【24h】

HYBRID SIMULATION OF SEISMIC WAVE PROPAGATION IN LATERALLY INHOMOGENEOUS MEDIA

机译:横向不均匀介质中地震波传播的混合模拟

获取原文

摘要

The main aim of this work is to develop, validate and applied in simulation study an efficient hybrid approach to study 2D seismic wave propagation in local multilayered geological region rested on inhomogeneous in depth half-space with a seismic source. Plane strain state is considered. The vertically varying of the soil properties in the half space is modelled by a set of horizontal flat isotropic, elastic and homogeneous layers. The finite local region is with nonparallel layers and with a free surface relief. The hybrid computational tool is based on the analytical wave number integration method (WNIM) and the numerical boundary integral equation method (BIEM). The WNIM is applied considering the bedrock model to compute the input signals for the laterally varying part where the signals are obtained by BIEM at a set of sites. The numerical simulation results reveal that the hybrid method is able to demonstrate the sensitivity of the obtained synthetic signals to the seismic source properties, to the heterogeneous character of the wave path and to the relief peculiarities of the local stratified geological deposit.
机译:这项工作的主要目的是开发,验证并在模拟研究中应用的有效混合方法来研究在本地多层地质区域2D地震波传播歇不均匀深度半空间与地震源。平面应变状态被认为。垂直改变在半空间中的土壤性质的由一组水平的平坦各向同性的,弹性的和均匀的层的建模。有限局部区域是具有非平行的层和具有自由表面浮雕。所述混合计算工具是基于所述分析的波数积分法(WNIM)和数值边界积分方程方法(BIEM)。所述WNIM已应用考虑基岩模型来计算所述输入信号,用于在信号被BIEM在一组位点的获得的横向变化的部分。数值模拟结果表明,该混合方法能够将得到的合成信号的灵敏度展示给地震源性质,于波路径的多相性质和本地分层地质沉积物的浮雕特殊性。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号