1887

Abstract

In this paper we show through a molecular scale mechanics simulation that structural order of water near charged surfaces results in a finite shear stiffness of the water phase. This interpretation is supported with experimental data on compacted claystone. We illustrate how the results may be applied in a rock physics model for mudstone / shale.

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/content/papers/10.3997/2214-4609.20145399
2010-04-26
2021-01-28
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.20145399
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