集中力作用下的两相饱和介质位移场Green函数

以复模两相饱和介质Biot动力学方程为基础,根据该方程D'Alembert解的Fourier变换所属的Homholtz方程特性,由Biot方程解的相容性条件及δ函数性质较好地解决了快、慢纵波位势的耦合问题.较为简便地得到了两相饱和介质在集中力作用下低频(ω＜ωc)时的频域和时域的Green函数.     

Dynamic Green’s functions of a two-phase saturated medium subjected to a concentrated force

The Green’s functions of a two-phase saturated medium subjected to a concentrated force are known to play an important role in seismology, earthquake engineering, soil dynamics, geophysics, and dynamic foundation theory. This paper presents a physical method for obtaining the dynamic Green’s functions of a two-phase saturated medium for materials considered to be isotropic and for low frequencies. First, the pore-fluid pressure in a two-phase saturated medium is divided into two parts: flow pressure and deformation pressure. Next, based on the compatibility condition of Biot’s equation and the property of the δ-function, the problem of coupled_fast and slow dilational waves is solved using the decomposition condition of the potential dilation field. The Green’s function for a concentrated force is then obtained by solving Biot’s complex modular equations, and their physical characteristics are discussed. The behavior of Green’s functions for the solid and fluid phases of a δ-impulsive force is investigated, from which the Green’s functions for a unit Heaviside force are also obtained by time integration. Finally, the present Green’s functions for a unit Heaviside force are compared with those obtained by a purely mathematical method; the two differ in form, but the numerical results are identical. The physical meaning of the expressions of Green’s functions obtained in this paper is evident. Therefore, the results may benefit future research on the dynamic responses of a two-phase saturated medium.     

Lamb's integral formulas of two-phase saturated medium for soil dynamic with drainage

When dynamic force is applied to a saturated porous soil,drainage is common.In this paper,the saturated porous soil with a two-phase saturated medium is simulated,and Lamb's integral formulas with drainage and stress formulas for a two-phase saturated medium are given based on Biot's equation and Betti's theorem(the reciprocal theorem).According to the basic solution to Biot's equation,Green's function Gij and three terms of Green's function G4i,Gi4,and G44 of a two-phase saturated medium subject to a concentrated force on a spherical coordinate are presented.The displacement field with drainage,the magnitude of drainage,and the pore pressure of the center explosion source are obtained in computation.The results of the classical Sharpe's solutions and the solutions of the two-phase saturated medium that decays to a single-phase medium are compared.Good agreement is observed.     

Lamb＇s integral formulas of two-phase saturated medium for soil dynamic with drainage

When dynamic force is applied to a saturated porous soil, drainage is common. In this paper, the saturated porous soil with a two-phase saturated medium is simulated, and Lamb＇s integral formulas with drainage and stress formulas for a two-phase saturated medium are given based on Biot＇s equation and Betti＇s theorem （the reciprocal theorem）. According to the basic solution to Biot＇s equation, Green＇s function Gij and three terms of Green＇s function G4i, Gi4, and G44 of a two-phase saturated medium subject to a concentrated force on a spherical coordinate are presented. The displacement field with drainage, the magnitude of drainage, and the pore pressure of the center explosion source are obtained in computation. The results of the classical Sharpe＇s solutions and the solutions of the two-phase saturated medium that decays to a single-phase medium are compared. Good agreement is observed.     

Solutions of Green's function for Lamb's problem of a two-phase saturated medium

The solutions of Green's function are significant for simplification of problem on a two-phase saturated medium. Using transformation of axisymmetric cylindrical coordinate and Sommerfeld's integral, superposition of the influence field on a free surface, authors obtained the solutions of a two-phase saturated medium subjected to a concentrated force on the semi-space.     

A 2.5-D dynamic model for a saturated porous medium: Part I. Green’s function

Based on Biot’s theory, the dynamic 2.5-D Green’s function for a saturated porous medium is obtained using the Fourier transform and the potential decomposition methods. The 2.5-D Green’s function corresponds to the solutions for the following two problems: the point force applied to the solid skeleton, and the dilatation source applied within the pore fluid. By performing the Fourier transform on the governing equations for the 3-D Green’s function, the governing differential equations for the two parts of the 2.5-D Green’s function are established and then solved to obtain the dynamic 2.5-D Green’s function. The derived 2.5-D Green’s function for saturated porous media is verified through comparison with the existing solution for 2.5-D Green’s function for the elastodynamic case and the closed-form 3-D Green’s function for saturated porous media. It is further demonstrated that a simple form 2-D Green’s function for saturated porous media can be been obtained using the potential decomposition method.     

双相介质半空间内椭圆夹杂对透射SH波的散射

为探究双相介质弹性半空间内椭圆弹性夹杂对透射SH波的散射问题,主要采用Green函数法、复变函数法、保角映射法和极坐标移动技术。首先,引入复变量并在复平面上运用保角映射的方法将椭圆边界映射为单位圆边界;然后,将双相介质沿垂直边界剖开分成两个四分之一空间,在剖分面上作用附加力系使SH波在垂直边界上满足位移和应力连续的条件,并构造四分之一空间内点源荷载作用下的Green函数位移场;进而,利用"契合"的思想在垂直边界上建立定解积分方程组,并利用SH波衰减的性质进行有限项截断来求解未知附加力系。最后,通过具体算例得出在不同参数情况下椭圆夹杂周边动应力集中因子分布情况。结果得知,SH波的入射角度和频率以及介质的性质对夹杂周边动应力集中分布有一定影响。     

双相介质半空间中圆孔对透射SH波的稳态分析

研究了平面SH波在半空间双相弹性介质中的传播。通过Green函数和积分方程方法,按照复变函数描述,对透射波被圆孔散射的情况进行稳态分析。将双相介质半空间沿界面剖分为1/4空间介质Ⅰ和含圆孔的1/4空间介质Ⅱ,分别构造了介质Ⅰ和介质Ⅱ中反平面点源荷载的Green函数,按双相介质中平面SH波的处理方法,给出介质Ⅰ和介质Ⅱ中的平面位移波,两种介质之间的相互作用力与对应Green函数的乘积沿界面的积分与平面位移波叠加得到介质Ⅰ和介质Ⅱ中的全部位移场。按照界面的位移连续条件,定解积分方程组,得到问题的稳态解,并给出圆孔位置和介质参数对散射的影响。     

非饱和土-隧道系统动力响应计算的波函数法

针对非饱和地基土中埋置隧道的三维动力响应计算问题, 提出了波函数法.采用无限长的Flügge薄壁圆柱壳模拟圆形隧道衬砌,采用流、固、气组成的三相介质模拟非饱和地基土体.分别采用分离变量法以及Helmholtz矢量分解定理求解薄壁圆柱壳的振动控制方程与非饱和土的波动方程.根据隧-土交界面与地表面处的应力、位移以及孔隙流体压力等边界条件,利用平面波与柱面波的转换性质,实现了隧道内作用单位简谐载荷时隧道衬砌与土体系统动力响应的耦合求解.通过与既有单相弹性介质2.5维有限元-边界元法、两相饱和多孔介质2.5维有限元-边界元法以及三相非饱和介质Pip in Pip半解析法的计算结果进行对比, 验证了本文计算方法的可靠性. 最后,基于该方法, 通过算例分析了不同饱和度下非饱和土-隧道系统的动力响应特征.结果表明, 饱和度对土体动位移与超孔隙水压力的幅值响应有较大影响.该方法的非饱和地基土参数退化后,也可用来计算和分析饱和地基土或单相弹性地基土与隧道系统的动力响应.      

非饱和土半空间Lamb问题及能量传输特性

地球表面绝大多数土层处于非饱和状态, 故采用传统饱和两相介质理论进行动力学分析时, 结果往往与实际情况不符. 针对这一问题, 本文以非饱和半空间作为研究对象, 基于连续介质力学和多孔介质理论, 考虑非饱和多孔介质中各相的质量守恒方程、动量守恒方程、本构方程以及有效应力原理等基本方程, 建立了以骨架位移、孔隙水压力和孔隙气压力为基本未知量的动力学控制方程. 针对非饱和半空间表面在竖向集中简谐荷载作用下的动力学响应及能量传输问题, 建立了频域内经典Lamb问题的轴对称计算模型, 采用Helmholtz分解法, 通过引入势函数Φ和Ψ表示骨架的位移分量, 结合本构方程获得了不同边界条件下半空间表面位移场和能量场等物理量的解析解答, 并通过数值算例对荷载参数(激振频率)、材料参数(饱和度、渗透系数)等影响因素进行了分析与讨论. 结果表明: (1)饱和度的升高或者激振频率下降, 都会提高非饱和半空间的表面位移幅值; (2)当渗透系数下降至一临界值时, 地表位移幅值会趋于一极限值, 并且透水(气)边界与不透水(气)边界条件下渗透系数的影响表现出明显的差异性.      

饱和土中球空腔的瞬态动力响应

采用工程上通用的饱和土力学模型,考虑流体与固全之间的耦合作用,利用Ｌａｐｌａｃｅ变换求解了饱和土中球空腔的瞬态动力响应问题,得到了变换域内的解析解,借助数值Ｌａｐｌａｃｅ换求解了饱和土中球空腔瞬态动力响应的位移、应力及孔压的变化规律,为分析地下结构瞬态动力响应提供了一种有效的方法,模型符合工程实际,有一定的工程应用价值。     

爆炸荷载作用下饱和半空间中衬砌隧道弹性动力响应IBIEM模拟

基于Biot两相介质理论,采用一种高精度间接边界积分方程法（IBIEM）研究了饱和半空间中浅埋衬砌隧道在内部爆炸荷载作用下的瞬态弹性动力反应。通过典型算例,给出了爆炸荷载作用下隧道附近地表位移、衬砌动应力、围岩径向位移和衬砌表面孔隙水压的时程响应,并对比分析了饱和半空间和全空间中隧道动力响应的区别。研究表明：覆土层厚度对浅埋隧道-围岩整体动力响应特征具有明显影响;衬砌表面透水状态对爆炸荷载的时程响应的影响不显著;随半空间饱和介质孔隙率增加,围岩受隧道内部爆炸影响程度降低,衬砌承担的爆炸作用增大;当和直达波、衬砌内部反射波的峰值叠加作用时,半空间表面反射波对衬砌隧道拱顶附近响应影响显著,使得衬砌动应力幅值、径向位移相比深埋情况大幅度增加。     

Response of saturated porous media subjected to local thermal loading on the surface of semi-infinite space

Heat source function method is adopted in the present paper to derive elementary solutions of coupled thermo-hydro-mechanical consolidation for saturated porous media under conjunct actions of instantaneous point heat source, instantaneous point fluid source and constant volume force. By using the so-called fictitious heat source method and images method, the solutions of a semi-infinite saturated porous medium subjected to a local heat source with time-varied intensity on its free surface are developed from elementary solutions. The numerical integral methods for calculating the unsteady temperature, pore pressure and displacement fields are given. The thermomechanical response are analyzed for the case of a circular planar heat source. Besides, the thermal consolidation characteristics of a saturated porous medium subjected to a harmonic thermal loading are also given, and the fluctuation processes of the field variables located below the center of heat source are analyzed. The project supported by the National Natural Science Foundation of China (50578008) The English text was polished byYunming Chen.     

SH波对内含裂纹衬砌结构的散射及动应力集中

当衬砌结构内含裂纹时 ,采用Green函数的方法 ,研究了SH波对裂纹的散射及其动应力集中 ,构造了在含有半圆形衬砌的弹性半空间上 ,在水平面上任一点承受时间谐和出平面线源载荷作用时的位移函数作为Green函数 ;推导了SH波对衬砌内有裂纹的散射定解积分方程组 ,进而求得裂纹尖端的动应力因子 ,重点讨论了衬砌及周围介质对裂纹尖端动应力因子的影响 ,给出了介质参数变化对裂纹尖端动应力因子的影响曲线 ,为工程设计提供了依据。     

The parameter perturbation method on elastic wave equation in inhomogeneous medium

I.IntroductionTheelasticwaveininhomogeneousmediumiscomplicatedbecauseofthediffracting,scattering,andtransmutingofthewavetapes.Exceptforsomesimpleandregularmediummode1s,thesolutionofelasticwavehasnotbeengotyet.Nowadays,theresearchoftheelasticwavescattering…     

Green’s functions for plane problem under various boundary conditions and applications

Green’s functions of a point dislocation as well as a concentrated force for the plane problem of an infinite plane containing an arbitrarily shaped hole under stress, displacement, and mixed boundary conditions are stated. The Green’s functions are obtained in closed forms by using the complex stress function method along with the rational mapping function technique, which makes it possible to deal with relatively arbitrary configurations. The stress functions for these problems consist of two parts: a principal part containing singular and multi-valued terms, and a complementary part containing only holomorphic terms. These Green’s functions can be derived without carrying out any integration. The applications of the Green’s functions are demonstrated in studying the interaction of debonding and cracking from an inclusion with a line crack in an infinite plane subjected to remote uniform tension. The Green’s functions should have many other potential applications such as in boundary element method analysis. The boundary integral equations can be simplified by using the Green’s functions as the kernels.     

三维粘弹性层状半空间埋置集中荷载动力格林函数求解—修正刚度矩阵法

针对三维粘弹性层状半空间埋置集中荷载作用下动力响应问题,在柱面坐标下,结合径向Hankel积分变换,提出了一种新的求解方法—修正刚度矩阵法。方法基于位势函数理论,将三维问题分解为平面内反应(P-SV波型)和平面外反应（SH波型）两个二维问题的叠加;借鉴结构力学中超静定结构的位移法原理,首先固定荷载所在层的上下界面,通过对波动方程的特解和齐次解叠加得到“固端”反力。进而放松两“固端约束”,利用直接刚度法求得各层面位移,荷载作用层内反应另需叠加上该“固定层”内解,并将特解部分积分（直达波）由全空间解析解代替,解决了当接收点和源点作用水平面接近时的积分收敛问题。算例分析表明,对于低频（可退化为静力状态）和高频问题,本文方法均具有很高的计算效率和精度。     

集中力作用下铝合金材料内部柱状缺陷检测的研究

工程中,构件的内部会因为各种原因不可避免地存在各种损伤或缺陷。本文通过弹性力学理论给出含柱状缺陷的铝合金材料在受到集中力作用下的离面位移场。同时运用电子散斑干涉方法成功地测量出试件缺陷覆盖层在受到集中力情况下的离面位移。理论和实验结果对比表明,利用电子散斑干涉术技术能够精确地测量含缺陷材料表面的离面位移。此实验方法可以作为一种新型的探测物体内部缺陷所处的位置和大小的评估办法。     

饱和地基上基础动力阻抗函数的一种分析方法

提出了一种基础阻抗函数的时域求解方法, 并用于饱和地基情形. 通过给基础输入脉冲位移, 应用集中质量显式有限元方法结合局部透射人工边界, 得到地基施加于基础的反力时程, 然后根据阻抗函数的定义, 应用傅立叶变换求得基础阻抗函数. 通过算例, 与 Halpern 的结果进行了对比, 验证了该方法的有效性. 并以一方形基础为例, 分别讨论了泊松比、孔隙率、渗透系数和埋深对无量纲动力柔度的影响. 与以往方法相比, 该方法可以考虑复杂地基情形和不规则基础形式.      

饱和多孔介质中Lamb问题的Green函数解答

利用作者根据饱和多孔介质动力学方程快、 慢纵波解耦求得的集中力作用下饱和多孔介 质Green函数解答, 通过柱坐标变换, 运用Sommerfeld积分, 再根据自由表面应力为零的特 征, 添加自由表面影响场, 从而求得半无限空间集中力作用下饱和多孔介质动力学问题的解 答. 其结果与Philippacopoulos解答结果一致; 当饱和多孔蜕化为单相时与Lamb的方程一 致. 整个推导过程明了, 物理意义也较为清晰; 方法符合常规解法. 因此, 该方法为简化与 规范饱和多孔介质动力学问题的解答提供了基础; 并且能为一直未解决的半无限空间饱和多 孔介质动力学问题的流相解答(诸如孔隙压、排水量)提供解决途径.