Advective Displacement Method for the Characterisation of Pore Water Chemistry and Transport Properties in Claystone

The advective displacement method applies large hydraulic gradients to a confined rock core sample to yield small aliquots of the preserved in situ pore water, applicable to aquitard rocks with hydraulic conductivities as low as 10−14 m/s. Examples from argillaceous rocks indicate that only minor ar...

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Bibliographic Details
Main Author: Urs Mäder
Format: Article
Language:English
Published: Wiley 2018-01-01
Series:Geofluids
Online Access:http://dx.doi.org/10.1155/2018/8198762
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