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1679年三河-平谷8级地震近断层强地震动的有限元模拟 被引量:11
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作者 潘波 许建东 刘启方 《地震地质》 EI CSCD 北大核心 2009年第1期69-83,共15页
文中通过收集整理三河-平谷8级地震的历史记录、野外地质调查和区域地震等资料,建立了该地震的震源模型;以穿过研究区的12条测线和区域第四纪、新近纪、古近纪沉积等厚度图等资料为基础,建立了北京地区的传播介质模型;利用哈尔滨工程力... 文中通过收集整理三河-平谷8级地震的历史记录、野外地质调查和区域地震等资料,建立了该地震的震源模型;以穿过研究区的12条测线和区域第四纪、新近纪、古近纪沉积等厚度图等资料为基础,建立了北京地区的传播介质模型;利用哈尔滨工程力学研究所的近断层强地震动有限元程序和40节点的高性能并行计算机计算了北京地区震后60s内地表各点的地震动速度时程和峰值速度。为检验模拟结果的质量,我们取2排测点的速度时程和水平向峰值速度等值线图进行了分析,发现计算结果与历史地震记录及实际地震观测资料吻合良好,说明了我们的模拟结果的可信性和模拟方法的客观性。 展开更多
关键词 强地震动 右旋走滑正断层 传播介质模型 并行计算 峰值速度 方向性效应 盆地效应
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Analysis of wave propagation on human body based on stratified media model 被引量:2
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作者 马力 沈海斌 刘磊 《Journal of Central South University》 SCIE EI CAS 2013年第12期3545-3551,共7页
Human body communication(HBC) is a promising near-field communication(NFC) method emerging in recent years. But existing theoretical models of HBC are too simple to simulate the wave propagation on human body. In this... Human body communication(HBC) is a promising near-field communication(NFC) method emerging in recent years. But existing theoretical models of HBC are too simple to simulate the wave propagation on human body. In this work, in order to clarify the propagation mechanism of electromagnetic wave on human body, a surface waveguide HBC theoretical model based on stratified media cylinder is presented. A numerical model analyzed by finite element method(FEM) is used for comparing and validating the theoretical model. Finally, results of theoretical and numerical models from 80 MHz to 200 MHz agree fairly well, which means that theoretical model can characterize accurate propagation mechanism of HBC signal. Meanwhile, attenuation constants derived from two kinds of models are within the range from 1.64 to 3.37, so that HBC signal can propagate effectively on human body. The propagation mechanism derived from the theoretical model is useful to provide design information for the transmitter and the modeling of the propagation channel in HBC. 展开更多
关键词 human body communication surface waveguide propagation mechanism stratified media propagation constant attenuation constant
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Modeling seismic wave propagation in a coal-bearing porous medium by a staggered-grid finite difference method
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作者 Zou Guangui Peng Suping Yin Caiyun Deng Xiaojuan Chen Fengying Xu Yanyong 《Mining Science and Technology》 EI CAS 2011年第5期727-731,共5页
A staggered-grid finite difference method is used to model seismic wave records in a coal bearing, porous medium. The variables analyzed include the order of the difference calculations, the use of a perfect match lay... A staggered-grid finite difference method is used to model seismic wave records in a coal bearing, porous medium. The variables analyzed include the order of the difference calculations, the use of a perfect match layer to provide absorbing boundary conditions, the source location, the stability conditions, and dispersion in the medium. The results show that the location of the first derivative of the dynamic variable with respect to space is coincident with the location of the first derivative of the kinematic varable with respect to time. Outgoing waves are effectively absorbed and reflection at the boundary is very weak when more than 20 perfect match layer cells are used. Blot theory considers the liquid phase to be homogeneous so the ratio of liquid to solid exposure of the seismic source depends upon the medium porosity. Numerical dispersion and generation of false frequencies is reduced by increasing the accuracy of the difference calculations and by reducing the grid size and time step. Temporal second order accuracy, a tenth order spatial accuracy, and a wavelength over more than ten grid points gave acceptable numerical results. Larger grid step sizes in the lateral direction and smaller grid sizes in the vertical direction allow control of dispersion when the medium is a low speed body. This provides a useful way to simulate seismic waves in a porous coal bearing medium. 展开更多
关键词 CoalPorous mediaStaggered-grid finite differenceSeismic wave propagation
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