elastic wave equation
英 [ɪˈlæstɪk weɪv ɪˈkweɪʒn]
美 [ɪˈlæstɪk weɪv ɪˈkweɪʒn]
网络 弹性波方程
双语例句
- The Study of Inverse Method with Parameters about Two-Dimensional Elastic Wave Equation
二维弹性波方程参数反演方法研究 - Wave field separation numerical modeling of second order elastic wave equation by high-precision staggered-grid finite difference scheme
二阶弹性波动方程高精度交错网格波场分离数值模拟 - In order to study the wave field characteristics in the elastic random medium models, through the simulations of the elastic wave equation, we simulated the propagation of the plane wave in the 2-D elastic random medium models.
为研究弹性随机介质模型中的波场特征，本文使用弹性波动方程正演模拟了平面波在二维弹性随机介质模型中的传播。 - In the theoretical part, the elastic wave equation in a semi-infinite media, and the wave propagation on a layered material, as well as its interaction on phase velocity have been studied, which provided the basis and hypothesis for the further research. 2.
从理论方面，研究半无限大介质内弹性波的波动方程，分析了分层材料内表面物理性能相对弹性波传播速度的相对关系，为后续研究工作提供了理论支持和技术假设。 - The study puts forward the precision difference solution to elastic wave equation, using staggered mesh random even rank, and formula for tilted contact surface's refraction blind zones.
研究提出了弹性波方程交错网格任意偶数阶精度差分解法及倾斜界面地表折射盲区计算公式。 - Through the elastic wave equation numerical simulation results of the typical fluctuation surface and near-surface velocity mode, understanding and analyzing the characteristics of seismic wave field, main types of seismic waves and seismic wave propagation, thus the near-surface analysis of the impact of reflected wave field.
通过典型起伏地表和近地表速度模型的弹性波方程数值模拟结果，来认识、分析地震波波场特征、地震波主要类型以及地震波传播规律，从而分析复杂地表对地下反射波场的影响。 - 36 formulae of reflection and transmission coefficients on anisotropic interface are derived from elastic wave equation in anisotropic medium.
本文从各向异性介质的弹性波波动方程出发，推导出各向异性介质界面上36个反射和透射系数的计算公式。 - The classical elasticity mathematics theory was established for ideal medium abiding Hooke law grimly, the earth medium is a viscoelastic medium with viscosity in fact, so elastic wave equation can not be used to describe the propagation of seismic waves in real media.
经典弹性数学理论是对精确遵守虎克定律的理想介质建立的，而实际大地介质是具有粘滞性的粘弹性介质，所以完全弹性波动方程不能够准确地描述地震波在实际介质中的传播过程。 - Hybrid method combining finite difference and pseudospectral method for solving the elastic wave equation
有限元法与伪谱法混合求解弹性波动方程 - Multi-component combined post-stack reverse-time migration of anisotropic elastic wave equation
各向同性等离子体层各向异性弹性波动方程多分量联合叠后逆时偏移