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Morfología Fluvial.-Morpholgical change in a stream channel as consequence of the fluvial dynamics (Vallcebre)

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dc.contributor.authorSoler, M.
dc.contributor.authorNord, G.
dc.contributor.authorLatron, J.
dc.contributor.authorGallart, F.
dc.contributor.otherUniversidad de Murciaes
dc.date.accessioned2020-10-27T15:58:29Z
dc.date.available2020-10-27T15:58:29Z
dc.date.created2009-09
dc.description.abstractABSTRACT This study shows the morpholgical changes observed in a stream channel as consequence of the fluvial dynamics in an experimental research basin (Vallcebre,Eastern Pyrenees). Three cross sections were surveyed along a 100 metres distance near the basin outlet. The cross sections were measured 21 times from 2003 to 2008. Along the study period, higher deposition rates were observed in summer whereas higher erosion rates were observed in April. Considering the whole period, an average resulting deposition of 7 cm has been measured. At the flood scale, correlation analysis, revealed weak correlations between the magnitude of the changes in the stream bed and the main hydrometeorological variableses
dc.formatapplication/pdfes
dc.format.extent4es
dc.identifier.urihttp://hdl.handle.net/10201/97690
dc.languagespaes
dc.languageenges
dc.relationSin financiación externa a la Universidad de Murciaes
dc.relation.ispartofCongreso internacional sobre desertizaciónes
dc.rightsinfo:eu-repo/semantics/openAccesses
dc.rightsAttribution-NonCommercial-NoDerivatives 4.0 International*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0/*
dc.subjectstream channeles
dc.subjectcross sectiones
dc.subjecterosion/depositiones
dc.subjecttest Spearmanes
dc.subject.otherCDU::5 - Ciencias puras y naturales::55 - Geología. Meteorologíaes
dc.titleMorfología Fluvial.-Morpholgical change in a stream channel as consequence of the fluvial dynamics (Vallcebre)es
dc.typeinfo:eu-repo/semantics/otheres
dspace.entity.typePublicationes
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