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机构地区:[1]滨州学院,山东滨州256603 [2]中化地质矿山总局山东地质勘查院,山东济南250013
出 处:《物探化探计算技术》2012年第5期533-540,500,共8页Computing Techniques For Geophysical and Geochemical Exploration
基 金:滨州学院科研基金(BZXYL1107)
摘 要:应用双相介质波动方程,推导了双相横向各向同性介质(TI)中波动方程的有限差分格式,对双相TI介质中弹性波有限差分数值进行了模拟。结果表明,弹性波在双相TI介质中传播时,除了存在常规的快纵波(qP1)和横波以外,还存在慢纵波(qP2)。并且慢纵波的速度明显小于快纵波,而且受耗散系数的影响衰减地很快,所以在实际中很难观测到慢纵波。快纵波在固相和流相中相位相同,而慢纵波在固相和流相中的相位相反。慢纵波在流相中振幅大,而在固相中的振幅较小。Finite differential format of wave equation in two-phase transverse isotropic media(TI) is obtained by solving two-phase media wave equation,and the numerical simulation of elastic wave finite difference is carried out in two-phase TI media.The results show that in the two-phase elastic wave propagation in TI media,in addition to existing conventional fast P wave(qP1) and S wave,there is slow P wave(qP2),slow P wave was significantly less than the speed of fast P wave,and the dissipation coefficient attenuate very quickly,so in practice it is difficult to observe slow P wave.The phase of the fast P wave is same in both solid phase and liquid phase,and that of the slow P wave is reverse.the amplitude of the slow P wave in liquid phase is bigger than that in solid phase.
关 键 词:双相横向各向同性介质 交错网格 有限差分法 弹性波
分 类 号:P631.4[天文地球—地质矿产勘探]
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