Investigation of flow and solute transport through unsaturated chalk
The Chalk is a fractured rock with a fine-grained porous matrix, where the matrix provides most of the porosity and storage capacity and the fractures greatly enhance the permeability. For the unsaturated zone, the role of the fractures and the matrix in flow and solute transport is not well underst...
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University College London (University of London)
2005
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| Online Access: | http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.417027 |