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1.
地表下圆形夹塞区出平面散射对地面运动的影响   总被引:21,自引:0,他引:21       下载免费PDF全文
采用波函数展开方法,提出弹性半空间埋藏的圆形弹性夹塞区对平面SH波二维散射的封闭级数解答.利用内域型Graf加法公式,将解答归结为一组无穷代数方程组的求解.通过对无穷方程组的截断计算,得到了解答的数值结果;并通过边值条件的收敛,检验了截断计算的精度.最后给出若干典型算例说明夹塞区产生的散射场对地表运动的复杂影响.  相似文献   

2.
半空间异质隆起的出平面动力响应:闭合级数解答   总被引:1,自引:0,他引:1  
采用分区思想和辅助函数方法,利用波函数展开技术,提出了水平地表圆形非匀质隆起出平面动力响应的闭合级数解答。将解答归结为一组无穷代数方程组的求解,解答的数值结果可由无穷方程的截断计算得出。计算结果表明,给出的闭合解答在宽频带内能很快收敛。  相似文献   

3.
任意圆弧形凸起地形对平面SH波的散射   总被引:22,自引:10,他引:22  
本文采用波函数展开方法提出弹性半空间表面一任意圆弧形凸起边界对平面SH波二维散射的封闭级数解答,利用引入的辅助函数和推广的外域型Graf加法公式将解答归结为一代无穷代数方程组的求解,解答的数值结果可由无穷方程的截断计算得出,文中从级数项数增加时计算结果的收敛以及边界条件的收敛满足两方面检验了截断计算的精度,并指出了位移解答的收敛速度与主要参数之间的关系,同时,对凸起角点的应力奇异性及其对解答精度的  相似文献   

4.
本文用有限阶截断矩阵和抛物线叠代近似求根法数值求解了大气潮汐全日振荡模的本征值一本征函数问题,求得了20×20阶截断本征值和本征向量。计算结果表明本征值的虚部比实部小若干量级,从而由计算实验证实了大气潮汐本征值问题有限阶截断矩阵的近似厄密特性。文中还叙述了变矩阵阶次以确定计算收敛性的实验结果,并与前人的结果进行了对比分析。  相似文献   

5.
半无限空间中圆形孔洞周围SH波的散射   总被引:14,自引:5,他引:14  
建立了求解在含有圆形孔洞的弹性半空间中SH波散射与圆形孔洞附近动应力集中问题的解析方法。利用SH波散射的对称性和多极坐标的方法,构造了一个可以预先满足半空间自由表面上应力自由边界条件的圆形孔洞对SH波散射的波函数。利用这一波函数,则可将该问题转化成对一个圆形孔洞散射的求解问题。该问题的解答最终又可归结为对一组无究代数方程组的求解问题,并可利用截断有限项的方法对其进行计算,最后给出了有关圆形也洞附近动应力集中问题的算例和数值结果,并讨论了波数与圆孔至自由边界距离变化对动应力集中的影响。  相似文献   

6.
速度、密度之间的相互耦合使得密度在多参数全波形反演中较难获得.本文将截断高斯-牛顿法用于声介质速度、密度双参数全波形反演,通过考虑近似Hessian矩阵中反映速度、密度相互作用的非主对角块元素,有效解决了多参数全波形反演中速度、密度之间的耦合问题,在不采用反演策略的情况下,仍能够获得精度较高的速度、密度反演结果.常规的截断牛顿类全波形反演通常利用一阶伴随状态法求取目标函数对模型参数的梯度,利用二阶伴随状态法或有限差分法求解Hessian-向量乘,在每一步内循环迭代过程中需要额外求解两次正演问题,计算量较大.本文基于Born近似,将梯度计算中的核函数-向量乘表示为具有明确物理意义的向量-标量乘的累加运算,同时将Hessian-向量乘转化为两次核函数-向量乘,无需额外求解正演问题,有效降低了计算量.数值实验证明了本文提出的方法的有效性.  相似文献   

7.
文章利用“契合”思想,给出了地下弹性夹杂与地面上的等腰三角形凸起地形引起的SH波散射问题的解析解答。利用复平面下坐标移动,通过区域Ⅰ和区域Ⅱ以及区域Ⅱ和区域Ⅲ的“公共边界”位移应力连续条件,建立起求解该问题的无穷代数方程组并截断有限项进行求解,最后通过具体算例及结果分析得出相应结论。  相似文献   

8.
四阶非线性海浪波面高度的统计分布   总被引:5,自引:3,他引:5  
基于非线性随机海浪模型,在四阶近似下,通过直接求矩的方法,导出了海浪波面高度统计分布为截断的Gram-Charlier级数.解释了Huang等发现的增致λ~g时符合更坏的现象.讨论了近似阶次对级数截断和系数确定的影响.对于m阶近似,分布级数的截断项为H_(3m-3),并且H_(3m-4)项不出现,H_(3m-3)与H_(3m-6)项的系数间存在简单的代数关系.  相似文献   

9.
地面导线环是变频测深发射天线的一种形式.Wait曾计算了离地面高度为h的小导线环的辐射电阻,但由于所用近似方法的限制,他得出的结果不能用在置于地面的导线环的情况(若令h=0,所给出的辐射电阻将等于∞).在本文中,我们导出了具有有限半径的地面导线环的辐射电阻表达式(准确的以及近似的),并给出了数值计算的结果.  相似文献   

10.
胶莱盆地重磁资料解释与构造特征分析   总被引:9,自引:0,他引:9  
胶莱盆地位于郯庐断裂带东侧,是典型的拉张盆地,内部划分为诸城凹陷、柴沟地垒、高密凹陷、大野头凸起、莱阳凹陷、牟平──即墨断裂带、海阳凹陷。运用重力资料一级近似解法,定量计算了胶莱盆地基底埋深,结合磁异常解释等,本文重点讨论了盆地内主要断裂的形成时期,切割深度及空间演化。并进一步将诸城凹陷细分为胶县洼陷、集王疃洼陷、平度洼陷、马山构造带、刘家庄构造带、李党家构造带。讨论总结了该盆地构造特征及其发育规律,为该区油气勘探提供了新的认识与依据。  相似文献   

11.
A closed-form solution of two-dimensional scattering of plane SH waves by a cylindrical alluvial valley of circular-arc cross-section in a half-space is presented using the wave functions expansion. The solution is reduced to solving a set of infinite linear algebraic equations using the exterior region form of Graf's addition theorem. Numerical solutions are obtained by truncation of the infinite equations and their accuracies are demonstrated by convergence of the numerical results to the exact boundary condition with the increasing of the truncation order. The present solution is compared with the existing one presented by Todorovska and Lee for the same problem and their differences are analysed. Complicated effects of the depth-to-width ratio of the alluvial valley on surface ground motion are finally illustrated.  相似文献   

12.
A closed-form solution of two-dimensional scattering of plane SH waves by a cylindrical canyon of circular-arc cross-section in a half-space is studied using the wave functions expansion method. The solution is reduced to solving infinite linear algebraic equations using the Graf's addition theorem in an appropriate form. Numerical results of the solution are obtained by truncation of the infinite equations and accuracies of the truncation are checked by the extent to which the numerical results fit the boundary condition and by convergence of the numerical results with the truncation order. Complicated effects of the depth-to-width ratio of the canyon on surface ground motion are shown by the numerical results for typical cases.  相似文献   

13.
A closed-form solution of two-dimensional scattering of plane SH waves by a cylindrical hill of circular-arc cross-section in a half-space is presented using the wave functions expansion method. The solution is reduced to solving a set of infinite linear algebraic equations, using the auxiliary functions and the exterior region form of the Graf's addition theorem. Numerical solutions are obtained by truncation of the infinite equations and their accuracies are demonstrated by convergence of the numerical results and by the extent to which the numerical results fit the exact boundary conditions with increasing the truncation order. The numerical results for some typical cases are then presented for checking accuracies of various numerical methods. The effects of the height-to-width ratio of the hill on surface ground motion are finally illustrated.  相似文献   

14.
A closed-form analytic solution of two-dimensional scattering and diffraction of plane SH waves by a semicylindrical hill with a semi-cylindrical concentric tunnel inside an elastic half-space is presented using the cylindrical wave functions expansion method. The solution is reduced to solving a set of infinite linear algebraic equations. Fourier expansion theorem with the form of complex exponential function and cosine function is used. Numerical solutions are obtained by truncation of the infinite equations. The accuracy of the presented numerical results is carefully verified.  相似文献   

15.
张郁山 《地球物理学报》2010,53(9):2129-2143
利用波函数的Fourier-Bessel级数展开法,推导出了含任意多个圆弧状沉积层的谷地在Rayleigh波入射下二维稳态动力响应的解析解,分析了该级数形式解析解随截断项数的收敛问题,讨论了在获取该解析解的过程中,用于计算Rayleigh波自由场的有限Fourier级数的项数和用于模拟水平地表的大圆弧的半径对解的影响.研究结果表明,该解析解能够在一个非常宽的频带内收敛.最后,利用该解析解,在一个较宽的频带范围内,讨论了谷地中沉积介质的成层性,包括沉积层的层数、软弱夹层的存在及其厚度等因素对地面运动的影响.  相似文献   

16.
Dynamic response of an alluvial valley consisting of three different types of soil was studied. In the two-dimensional model, the alluvial valley was assumed to have half-cylindrical shape. The alluvial valley contained three different types of soil with different shapes. The valley was surrounded by a half-space. All of the soil types and the half-space were assumed to be isotropic, homogeneous and linear elastic. The half-space was excited by simple harmonic SH-waves radiated from a strike-slip fault. The fault was assumed to have circular-arc shape in the mathematical model. The governing equations were solved by using wave function expansion method where boundary conditions were relatively simple. In the regions where boundary conditions were more complex, finite difference method was employed. Consequently, the wave propagation problem was solved semi-analytically. The obtained numerical results showed that surface displacement amplitudes are significantly affected by the material properties of the different soil types of the alluvial valley. It was also observed that the shapes of the soil types in the alluvial valley played a considerable role in surface displacements.  相似文献   

17.
圆弧状沉积盆地与软土单覆盖层出平面地表运动对比   总被引:2,自引:0,他引:2  
采用解析方法,通过圆弧状沉积盆地与同样参数的软土均匀单覆盖层的对比,研究沉积盆地对平面SH波二维散射效应和其出平面地表运动。数值对比结果表明:(1)波垂直入射时盆地中央地表位移幅值反应,其随频率变化形式与软土单覆盖层的地表运动有较强的对应性,且此时单覆盖层地表位移幅值为其下降;(2)盆地的二维散射效应特点显著波的汇聚作用使盆地中的地表运动显著放大,总体上较软土单覆盖层的地表位移幅值要大,其频域内的最大反应则明显大于单覆盖层情况,但最大反应在盆地表面出现的位置依赖于入射波角度、盆地深宽比和盆地的软硬程度;(3)沉积盆地中地表位移运动有强烈扭转效应,且随盆地变软和入射波频率增高而增强。  相似文献   

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