2009
DOI: 10.1016/j.ijrmms.2008.04.005
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On the relationship between stress and elastic strain for porous and fractured rock

Abstract: a b s t r a c tModeling the mechanical deformations of porous and fractured rocks requires a stress-strain relationship. Experience with inherently heterogeneous earth materials suggests that different varieties of Hooke's law should be applied within regions of the rock having significantly different stress-strain behavior. We apply this idea by dividing a rock body conceptually into two distinct parts. The natural strain (volume change divided by rock volume at the current stress state), rather than the engi… Show more

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Cited by 208 publications
(174 citation statements)
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“…The existence of the residual fracture aperture for fractured rock has been well documented in the rock-mechanics literature (e.g., Rutqvist et al 2002;Liu et al 2009). However, the existence of such an aperture is not totally clear yet for coal cleats.…”
Section: Fracture Permeabilitymentioning
confidence: 95%
See 1 more Smart Citation
“…The existence of the residual fracture aperture for fractured rock has been well documented in the rock-mechanics literature (e.g., Rutqvist et al 2002;Liu et al 2009). However, the existence of such an aperture is not totally clear yet for coal cleats.…”
Section: Fracture Permeabilitymentioning
confidence: 95%
“…Because of the similarity between coal-seam permeability-stress relationships and those for fractured rock, research results from the field of rock mechanics (focused on understanding fracture-matrix interactions and their effects on fracture permeability) can be utilized for this study. Recently, Liu et al (2009) developed a new theoretical relationship between stress and elastic strain for porous and fractured rock, based on the reasoning that as a result of the heterogeneous nature of rock materials, different varieties of Hooke's law should be applied for different regions of the rock having significantly different stress-strain behaviors. They applied this idea by dividing a rock body (or a fracture) conceptually into two distinct parts, and further argued that the natural strain (volume change divided by rock volume at the current stress state), rather than the engineering strain (volume change divided by the unstressed rock volume), should be used in Hooke's law for accurate modeling of the elastic deformation of the part subject to a relatively large degree of relative deformation.…”
Section: Fracture Permeabilitymentioning
confidence: 99%
“…For this analysis, the layering of the OPA is explicitly implemented by alternating layers of different material properties, allowing the soft layer to deform more than the stiffer layer, similar to the two-part Hooke's model described in Liu et al (2009) . This allows preferential gas migration into "softer" interlayers having somewhat higher porosity and correspondingly enhancing permeability before migrating to the next interlayer.…”
Section: Modeling Approachmentioning
confidence: 99%
“…However, as described by Settari and Mourits (1998), in practice it is more important to consider the nonlinear stress-dependent effects on porosity and permeability over the range of stress expected in a problem. Such properties may be derived directly from laboratory data and fitted to theoretical or empirical functions (e.g., Liu et al, 2009) or by calibration to field experiments (e.g., Rutqvist et al, 2008).…”
Section: Comparison Of Rocmas and Tough-flac To Other Thm Codesmentioning
confidence: 99%