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Two-level iterative finite element methods for the stationary natural convection equations with different viscosities based on three corrections
被引:1
|作者:
Zhang, Huifang
[1
]
Chen, Chuanjun
[1
]
Zhang, Tong
[1
]
机构:
[1] Yantai Univ, Sch Math & Informat Sci, Yantai 264005, Peoples R China
来源:
基金:
中国国家自然科学基金;
关键词:
The natural convection equations;
Two-level methods;
Iterative method;
Stability;
Convergence;
VARIATIONAL MULTISCALE METHOD;
CONVERGENCE ANALYSIS;
STOKES EQUATIONS;
ALGORITHM;
MAGNETOHYDRODYNAMICS;
STABILITY;
SCHEME;
CAVITY;
D O I:
10.1007/s40314-022-02147-z
中图分类号:
O29 [应用数学];
学科分类号:
070104 ;
摘要:
This paper considers the two-level iterative finite element methods for the steady natu-ral convection equations under some uniqueness conditions with the Simple-, Oseen-and Newton-type corrections. Firstly, the stability and convergence of the one-level iterative finite element methods are analyzed under some restrictions on physical parameters. Secondly, under the strong uniqueness condition, we develop the two-level finite element method with Simple, Oseen and Newton iterations of m times on the coarse mesh tau H with mesh size H, and then, the considered problem is linearized in three correction schemes with the Simple, Oseen and Newton corrections one time on the fine grid tau h with mesh size h << H based on the obtained iterative solutions. From the theoretical point of view, the results obtained by the two-level iterative methods have the same precision as those obtained by the one-level method which mesh sizes satisfy h = O(H-2) and the iterative steps are greater than some constants. Thirdly, the stability and convergence of one-level Oseen iterative scheme with respect to the mesh size and the iterative time m are provided under a weak uniqueness condi-tion. Finally, some numerical experiments are designed to confirm the established theoretical findings and verify the performance of the proposed numerical schemes.
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页数:29
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