幂律流体边界层方程的近似解析解和壁摩擦因数的近似值

对幂率流体层流平板边界层的解析解进行了研究．对该问题提供了Adomian分解方法并且推导出了问题的级数形式的近似解析解,该近似解析解具有快速收敛性和易于计算性．对不同的幂率给出了方程的近似解析解和相应的壁摩擦因数近似值,最后对近似解所推出结果和所得壁摩擦因数与文献中的数值解进行了比较验证,证实了该文提出的解析近似方法的准确性和可靠性,说明了该近似解能够应用于提供所研究问题的壁摩擦因数．     

N—解析函数的Riemamm—Hilbert问题

在N-解析函数类中,对于无穷直线上的Riemann-Hilbert边值问题,通过轴的对称扩张法将其转化为在附加条件下相应的Riemann边值问题,从而建立了其齐次和非齐次问题的可解性理论。     

一种求三维弹性力学基本解析解的特征方程解法

提出了一种简单的推导各向同性材料,三维弹性力学问题基本解析解的特征方程解法．应用三维问题控制微分方程的算子矩阵,通过计算其行列式可得到问题特征通解所需满足的特征方程．将满足各种不同简化特征方程的特征通解,代入到微分方程算子矩阵所对应的不同的缩减伴随矩阵,可推导得出相应的三维弹性力学问题的基本解析解,包括B-G解、修正的P-N（P-N-W）解和类胡海昌解．进一步对各类多项式形式的基本解析解的独立性进行了讨论．这些工作为构造数值方法中所需的完备独立的解析试函数奠定了基础．     

一维正方准晶中半无限裂纹问题的解析解

运用广义复变函数方法,通过构造适当的广义保角映射,研究了含有沿准周期方向穿透的半无限裂纹的一维正方准晶的反平面弹性问题,给出了在部分裂纹面上受均匀面外剪切时应力场和裂纹尖端应力强度因子的解析解.将此方法进一步推广到半无限裂纹垂直于一维正方准晶的准周期方向穿透的情形中,得到了相应的平面弹性问题的解析解.当准晶体的对称性增加时,还可以得出一维四方准晶相应问题的解析解.     

关于Berestycki一些结果的注记

本文讨论如下 Ｓｔｕｒｍ－Ｌｉｏｕｖｉｌｌｅ问题的非平凡解的全局结构：其中ｆ： Ｒ→Ｒ连续,且满足一些附加条件．所得结果推广了 Ｂｅｒｅｓｔｙｃｋｉ的一些结果．     

关于实轴上多解析函数Riemann边值问题的可解性

本文研究了实轴上具有不同因子的多解析函数的Riemann边值问题的可解性．利用所谓的转化法．建立了Riemann问题的可解性与其相联问题的解之间的关系。该结果推广了解析函数的相应理论。     

基于变分法对一类非线性扩散方程解析解研究北大核心CSCD

本文分别针对一类扩散系数为非线性指数函数和幂函数的扩散方程,基于变分原理中的泛函极值理论分别提出了求解该方程Dirichlet边界和Neumann边界问题解析解的新方法,并证明了新方法是泛函问题极值解的充要性．以非饱和土壤水分运动问题为背景,给出了积水和恒通量条件下水平吸渗问题的解析解,并通过数值算例将解析解与数值解进行了比较分析,结果表明本文方法得到的解析解能够准确预测非饱和土壤水分水平吸渗问题的土壤含水量分布,是一种有效方法．因此本文方法为求解这一类非线性扩散方程提供了一种有效的新方法．     

叠合度的缺方向性与边值共振问题的非平凡解

本文在无任何附加条件的情况下证明了叠合度也具有Ｌｅｒａｙ－Ｓｃｈａｕｄｅｒ度的缺方向性质,完全解决了前人工作中的遗留问题．作为这一结果的应用,证明了一类ｍ－点边值问题和Ｄｕｆｆｉｎｇ方程周期边值问题非平凡解的存在性结果．     

一般形式的一阶椭圆型偏微分方程组拟线性Riemann-Hilbert问题

在文［ｌ，２，３］中，Ｅ．Ｗｅｇｅｒｔ和Ｌ．Ｖ．Ｗｏｌｆｅｒｓｄｏｒｆ等人讨论了一类全纯函数的拟线性Ｒｉｅｍａｎｎ－Ｈｉｌｂｅｒｔ 问题在 Ｈａｒｄｙ空间中的可解性，在文［４］中，讨论了广义解析函数的拟线性 Ｒｉｅｍａｎｎ－Ｈｉｌｂｅｒｔ问题，同样得到该边值问题在Ｈ２类解空间中的可解性、本文在前面研究工作的基础上，对一般形式的一阶椭圆型偏微分方程组拟线性Ｒｉｅｍａｎｎ－Ｈｉｌｂｅｒｔ问题作了更深入的讨论，在适当的假设条件下，应用积分算子理论，函数论方法及不动点原理，证明了该边值问题在相应的泛函空间中同样是可解的．     

常系数线性微分方程RMI解题机

本文介绍的常系数线性微分方程解题机是利用数学方法论的研究成果，摸拟人的数学思维过程，采用关系映射反演（ＲＭＩ）方法，通过符号推理给出微分方程解析解的数学软件．文中介绍了研制该解题机的基本思想和实现技术，并给出了用解题机求解微分方程和微分方程组的几个实例．     

二维井间模型势函数重建

本主考虑在边界脉冲源激发下，二维波动方程的势函数反演问题．利用并间测量数据及地表测量数据重建势函数ｑ（ｘ，ｚ），利用反演问题的算子方程形式，通过Ｆｒｅｃｈｅｔ导数及对时间卷积的方法，得到了重建ｑ（ｘ，ｚ）的迭代方法．     

层状不均匀介质的一维地球模型物性参数反演

本文建立了层状不均匀非吸收介质的反问题模型，与已有的模型相比，它更切合实际，讨论了这种模型下介质的物性参数和几何参数的反演问题，它包括特性阻抗Ｋ（ｘ）间断状态参数Ｃ１，Ｘｉ，ｎ。借助于行波传播算子Ｋ１和有间断系数的方程的弱Ｒｉｅｍａｎｎ函数，得出每一层上波场正问题的表达式，供助于此表达式把反演物性参数的问题，转化为确定Ｍ＾ｋ（ｘ，ｙ，０）的问题，而关于Ｍ＾ｋ（ｘ，ｙ，０）我们得到的是一个第二类ＦＲ     

Stably numerical solving inverse boundary value problem for data assimilation

In remote sensing data assimilation, inverse methods are often used to retrieve the boundary conditions from some of the observations in the interior scanning region. Needless to say, the inverse boundary value problem (IBVP) is ill-conditioned in general. Ultimately, the data assimilation must include mechanisms that enable them to overcome the numerical instability for solving IBVP. In this paper, we begin by studying the behavior of ill-conditioned IBVP, and find that the condition number varies with the number of the observations and distribution locations of the observations. Next, we define the number of equivalent independent equations as a novel measurement of ill-conditioning of a problem, which can measure the degree of bad conditions. Furthermore, the novel measure can answer how many additional observations are needed to stabilize the retrieving problem, and where additional observations are fixed up. Finally, we illustrate the proposed methodology by applying it to the study of precipitation data assimilation, with a particular emphasis on the analysis of the effect of the number of observations and their distribution locations. The new methodology appears to be particularly efficient in tackling the instability of the retrieving problem in data assimilation.     

Iterative method for solving an inverse coefficient problem for a hyperbolic equation

For a hyperbolic equation, we consider an inverse coefficient problem in which the unknown coefficient occurs in both the equation and the initial condition. The solution values on a given curve serve as additional information for determining the unknown coefficient. We suggest an iterative method for solving the inverse problem based on reduction to a nonlinear operator equation for the unknown coefficient and prove the uniform convergence of the iterations to a function that is a solution of the inverse problem.     

Stability estimate for a multidimensional inverse spectral problem with partial spectral data

In Bellassoued, Choulli and Yamamoto (2009) [4] we proved a log-log type stability estimate for a multidimensional inverse spectral problem with partial spectral data for a Schrödinger operator, provided that the potential is known in a small neighbourhood of the boundary of the domain. In the present paper we discuss the same inverse problem. We show a log type stability estimate under an additional condition on potentials in terms of their X-ray transform. In proving our result, we follow the same method as in Alessandrini and Sylvester (1990) [1] and Bellassoued, Choulli and Yamamoto (2009) [4]. That is we relate the stability estimate for our inverse spectral problem to a stability estimate for an inverse problem consisting in the determination of the potential in a wave equation from a local Dirichlet to Neumann map (DN map in short).     

Inverse problems for elliptic equations in the space: II

We consider inverse problems of finding the right-hand side of a linear second-order elliptic equation of general form. The first boundary value problem is studied. We consider two ways of indicating additional information (overdetermination): the trace of the solution can be given on some lower-dimensional manifold inside the domain, or the normal derivative can be specified on part of the boundary. On the basis of the Fredholm alternative proved in the first part of the present paper for the inverse problems in question, we single out conditions on the given functions under which the inverse problem is uniquely solvable. Various types of such conditions are considered. The study is carried out in the class of continuous functions whose derivatives satisfy the Hölder condition.     

Iterative solutions of the split common fixed point problem for strictly pseudo-contractive mappings

In this paper, we study the the split common fixed point problem in Hilbert spaces. We establish a weak convergence theorem for the method recently introduced by Wang, which extends a existing result from firmly nonexpansive mappings to strictly pseudo-contractive mappings. Moreover, our condition that guarantees the weak convergence is much weaker than that of Wang’s. A strong convergence theorem is also obtained under some additional conditions. As an application, we obtain several new methods for solving various split inverse problems and split equality problems. Numerical examples are included to illustrate the applications in signal processing of the proposed algorithm.     

Inverse problem for Navier-Stokes systems with finite-dimensional overdetermination

We consider an inverse problem for an evolution equation with a quadratic nonlinearity. In this problem, one should find the right-hand side belonging at each time to a finitedimensional subspace on the basis of the given projection of the solution onto that subspace. We prove the time-nonlocal solvability of the inverse problem. Under the condition of additional regularity of the original data and a sufficiently large dimension of the observation subspace, we show that the solution of the inverse problem is unique and more smooth. By way of application, we consider the inverse problem for the three-dimensional Navier-Stokes equations describing the dynamics of a viscous incompressible fluid.     

Numerical identification of the leading coefficient of a parabolic equation

For a multidimensional parabolic equation, we study the problem of finding the leading coefficient, which is assumed to depend only on time, on the basis of additional information about the solution at an interior point of the computational domain. For the approximate solution of the nonlinear inverse problem, we construct linearized approximations in time with the use of ordinary finite-element approximations with respect to space. The numerical algorithm is based on a special decomposition of the approximate solution for which the transition to the next time level is carried out by solving two standard elliptic problems. The capabilities of the suggested numerical algorithm are illustrated by the results of numerical solution of a model inverse two-dimensional problem.     

Homogenization of the layer-structured dam problem with isotropic permeability

In this paper we address the homogenization of a free boundary model for a stratified porous dam problem. The motivation of the problem lies in the presence of a highly oscillating permeability to take into account the multilayer structure. Although several papers in the literature have partially studied this problem, we provide new additional results by using the periodic unfolding method. Furthermore, by using appropriate numerical techniques based on the combination of characteristics, duality and finite elements methods, several examples illustrate the here stated theoretical results and show the performance of the numerical methods.