具微结构地壳中非线性地震波的演化  

Evolution of nonlinear seismic waves in microstructured earth crust

作　　者：韩海英[1] 那仁满都拉[1] 双山[1] 

机构地区：[1]内蒙古民族大学物理与电子信息学院,通辽028043

出　　处：《物理学报》2012年第5期519-524,共6页Acta Physica Sinica

基　　金：国家自然科学基金(批准号:10862003;40564001);内蒙古民族大学科研创新团队建设计划资助的课题~~

摘　　要：非线性地震波在地壳中传播及演化规律的研究具有重要实际意义.利用有限差分方法,对非线性地震纵波和横波在具微结构地壳中的演化过程进行了详细的数值模拟.结果表明,非线性地震纵波和横波在具微结构地壳中可以逐渐演化成一个孤立波或两个孤立波或孤立波列或消失.地震波的初始幅度、频散系数和体力因子对演化过程和结果都有重要影响.研究结果揭示了非线性地震波在一种微结构地壳中的演化规律,这有助于在理论上解释一些特殊地震波现象.Study of propagation and evolution of nonlinear seismic wave in earth crust is of important practical significance. In this paper, evolutions of nonlinear seismic longitudinal wave and transverse wave in microstructured earth crust are simulated detailedly by using the finite difference method. The results indicate that nonlinear seismic longitudinal wave and transverse wave in microstructured earth crust may evolve into one solitary wave or two solitary waves or solitary wave train, or disappearance. The initial amplitude of seismic wave, dispersion coefficient and body force factor significantly influence the evolution process. Our results reveal the evolution law of nonlinear seismic wave in a microstructured earth crust, which will heln to exnlnin

关 键 词：地震波 孤立波 微结构地壳 

分 类 号：P631.4[天文地球—地质矿产勘探]