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首页> 外文期刊>Science in China. Series D, Earth sciences >Seismic wave propagating in Kelvin-Voigt homogeneous visco-elastic media
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Seismic wave propagating in Kelvin-Voigt homogeneous visco-elastic media

机译:开尔文-沃伊特均质粘弹性介质中的地震波传播

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摘要

This paper studies, under a small disturbance, the responses of seismic transient wave in the visco-elastic media and the analytic solution of the corresponding third-order partial differential equation. A plane wave solution of Kelvin-Voigt homogeneous visco-elastic third-order partial differential equation with a pulse source is obtained. By the principle of pulse stacking of particle vibration, the result is extended to the solution of Kelvin-Voigt homogeneous visco-elastic third-order partial differential equation with any source. The velocities of seismic wave propagating and the attenuation of seismic wave in Kelvin-Voigt homogeneous visco-elastic media are discussed. The velocities of seismic wave propagating and the coefficient of attenuation of seismic wave in Kelvin-Voigt homogeneous visco-elastic media are derived, expressed as functions of density of the media, elastic modulus and visco-elastic coefficient. These results can be applied in inversing lithology parameters in geophysical prospecting.
机译:本文在小扰动下研究了粘弹性介质中地震瞬态波的响应以及相应的三阶偏微分方程的解析解。得到了带脉冲源的开尔文-沃格特均质粘弹性三阶偏微分方程的平面波解。根据粒子振动的脉冲叠加原理,将结果推广到任何源的开尔文-沃格特均质粘弹性三阶偏微分方程的解。讨论了开尔文-沃格特均质粘弹性介质中地震波传播的速度和地震波的衰减。推导了开尔文-沃格特均质粘弹性介质中地震波传播的速度和地震波的衰减系数,表示为介质密度,弹性模量和粘弹性系数的函数。这些结果可用于反演岩性参数的地球物理勘探中。

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