Inverse Solutions for Two-Dimensional Elastic Waves in a Nonhomogeneous Medium
スポンサーリンク
概要
- 論文の詳細を見る
An inverse procedure has been developed to obtain an exact solution for the travel time of seismic rays transmitted through a nonhomogeneous medium in which the seismic velocity depends only on depth from the surface. If the nonhomogenity is in the form of distinct, horizontal layers (graded material), then the procedure of ensuring continuous displacement and stress across the interface between homogeneous layers is straight forward but involves a considerable amount of algebra. However, if the nonhomogeneous medium has a continuous variation of properties (gradient material), then the problems are reduced to Abel's integral equation.
- 一般社団法人日本機械学会の論文
- 1987-12-16
著者
関連論文
- Steady Thermal Stresses in Bonded Dissimilar Finite Plates Containing External Interface Cracks
- The Inverse Problem for the String or Rod Clamped at Both Sides
- Inverse Solutions for Two-Dimensional Elastic Waves in a Nonhomogeneous Medium