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1.
DEGENERATEPARABOLICEQUATIONANDUNILATERALCONSTRAINTSYSTEMSGuoXingming(郭兴明)(ShanghaiUniversity,ShanghaiInstituteofAppliedMathem...  相似文献   

2.
A-HIGH-ORDERACCURACYEXPLICITDIFFERENCESCHEMEFORSOLVINGTHEEQUATIONOFTWO-DIMENSIONALPARABOLICTYPEMaMingshu(马明书)(ReceivedJune2,1...  相似文献   

3.
In this paper,we discuss singularly perturbed semi-linear parabolic equations for one dimension and two dimension,we find numerical solutions by using both the line-method and the exact difference scheme on a special non-uniform discretization mesh.The uniform convergence in e of the first order accuracy is obtained.  相似文献   

4.
IntroductionLetΩbeanopenboundeddomainofRN,Q=Ω× (0 ,T) ,0 <T<∞ ,2 ≤p<∞ ,(1 /p) (1 /p′) =1 .Forconvenience ,wesetV =W1,p0 (Ω) ,V′=W- 1,p′(Ω)inthesequel.ThenVisarealreflexiveBanachspacedenselyandcompactlyimbeddedintoLp(Ω) .ThenormofanyBanachspaceBisdenotedby‖·‖B.ThepairingbetweenBan…  相似文献   

5.
SiJianguo(司建国)(ReceivedMay30,1994,CommunicatedbyLinZongchi)DISCUSSIONONTHEPERIODICSOLUTIONSFORHIGHER-ORDERLINEAREQUATIONOFNEU...  相似文献   

6.
A semiimplicit discretization of a parabolic equation is considered. The resulting diffepmorphism is shown to be generically Morse-Smale. Uniform bounds for the dimension of its attractor are given and numerical trajectories—including round-off errors—are shown to approximate the attractor.  相似文献   

7.
This paper puts forward a new method to solve the electromagnetic parabolic equation (EMPE) by taking the vertically-layered inhomogeneous characteristics of the atmospheric refractive index into account. First, the Fourier transform and the convo- lution theorem are employed, and the second-order partial differential equation, i.e., the EMPE, in the height space is transformed into first-order constant coefficient differential equations in the frequency space. Then, by use of the lower triangular characteristics of the coefficient matrix, the numerical solutions are designed. Through constructing ana- lytical solutions to the EMPE, the feasibility of the new method is validated. Finally, the numerical solutions to the new method are compared with those of the commonly used split-step Fourier algorithm.  相似文献   

8.
对一类时滞抛物型方程初边值问题,提出了关于空间步长是四阶精度的高精度无条件稳定的精细积分法.数值算例表明,本文提出的精细积分法具有很高的精度,因而是一种有效的数值方法.  相似文献   

9.
Abstract In this paper, the blow-up rate is obtained for a porous medium equation with a nonlinear gradient term and a nonlinear boundary flux. By using a scaling method and regularity estimates of parabolic equations, the blow-up rate determined by the interaction between the diffusion and the boundary flux is obtained. Compared with previous results, the gradient term, whose exponent does not exceed two, does not affect the blow-up rate of the solutions.  相似文献   

10.
This paper proposes a new method to improve the stability condition of differencescheme of a parabolic equation.Necessary and sufficient conditions of the stability of thisnew method are given and proved.Some numerical examples show that this method hassome calculation advantages.  相似文献   

11.
In this paper,we discuss the parabolic equation with a small parameter on thederivative in time variable.We construct difference scheme on the non-uniform meshaccording to Bakhvalov,and prove the one-order uniform convergence of this scheme.Numerical results are presented.  相似文献   

12.
The numerical solution of a singularly perturbed problem for the semilinear parabolicdifferential equation with parabolic boundary layers is discussed.A nonlinear two-leveldifference scheme is constructed on the special non-uniform grids.The uniform convergenceof this scheme is proved and some numerical examples are given.  相似文献   

13.
Dynamic parallel Galerkin domain decomposition procedures with grid modification for semi‐linear parabolic equation are given. These procedures allow one to apply different domain decompositions, different grids, and interpolation polynomials on the sub‐domains at different time levels when necessary, in order to capture time‐changing localized phenomena, such as, propagating fronts or moving layers. They rely on an implicit Galerkin method in the sub‐domains and simple explicit flux calculation on the inter‐domain boundaries by integral mean method to predict the inner‐boundary conditions. Thus, the parallelism can be achieved by these procedures. These procedures are conservative both in the sub‐domains and across inter‐boundaries. The explicit nature of the flux prediction induces a time step limitation that is necessary to preserve stability, but this constraint is less severe than that for a fully explicit method. Stability and convergence analysis in L2‐norm are derived for these procedures. The experimental results are presented to confirm the theoretical results. Copyright © 2010 John Wiley & Sons, Ltd.  相似文献   

14.
We consider the numerical solution of a singularly perturbed problem for the quasilinear parabolic differential equation, and construct a linear three-level finite difference scheme on a nonuniform grid. The uniform convergence in the sense of discrete L~2 norm is proved and numerical examples are presented.  相似文献   

15.
In the present paper,a new numerical method for solving initial-boundary valueproblems of evolutionary equations is proposed and studied,combining difference methodwith high accuracy with boundary integral equation method.The numerical approximateschemes for both problems on a bounded or unbounded domain in R~3 are proposed and theirprior error estimates are obtained.  相似文献   

16.
The inverse heat conduction problem (IHCP) is a severely ill-posed problem in the sense that the solution ( if it exists) does not depend continuously on the data. But now the results on inverse heat conduction problem are mainly devoted to the standard inverse heat conduction problem. Some optimal error bounds in a Sobolev space of regularized approximation solutions for a sideways parabolic equation, i. e. , a non-standard inverse heat conduction problem with convection term which appears in some applied subject are given.  相似文献   

17.
Galerkin domain decomposition procedures for parabolic equations with three cases of boundary conditions on rectangular domain are discussed. These procedures are non‐iterative and non‐overlapping ones. They rely on implicit Galerkin method in the sub‐domains and integral mean method on the inter‐domain boundaries to present explicit flux calculation. Thus, the parallelism can be achieved by the use of these procedures. Two kinds of approximating schemes are presented. Because of the explicit nature of the flux calculation, a less severe time‐step constraint is derived to preserve stability. To bound L2‐norm error estimates, new elliptic projections are established and analyzed. Numerical experiments are provided to confirm theoretical results. Copyright © 2009 John Wiley & Sons, Ltd.  相似文献   

18.
A highly efficient H1-Galerkin mixed finite element method(MFEM) is presented with linear triangular element for the parabolic integro-differential equation.Firstly, some new results about the integral estimation and asymptotic expansions are studied. Then, the superconvergence of order O(h2) for both the original variable u in H1(π) norm and the flux p =u in H(div,π) norm is derived through the interpolation post processing technique. Furthermore, with the help of the asymptotic expansions and a suitable auxiliary problem, the extrapolation solutions with accuracy O(h3) are obtained for the above two variables. Finally, some numerical results are provided to confirm validity of the theoretical analysis and excellent performance of the proposed method.  相似文献   

19.
In this paper, using nonumiform mesh and exponentially fitted difference method,a uniformly convergent difference scheme .for an initial-boundary value problem of linear parabolic differential equation with the nonsmooth boundary layer function with respect to small parameter ε is given, and error estimate and numerical result are also given.  相似文献   

20.
IntroductionWeoftenmeettheproblemofsolvingequationofparabolictypeinmanyfieldssuchasseepage ,diffusion ,heatconductionandsoon .Inthecaseof3_dimension ,themodelisaninitialandboundaryvalueproblemasfollows: u t = 2 u x2 2 u y2 2 u z2      (0 <x,y,z<1 ;t>0 ) ,u(x ,y,z,0 ) =φ(x ,y ,z)…  相似文献   

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