isotropic medium

基本解释

The method can be used to both crystal crystal and isotropic medium crystal interfaces.
这一方法既能应用于晶体-晶体界面，也能应用于各向同性媒质-晶体界面。
However, coal is usually assumed to be an isotropic medium in the traditional coal seismic exploration, and the impacts of fractures on seam are not taken into account.
传统的煤田地震勘探将煤层假设为单一的各向同性介质，没有考虑其中裂隙对煤层的影响。
By use of coordinate transformation, the multilayered anisotropic medium is changed into a homogeneous isotropic medium and a theoretical T-D equation of seismic reflection wave is derived.
利用坐标变换方法，将多层的各向异性介质转换成均匀各向同性介质，从而推导出地震反射波理论时-深方程。通过模型的测定，介绍了各向异性系数的求取及地质剖面的构制方法。