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