasing summer water deficit in the sub‐humid zone between the Central Pyrenees and Pre‐Pyrenees. Soil survey combined with experiments for the determination of infiltration, runoff and erosion were applied for understanding the degradation history and the future development of the soils. All areas are dominated by Entisols, but also Inceptisols and Alfisols are found, and even soils with hydromorphic features. The soils show signs of heavy erosion. The parental material determines the nutrient supply and the general chemical properties. All sites show a weak water storing capacity, as a result of the removal of fine material by erosion and due to the depletion of soil organic matter. In addition, infiltration capacity and runoff generation are high within the studied areas, averaging between 27 and 37 per cent. The driest area studied shows an ongoing trend to degradation, with high erosion rates combined with a high degradations status of the soil. The other areas are characterised by a patchy pattern of soil degradation and regradation processes. Copyright © 2008 John Wiley & Sons, Ltd.</p></abstract><textClass xml:lang="en"><keywords scheme="keyword"><list><head>keywords</head><item><term>soils</term></item><item><term>soil erosion processes</term></item><item><term>abandoned fields</term></item><item><term>rainfall simulations</term></item><item><term>Spain</term></item></list></keywords></textClass><textClass><keywords scheme="Journal Subject"><list><head>article-category</head><item><term>Research Article</term></item></list></keywords></textClass></profileDesc><revisionDesc><change when="2007-08-13">Received</change><change when="2008-01-18">Registration</change><change when="2008-09">Published</change></revisionDesc></teiHeader></istex:fulltextTEI><json:item><extension>txt</extension><original>false</original><mimetype>text/plain</mimetype><uri>https://api.istex.fr/document/12DD8023E3D138B551FA35BF088201AF8DE9E0C3/fulltext/txt</uri></json:item></fulltext><metadata><istex:metadataXml wicri:clean="Wiley, elements deleted: body"><istex:xmlDeclaration>version="1.0" encoding="UTF-8" standalone="yes"</istex:xmlDeclaration><istex:document><component version="2.0" type="serialArticle" xml:lang="en"><header><publicationMeta level="product"><publisherInfo><publisherName>John Wiley & Sons, Ltd.</publisherName><publisherLoc>Chichester, UK</publisherLoc></publisherInfo><doi registered="yes">10.1002/(ISSN)1099-145X</doi><issn type="print">1085-3278</issn><issn type="electronic">1099-145X</issn><idGroup><id type="product" value="LDR"></id></idGroup><titleGroup><title type="main" xml:lang="en" sort="LAND DEGRADATION AND DEVELOPMENT">Land Degradation & Development</title><title type="short">Land Degrad. 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B.</givenNames><familyName>Ries</familyName></personName></creator></creators><affiliationGroup><affiliation xml:id="af1" countryCode="DE" type="organization"><unparsedAffiliation>Department of Physical Geography, University of Trier, D‐54286 Trier, Germany</unparsedAffiliation></affiliation></affiliationGroup><keywordGroup xml:lang="en" type="author"><keyword xml:id="kwd1">soils</keyword><keyword xml:id="kwd2">soil erosion processes</keyword><keyword xml:id="kwd3">abandoned fields</keyword><keyword xml:id="kwd4">rainfall simulations</keyword><keyword xml:id="kwd5">Spain</keyword></keywordGroup><abstractGroup><abstract type="main" xml:lang="en"><title type="main">Abstract</title><p>The Pyrenean and Pre‐Pyrenean mountain areas have been intensively used at least since roman times, but nowadays depopulation has lead to widespread land abandonment without a steering land‐management. Vegetation recovery is weak in most abandoned fields. Soil formation and characteristics are conditioned by this fact, and for this, soils show past degradation processes and are mostly predominant factors for continuing land degradation or restoration. Three study areas were set up along a climatic gradient with increasing summer water deficit in the sub‐humid zone between the Central Pyrenees and Pre‐Pyrenees. Soil survey combined with experiments for the determination of infiltration, runoff and erosion were applied for understanding the degradation history and the future development of the soils. All areas are dominated by Entisols, but also Inceptisols and Alfisols are found, and even soils with hydromorphic features. The soils show signs of heavy erosion. The parental material determines the nutrient supply and the general chemical properties. All sites show a weak water storing capacity, as a result of the removal of fine material by erosion and due to the depletion of soil organic matter. In addition, infiltration capacity and runoff generation are high within the studied areas, averaging between 27 and 37 per cent. The driest area studied shows an ongoing trend to degradation, with high erosion rates combined with a high degradations status of the soil. The other areas are characterised by a patchy pattern of soil degradation and regradation processes. Copyright © 2008 John Wiley & Sons, Ltd.</p></abstract></abstractGroup></contentMeta></header></component></istex:document></istex:metadataXml><mods version="3.6"><titleInfo lang="en"><title>Soil degradation and soil surface process intensities on abandoned fields in Mediterranean mountain environments</title></titleInfo><titleInfo type="abbreviated" lang="en"><title>SOIL DEGRADATION IN MEDITERRANEAN MOUNTAIN ENVIRONMENTS</title></titleInfo><titleInfo type="alternative" contentType="CDATA" lang="en"><title>Soil degradation and soil surface process intensities on abandoned fields in Mediterranean mountain environments</title></titleInfo><name type="personal"><namePart type="given">M.</namePart><namePart type="family">Seeger</namePart><affiliation>Department of Physical Geography, University of Trier, D‐54286 Trier, Germany</affiliation><affiliation>Department of Physical Geography, University of Trier, D‐54286 Trier, Germany.</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">J. B.</namePart><namePart type="family">Ries</namePart><affiliation>Department of Physical Geography, University of Trier, D‐54286 Trier, Germany</affiliation><role><roleTerm type="text">author</roleTerm></role></name><typeOfResource>text</typeOfResource><genre type="article" displayLabel="article"></genre><originInfo><publisher>John Wiley & Sons, Ltd.</publisher><place><placeTerm type="text">Chichester, UK</placeTerm></place><dateIssued encoding="w3cdtf">2008-09</dateIssued><dateCaptured encoding="w3cdtf">2007-08-13</dateCaptured><dateValid encoding="w3cdtf">2008-01-18</dateValid><copyrightDate encoding="w3cdtf">2008</copyrightDate></originInfo><language><languageTerm type="code" authority="rfc3066">en</languageTerm><languageTerm type="code" authority="iso639-2b">eng</languageTerm></language><physicalDescription><internetMediaType>text/html</internetMediaType><extent unit="figures">6</extent><extent unit="tables">4</extent><extent unit="references">47</extent></physicalDescription><abstract lang="en">The Pyrenean and Pre‐Pyrenean mountain areas have been intensively used at least since roman times, but nowadays depopulation has lead to widespread land abandonment without a steering land‐management. Vegetation recovery is weak in most abandoned fields. Soil formation and characteristics are conditioned by this fact, and for this, soils show past degradation processes and are mostly predominant factors for continuing land degradation or restoration. Three study areas were set up along a climatic gradient with increasing summer water deficit in the sub‐humid zone between the Central Pyrenees and Pre‐Pyrenees. Soil survey combined with experiments for the determination of infiltration, runoff and erosion were applied for understanding the degradation history and the future development of the soils. All areas are dominated by Entisols, but also Inceptisols and Alfisols are found, and even soils with hydromorphic features. The soils show signs of heavy erosion. The parental material determines the nutrient supply and the general chemical properties. All sites show a weak water storing capacity, as a result of the removal of fine material by erosion and due to the depletion of soil organic matter. In addition, infiltration capacity and runoff generation are high within the studied areas, averaging between 27 and 37 per cent. The driest area studied shows an ongoing trend to degradation, with high erosion rates combined with a high degradations status of the soil. The other areas are characterised by a patchy pattern of soil degradation and regradation processes. Copyright © 2008 John Wiley & Sons, Ltd.</abstract><subject lang="en"><genre>keywords</genre><topic>soils</topic><topic>soil erosion processes</topic><topic>abandoned fields</topic><topic>rainfall simulations</topic><topic>Spain</topic></subject><relatedItem type="host"><titleInfo><title>Land Degradation & Development</title></titleInfo><titleInfo type="abbreviated"><title>Land Degrad. 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