Assessment of soil erosion in a small watershed covered by loess
Identifieur interne : 000B19 ( Istex/Corpus ); précédent : 000B18; suivant : 000B20Assessment of soil erosion in a small watershed covered by loess
Auteurs : Ádám Kertész ; Béla Márkus ; Gerold RichterSource :
- GeoJournal [ 0343-2521 ] ; 1995-06-01.
Abstract
Abstract: Loose sediments like loess are easily erodable especially on hillslopes used for agriculture. Erosion contributes to the sedimentation and pollution of lakes such threatening quasi-natural ecosystems. On the other hand soil erosion damages fertile soils. The aim of the present paper is the assessment of soil and nutrient loss in a tributary catchment of Lake Balaton, including geoecological aspects of the lake ecosystem and of the slopes mantled by loess. The USLE is applied for small topological units, for the so called erotops. Rainfall simulation experiments were applied for the determination of the erodibility of soils. The calculation is based on a new, GIS aided method. Control measurements have been going on for four years at a gauging station to check how much sediment and water actually leaves the catchment. Results of sediment yield measurements were compared with the results obtained by the application of USLE for the whole catchment. According to this comparison only 2% leaves the catchment so that redeposition processes within the catchment are very important whereas the contribution of soil erosion to the eutrophication of the lake is not very significant in the small tributaries in the northern part of Lake Balaton catchment.
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DOI: 10.1007/BF00813188
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Erosion contributes to the sedimentation and pollution of lakes such threatening quasi-natural ecosystems. On the other hand soil erosion damages fertile soils. The aim of the present paper is the assessment of soil and nutrient loss in a tributary catchment of Lake Balaton, including geoecological aspects of the lake ecosystem and of the slopes mantled by loess. The USLE is applied for small topological units, for the so called erotops. Rainfall simulation experiments were applied for the determination of the erodibility of soils. The calculation is based on a new, GIS aided method. Control measurements have been going on for four years at a gauging station to check how much sediment and water actually leaves the catchment. Results of sediment yield measurements were compared with the results obtained by the application of USLE for the whole catchment. According to this comparison only 2% leaves the catchment so that redeposition processes within the catchment are very important whereas the contribution of soil erosion to the eutrophication of the lake is not very significant in the small tributaries in the northern part of Lake Balaton catchment.</div></front></TEI><istex><corpusName>springer</corpusName><author><json:item><name>Ádám Kertész</name><affiliations><json:string>Geographical Research Institute, Hungarian Academy of Sciences, Andrássy út 62, H-1062, Budapest, Hungary</json:string></affiliations></json:item><json:item><name>Béla Márkus</name><affiliations><json:string>College for Surveying and County-Planning, University of Forestry and Timber Industry, H-8002, Székesfehérvár, Hungary</json:string></affiliations></json:item><json:item><name>Gerold Richter</name><affiliations><json:string>University of Trier, POB 3825, 54296, Trier, Germany</json:string></affiliations></json:item></author><articleId><json:string>BF00813188</json:string><json:string>Art34</json:string></articleId><language><json:string>eng</json:string></language><originalGenre><json:string>OriginalPaper</json:string></originalGenre><abstract>Abstract: Loose sediments like loess are easily erodable especially on hillslopes used for agriculture. Erosion contributes to the sedimentation and pollution of lakes such threatening quasi-natural ecosystems. On the other hand soil erosion damages fertile soils. The aim of the present paper is the assessment of soil and nutrient loss in a tributary catchment of Lake Balaton, including geoecological aspects of the lake ecosystem and of the slopes mantled by loess. The USLE is applied for small topological units, for the so called erotops. Rainfall simulation experiments were applied for the determination of the erodibility of soils. The calculation is based on a new, GIS aided method. Control measurements have been going on for four years at a gauging station to check how much sediment and water actually leaves the catchment. Results of sediment yield measurements were compared with the results obtained by the application of USLE for the whole catchment. According to this comparison only 2% leaves the catchment so that redeposition processes within the catchment are very important whereas the contribution of soil erosion to the eutrophication of the lake is not very significant in the small tributaries in the northern part of Lake Balaton catchment.</abstract><qualityIndicators><score>4.497</score><pdfVersion>1.3</pdfVersion><pdfPageSize>594 x 778 pts</pdfPageSize><refBibsNative>false</refBibsNative><keywordCount>0</keywordCount><abstractCharCount>1270</abstractCharCount><pdfWordCount>2121</pdfWordCount><pdfCharCount>10659</pdfCharCount><pdfPageCount>4</pdfPageCount><abstractWordCount>198</abstractWordCount></qualityIndicators><title>Assessment of soil erosion in a small watershed covered by loess</title><refBibs><json:item><author><json:item><name>Z Dezs6ny</name></json:item></author><host><volume>66</volume><pages><last>324</last><first>311</first></pages><author></author><title>Viz/.igyi K0zlem6nyek</title></host><title>A lehets6ges er6zi6 t6rk~pez~se 6s az er6zi6vesz~ly vizsg~ilata a Balaton-vizgyfijt6 tertilet6n (Mapping of potential erosion and the investigation of erosion hazard in Lake Balaton catchment)</title></json:item><json:item><author><json:item><name>A Kert6sz</name></json:item></author><host><volume>17</volume><pages><last>238</last><first>233</first></pages><author></author><title>Computers, Environment and Urban Systems</title><publicationDate>1993</publicationDate></host><title>Application of GIS methods in soil erosion modelling</title><publicationDate>1993</publicationDate></json:item><json:item><author><json:item><name>G Richter</name></json:item><json:item><name>G Mez6si</name></json:item></author><host><volume>2830</volume><pages><last>82</last><first>67</first></pages><author></author><title>Acta Geogr. Szegediensis</title><publicationDate>1990</publicationDate></host><title>Bodenerosion, Winderosion und Bodenfruchtbarkeit -eine quantitative N~iherung mit der EPIC Model</title><publicationDate>1990</publicationDate></json:item><json:item><author><json:item><name>P Stefanovits</name></json:item><json:item><name> Vfirallyay</name></json:item><json:item><name> Gy</name></json:item></author><host><pages><last>95</last><first>79</first></pages><author></author><title>Proceedings</title><publicationDate>1992-03-01</publicationDate></host><title>State and Management of Soil Erosion in Hungary. Soil Erosion and Remediation Workshop</title><publicationDate>1992-03-01</publicationDate></json:item><json:item><host><author><json:item><name>W,H Wischmeier</name></json:item><json:item><name>D,D Smith</name></json:item></author><title>Predicting rainfall erosion losses -a guide to conservation planning: USDA Agricultural Handbook 537</title><publicationDate>1978</publicationDate></host></json:item><json:item><host><author></author><title>Recent dramatic socio-economic changes of the nation have made the updating of the National Atlas of Hungary (NAH) an actual task. Maps series to be issued continuously are to cover demographic changes based on the 1990 census data and to present various aspects of the ongoing political-administrative and economic transformation</title></host></json:item><json:item><host><author></author><title>The atlas is fully bi-lingual (English/Hungarian) and prepared using computer aided mapping (Arc/Info program). The following four booklets were prepared</title><publicationDate>1994</publicationDate></host></json:item></refBibs><genre><json:string>research-article</json:string></genre><host><volume>36</volume><pages><last>288</last><first>285</first></pages><issn><json:string>0343-2521</json:string></issn><issue>2-3</issue><subject><json:item><value>Hydrogeology</value></json:item><json:item><value>Ecology</value></json:item><json:item><value>Environmental Management</value></json:item><json:item><value>Methodology of the Social Sciences</value></json:item></subject><journalId><json:string>10708</json:string></journalId><genre><json:string>journal</json:string></genre><language><json:string>unknown</json:string></language><eissn><json:string>1572-9893</json:string></eissn><title>GeoJournal</title><publicationDate>1995</publicationDate><copyrightDate>1995</copyrightDate></host><categories><wos></wos><scienceMetrix><json:string>economic & social sciences</json:string><json:string>social sciences</json:string><json:string>geography</json:string></scienceMetrix></categories><publicationDate>1995</publicationDate><copyrightDate>1995</copyrightDate><doi><json:string>10.1007/BF00813188</json:string></doi><id>D9B8E6033593CA36E453272AC00ED934E8599FFA</id><score>0.85551393</score><fulltext><json:item><extension>pdf</extension><original>true</original><mimetype>application/pdf</mimetype><uri>https://api.istex.fr/document/D9B8E6033593CA36E453272AC00ED934E8599FFA/fulltext/pdf</uri></json:item><json:item><extension>zip</extension><original>false</original><mimetype>application/zip</mimetype><uri>https://api.istex.fr/document/D9B8E6033593CA36E453272AC00ED934E8599FFA/fulltext/zip</uri></json:item><istex:fulltextTEI uri="https://api.istex.fr/document/D9B8E6033593CA36E453272AC00ED934E8599FFA/fulltext/tei"><teiHeader><fileDesc><titleStmt><title level="a" type="main" xml:lang="en">Assessment of soil erosion in a small watershed covered by loess</title><respStmt><resp>Références bibliographiques récupérées via GROBID</resp><name resp="ISTEX-API">ISTEX-API (INIST-CNRS)</name></respStmt><respStmt><resp>Références bibliographiques récupérées via GROBID</resp><name resp="ISTEX-API">ISTEX-API (INIST-CNRS)</name></respStmt></titleStmt><publicationStmt><authority>ISTEX</authority><publisher>Kluwer Academic Publishers</publisher><pubPlace>Dordrecht</pubPlace><availability><p>Kluwer Academic Publishers, 1995</p></availability><date>1995</date></publicationStmt><sourceDesc><biblStruct type="inbook"><analytic><title level="a" type="main" xml:lang="en">Assessment of soil erosion in a small watershed covered by loess</title><author xml:id="author-1"><persName><forename type="first">Ádám</forename><surname>Kertész</surname></persName><note type="biography">Dr.</note><affiliation>Dr.</affiliation><affiliation>Geographical Research Institute, Hungarian Academy of Sciences, Andrássy út 62, H-1062, Budapest, Hungary</affiliation></author><author xml:id="author-2"><persName><forename type="first">Béla</forename><surname>Márkus</surname></persName><note type="biography">Dr.</note><affiliation>Dr.</affiliation><affiliation>College for Surveying and County-Planning, University of Forestry and Timber Industry, H-8002, Székesfehérvár, Hungary</affiliation></author><author xml:id="author-3"><persName><forename type="first">Gerold</forename><surname>Richter</surname></persName><note type="biography">Prof. Dr.</note><affiliation>Prof. Dr.</affiliation><affiliation>University of Trier, POB 3825, 54296, Trier, Germany</affiliation></author></analytic><monogr><title level="j">GeoJournal</title><title level="j" type="sub">An International Journal on Human Geography and Environmental Sciences</title><title level="j" type="abbrev">GeoJournal</title><idno type="journal-ID">10708</idno><idno type="pISSN">0343-2521</idno><idno type="eISSN">1572-9893</idno><idno type="issue-article-count">43</idno><idno type="volume-issue-count">4</idno><imprint><publisher>Kluwer Academic Publishers</publisher><pubPlace>Dordrecht</pubPlace><date type="published" when="1995-06-01"></date><biblScope unit="volume">36</biblScope><biblScope unit="issue">2-3</biblScope><biblScope unit="page" from="285">285</biblScope><biblScope unit="page" to="288">288</biblScope></imprint></monogr><idno type="istex">D9B8E6033593CA36E453272AC00ED934E8599FFA</idno><idno type="DOI">10.1007/BF00813188</idno><idno type="ArticleID">BF00813188</idno><idno type="ArticleID">Art34</idno></biblStruct></sourceDesc></fileDesc><profileDesc><creation><date>1995</date></creation><langUsage><language ident="en">en</language></langUsage><abstract xml:lang="en"><p>Abstract: Loose sediments like loess are easily erodable especially on hillslopes used for agriculture. Erosion contributes to the sedimentation and pollution of lakes such threatening quasi-natural ecosystems. On the other hand soil erosion damages fertile soils. The aim of the present paper is the assessment of soil and nutrient loss in a tributary catchment of Lake Balaton, including geoecological aspects of the lake ecosystem and of the slopes mantled by loess. The USLE is applied for small topological units, for the so called erotops. Rainfall simulation experiments were applied for the determination of the erodibility of soils. The calculation is based on a new, GIS aided method. Control measurements have been going on for four years at a gauging station to check how much sediment and water actually leaves the catchment. Results of sediment yield measurements were compared with the results obtained by the application of USLE for the whole catchment. According to this comparison only 2% leaves the catchment so that redeposition processes within the catchment are very important whereas the contribution of soil erosion to the eutrophication of the lake is not very significant in the small tributaries in the northern part of Lake Balaton catchment.</p></abstract><textClass><keywords scheme="Journal Subject"><list><head>Geography</head><item><term>Hydrogeology</term></item><item><term>Ecology</term></item><item><term>Environmental Management</term></item><item><term>Methodology of the Social Sciences</term></item></list></keywords></textClass></profileDesc><revisionDesc><change when="1995-06-01">Published</change><change xml:id="refBibs-istex" who="#ISTEX-API" when="2016-11-23">References added</change><change xml:id="refBibs-istex" who="#ISTEX-API" when="2017-01-21">References 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AffiliationIDS="Aff3"><AuthorName DisplayOrder="Eastern"><GivenName>Gerold</GivenName><FamilyName>Richter</FamilyName></AuthorName><Role>Prof. Dr.</Role></Author><Affiliation ID="Aff1"><OrgDivision>Geographical Research Institute</OrgDivision><OrgName>Hungarian Academy of Sciences</OrgName><OrgAddress><Street>Andrássy út 62</Street><Postcode>H-1062</Postcode><City>Budapest</City><Country>Hungary</Country></OrgAddress></Affiliation><Affiliation ID="Aff2"><OrgDivision>College for Surveying and County-Planning</OrgDivision><OrgName>University of Forestry and Timber Industry</OrgName><OrgAddress><Postcode>H-8002</Postcode><City>Székesfehérvár</City><Country>Hungary</Country></OrgAddress></Affiliation><Affiliation ID="Aff3"><OrgName>University of Trier</OrgName><OrgAddress><Postbox>POB 3825</Postbox><Postcode>54296</Postcode><City>Trier</City><Country>Germany</Country></OrgAddress></Affiliation></AuthorGroup><Abstract ID="Abs1" Language="En"><Heading>Abstract</Heading><Para>Loose sediments like loess are easily erodable especially on hillslopes used for agriculture. Erosion contributes to the sedimentation and pollution of lakes such threatening quasi-natural ecosystems. On the other hand soil erosion damages fertile soils.</Para><Para>The aim of the present paper is the assessment of soil and nutrient loss in a tributary catchment of Lake Balaton, including geoecological aspects of the lake ecosystem and of the slopes mantled by loess.</Para><Para>The USLE is applied for small topological units, for the so called erotops. Rainfall simulation experiments were applied for the determination of the erodibility of soils. The calculation is based on a new, GIS aided method. Control measurements have been going on for four years at a gauging station to check how much sediment and water actually leaves the catchment.</Para><Para>Results of sediment yield measurements were compared with the results obtained by the application of USLE for the whole catchment. According to this comparison only 2% leaves the catchment so that redeposition processes within the catchment are very important whereas the contribution of soil erosion to the eutrophication of the lake is not very significant in the small tributaries in the northern part of Lake Balaton catchment.</Para></Abstract></ArticleHeader><NoBody></NoBody></Article></Issue></Volume></Journal></Publisher></istex:document></istex:metadataXml><mods version="3.6"><titleInfo lang="en"><title>Assessment of soil erosion in a small watershed covered by loess</title></titleInfo><titleInfo type="alternative" contentType="CDATA" lang="en"><title>Assessment of soil erosion in a small watershed covered by loess</title></titleInfo><name type="personal"><namePart type="given">Ádám</namePart><namePart type="family">Kertész</namePart><affiliation>Geographical Research Institute, Hungarian Academy of Sciences, Andrássy út 62, H-1062, Budapest, Hungary</affiliation><role><roleTerm type="text">author</roleTerm></role><description>Dr.</description></name><name type="personal"><namePart type="given">Béla</namePart><namePart type="family">Márkus</namePart><affiliation>College for Surveying and County-Planning, University of Forestry and Timber Industry, H-8002, Székesfehérvár, Hungary</affiliation><role><roleTerm type="text">author</roleTerm></role><description>Dr.</description></name><name type="personal"><namePart type="given">Gerold</namePart><namePart type="family">Richter</namePart><affiliation>University of Trier, POB 3825, 54296, Trier, Germany</affiliation><role><roleTerm type="text">author</roleTerm></role><description>Prof. Dr.</description></name><typeOfResource>text</typeOfResource><genre type="research-article" displayLabel="OriginalPaper"></genre><originInfo><publisher>Kluwer Academic Publishers</publisher><place><placeTerm type="text">Dordrecht</placeTerm></place><dateIssued encoding="w3cdtf">1995-06-01</dateIssued><copyrightDate encoding="w3cdtf">1995</copyrightDate></originInfo><language><languageTerm type="code" authority="rfc3066">en</languageTerm><languageTerm type="code" authority="iso639-2b">eng</languageTerm></language><physicalDescription><internetMediaType>text/html</internetMediaType></physicalDescription><abstract lang="en">Abstract: Loose sediments like loess are easily erodable especially on hillslopes used for agriculture. Erosion contributes to the sedimentation and pollution of lakes such threatening quasi-natural ecosystems. On the other hand soil erosion damages fertile soils. The aim of the present paper is the assessment of soil and nutrient loss in a tributary catchment of Lake Balaton, including geoecological aspects of the lake ecosystem and of the slopes mantled by loess. The USLE is applied for small topological units, for the so called erotops. Rainfall simulation experiments were applied for the determination of the erodibility of soils. The calculation is based on a new, GIS aided method. Control measurements have been going on for four years at a gauging station to check how much sediment and water actually leaves the catchment. Results of sediment yield measurements were compared with the results obtained by the application of USLE for the whole catchment. According to this comparison only 2% leaves the catchment so that redeposition processes within the catchment are very important whereas the contribution of soil erosion to the eutrophication of the lake is not very significant in the small tributaries in the northern part of Lake Balaton catchment.</abstract><relatedItem type="host"><titleInfo><title>GeoJournal</title><subTitle>An International Journal on Human Geography and Environmental Sciences</subTitle></titleInfo><titleInfo type="abbreviated"><title>GeoJournal</title></titleInfo><genre type="journal" displayLabel="Archive Journal"></genre><originInfo><dateIssued encoding="w3cdtf">1995-06-01</dateIssued><copyrightDate encoding="w3cdtf">1995</copyrightDate></originInfo><subject><genre>Geography</genre><topic>Hydrogeology</topic><topic>Ecology</topic><topic>Environmental Management</topic><topic>Methodology of the Social Sciences</topic></subject><identifier type="ISSN">0343-2521</identifier><identifier type="eISSN">1572-9893</identifier><identifier type="JournalID">10708</identifier><identifier type="IssueArticleCount">43</identifier><identifier type="VolumeIssueCount">4</identifier><part><date>1995</date><detail type="volume"><number>36</number><caption>vol.</caption></detail><detail type="issue"><number>2-3</number><caption>no.</caption></detail><extent unit="pages"><start>285</start><end>288</end></extent></part><recordInfo><recordOrigin>Kluwer Academic Publishers, 1995</recordOrigin></recordInfo></relatedItem><identifier type="istex">D9B8E6033593CA36E453272AC00ED934E8599FFA</identifier><identifier type="DOI">10.1007/BF00813188</identifier><identifier type="ArticleID">BF00813188</identifier><identifier type="ArticleID">Art34</identifier><accessCondition type="use and reproduction" contentType="copyright">Kluwer Academic Publishers, 1995</accessCondition><recordInfo><recordContentSource>SPRINGER</recordContentSource><recordOrigin>Kluwer Academic Publishers, 1995</recordOrigin></recordInfo></mods></metadata><serie></serie></istex></record>Pour manipuler ce document sous Unix (Dilib)
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