Effects of Water-Rock Interaction on Elastic Behaviors of Fully Water-Saturated Lacustrine Clay-Rich Shales: Experimental Investigation and Theoretical Modeling

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ID: 322832
2026
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Abstract
Summary Unlike marine shales, lacustrine Gulong shales deposited in semi-deep-to-deep lakes typically exhibit complex fluid-phase behavior and high clay mineral content. To study the saturation effects (e.g, frame stiffness, clay-water weakening) of in-situ shale, ultrasonic investigations into lacustrine shales from the Qingshankou (QSK) Formation were conducted under 100% water-saturated and confining (e.g, 5 -25 MPa) conditions. The data indicate that water saturation increases the P-wave velocity propagating perpendicular to the bedding plane (P0) by ~14%, while exerting a negligible effect on the P-wave velocity parallel to the bedding plane (P90); S-wave velocities consistently decrease (~10% for SH-wave and ~6% for SV-wave) from dry to fully saturated states. Furthermore, the experimental observations indicate a saturation-induced frame-weakening response in clay-rich shales, leading to a ~18% decrease in shear modulus at 100% water saturation. In addition, to qualitatively capturing the frame-weakening effect in 100% water-saturated shales in the velocity estimation, we proposed a Porosity-Clay modified Gurevich Squirt Flow (PCGS) model, which was introduced as a data-constrained phenomenological extension that accounts for effective saturation-induced frame weakening through empirical fitting of modulus variations. Compared with traditional fluid-substitution models, the PCGS model exhibits substantially improved accuracy (~10% for bulk modulus and ~15% for shear modulus).
Reference Key
openalex_W7171504473 Use this key to autocite in the manuscript while using SciMatic Manuscript Manager or Thesis Manager
Authors Li Zhu, Hui Li, Hao Zhang, Qingyuan Feng, Jinghuai Gao
Journal geophysical journal international
Year 2026
DOI
10.1093/gji/ggag300
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