arXivDaily arXiv每日学术速递 周一至周五更新
arXiv 1809.08313math.AP
收藏

弹性位错物理模型的分析

Analysis of a model of elastic dislocations in geophysics

Andrea Aspri, Elena Beretta, Anna L. Mazzucato, Maarten V. de Hoop

摘要:

我们分析了一个数学模型的弹性位错与应用程序的电子物理学,其中的弹性位错,我们的意思是一个开放的,有方向的Lipschitz表面在内部的弹性固体,有一个不连续的位移。我们将地球模型化为一个无限的、各向同性的、非均匀的、弹性的、占据半个空间的介质,并且只假设Lamé参数的Lipschitz连续性。我们研究的适定性的非常弱解的正问题,通过施加牵引-自由边界条件的表面,牵引的连续性和给定的跨越断层的位移跳跃确定的位移。我们采用适当的加权索伯列夫空间的分析。利用正问题的适定性和唯一延拓性,建立了由测量地球表面位移确定位错面和位移跃变的反问题的唯一性。对于切向跳跃或法向跳跃,在曲面上的某些几何条件下,唯一性成立。

英文摘要:

We analyze a mathematical model of elastic dislocations with applications to geophysics, where by an elastic dislocation we mean an open, oriented Lipschitz surface in the interior of an elastic solid, across which there is a discontinuity of the displacement. We model the Earth as an infinite, isotropic, inhomogeneous, elastic medium occupying a half space, and assume only Lipschitz continuity of the Lamé parameters. We study the well posedness of very weak solutions to the forward problem of determining the displacement by imposing traction-free boundary conditions at the surface, continuity of the traction and a given jump on the displacement across the fault. We employ suitable weighted Sobolev spaces for the analysis. We utilize the well posedness of the forward problem and unique-continuation arguments to establish uniqueness in the inverse problem of determining the dislocation surface and the displacement jump from measuring the displacement at the surface of the Earth. Uniqueness holds for tangential or normal jumps and under some geometric conditions on the surface.

机构、总结、中文摘要均由AI分析而来,可能存在错误,请以论文正文为准。

↑