Variations in soil dispersivity across a gully head displaying shallow subsurface pipes, and the role of shallow pipes in rill initiation
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AbstractThis 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.
CitationEarth surface processes and landforms, 2004, 29(9), pp. 1143-1160.
PublisherJohn Wiley & Sons
DescriptionThis article is not available through ChesterRep.
SponsorsThis article was submitted to the RAE2008 for the University of Chester - Geography and Environmental Studies.