Soil erosion processes and their measurement in the german area of the Moselle river
Identifieur interne : 000A33 ( Istex/Corpus ); précédent : 000A32; suivant : 000A34Soil erosion processes and their measurement in the german area of the Moselle river
Auteurs : Gerold Richter ; Jörg F. W. NegendankSource :
- Earth Surface Processes [ 0360-1269 ] ; 1977-04.
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- KwdEn :
Abstract
Measurements and observations of soil erosion processes in vineyards on steep slopes in the German portion of the Moselle valley‐are described. Rates of erosion caused by gravitational mass movements and the action of running water differ. Catastrophic geomorphic events since 1972 are described qualitatively while quantitative data on precipitation, runoff, soil and solute loss during one year (1974‐5) from 13 plots in old and new vineyards (measuring 2m × 8, 16, 24, 32 and 48m) are presented. On the 20° slope plots erosion rates were 2.7cm/1,000 years in the old vineyard and 4.4 cm/1,000 years in the new vineyard. These results compare favourably with rates of 0.75‐4‐4 cm/1.000 years calculated from geological evidence. Both values are lower than those from many other agricultural plots and probably reflect the relative stability of the stony loams.
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DOI: 10.1002/esp.3290020217
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ISTEX:F6D840B99079209BFEA36209DB17CEEF256B3261Le document en format XML
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Rates of erosion caused by gravitational mass movements and the action of running water differ. Catastrophic geomorphic events since 1972 are described qualitatively while quantitative data on precipitation, runoff, soil and solute loss during one year (1974‐5) from 13 plots in old and new vineyards (measuring 2m × 8, 16, 24, 32 and 48m) are presented. On the 20° slope plots erosion rates were 2.7cm/1,000 years in the old vineyard and 4.4 cm/1,000 years in the new vineyard. These results compare favourably with rates of 0.75‐4‐4 cm/1.000 years calculated from geological evidence. Both values are lower than those from many other agricultural plots and probably reflect the relative stability of the stony loams.</div></front></TEI><istex><corpusName>wiley</corpusName><author><json:item><name>Gerold Richter</name><affiliations><json:string>Physische Geographie und Bodenerosionsforschungsstelle Mertesdorf der Universität Trier, Schneidershof, D‐5500 Trier, Germany</json:string></affiliations></json:item><json:item><name>Jörg F. W. Negendank</name><affiliations><json:string>Geowissenschqftl. Laboratorium und Geolog. Begleitstudium der Fachgruppe Geographie der Universität Trier, Schneidershof, C‐5500 Trier, Germany</json:string></affiliations></json:item></author><subject><json:item><lang><json:string>eng</json:string></lang><value>Soil erosion</value></json:item><json:item><lang><json:string>eng</json:string></lang><value>Erosion plots</value></json:item><json:item><lang><json:string>eng</json:string></lang><value>Mass movement</value></json:item><json:item><lang><json:string>eng</json:string></lang><value>Vineyards</value></json:item></subject><articleId><json:string>ESP3290020217</json:string></articleId><language><json:string>eng</json:string></language><originalGenre><json:string>article</json:string></originalGenre><abstract>Measurements and observations of soil erosion processes in vineyards on steep slopes in the German portion of the Moselle valley‐are described. Rates of erosion caused by gravitational mass movements and the action of running water differ. Catastrophic geomorphic events since 1972 are described qualitatively while quantitative data on precipitation, runoff, soil and solute loss during one year (1974‐5) from 13 plots in old and new vineyards (measuring 2m × 8, 16, 24, 32 and 48m) are presented. On the 20° slope plots erosion rates were 2.7cm/1,000 years in the old vineyard and 4.4 cm/1,000 years in the new vineyard. These results compare favourably with rates of 0.75‐4‐4 cm/1.000 years calculated from geological evidence. Both values are lower than those from many other agricultural plots and probably reflect the relative stability of the stony loams.</abstract><qualityIndicators><score>4.167</score><pdfVersion>1.3</pdfVersion><pdfPageSize>558 x 738 pts</pdfPageSize><refBibsNative>true</refBibsNative><abstractCharCount>862</abstractCharCount><pdfWordCount>2559</pdfWordCount><pdfCharCount>18115</pdfCharCount><pdfPageCount>18</pdfPageCount><abstractWordCount>134</abstractWordCount></qualityIndicators><title>Soil erosion processes and their measurement in the german area of the Moselle river</title><refBibs><json:item><author><json:item><name>I. Bosse</name></json:item></author><host><volume>15</volume><pages><last>397</last><first>385</first></pages><author></author><title>Weinberg und Keller</title></host><title>Ein Versuch zur Bekämpfung der Bodenerosion in Hanglagen des Weinbaus durch Müllkompost</title></json:item><json:item><author><json:item><name>E. 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Toronto.</title></host></json:item><json:item><author><json:item><name>B. Walter</name></json:item></author><host><volume>7</volume><pages><last>210</last><first>207</first></pages><author></author><title>Rebe und Wein</title></host><title>Maßnahmen zur Bodenhaltung bei Flurbereinigungsverfahren weinbaulich genutzter Hanglagen</title></json:item><json:item><author><json:item><name>B. Walter</name></json:item></author><host><volume>15</volume><pages><last>333</last><first>319</first></pages><author></author><title>Weinberg und Keller</title></host><title>Die Gestaltung der Struktur unserer Weinbergsböden zur Erhaltung ihrer Fruchtbarkeit</title></json:item><json:item><author><json:item><name>A. 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Rates of erosion caused by gravitational mass movements and the action of running water differ. Catastrophic geomorphic events since 1972 are described qualitatively while quantitative data on precipitation, runoff, soil and solute loss during one year (1974‐5) from 13 plots in old and new vineyards (measuring 2m × 8, 16, 24, 32 and 48m) are presented. On the 20° slope plots erosion rates were 2.7cm/1,000 years in the old vineyard and 4.4 cm/1,000 years in the new vineyard. These results compare favourably with rates of 0.75‐4‐4 cm/1.000 years calculated from geological evidence. 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W.</namePart><namePart type="family">Negendank</namePart><affiliation>Geowissenschqftl. Laboratorium und Geolog. Begleitstudium der Fachgruppe Geographie der Universität Trier, Schneidershof, C‐5500 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">Sussex</placeTerm></place><dateIssued encoding="w3cdtf">1977-04</dateIssued><copyrightDate encoding="w3cdtf">1977</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">16</extent><extent unit="tables">4</extent><extent unit="references">14</extent></physicalDescription><abstract lang="en">Measurements and observations of soil erosion processes in vineyards on steep slopes in the German portion of the Moselle valley‐are described. Rates of erosion caused by gravitational mass movements and the action of running water differ. Catastrophic geomorphic events since 1972 are described qualitatively while quantitative data on precipitation, runoff, soil and solute loss during one year (1974‐5) from 13 plots in old and new vineyards (measuring 2m × 8, 16, 24, 32 and 48m) are presented. On the 20° slope plots erosion rates were 2.7cm/1,000 years in the old vineyard and 4.4 cm/1,000 years in the new vineyard. These results compare favourably with rates of 0.75‐4‐4 cm/1.000 years calculated from geological evidence. Both values are lower than those from many other agricultural plots and probably reflect the relative stability of the stony loams.</abstract><note type="funding">Deutsche Forschungsgeminschaft - No. Ri 147/9/10; </note><subject lang="en"><genre>keywords</genre><topic>Soil erosion</topic><topic>Erosion plots</topic><topic>Mass movement</topic><topic>Vineyards</topic></subject><relatedItem type="host"><titleInfo><title>Earth Surface Processes</title></titleInfo><titleInfo type="abbreviated"><title>Earth Surf. 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|clé= ISTEX:F6D840B99079209BFEA36209DB17CEEF256B3261
|texte= Soil erosion processes and their measurement in the german area of the Moselle river
}}
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