聚变等离子体理想动力系统的非线性热不稳定性

本文讨论氖氖聚变等离子体理想动力系统的非线性热不稳定性问题，这个系统与外界有物质与能量交换。采用几何上零维近似的演化方程。对自治系统，讨论了在各种不同粒子约束定律和能量约束定律下的非线性热不稳定性问题，给出稳定性判据。研究了自治系统不稳定解的非线性演化。     

孤立波与多个潜水障碍物相互作用的数值研究

本文以完整二维Navier-Stokes方程为控制方程,采用VOF界面跟踪技术和差分方法,数值计算孤立波与多个淹没水下物体相互作用的问题。本文对潜水物体的高度接近水深时,孤立波通过水下孤立直立方柱、两个间距较大的水下直立方柱和两个间距较小的水下直立方柱等三种情况分别进行了计算,给出了波形随时间的演化图,可以看到反射波、前传波和跟随振荡型小波列的生成。对孤立波通过水下孤立直立方柱情形的计算结果,与实验结果和势流理论结果进行了比较。     

欧拉流体力学数值方法中的界面计算

本文所提算法适用于二维和三维多介质流体力学两步欧拉数值方法中输运计算的混合网格(包括自由面网格)界面处理。在一个混合网格中，界面被近似地看作直线(二维)或平面(三维)。整个方法分为三步：(1)第一步，用混合网格周围的八个网格的介质面积份额(二维)或二十六个网格的介质体积份额(三维)确定界面的法线方向；第二步，用混合网格的本身的介质面积份额(二维)或体积份额(三维)确定界面的方程(位置)；第三步，用此直线方程求出通过网格边界的流以及下一时刻网格的面积份额(二维)或体积份额(三维)。最后给出了用此方法所做的一些数值计算及与SLIC算法的比较。     

具有精确色散性的非线性波浪数学模型

以完全非线性的自由表面边界条件为基础,以波面升高\eta和自由表面速度势\phi _\eta为待求变量,建立了新的波浪方程．方程在色散性上是完全精确的,非线性近似至三阶．与缓坡方程相比较,两者都具有精确的色散性,但该方程属于非线性模型,可模拟波浪的非线性效应,且适用于不规则波．方程的特点是属于微分-积分方程,对如何处理方程中积分项进行了讨论,并数值模拟了不同周期的线性波和二阶Stokes波,也模拟了波群的非线性演化,以对模型进行验证．      

基底弹性对蒸发超薄液膜去润湿过程的影响

研究了基底的弹性变形对蒸发超薄膜的稳定性和去润湿动力学过程的影响. 基于长波近似, 得到了关于液体薄膜厚度的演化方程. 运用线性稳定性理论和数值模拟两种方法, 研究了基底弹性、范德华力以及液体蒸发等因素对液体薄膜的稳定性和去润湿过程的影响. 研究结果表明增大基底的弹性系数或者减小液体的表面张力, 都能加速液膜的破碎, 并且能够影响气液界面波的波长; 液体蒸发能促进气液界面扰动的增长, 有助于液膜的破裂.      

损伤统计演化方程的性质和数值模拟

通过对一种含成核尺寸效应的损伤统计演化方程性质的分析和数值模拟,揭示了损伤率主要是由微损伤在二维相空间中的前沿的运动所决定的这也就是Kachanov提出的损伤率演化方程的物理基础数值结果进一步显示了含成核尺寸效应模型在损伤发展上与-维模型的区别而且,由几种形式的细观动力学算出的损伤率与损伤的关系简单,可近似拟合为宏观上封闭的形式     

Klein-Gordon波动方程多波传播的非线性特性

基于双波初值问题，讨论非线性对多波传播的影响。通过选取合适的多重尺度，对Klein-Gordon波动方程进行变形，得到方程的解的多尺度展式首项近似和三波传播时速度相互影响的定量关系，揭示了多波传播的非线性特性；最后，应用Mathematica对波动方程进行数值仿真。研究结果表明，另外多个波的存在会使波的传播速度（相速）超过独自传播时的速度（相速）。     

Boussinesq方程的发展形式与Airy波理论差异性研究

应用势流理论，采用递推函数方法推导出一个新形式的Ｂｏｕｓｉｎｅｓｑ方程。通过对新方程的参数设置，可以讨论出Ｂｏｕｓｓｉｎｅｓｑ方程发展趋势和不同的发展形式。对浅水波动的描述方程，Ｂｏｕｓｓｉｎｅｓｑ方程的发展趋势为适用水深范围的拓展。拓展应用范围的大小则由其方程频散特征向Ａｉｒｙ波频散解逼近程度来决定。而Ｂｏｕｓｉｎｅｑ方程又不同于Ａｉｒｙ波，主要原因是Ｂｏｕｓｓｉｎｅｓｑ方程中含有线性频散项，Ａｉｒｙ波则只是长波首项近似，无线性频散项。其频散特征为精确的线性频散解。对实际水波传播而言，Ａｉｒｙ波理论的局限性是不言而喻的。     

界面不稳定性引起混合过程的二维数值计算

在可压缩多介质流体动力学高精度欧拉计算方法多介质流体分段抛物方法(multi-fluid piecewise parabolic method, MFPPM)基础上,运用算子分裂技术,增加二阶空间中心差方法和两步Rung-Kutta时间推进方法计算动力学黏性以及热流部分对流场的影响,发展适用于NS(Navier-Stokes)方程的可压缩多介质黏性流体计算方法多介质黏性流体分段抛物方法(multi-viscousity-fluid piecewise parabolic method, MVPPM). 文中采用MVPPM对英国AWE(atomic weapons establishment)激波管实验进行二维计算,给出了与实验图像基本一致的计算结果;应用MFPPM和MVPPM分别对二维柱对称内爆动力学界面不稳定性及其后期混合过程进行数值模拟,给出内外界面演化、速度历史以及后期中心气穴不同半径内因RT(Rayleigh-Taylor)界面不稳定性引起的混合量分布情况,从计算结果比较可见黏性对物质界面处混合量的分布影响明显.      

用格子Boltzmann方程模拟浅水波问题

提出了用格子Ｂｏｌｔｚｍａｎｎ方程（ＬＢＥ）模拟浅水波问题的方法．通过无粘气体运动方程与浅水波方程的比较，确定了ＬＢＥ方法中平衡态的形式，使宏观方程与浅水波方程一致．计算了二维浅水波的一个问题，数值结果与精确解做了比较．     

COMPARISON OF STABILITY BETWEEN NAVIER-STOKES AND EULER EQUATIONS

The stability about Navier-Stokes equation and Euler equation was brought into comparison. And by taking their typical initial value problem for example, the reason of leading to the difference in stability between Navier-Stokes equation and Euler equation was also analyzed.     

扩散抛物化Navier-Stokes方程数值解法评述

20世纪60年代末期在边界层理论基础上发展起来的各种简化Navier-Stokes (N-S)方程(统称为扩散抛物化N-S方程)及其算法, 较为彻底地解决了无黏流及黏流的相互干扰问题, 并为高雷诺数大型复杂黏性流场的数值模拟开辟了新的途径. 本文将系统地评述这一领域的主要成果, 包括各种简化N-S模型的优缺点; 数学奇性及正则化方法; 代表性的数值解法以及最近几年的新进展.      

Stochastic differential equations for the kinetic and hydrodynamic equations

A finite system of stochastic interacting particles is considered. The system approximates the solutions of the kinetic equations (the Boltzmann equation, the Boltzmann-Enskog equation) as well as the solutions describing the macroscopic evolution of fluids: the Euler and the Navier-Stokes hydrodynamic equations.     

TheC k instability of navier-Stokes equation appending polynomials of unknown functions

Applying the theory of stratification, the solution space structure about a class of deformed Navier-Stokes equation isdetermined. It is proved that such kind of equation has no C^k (k≥2) stable solution by the fact that the strate transversale is a null set. Foundation item: the National Natural Science Foundation of China (19971054), Shanghai Natural Science Foundation (99ZA14034) Biography: HE You-hua (1960-)     

ARC-length method for differential equations

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A New Model for Viscous Dissipation in Porous Media Across a Range of Permeability Values

In this paper a unified mathematical theory for the viscous dissipation term in the governing Brinkman equation is derived. This term has, unlike other models, the correct asymptotic behaviour in both the fully Darcy and Newtonian fluid flow limits.     

Singular perturbation of the fourth order elliptic equation when the limit equation is elliptic-parabolic

3@1In this paper we cosider the singular perturbation of the fourth order elliptic equation-ε~2△~2u y~m(α~2u)/(αy~2) (α~2u)/(αx~2) α(x,y)-(αu)/(αy) b(x,y)(αu)/(αx) c(x,y)=0 when the limit equationis elliptic-parabolic,where εis a positive parameter,m is a positive real number,△isLaplacian operator,a.b.c are sufficiently smooth.Under appropriate condition we derivethe sufficient condition of solvability and prove the existence of solution and give auniformly valid asymptotic solution of arbitrary order.     

ON PERIODIC SOLUTIONS OF SEVERAL CLASSES 0F RICCATI'S EQAUTION AND SECOND一ORDER DIFFERENTIAL EQUATIONS

In this paper, the problem on periodic solutions of several classes of Riccati's equation with periodic coefficients is discussed, and the conditions, under which several classes of secondorder equations with periodic coefficients have periodic solutions, are given.     

UPWIND LOCAL DIFFERENTIAL QUADRATURE METHOD FOR SOLVING COUPLED VISCOUS FLOW AND HEAT TRANSFER EQUATIONS

The differential quadrature method (DQM) has been applied successfully to solve numerically many problems in the fluid mechanics. But it is only limited to the flow problems in regular regions. At the same time, here is no upwind mechanism to deal with the convective property of the fluid flow in traditional DQ method. A local differential quadrature method owning upwind mechanism (ULDQM) was given to solve the coupled problem of incompressible viscous flow and heat transfer in an irregular region. For the problem of flow past a contraction channel whose boundary does not parallel to coordinate direction, the satisfactory numerical solutions were obtained by using ULDQM with a few grid points. The numerical results show that the ULDQM possesses advantages including well convergence, less computational workload and storage as compared with the low-order finite difference method.     

GLOBAL SOLUTION OF THE INVERSE PROBLEM FOR ACLASS OF NONLINEAR EVOLUTION EQUATIONSOF DISPERSIVE TYPE

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