Recent trends of experimental geomorphology in the field
Identifieur interne : 000A52 ( Istex/Corpus ); précédent : 000A51; suivant : 000A53Recent trends of experimental geomorphology in the field
Auteurs : G. RichterSource :
- Earth Surface Processes and Landforms [ 0197-9337 ] ; 1981-05.
English descriptors
Abstract
Experimental geomorphology is a part of functional geomorphology. It tries to reach an exact analysis of the processes and to give statements on their importance for the recent relief forming. In all cautiousness the results may be transformed into more extensive areas and other time periods. Experimental geomorphology plays a differing role within the geomorphological research of the European countries. Most of the investigations deal with process studies and the quantification of weathering, mass movement, deflation, surface runoff, sediment transport in stream channels and denudation of watersheds. Experimental geomorphology should not be a goal in itself, but should be used as an applied geomorphology and for the examination of geomorphological theories as well.
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DOI: 10.1002/esp.3290060303
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ISTEX:BF6622EADA2089C28DA7B04F4F7B09A024B55E7ELe document en format XML
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Richter</name><affiliation><mods:affiliation>Abteilung Physische Geographie, Universität Trier, Postfach 3825, 5500 Trier, Federal Republic of Germany</mods:affiliation></affiliation></author></titleStmt><publicationStmt><idno type="wicri:source">ISTEX</idno><idno type="RBID">ISTEX:BF6622EADA2089C28DA7B04F4F7B09A024B55E7E</idno><date when="1981" year="1981">1981</date><idno type="doi">10.1002/esp.3290060303</idno><idno type="url">https://api.istex.fr/document/BF6622EADA2089C28DA7B04F4F7B09A024B55E7E/fulltext/pdf</idno><idno type="wicri:Area/Istex/Corpus">000A52</idno><idno type="wicri:explorRef" wicri:stream="Istex" wicri:step="Corpus" wicri:corpus="ISTEX">000A52</idno></publicationStmt><sourceDesc><biblStruct><analytic><title level="a" type="main" xml:lang="en">Recent trends of experimental geomorphology in the field</title><author><name sortKey="Richter, G" sort="Richter, G" uniqKey="Richter G" first="G." last="Richter">G. Richter</name><affiliation><mods:affiliation>Abteilung Physische Geographie, Universität Trier, Postfach 3825, 5500 Trier, Federal Republic of Germany</mods:affiliation></affiliation></author></analytic><monogr></monogr><series><title level="j">Earth Surface Processes and Landforms</title><title level="j" type="abbrev">Earth Surf. Process. Landforms</title><idno type="ISSN">0197-9337</idno><idno type="eISSN">1096-9837</idno><imprint><publisher>John Wiley & Sons, Ltd</publisher><pubPlace>Sussex</pubPlace><date type="published" when="1981-05">1981-05</date><biblScope unit="volume">6</biblScope><biblScope unit="issue">3‐4</biblScope><biblScope unit="page" from="215">215</biblScope><biblScope unit="page" to="219">219</biblScope></imprint><idno type="ISSN">0197-9337</idno></series><idno type="istex">BF6622EADA2089C28DA7B04F4F7B09A024B55E7E</idno><idno type="DOI">10.1002/esp.3290060303</idno><idno type="ArticleID">ESP3290060303</idno></biblStruct></sourceDesc><seriesStmt><idno type="ISSN">0197-9337</idno></seriesStmt></fileDesc><profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Denudation</term><term>Mass movement</term><term>Sediment transport</term><term>Soil erosion</term><term>Surface runoff</term></keywords></textClass><langUsage><language ident="en">en</language></langUsage></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">Experimental geomorphology is a part of functional geomorphology. It tries to reach an exact analysis of the processes and to give statements on their importance for the recent relief forming. In all cautiousness the results may be transformed into more extensive areas and other time periods. Experimental geomorphology plays a differing role within the geomorphological research of the European countries. Most of the investigations deal with process studies and the quantification of weathering, mass movement, deflation, surface runoff, sediment transport in stream channels and denudation of watersheds. Experimental geomorphology should not be a goal in itself, but should be used as an applied geomorphology and for the examination of geomorphological theories as well.</div></front></TEI><istex><corpusName>wiley</corpusName><author><json:item><name>G. 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It tries to reach an exact analysis of the processes and to give statements on their importance for the recent relief forming. In all cautiousness the results may be transformed into more extensive areas and other time periods. Experimental geomorphology plays a differing role within the geomorphological research of the European countries. Most of the investigations deal with process studies and the quantification of weathering, mass movement, deflation, surface runoff, sediment transport in stream channels and denudation of watersheds. Experimental geomorphology should not be a goal in itself, but should be used as an applied geomorphology and for the examination of geomorphological theories as well.</abstract><qualityIndicators><score>4.254</score><pdfVersion>1.3</pdfVersion><pdfPageSize>576 x 756 pts</pdfPageSize><refBibsNative>true</refBibsNative><abstractCharCount>776</abstractCharCount><pdfWordCount>2898</pdfWordCount><pdfCharCount>18249</pdfCharCount><pdfPageCount>5</pdfPageCount><abstractWordCount>113</abstractWordCount></qualityIndicators><title>Recent trends of experimental geomorphology in the field</title><refBibs><json:item><author><json:item><name>F. Ahnert</name></json:item></author><host><volume>25</volume><pages><last>49</last><first>29</first></pages><author></author><title>Zeitschrift für Geomorphologie Supp.</title></host><title>Brief description of a comprehensive three‐dimensional process‐response model of landform development</title></json:item><json:item><author><json:item><name>F. 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Young</name></json:item></author><host><volume>29</volume><pages><last>110</last><first>104</first></pages><author></author><title>Zeitschrift für Geomorphologie Suppl.</title></host><title>A twelve‐year record of soil movement on a slope</title></json:item></refBibs><genre><json:string>article</json:string></genre><host><volume>6</volume><publisherId><json:string>ESP</json:string></publisherId><pages><total>5</total><last>219</last><first>215</first></pages><issn><json:string>0197-9337</json:string></issn><issue>3‐4</issue><subject><json:item><value>Article</value></json:item></subject><genre><json:string>journal</json:string></genre><language><json:string>unknown</json:string></language><eissn><json:string>1096-9837</json:string></eissn><title>Earth Surface Processes and Landforms</title><doi><json:string>10.1002/(ISSN)1096-9837</json:string></doi></host><categories><wos><json:string>science</json:string><json:string>geosciences, multidisciplinary</json:string><json:string>geography, physical</json:string></wos><scienceMetrix><json:string>economic & social sciences</json:string><json:string>social sciences</json:string><json:string>geography</json:string></scienceMetrix></categories><publicationDate>1981</publicationDate><copyrightDate>1981</copyrightDate><doi><json:string>10.1002/esp.3290060303</json:string></doi><id>BF6622EADA2089C28DA7B04F4F7B09A024B55E7E</id><score>0.7083943</score><fulltext><json:item><extension>pdf</extension><original>true</original><mimetype>application/pdf</mimetype><uri>https://api.istex.fr/document/BF6622EADA2089C28DA7B04F4F7B09A024B55E7E/fulltext/pdf</uri></json:item><json:item><extension>zip</extension><original>false</original><mimetype>application/zip</mimetype><uri>https://api.istex.fr/document/BF6622EADA2089C28DA7B04F4F7B09A024B55E7E/fulltext/zip</uri></json:item><istex:fulltextTEI uri="https://api.istex.fr/document/BF6622EADA2089C28DA7B04F4F7B09A024B55E7E/fulltext/tei"><teiHeader><fileDesc><titleStmt><title level="a" type="main" xml:lang="en">Recent trends of experimental geomorphology in the field</title></titleStmt><publicationStmt><authority>ISTEX</authority><publisher>John Wiley & Sons, Ltd</publisher><pubPlace>Sussex</pubPlace><availability><p>Copyright © 1981 John Wiley & Sons, Ltd</p></availability><date>1981</date></publicationStmt><sourceDesc><biblStruct type="inbook"><analytic><title level="a" type="main" xml:lang="en">Recent trends of experimental geomorphology in the field</title><author xml:id="author-1"><persName><forename type="first">G.</forename><surname>Richter</surname></persName><affiliation>Abteilung Physische Geographie, Universität Trier, Postfach 3825, 5500 Trier, Federal Republic of Germany</affiliation></author></analytic><monogr><title level="j">Earth Surface Processes and Landforms</title><title level="j" type="abbrev">Earth Surf. Process. Landforms</title><idno type="pISSN">0197-9337</idno><idno type="eISSN">1096-9837</idno><idno type="DOI">10.1002/(ISSN)1096-9837</idno><imprint><publisher>John Wiley & Sons, Ltd</publisher><pubPlace>Sussex</pubPlace><date type="published" when="1981-05"></date><biblScope unit="volume">6</biblScope><biblScope unit="issue">3‐4</biblScope><biblScope unit="page" from="215">215</biblScope><biblScope unit="page" to="219">219</biblScope></imprint></monogr><idno type="istex">BF6622EADA2089C28DA7B04F4F7B09A024B55E7E</idno><idno type="DOI">10.1002/esp.3290060303</idno><idno type="ArticleID">ESP3290060303</idno></biblStruct></sourceDesc></fileDesc><profileDesc><creation><date>1981</date></creation><langUsage><language ident="en">en</language></langUsage><abstract xml:lang="en"><p>Experimental geomorphology is a part of functional geomorphology. It tries to reach an exact analysis of the processes and to give statements on their importance for the recent relief forming. 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It tries to reach an exact analysis of the processes and to give statements on their importance for the recent relief forming. In all cautiousness the results may be transformed into more extensive areas and other time periods. Experimental geomorphology plays a differing role within the geomorphological research of the European countries. Most of the investigations deal with process studies and the quantification of weathering, mass movement, deflation, surface runoff, sediment transport in stream channels and denudation of watersheds. 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It tries to reach an exact analysis of the processes and to give statements on their importance for the recent relief forming. In all cautiousness the results may be transformed into more extensive areas and other time periods. Experimental geomorphology plays a differing role within the geomorphological research of the European countries. Most of the investigations deal with process studies and the quantification of weathering, mass movement, deflation, surface runoff, sediment transport in stream channels and denudation of watersheds. Experimental geomorphology should not be a goal in itself, but should be used as an applied geomorphology and for the examination of geomorphological theories as well.</abstract><subject lang="en"><genre>keywords</genre><topic>Mass movement</topic><topic>Surface runoff</topic><topic>Soil erosion</topic><topic>Sediment transport</topic><topic>Denudation</topic></subject><relatedItem type="host"><titleInfo><title>Earth Surface Processes and Landforms</title></titleInfo><titleInfo type="abbreviated"><title>Earth Surf. Process. 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