Variations in soil dispersivity across a gully head displaying shallow subsurface pipes, and the role of shallow pipes in rill initiation
Abstract
This article discusses how three-dimensional patterns of geochemistry and sediment size can be related to hydraulic gradients in the local marl bedrock of Almería in southern Spain.Citation
Earth surface processes and landforms, 2004, 29(9), pp. 1143-1160.Publisher
John Wiley & SonsDOI
10.1002/esp.1109Additional Links
http://eu.wiley.com/WileyCDA/WileyTitle/productCd-ESP.htmlType
ArticleLanguage
enDescription
This article is not available through ChesterRep.ISSN
01979337Sponsors
This article was submitted to the RAE2008 for the University of Chester - Geography and Environmental Studies.ae974a485f413a2113503eed53cd6c53
10.1002/esp.1109