With discrete mathematical method, the transformed equation is solved by finite control volume method and Galerkin finite element method.
最后用有限控制体积法和伽略金有限元法对变换后的方程进行数学离散并求解。
The equation is discretized by discontinuous Galerkin finite element method, that is approximating functions being discontinuous at the nodes of partition in time.
利用间断时空有限元方法对方程进行离散，即允许近似函数在时间节点处是间断的。
The pressure is approximated by a finite element method, and the concentration is approximated by the combination of a Galerkin finite element method and characteristics-finite element method.
压力方程由标准有限元方法逼近，浓度方程则用特征有限元方法逼近。
The finite-length beam on elastic foundation is solved by the wavelet Galerkin finite element method. In comparison with the analytical results, the solution has better accuracy and convergence.
用此方法求解弹性地基上的有限长梁，从结果对比可以看出其解具有良好的精确性和收敛性。
The Galerkin finite element method is applied to obtain simultaneous solutions in the space domain to the governing equations where the displacements and the fluid pressures are the primary unknowns.
利用有限元方法得到了控制方程中未知的位移和流体压力在几何域上的耦合解。
The relevant theories of three-dimensions Element-free Galerkin method and Nonlinear Finite Element method are introduced in this paper.
本文分别介绍了三维无单元伽辽金法和非线性有限单元法及其相关理论。
The time difference equation derived from unsaturated flow equation can be approximated by Galerkin finite element or finite difference method for space coordinate derivatives.
所得的非饱和土壤水运动方程对时间的差分方程，在空间上不仅可用有限元法而且可用有限差分法处理。
First, the penalty finite element balance equation for quasi-static problem is obtained by the application of Galerkin weighted residual method and the introduction of penalty parameter.
首先，采用伽辽金加权余量法推导有限元平衡方程，利用罚方法得到求解拟静态问题的罚有限元公式。
In the paper, the Galerkin penalty finite element method was applied to simulate the flows in the emitter.
该文采用加罚有限元方法对滴头内流动进行数值模拟，详细分析了“迷宫式”滴头在不同流量时的流动特性。
The finite element equation of 3d3c CSAMT electric field is derived from Maxwell equations using Galerkin method.
首先从麦克斯韦方程出发，用伽里金方法推导了三维三分量CSAMT法的有限元方程。
The ground water resource in the leaky aquifer is evaluated by the Galerkin s finite element method on condition that the water table of the above recharge aquifer changes with pumping.
越流含水层系统在我国分布十分广泛，但国内有关越流含水层系统的地下水污染模型尚未见报导。
The ground water resource in the leaky aquifer is evaluated by the Galerkin s finite element method on condition that the water table of the above recharge aquifer changes with pumping.
越流含水层系统在我国分布十分广泛，但国内有关越流含水层系统的地下水污染模型尚未见报导。
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