2018
DOI: 10.3390/pr6080107
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Effect of Pore Fluid Pressure on the Normal Deformation of a Matched Granite Joint

Abstract: The influence of pore fluid pressure on the normal deformation behaviors of joints is vital for understanding the interaction between hydraulic and mechanical processes of joints. The effect of pore fluid pressure on the normal deformation of a granite matched joint was investigated by laboratory experiments. Experimental results indicate pore fluid pressure significantly affects the normal deformation of jointed sample, and the relative normal deformation of jointed sample during fluid injection consists of t… Show more

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Cited by 12 publications
(4 citation statements)
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“…We have already used the same cores to study the influence of the intermediate principal stress (σ 2 ) on the permeability evolution during true triaxial compression [41]. Although this paper emphasizes the effect of confining pressure (P c ) on the strain-permeability behavior of mudstone, which can be tested by a conventional triaxial apparatus with a cylindrical specimen, the true triaxial apparatus for rocks [41][42][43][44][45] at the Institute of Rock and Soil Mechanics, Chinese Academy of Sciences, which can exert three stresses independently, was still employed in this study because the specimen usually failed with a relatively flat fault parallel to σ 2 [42,[46][47][48]; the flow in the σ 2 direction can still be regarded as a one-dimensional flow. In contrast, the fault of the specimen in the CTC is not only very rough but also oblique to the flow direction [40,49] and the fluid flow inside the specimen near or after failure cannot be approximated as a one-dimensional flow; therefore, the cores in this study were also processed into cuboid specimens of 5 cm square by 10 cm long ( Figure 1) and the permeability in the σ 2 direction was monitored during deviatoric loading.…”
Section: Specimen Apparatus and Experimental Proceduresmentioning
confidence: 99%
“…We have already used the same cores to study the influence of the intermediate principal stress (σ 2 ) on the permeability evolution during true triaxial compression [41]. Although this paper emphasizes the effect of confining pressure (P c ) on the strain-permeability behavior of mudstone, which can be tested by a conventional triaxial apparatus with a cylindrical specimen, the true triaxial apparatus for rocks [41][42][43][44][45] at the Institute of Rock and Soil Mechanics, Chinese Academy of Sciences, which can exert three stresses independently, was still employed in this study because the specimen usually failed with a relatively flat fault parallel to σ 2 [42,[46][47][48]; the flow in the σ 2 direction can still be regarded as a one-dimensional flow. In contrast, the fault of the specimen in the CTC is not only very rough but also oblique to the flow direction [40,49] and the fluid flow inside the specimen near or after failure cannot be approximated as a one-dimensional flow; therefore, the cores in this study were also processed into cuboid specimens of 5 cm square by 10 cm long ( Figure 1) and the permeability in the σ 2 direction was monitored during deviatoric loading.…”
Section: Specimen Apparatus and Experimental Proceduresmentioning
confidence: 99%
“…The effective stress principle is essential in stress-seepage field coupling [39]. A great deal of research has been conducted on this: Terzaghi [40] first proposed the concept of effective stress to describe the geotechnical medium via the coupling of external stress and pore water pressure. The formulation is as follows:…”
Section: Effective Stress Analysis Under Stress-seepage Couplingmentioning
confidence: 99%
“…The literature [40] suggests that an exponential model can be used to describe the relationship between permeability and effective stress in porous rocks:…”
Section: Effective Stress Analysis Under Stress-seepage Couplingmentioning
confidence: 99%
“…Based on orthogonal triaxial stress experiments with CH 4 seepage, the complete stress-strain relationship and the corresponding evolution of the volumetric strain and permeability were obtained. Zhang et al (2018) investigated the effect of pore-fluid pressure on normal deformation through laboratory experiments. The results indicated that the pore-fluid pressure significantly affects the normal deformation of a jointed sample.…”
Section: Introductionmentioning
confidence: 99%