Titlebook: Rock Physics and Natural Hazards; Sergio Vinciguerra,Yves Bernabé Book 2009 Birkh?user Basel 2009 Earthquake.fault.mechanical properties o

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Oscillating Flow of a Compressible Fluid through Deformable Pipes and Pipe Networks: Wave Propagatinductivities are introduced. Superposed on the classic viscous-inertial flow transition (controlled by the value of the pipe radius), these complex-valued parameters show another transition between an interference-free regime at low frequencies and a strong interference regime above a critical frequ

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Laboratory Characterization of Permeability and Its Anisotropy of Chelungpu Fault Rocks,an order of magnitude higher, ranging from 10. to 10. m.. To characterize permeability anisotropy associated with the bedding structure of the rocks of the Chelungpu fault, cylindrical samples were taken from the TCDP drillcores along three orthogonal directions, denoted X, Y and Z respectively. Dir

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Microstructural Inhomogeneity and Mechanical Anisotropy Associated with Bedding in Rothbach Sandstot (1) mechanical anisotropy is controlled by a preferred intergranular contact alignment parallel to the bedding and that (2) localization of compaction is controlled by bedding laminations and grain scale heterogeneity, which both prevent the development of well localized compaction features.

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Pressure-dependent Production Efficiency of an Enhanced Geothermal System (EGS): Stimulation Results a strong dependence on reservoir pressure. At increased reservoir pressure the artificial fractures of all stimulated intervals are highly conductive and subsequently become less conductive during pressure decline. Hence the range of a suitable reservoir pressure is constrained by this fracture ef

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Impact of Poroelastic Response of Sandstones on Geothermal Power Production,rmeability decreased by 21% at an effective pressure range from 3 to 30 MPa, the porosity decreased by 11% (..=6 to 65 MPa) and the Skempton coefficient decreased by 24% (..=4 to 25 MPa). We will show which mechanisms lead to the change of the mentioned hydraulic and poroelastic parameters and the i

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2504-3625 geologic objects and in laboratory samples. The remaining papers treat various aspects of rock physics and their industrial applications such as geothermics and reservoir characterization..978-3-0346-0121-4978-3-0346-0122-1Series ISSN 2504-3625 Series E-ISSN 2504-3633

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