Closing an open system: Pore pressure changes in permeable edifice rock at high strain rates
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文摘

“Undrained” describes deformation on a timescale that precludes fluid movement.

In this case, dilatancy reduces pore pressure and compaction increases pore pressure.

Microcracked and porous volcanic rocks do not exhibit dilatancy hardening.

Undrained compaction does not result in pore pressure embrittlement.

Implications for edifice stability and outgassing are discussed.

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