上海国土资源
上海國土資源
상해국토자원
SHANGHAI LAND&RESOURCES
2014年
1期
97-100
,共4页
霍凤斌%李振鹏%徐发%张涛
霍鳳斌%李振鵬%徐髮%張濤
곽봉빈%리진붕%서발%장도
地震波场%波动方程%有限差分%边界条件%交错网格
地震波場%波動方程%有限差分%邊界條件%交錯網格
지진파장%파동방정%유한차분%변계조건%교착망격
seismic wave-ifeld%wave equation%ifnite difference%boundary condition%staggered grid
应用高阶交错网格有限差分算法,并加入吸收边界条件和衰减带,对弹性波方程进行模拟,分析了其稳定性和收敛性。通过对各向同性和各向异性介质模型的模拟表明,高阶差分波动方程模拟的网格频散较小、精度较高、效果较好,可为地震勘探及其资料解译提供技术手段。
應用高階交錯網格有限差分算法,併加入吸收邊界條件和衰減帶,對彈性波方程進行模擬,分析瞭其穩定性和收斂性。通過對各嚮同性和各嚮異性介質模型的模擬錶明,高階差分波動方程模擬的網格頻散較小、精度較高、效果較好,可為地震勘探及其資料解譯提供技術手段。
응용고계교착망격유한차분산법,병가입흡수변계조건화쇠감대,대탄성파방정진행모의,분석료기은정성화수렴성。통과대각향동성화각향이성개질모형적모의표명,고계차분파동방정모의적망격빈산교소、정도교고、효과교호,가위지진감탐급기자료해역제공기술수단。
This paper analyzes the stability and convergence of the seismic wave ifeld by using the high-order staggered-grid limited differential method of joining the absorbing boundary condition and attenuating zone to simulate the elastic wave equation. The results of the simulation of both isotropic-and anisotropic-medium models show that the grid frequency dispersion of the high-order differential wave equation simulation is smaller and more accurate. Therefore, this method should improve the efifciency of seismic prospecting and of the associated data interpretation.