On The Plane Creeping Flow Of Second Order Fluids With Mixed Boundary Conditions
Teodor M. Atanacković (1977)
Publications de l'Institut Mathématique
Similarity:
Teodor M. Atanacković (1977)
Publications de l'Institut Mathématique
Similarity:
Sozanov, V.G., Muzaev, I.D., Shumakov, N.S. (2001)
Vladikavkazskiĭ Matematicheskiĭ Zhurnal
Similarity:
Zaman, F.D., Al-Khairy, R. (2000)
Journal of Applied Mathematics and Stochastic Analysis
Similarity:
Jun Guo, Guozheng Yan, Jing Jin, Junhao Hu (2017)
Applications of Mathematics
Similarity:
We consider the inverse scattering problem of determining the shape and location of a crack surrounded by a known inhomogeneous media. Both the Dirichlet boundary condition and a mixed type boundary conditions are considered. In order to avoid using the background Green function in the inversion process, a reciprocity relationship between the Green function and the solution of an auxiliary scattering problem is proved. Then we focus on extending the factorization method to our inverse...
Tujin Kim (2022)
Applications of Mathematics
Similarity:
In this paper we are concerned with the steady Boussinesq system with mixed boundary conditions. The boundary conditions for fluid may include Tresca slip, leak, one-sided leak, velocity, vorticity, pressure and stress conditions together and the conditions for temperature may include Dirichlet, Neumann and Robin conditions together. For the problem involving the static pressure and stress boundary conditions, it is proved that if the data of the problem are small enough, then there...
Erhard V. Meister, L. Meister (2001)
Mathematica Bohemica
Similarity:
The initial boundary-transmission problems for electromagnetic fields in homogeneous and anisotropic media for canonical semi-infinite domains, like halfspaces, wedges and the exterior of half- and quarter-plane obstacles are formulated with the use of complex quaternions. The time-harmonic case was studied by A. Passow in his Darmstadt thesis 1998 in which he treated also the case of an homogeneous and isotropic layer in free space and above an ideally conducting plane. For thin layers...
Chakrabarti, A., Manna, D.P. (1994)
International Journal of Mathematics and Mathematical Sciences
Similarity:
Fleming, John L., Moser, Jessica (2009)
Mathematical Problems in Engineering
Similarity:
Březina, Jan
Similarity:
Richards' equation is a widely used model of partially saturated flow in a porous medium. In order to obtain conservative velocity field several authors proposed to use mixed or mixed-hybrid schemes to solve the equation. In this paper, we shall analyze the mixed scheme on 1D domain and we show that it violates the discrete maximum principle which leads to catastrophic oscillations in the solution.