A representation for the velocity and pressure fields in three-dimensional Stokes flow was presented in terms of a biharmonic function A and a harmonic function B.This representation was used to establish a general th...A representation for the velocity and pressure fields in three-dimensional Stokes flow was presented in terms of a biharmonic function A and a harmonic function B.This representation was used to establish a general theorem for the calculation of Stokes flow due to fundamental singularities in a region bounded by a stationary no-slip plane boundary.Collins's theorem for axisymmetric Stokes flow before a rigid plane follows as a special case of the theorem.A few illustrative examples are given to show its usefulness.展开更多
In this paper, using the orthonormal multiresolution analysis(MRA) of L^2(R^s), we get two important properties of the scaling function with dilation matrix A = MI of L^2 (R^s). These properties axe chaxacterize...In this paper, using the orthonormal multiresolution analysis(MRA) of L^2(R^s), we get two important properties of the scaling function with dilation matrix A = MI of L^2 (R^s). These properties axe chaxacterized by some inequalities and equalities.展开更多
文摘A representation for the velocity and pressure fields in three-dimensional Stokes flow was presented in terms of a biharmonic function A and a harmonic function B.This representation was used to establish a general theorem for the calculation of Stokes flow due to fundamental singularities in a region bounded by a stationary no-slip plane boundary.Collins's theorem for axisymmetric Stokes flow before a rigid plane follows as a special case of the theorem.A few illustrative examples are given to show its usefulness.
基金Supported by the Natural Science Foundation of Ningxia Province(NZ0691)
文摘In this paper, using the orthonormal multiresolution analysis(MRA) of L^2(R^s), we get two important properties of the scaling function with dilation matrix A = MI of L^2 (R^s). These properties axe chaxacterized by some inequalities and equalities.