As variaveis relevo e 'solo' na distribuicao desigual da umidade do solo. Avaliacao preliminar.

dc.contributorUniversidade Estadual Paulista (Unesp)
dc.date.accessioned2014-05-27T00:51:00Z
dc.date.accessioned2022-10-05T17:23:28Z
dc.date.available2014-05-27T00:51:00Z
dc.date.available2022-10-05T17:23:28Z
dc.date.created2014-05-27T00:51:00Z
dc.date.issued1985-12-01
dc.identifierGeociencias (Sao Paulo), v. 4, p. 101-110.
dc.identifierhttp://hdl.handle.net/11449/63741
dc.identifier2-s2.0-0022166066
dc.identifier.urihttp://repositorioslatinoamericanos.uchile.cl/handle/2250/3913924
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 summary
dc.languagepor
dc.relationGeociencias (Sao Paulo)
dc.rightsAcesso restrito
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.
dc.typeArtigo


Este ítem pertenece a la siguiente institución