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inconsistent equations相关的网络例句

查询词典 inconsistent equations

与 inconsistent equations 相关的网络例句 [注:此内容来源于网络,仅供参考]

Based on the projection theorem in the finite-dimensional inner product space, by making use of the generalized singular value decomposition and the canonical correlation decomposition of matrix pair simultaneously, we transform the least-squares problems of the abovementioned inconsistent matrix equations into the problems of solving the consistent matrix equations over given matrix set, and obtain the general expressions of the corresponding least-squares solutions.

S使得‖-X~*‖=‖-X~*‖,其中‖·‖为Frobenius范数,S分别表示矩阵方程 AXB=D,AXA~T+BYB~T=D,AXB+CYD=E和矩阵方程组=,=在一般矩阵集合或对称矩阵集合上不相容时的最小二乘解集合。

These equations are expanded by Fourier expansion method in order to unify the inconsistent fundamental functions of the electromagnetic fields related to the considered boundary.

本文还使用傅里叶展开的方法对这三个界面上相关区域的基函数的不一致性及定义域的不一致性作了统一处理。

We also adopt the iterative method to study the matrix nearness problem associated with these inconsistent matrix equations systematically in this dissertation, and characterize the minimization property of this iterative method by making use of the matrix function in subspace for the first time, which is the important improvement for the achievements of references.

本文还采用迭代方法系统地研究了问题Ⅰ,并首次利用子空间上的矩阵函数来刻画该迭代方法的极小化性质,这是对已有研究成果的重要补充和完善。

The conventional matrix decomposition methods have been used to find the least-squares solutions of the abovementioned inconsistent matrix equations over given matrix set in many references, and the general expressions of these solutions were obtained. But it is difficult to determine the solution of Problem I by utilizing these expressions due to the fact that the orthogonal invariance of Frobenius norm does no hold for the general nonsingular matrices.

对于求上述不相容矩阵方程在给定矩阵集合上的最小二乘解,很多文献中利用传统的矩阵分解方法得到了其通解表达式,但是利用该表达式很难得到问题Ⅰ的解,这是因为一般的非奇异矩阵并不满足Frobenius范数的正交不变性。

The inconsistent equations may be formed with the surveying data of the GPS network of monitoring crustal movement and deformation on the continent of China in 1994 and 1996, and by using the damping method of least squares and the interative computing method, the parameters of crustal movement and deformation can be obtained.

利用全国网1994年和1996年的两期GPS观测数据,组成矛盾方程组,应用阻尼最小二乘方法,经迭代解算,得到所需要的地壳运动与形变参数。

The computing plots of the solutions from the two methods were inconsistent under the specified boundary-initial conditions, which stirred up the debate of the effectiveness of Maxwell's equations in lossy medium. It is found that the differences between the two numerical curves can be viewed as the Gibbs phenomenon caused by cutting off the high frequency components in computing the infinite integral of the numerical curve of Harmuth's solution.

通过比较两种解析解的数值曲线得出:两者的差异在于求解Harmuth解的数值曲线时,采取无穷积分的高频截断近似产生了吉布斯现象;在计算Harmuth解的数值曲线时不断增大积分上限,其数值曲线的振荡不断向不连续点处收缩,而且衰减加快,因此在求解Harmuth解的数值曲线时,若积分区间取为理想无限大,则可以预见相同计算精度下两种方法的电场解的数值曲线是一致的。

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