2018
DOI: 10.1016/j.clay.2018.04.033
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Shale softening: Observations, phenomenological behavior, and mechanisms

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Cited by 62 publications
(26 citation statements)
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“…Du et al [16,17] used deionized water for 48 hours without heating or applying pressure to soften the shale and degradation of mechanical properties after treatment. However, water-clay interaction will be different for actual natural gas reservoirs subjected to high temperature and pressure.…”
Section: Introductionmentioning
confidence: 99%
“…Du et al [16,17] used deionized water for 48 hours without heating or applying pressure to soften the shale and degradation of mechanical properties after treatment. However, water-clay interaction will be different for actual natural gas reservoirs subjected to high temperature and pressure.…”
Section: Introductionmentioning
confidence: 99%
“…The shape of the force-displacement curve after exposure to water-based fluids became less sharp indicating that the material after exposure changed from brittle to more ductile. Deterioration of shale hardness and strength upon exposure to water based fluids is a well-known phenomenon termed "shale softening" [20]. According to the literature, the main mechanisms responsible for "shale softening" are: (1) interaction of the foreign fluids with swelling clays present in shales that result in volumetric changes of the clay particles, (2) electrostatic repulsion between similarly charged clay particles, and (3) dissolution of cementation minerals [20].…”
Section: Resultsmentioning
confidence: 99%
“…Mixing of the shale pore fluid with the exposure fluid will thus cause the system to undergo changes toward a new equilibrium state. These changes may thus include: (1) ion exchange between clays and the new pore fluid followed by volumetric response of swelling clays (swelling, Energies 2021, 14, 2342 6 of 14 shrinkage), (2) changes in the interparticle interactions, (3) dissolution of some minerals due to contact with undersaturated solution [16,20]. minerals due to contact with undersaturated solution [16,20].…”
Section: Resultsmentioning
confidence: 99%
“…Ferrage [80] where Å refers to Ångström (1 Å = 0.1 nanometer). The exposure of shale to fluids with compositions even slightly different from those of in situ pore fluid induces a difference in chemical potential and changes the swelling pressure [81]. Under constant strain conditions, the increase of pressure due to adsorption-induced swelling can be as high as a hundred MPa up to a few GPa [82,83].…”
Section: Water Sensitivity Of Shale Rocksmentioning
confidence: 99%