Anisotropic Rock Poroelasticity Evolution in Ultra‐low Permeability Sandstones under Pore Pressure, Confining Pressure, and Temperature: Experiments with Biot's Coefficient-Reference-Cited by-同舟云学术

Anisotropic Rock Poroelasticity Evolution in Ultra‐low Permeability Sandstones under Pore Pressure, Confining Pressure, and Temperature: Experiments with Biot's Coefficient

Published:2021-06 Issue:3 Volume:95 Page:937-945
ISSN:1000-9515
Container-title:Acta Geologica Sinica - English Edition
language:en
Short-container-title:Acta Geologica Sinica ‐ English Edition

Author:

DU Shuheng¹

Affiliation:

1. State Key Laboratory of Nonlinear Mechanics, Institute of Mechanics Chinese Academy of Sciences Beijing 100190 China

Publisher

Wiley

Subject

Geology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1111/1755-6724.13886

Reference54 articles.

1. Multi-dimensional consolidation of layered poroelastic materials with anisotropic permeability and compressible fluid and solid constituents

2. Biot's coefficient as an indicator of strength and porosity reduction: Calcareous sediments from Kerguelen Plateau

3. General Theory of Three‐Dimensional Consolidation

4. Theory of Elasticity and Consolidation for a Porous Anisotropic Solid

5. An assessment of the effective density fluid model for scattering from poroelastic sediments with inclusions

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