物探与化探
物探與化探
물탐여화탐
GEOPHYSICAL AND GEOCHEMICAL EXPLORATION
2014年
6期
1275-1283
,共9页
张伟%甘伏平%刘伟%郑智杰
張偉%甘伏平%劉偉%鄭智傑
장위%감복평%류위%정지걸
双相介质%瑞雷面波%有限差分%交错网格%PML吸收边界%镜像法自由边界%稳定性分析%起伏分界面模型
雙相介質%瑞雷麵波%有限差分%交錯網格%PML吸收邊界%鏡像法自由邊界%穩定性分析%起伏分界麵模型
쌍상개질%서뢰면파%유한차분%교착망격%PML흡수변계%경상법자유변계%은정성분석%기복분계면모형
biphasic media%Rayleigh surface wave%finite difference%staggered grids%PML absorbing boundary condition%free boundary condition of image method%stability analysis%undulating interface model
为了研究双相介质瑞雷面波的形成机制及传播规律,促进瑞雷面波资料处理方法的发展。文章根据弹性波动方程,采用交错网格有限差分算法,对二维各向同性弹性介质做解析解与数值解的对比,在此基础上,将PML吸收边界条件,改进的镜像法应用于双相介质波动方程中,并作了稳定性分析,对双相介质水平层状、起伏分界面等典型模型瑞雷面波及体波在内的全波场进行研究。结果表明:基于弹性介质解析解与数值解的对比,在误差接受范围内,研究双相介质是可行的;把稍作改进的镜像法应用于双相介质中,能够有效地处理瑞雷面波自由边界问题;通过详细分析双相介质瑞雷面波及体波在内的全波场的信息,对以双相介质为基础的地震波勘探有一定的指导作用。
為瞭研究雙相介質瑞雷麵波的形成機製及傳播規律,促進瑞雷麵波資料處理方法的髮展。文章根據彈性波動方程,採用交錯網格有限差分算法,對二維各嚮同性彈性介質做解析解與數值解的對比,在此基礎上,將PML吸收邊界條件,改進的鏡像法應用于雙相介質波動方程中,併作瞭穩定性分析,對雙相介質水平層狀、起伏分界麵等典型模型瑞雷麵波及體波在內的全波場進行研究。結果錶明:基于彈性介質解析解與數值解的對比,在誤差接受範圍內,研究雙相介質是可行的;把稍作改進的鏡像法應用于雙相介質中,能夠有效地處理瑞雷麵波自由邊界問題;通過詳細分析雙相介質瑞雷麵波及體波在內的全波場的信息,對以雙相介質為基礎的地震波勘探有一定的指導作用。
위료연구쌍상개질서뢰면파적형성궤제급전파규률,촉진서뢰면파자료처리방법적발전。문장근거탄성파동방정,채용교착망격유한차분산법,대이유각향동성탄성개질주해석해여수치해적대비,재차기출상,장PML흡수변계조건,개진적경상법응용우쌍상개질파동방정중,병작료은정성분석,대쌍상개질수평층상、기복분계면등전형모형서뢰면파급체파재내적전파장진행연구。결과표명:기우탄성개질해석해여수치해적대비,재오차접수범위내,연구쌍상개질시가행적;파초작개진적경상법응용우쌍상개질중,능구유효지처리서뢰면파자유변계문제;통과상세분석쌍상개질서뢰면파급체파재내적전파장적신식,대이쌍상개질위기출적지진파감탐유일정적지도작용。
In order to study the mechanism and propagation of Rayleigh surface wave in biphasic media and promote the development of data?processing method of Rayleigh surface wave, the authors applied finite difference method with staggered grids to simulate the 2D i?sotropic elastic media based on the elastic wave equation, and made a comparison between the analytical and numerical solutions. On such a basis, the PML absorbing boundary condition and improved image method can be applied to the two?phase medium wave equa?tion to simulate the typical media model including horizontal layer and undulating interface, analyze the full wave information including the Rayleigh surface wave and body wave, and make a stability analysis. The results show that, on the basis of the comparison between the numerical solution and the analytical solution of the elastic media within the acceptable range of the error, the study of biphasic me?dium is feasible. The slight improvement of the image method can be applied to biphasic media to deal with free boundary condition problem of the Rayleigh surface wave effectively. The detailed analysis of the full wave field information of biphasic media including the Rayleigh surface wave and body wave shows that it has played a guiding role in the seismic exploration on the basis of biphasic media.