Drained‐to‐undrained transition of bulk modulus in fluid‐saturated porous rock induced by dead volume variation

Author:

Tan Wenhui1,Müller Tobias M.12,Ba Jing1ORCID,Mikhaltsevitch Vassily3,Cao Chenghao4ORCID

Affiliation:

1. School of Earth Sciences and Engineering Hohai University Nanjing 211100 China

2. Department of Seismology Centro de Investigación Científica y de Educación Superior de Ensenada Ensenada Mexico

3. Faculty of Science and Engineering Curtin University Perth WA Australia

4. College of Transportation Science & Engineering Nanjing Tech University Nanjing 211100 China

Funder

National Natural Science Foundation of China

Consejo Nacional de Ciencia y Tecnología

Publisher

Wiley

Subject

Geochemistry and Petrology,Geophysics

Reference32 articles.

1. Seismic wave attenuation in carbonates

2. Rock anelasticity due to patchy‐saturation and fabric heterogeneity: A double double‐porosity model of wave propagation;Ba J.;Journal of Geophysical Research‐solid earth,2017

3. Fluid mobility and frequency-dependent seismic velocity — Direct measurements

4. General Theory of Three‐Dimensional Consolidation

5. Theory of Propagation of Elastic Waves in a Fluid‐Saturated Porous Solid. I. Low‐Frequency Range

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