共查询到18条相似文献，搜索用时 250 毫秒
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波动数值模拟的稳定性是获得可靠结果的前提.透射边界是一类具有高阶、高效等特点的人工边界,其引发的高频失稳是由内域格式和透射边界的不当耦合所致.本文针对P-SV波动有限元模拟中透射边界引发的失稳问题,基于GKS定理的群速度解释,通过对有限元和透射边界的频散分析揭示了数值失稳机理为透射边界和相邻内域格式支持了群速度指向内域的高频P波或SV波,波动能量将从边界进入内域引发数值失稳.同时,对比连续模型频散指出引发失稳的谐波是由有限元离散引入.本文采用修改的数值积分方法调整有限元刚度,以消除有限元中引发边界失稳的高频波动成分,从而稳定实现透射边界.理论分析和数值实验均表明本文稳定措施的有效性. 相似文献
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本文以紧凑形式给出了可以直接用于波动有限元计算的透射人工边界公式。为了阐明离散化误差和由人工边界引起的振荡失稳的基本概念,作者利用简单的一维模型详细分析了波动有限元模拟中遇到的这两个主要问题。基于在离散和连续模型中波动规律差别的分析,首先研究了离散化误差。这一研究导致对可能实现波动有限元模拟的频段的识别,以及采用一种兼备有限差和有限元优点的集中质量离散模型的建议。根据波在人工边界的放大效应和在有限离散模型中多次反射的概念在频域内阐明了这一常见的振荡失稳的机制。在此基础上提出了在保证数值计算精度的条件下通过对人工边界附近节点运动的修正来消除振荡失稳的措施。本文还以一维模型为例给出了人工边界条件的稳定性准则。 相似文献
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多次透射公式（MTF）物理概念简单，便于在计算机上实现时空解藕的高精度波动数值模拟。然而，MTF与其它局部人工边界条件类似，存在数值模拟失稳问题，如高频振荡便是可能出现的失稳现象。本文在分析MTF高频振荡失稳机理的基础上，提出了在波动有限元数值模拟中消除MTF高频振荡失稳的一种措施，即在整个有限元数值模拟区内施加与应变速率成正比的较小粘性阻尼；同时，讨论了这一稳定措施的有效性及其对数值计算精度的影响，并通过数值试验检验了这一稳定措施的可行性。结果表明，消除高频振荡失稳的措施行之有效，且只对波动有限元数值模拟中无意义的高频分量具有抑制作用，而对有意义的较低频段内的波动有限元数值模拟精度影响较小。 相似文献
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介绍了完美匹配层(PML)人工边界可以吸收不同频率和任意角度入射波的原理以及PML人工边界的构造方法. 在此基础上，将PML人工边界应用于地震波动数值模拟的速度应力混合有限元格式中，探讨了PML应用的可行性，并通过数值试验研究了PML人工边界的反射率，比较了PML人工边界与多次透射公式(MTF)人工边界应用于体波和面波模拟中数值反射的差异，对两种边界的透射效果进行了分析. 结果表明， 尽管数值离散后PML人工边界不再保持完美匹配特性，但PML人工边界在近场波动数值模拟中可获得比MTF人工边界更为理想的吸收效果，在角点透射、大角度掠射情形下尤为明显；PML人工边界在混合有限元格式的数值算法中，未见失稳等不良反应，比MTF人工边界有更好的稳定性；在合理选择参数的情况下，PML人工边界的运算量可接受. 相似文献
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本文对场地地震波动模拟中透射边界的稳定性问题进行了一系列研究。对已有的透射边界稳定措施做了比较分析,并给出了不同措施的适用性。结合粘弹性边界的物理模型提出了一个新的消除透射边界飘移失稳的措施,参考高频滤波的思路探讨了一种新的消除透射边界葛频振荡失稳的措施,并用数值试验验证了这两种新的透射边界稳定方法的有效性。将显式行限元一有限差分方法结合透射边界的数值解法的计算结果与解析结果作对比分析,验证这弹一套数值解法的计算精度。利用二维模型模拟了自贡土层和山脊地形的场地效应,利用显戈有限元一有限差分方法结合透射边界这套数值解法进行数值模拟计算,应用汶川地震的实示强震观测记录来验证这套数值解法对于实际地震波动模拟的有效性。 相似文献
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《地震工程与工程振动》2017,(1)
在波动数值模拟中,瑞利阻尼可近似描述介质耗散特性,且可用于抑制人工边界引发的高频和零频失稳,但瑞利阻尼对波动的影响尚未清晰认识。针对集中质量有限元模拟的一维波动,利用傅里叶模态分析了有阻尼离散网格中波动的性质。理论分析表明alpha阻尼必然使得波数为零及邻近的波动对应为非行进波,其使行波衰减一致,而beta阻尼不会导致波数为零及邻近的非行进波,其使行波衰减随着波数增大而增大。数值实验验证了上述结论。本文研究结果为进一步推进瑞利阻尼在波动数值模拟中的应用提供一定的理论依据。 相似文献
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波动数值模拟中透射边界的稳定实现 总被引：21，自引：0，他引：21
从波动能量在计算区内累积增大的观点出发,通过简单的一维弹性波模型,系统地阐明了在近场波动数值模拟中透射边界两类数值失稳--"高频振荡"和"零频飘移"的机理:前者源于对波动数值模拟无意义的高频波动在人工边界上的放大和波在有限计算区内多次反射产生的反复放大;后者则源于透射边界允许零频和接近零频的分量不断进入计算区. 由此提出了稳定实现透射边界的完整方案包括两项简单措施:第一,在全部计算区内按文中建议的方法注入小阻尼,以消除高频振荡;第二, 给出一种具有明确物理意义的消除零频飘移的算子算法. 最后,提供了三维波源问题和散射问题的详细数值试验结果. 相似文献
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Local coupling instability will occur when the numerical scheme of absorbing boundary condition and that of the field wave equation allow energies to spontaneously enter into the computational domain. That is, the two schemes support common wave solutions with group velocity pointed into the computation domain. The key to eliminate local coupling instability is to avoid such wave solutions. For lumped-mass finite element simulation of P-SV wave motion in a 2D waveguide, an approach for stable implementation of high order multi-transmitting formula is provided. With a uniform rectangular mesh, it is proven and validated that high-frequency local coupling instability can be eliminated by setting the ratio of the element size equal to or greater than \(\sqrt 2 \) times the ratio of the P wave velocity to the S wave velocity. These results can be valuable for dealing instability problems induced by other absorbing boundary conditions. 相似文献
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In numerical simulation of wave scattering under oblique incident body waves using the finite element method, the free field motion at the incident lateral boundary induced by the background layered half-space complicates the computational area. In order to replace the complex frequency domain method, a time-domain method to calculate the free field motion of a layered half-space subjected to oblique incident body waves is developed in this paper. The new method decouples the equations of motion used in the finite element method and offers an interpolation formula of the free field motion. This formula is based on the fact that the apparent horizontal velocity of the free field motion is constant and can be calculated exactly. Both the theoretical analysis and numerical results demonstrate that the proposed method offers a high degree of accuracy. 相似文献
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多次透射公式实用形式稳定性分析 总被引：1，自引：1，他引：0
景立平 《地震工程与工程振动》2004,24(4):20-24
本文以二维出平面波动方程为例,利用数值方法研究了多次透射公式的实用形式的稳定问题,结果表明：多次透射公式的实用形式与波动方程的集中质量显式有限元结合,不但存在零频漂移,而且同样存在高频振荡失稳,而与中心差分方法结合仅存在零频漂移失稳。 相似文献
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THE APPLICATION OF PML BOUNDARY CODITIONS IN THE SIMULATION OF SEISMIC WAVE BY THE HIGH-ORDER STAGGERED-GRID FINITE DIFFERENCES AT THE TRANSVERSELY ISOTROPIC MEDIA 
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下载免费PDF全文 In the realm of the numerical simulation, finite difference method and finite element method are more intuitive and effective than other simulation methods. In the process of simulating seismic wave propagation, the finite differences method is widely used because of its high computational efficiency and the advantage of the algorithm is more efficient. With the demand of precision, more and more researchers have proposed more effective methods of finite differences, such as the high-order staggered-grid finite differences method, which can restore the actual process of wave propagation on the premise of ensuring accuracy and improving the efficiency of operation. In the past numerical simulation of seismic wave field, different models of isotropic medium are mostly used, but it is difficult to reflect the true layer situation. With the research demand of natural seismology and seismic exploration, the research on anisotropic media is more and more extensive. Transversely isotropic(TI)media can well simulate the seismic wave propagation in the formation medium, such as gas-bearing sandstone, mudstone, shale et al., the character of TI media is reflected by introducing the Thomsen parameters to reflect its weak anisotropy of vertical direction by using Thomson parameter. Therefore, studying the process of seismic wave propagation in TI media can restore the true information of the formation to the greatest extent, and provide a more reliable simulation basis for the numerical simulation of seismic wave propagation. In the geodynamic simulation and the numerical simulation of the seismic wave field, under the limited influence of the calculation area, if no boundary conditions are added, a strong artificial boundary reflection will be generated, which greatly reduces the validity of the simulation. In order to minimize the influence of model boundaries on the reflection of seismic waves, it is often necessary to introduce absorbing boundary conditions. At present, there are three types of absorption boundary conditions: one-way wave absorption boundary, attenuation absorption boundary, and perfectly matched layer(PML)absorption boundary. In terms of numerical simulation of seismic waves, the boundary absorption effect of PML is stronger than the first two, which is currently the most commonly used method, and it also represents the cutting-edge development direction of absorption boundary technology. The perfectly matched layer absorbing boundary is effectively applied to eliminating the reflective waves from model boundaries, but for transversely isotropic medium, the effect of the absorbing is not very well. For this reason, the elastic dynamic wave equations in transversely isotropic media are derived, and we describe a second-order accurate time, tenth-order accurate space, formulation of the Madariaga-Virieux staggered-grid finite difference methods with the perfectly matched layer(PML)are given. In addition, we have established vertical transversely isotropic(VTI)media and arbitrary inclined tilted transversely isotropic(TTI)media models, using a uniform half-space velocity model and a two-layer velocity model, respectively. By combining the actual geoscience background, we set the corresponding parameters and simulation conditions in order to make our model more research-oriented. When setting model parameters, different PML thickness, incident angle, source frequency and velocity layer models were transformed to verify the inhibition of boundary reflection effect by PML absorption boundary layer. The implementations of this simulation show that the formula is correct and for the transversely isotropic(TI)media of any angular symmetry axis, when the thickness of the PML layer reaches a certain value, the seismic wave reflection effect generated by the artificial boundary can be well suppressed, and the absorption effect of PML is not subject to changes in incident angle and wave frequency. Therefore, the results of our study indicate that our research method can be used to simulate the propagation process of seismic waves in the transversely isotropic(TI)media without being affected by the reflected waves at the model boundary to restore the actual formation information and more valuable geological research. 相似文献
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应用高精度人工边界条件可有效提升近场波动数值模拟计算效率.完美匹配层是吸收层形式高精度人工边界条件,匹配层内场方程和界面条件通常分别采用复坐标延伸技术变换强形式无限域内波动方程和界面条件得到,亦曾将无限域界面条件当作匹配层界面条件.场方程和界面条件构建过程相互独立,可能出现匹配不合理而引发数值失稳、计算精度低下等问题.本文提出采用复坐标延伸技术变换弱形式无限域波动方程以构建完美匹配层的方法.弱形式波动方程耦合了波动方程及界面条件,进而规避了变换后所得场方程与界面条件之间的匹配不合理问题.新方法可直接建立弱形式匹配层,在此基础上亦可给出强形式匹配层.弱形式便于有限元离散,强形式便于有限差分离散.基于弱形式完美匹配层,结合勒让德谱元建立了弹性介质近场波动谱元模拟方案.利用算例验证了新方案的精度及数值稳定性.本文工作可直接推广至多相耦合介质近场波动数值模拟. 相似文献
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A local time-domain transmitting boundary for simulating cylindrical elastic wave propagation in infinite media 总被引：3，自引：0，他引：3
Finite element simulation of the time-dependent wave propagation in infinite media requires enforcing the transmitting boundary to replace the truncated far-field infinite domain so as to model the effect of the wave radiation towards infinity. This paper proposed a novel local time-domain transmitting boundary for simulating the cylindrical elastic wave radiation problem. This boundary is a mechanical model consisting of the spring, dashpot and mass elements, with the auxiliary degrees of freedom introduced, which is dynamically stable and easily implemented into the commercial finite element codes. Numerical analysis of the cylindrical elastic wave radiation problem indicates that the proposed transmitting boundaries with the order N=3 for cylindrical P and SV waves and with the order N=4 for cylindrical SH wave have very high accuracy, even when the artificial boundary at wave source. The proposed transmitting boundary with order N=0 can be applied approximately to the general two-dimensional infinite elastic wave problems that contain the more complex outgoing wave fields at artificial boundary than the cylindrical waves. The plane-strain Lamb problem is analyzed with the acceptable engineering accuracy achieved. On the other hand, the proposed transmitting boundary with higher order can be a tool to localize the temporal convolution that appears in an exact time-domain transmitting boundary for the general infinite wave problems. This potential applicability is mentioned. 相似文献
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A numerical scheme is developed in the paper for calculating torsional, vertical, horizontal, coupling and rocking impedances in frequency domain for axial-symmetric foundations embedded in layered media. In the scheme, the whole soil domain is divided into interior and exterior domains. For the exterior domain, the analytic solutions with unknown coefficients are obtained by solving three-dimensional (3D) wave equations in cylindrical coordinates satisfying homogeneous boundary conditions. For the interior domain, the analytical solutions are also obtained by solving the same 3D wave equations satisfying the homogeneous boundary conditions and the prescribed boundary conditions. The prescribed conditions are the interaction tractions at the interfaces between embedded foundation and surrounding soil. The interaction tractions are assumed to be piecewise linear. The piecewise linear tractions at the bottom surface of foundation will be decomposed into a series of Bessel functions which can be easily fitted into the general solutions of wave equations in cylindrical coordinates. After all the analytic solutions with unknown coefficients for both interior and exterior domains are found, the variational principle is employed using the continuity conditions (both displacements and stresses) at the interfaces between interior and exterior domains, interior domain and foundation, and exterior domain and foundation to find impedance functions. 相似文献
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P. Dangla 《地震工程与结构动力学》1988,16(8):1115-1128
A plane strain model for dynamic soil-structure interaction problems under harmonic state is presented. The boundary element method is used to study the response of a homogeneous isotropic linear elastic soil. The far field displacement at the free surface is approximated by an outgoing Rayleigh wave. The finite element method is used to describe the response of the building, of the foundation and possibly of a finite part of the inhomogeneous non-linear soil. Two coupling procedures are described. The model is applied to a problem previously studied in the antiplane case. Incident P, SV and Rayleigh waves are considered. The results show an amplification and an attenuation of the structure motion with frequency when incident Rayleigh waves and P, SV body waves are respectively considered. 相似文献