改进的浅水海底地震波场显式时域解法

IF 2.1 3区 地球科学 Q2 GEOSCIENCES, MULTIDISCIPLINARY
Weihao Cao , Guangli Cheng , Bao Liu , Yangfan Cai
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引用次数: 0

摘要

浅水海底地震波场是由流体-弹性介质耦合方程得到的。在耦合方程的时域解中,针对受时间步长和精度限制的显式时域法的稳定性,根据系统在稳定状态下的时间步长与固有频率的反比关系,在考虑计算效率的前提下,剔除不稳定模态,并根据残差最小准则,确定了三个步骤下的最优步权值。据此,提出了稳定显式三步中心差分法。与经典的显式中心差分法相比,该方法具有四阶精度,并通过海底地震波场模型对其计算性能进行了验证和分析。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Improved explicit time-domain solution for seafloor seismic wavefield in shallow water
The shallow water seafloor seismic wavefield is obtained by the coupled equation of fluid and elastic medium. In the time-domain solution of the coupled equation, for the stability of the explicit time-domain method which is limited by the time step and the accuracy, according to the inverse relationship between the time step and the natural frequency of the system under the stable condition, the unstable modes are removed and according to the criterion of the minimum residual difference under the premise of taking into consideration of the computational efficiency, the optimal step weight value under the three-step is determined. Accordingly, the stable explicit three-step center difference method is proposed. Compared with the classical explicit center difference method, the proposed method has fourth-order accuracy, and its better computational performance is verified and analyzed by using a seafloor seismic wavefield model.
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来源期刊
Journal of Applied Geophysics
Journal of Applied Geophysics 地学-地球科学综合
CiteScore
3.60
自引率
10.00%
发文量
274
审稿时长
4 months
期刊介绍: The Journal of Applied Geophysics with its key objective of responding to pertinent and timely needs, places particular emphasis on methodological developments and innovative applications of geophysical techniques for addressing environmental, engineering, and hydrological problems. Related topical research in exploration geophysics and in soil and rock physics is also covered by the Journal of Applied Geophysics.
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