In this paper,we propose a GL method for solving the ordinary and the partial differential equation in mathematical physics and chemics and engineering.These equations govern the acustic,heat,electromagnetic,elastic,p...In this paper,we propose a GL method for solving the ordinary and the partial differential equation in mathematical physics and chemics and engineering.These equations govern the acustic,heat,electromagnetic,elastic,plastic,flow,and quantum etc.macro and micro wave field in time domain and frequency domain.The space domain of the differential equation is infinite domain which includes a finite inhomogeneous domain.The inhomogeneous domain is divided into finite sub domains.We present the solution of the differential equation as an explicit recursive sum of the integrals in the inhomogeneous sub domains.Actualy,we propose an explicit representation of the inhomogeneous parameter nonlinear inversion.The analytical solution of the equation in the infinite homogeneous domain is called as an initial global field.The global field is updated by local scattering field successively subdomaln by subdomain.Once all subdomains are scattered and the updating process is finished in all the sub domains,the solution of the equation is obtained.We call our method as Global and Local field method,in short,GL method.It is different from FEM method,the GL method directly assemble inverse matrix and gets solution.There is no big matrix equation needs to solve in the GL method.There is no needed artificial boundary and no absorption boundary condition for infinite domain in the GL method.We proved several theorems on relationships between the field solution and Green's function that is the theoretical base of our GL method.The numerical discretization of the GL method is presented.We proved that the numerical solution of the GL method convergence to the exact solution when the size of the sub domain is going to zero.The error estimation of the GL method for solving wave equation is presented.The simulations show that the GL method is accurate,fast,and stable for solving elliptic,parabolic,and hyperbolic equations.The GL method has advantages and wide applications in the 3D electromagnetic(EM)field,3D elastic and plastic etc seismic field,acoustic field,flow field,and quantum field.The GL method software for the above 3D EM etc field are developed.展开更多
In this paper, a new iterative solution method is proposed for solving multiple linear systems A(i)x(i)=b(i), for 1≤ i ≤ s, where the coefficient matrices A(i) and the right-hand sides b(i) are arbitrary in general....In this paper, a new iterative solution method is proposed for solving multiple linear systems A(i)x(i)=b(i), for 1≤ i ≤ s, where the coefficient matrices A(i) and the right-hand sides b(i) are arbitrary in general. The proposed method is based on the global least squares (GL-LSQR) method. A linear operator is defined to connect all the linear systems together. To approximate all numerical solutions of the multiple linear systems simultaneously, the GL-LSQR method is applied for the operator and the approximate solutions are obtained recursively. The presented method is compared with the well-known LSQR method. Finally, numerical experiments on test matrices are presented to show the efficiency of the new method.展开更多
文摘In this paper,we propose a GL method for solving the ordinary and the partial differential equation in mathematical physics and chemics and engineering.These equations govern the acustic,heat,electromagnetic,elastic,plastic,flow,and quantum etc.macro and micro wave field in time domain and frequency domain.The space domain of the differential equation is infinite domain which includes a finite inhomogeneous domain.The inhomogeneous domain is divided into finite sub domains.We present the solution of the differential equation as an explicit recursive sum of the integrals in the inhomogeneous sub domains.Actualy,we propose an explicit representation of the inhomogeneous parameter nonlinear inversion.The analytical solution of the equation in the infinite homogeneous domain is called as an initial global field.The global field is updated by local scattering field successively subdomaln by subdomain.Once all subdomains are scattered and the updating process is finished in all the sub domains,the solution of the equation is obtained.We call our method as Global and Local field method,in short,GL method.It is different from FEM method,the GL method directly assemble inverse matrix and gets solution.There is no big matrix equation needs to solve in the GL method.There is no needed artificial boundary and no absorption boundary condition for infinite domain in the GL method.We proved several theorems on relationships between the field solution and Green's function that is the theoretical base of our GL method.The numerical discretization of the GL method is presented.We proved that the numerical solution of the GL method convergence to the exact solution when the size of the sub domain is going to zero.The error estimation of the GL method for solving wave equation is presented.The simulations show that the GL method is accurate,fast,and stable for solving elliptic,parabolic,and hyperbolic equations.The GL method has advantages and wide applications in the 3D electromagnetic(EM)field,3D elastic and plastic etc seismic field,acoustic field,flow field,and quantum field.The GL method software for the above 3D EM etc field are developed.
文摘In this paper, a new iterative solution method is proposed for solving multiple linear systems A(i)x(i)=b(i), for 1≤ i ≤ s, where the coefficient matrices A(i) and the right-hand sides b(i) are arbitrary in general. The proposed method is based on the global least squares (GL-LSQR) method. A linear operator is defined to connect all the linear systems together. To approximate all numerical solutions of the multiple linear systems simultaneously, the GL-LSQR method is applied for the operator and the approximate solutions are obtained recursively. The presented method is compared with the well-known LSQR method. Finally, numerical experiments on test matrices are presented to show the efficiency of the new method.
