da Costa Filho Carlos Alberto, Ravasi Matteo, Curtis Andrew, Meles Giovanni Angelo
School of GeoSciences, University of Edinburgh, Grant Institute, James Hutton Road, Edinburgh EH9 3FE, United Kingdom.
Phys Rev E Stat Nonlin Soft Matter Phys. 2014 Dec;90(6):063201. doi: 10.1103/PhysRevE.90.063201. Epub 2014 Dec 1.
The solution of the inverse scattering problem for the one-dimensional Schrödinger equation is given by the Marchenko equation. Recently, a Marchenko-type equation has been derived for three-dimensional (3D) acoustic wave fields, whose solution has been shown to recover the Green's functions from points within the medium to its exterior, using only single-sided scattered data. Here we extend this approach to 3D vectorial wave fields that satisfy the elastodynamic wave equation and recover Green's functions from points interior to an elastic, solid-state medium from purely external and one-sided measurements. The method is demonstrated in a solid-earth-like model to construct Green's functions using only subsurface sources, from earth-surface force and deformation sources and particle velocity and stress measurements.
一维薛定谔方程逆散射问题的解由马尔琴科方程给出。最近,针对三维(3D)声波场推导了一种马尔琴科型方程,其解已被证明仅使用单侧散射数据就能从介质内部的点恢复到外部的格林函数。在此,我们将此方法扩展到满足弹性动力学波动方程的三维矢量波场,并从纯外部和单侧测量中恢复弹性固态介质内部点的格林函数。该方法在一个类似固体地球的模型中得到了验证,即仅使用地下源、地表力和变形源以及质点速度和应力测量来构建格林函数。