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Normal compression wave scattering by a permeable crack in a fluid-saturated poroelastic solid 被引量:2
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作者 Yongjia Song hengshan hu John W. Rudnicki 《Acta Mechanica Sinica》 SCIE EI CAS CSCD 2017年第2期356-367,共12页
A mathematical formulation is presented for the dynamic stress intensity factor (mode I) of a finite permeable crack subjected to a time-harmonic propagating longitudinal wave in an infinite poroelastic solid. In part... A mathematical formulation is presented for the dynamic stress intensity factor (mode I) of a finite permeable crack subjected to a time-harmonic propagating longitudinal wave in an infinite poroelastic solid. In particular, the effect of the wave-induced fluid flow due to the presence of a liquid-saturated crack on the dynamic stress intensity factor is analyzed. Fourier sine and cosine integral transforms in conjunction with Helmholtz potential theory are used to formulate the mixed boundary-value problem as dual integral equations in the frequency domain. The dual integral equations are reduced to a Fredholm integral equation of the second kind. It is found that the stress intensity factor monotonically decreases with increasing frequency, decreasing the fastest when the crack width and the slow wave wavelength are of the same order. The characteristic frequency at which the stress intensity factor decays the fastest shifts to higher frequency values when the crack width decreases. 展开更多
关键词 Poroelasticity Biot's theory Finite crack Dynamic stress intensity factor
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The Parameter Averaging Technique in Finite-Difference Modeling of Elastic Waves in Combined Structures with Solid,Fluid and Porous Subregions
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作者 Wei Guan hengshan hu 《Communications in Computational Physics》 SCIE 2011年第8期695-715,共21页
To finite-difference model elastic wave propagation in a combined structure with solid,fluid and porous subregions,a set of modified Biot’s equations are used,which can be reduced to the governing equations in solids... To finite-difference model elastic wave propagation in a combined structure with solid,fluid and porous subregions,a set of modified Biot’s equations are used,which can be reduced to the governing equations in solids,fluids as well as fluidsaturated porous media.Based on the modified Biot’s equations,the field quantities are finite-difference discretized into unified forms in the whole structure,including those on any interface between the solid,fluid and porous subregions.For the discrete equations on interfaces,however,the harmonic mean of shear modulus and the arithmetic mean of the other parameters on both sides of the interfaces are used.These parameter averaging equations are validated by deriving from the continuity conditions on the interfaces.As an example of using the parameter averaging technique,a 2-D finite-difference scheme with a velocity-stress staggered grid in cylindrical coordinates is implemented to simulate the acoustic logs in porous formations.The finitedifference simulations of the acoustic logging in a homogeneous formation agree well with those obtained by the analytical method.The acoustic logs with mud cakes clinging to the borehole well are simulated for investigating the effect of mud cake on the acoustic logs.The acoustic logs with a varying radius borehole embedded in a horizontally stratified formation are also simulated by using the proposed finite-difference scheme. 展开更多
关键词 FINITE-DIFFERENCE wave equation porous medium acoustic logging numerical simulation
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