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Please use this identifier to cite or link to this item: http://acervodigital.unesp.br/handle/11449/63741
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dc.contributor.authorBarbosa, C. F.-
dc.contributor.authorDa, J. R.-
dc.date.accessioned2014-05-27T00:51:00Z-
dc.date.accessioned2016-10-25T18:12:02Z-
dc.date.available2014-05-27T00:51:00Z-
dc.date.available2016-10-25T18:12:02Z-
dc.date.issued1985-12-01-
dc.identifier.citationGeociencias (Sao Paulo), v. 4, p. 101-110.-
dc.identifier.urihttp://hdl.handle.net/11449/63741-
dc.identifier.urihttp://acervodigital.unesp.br/handle/11449/63741-
dc.description.abstractIn a general way the analysis of soil water content enabled one to define which of the colluvium units hold larger water retention capacity. They are: Bela Vista, Piracema I, Campo Alegre, Bom Retiro and Treviso II. These results suggest that the contact zones among alostratigraphic units with high and low water retention capacity are potential zones for the generation of subsurface flow (throughflow). -from English summaryen
dc.format.extent101-110-
dc.language.isopor-
dc.sourceScopus-
dc.subjecthillslope hydrology-
dc.subjectsoil erosion-
dc.subjectsoil water content-
dc.subjectsubsurface flow-
dc.titleAs variaveis relevo e 'solo' na distribuicao desigual da umidade do solo. Avaliacao preliminar.pt
dc.title.alternativeTopography and soil as factors affecting the soil water content distribution: a preliminary evaluationen
dc.typeoutro-
dc.contributor.institutionUniversidade Estadual Paulista (UNESP)-
dc.rights.accessRightsAcesso restrito-
dc.relation.ispartofGeociencias (Sao Paulo)-
dc.identifier.scopus2-s2.0-0022166066-
Appears in Collections:Artigos, TCCs, Teses e Dissertações da Unesp

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