Self-potential during multiphase flow in complex porous media
The rock pore space in many subsurface settings is saturated with water and one or more immiscible fluid phases; examples include non-aqueous-phase liquids (NAPLs) in contaminated aquifers, supercritical CO2 during sequestration in deep saline aquifers, the vadose zone, and hydrocarbon reservoirs. S...
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Imperial College London
2017
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Online Access: | https://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.718448 |