Recovery of flow parameters of viscous heat-conducting fluid by some changes at its surface
Vestnik Ûžno-Uralʹskogo gosudarstvennogo universiteta. Seriâ, Matematika, mehanika, fizika, Tome 10 (2018) no. 1, pp. 27-36 Cet article a éte moissonné depuis la source Math-Net.Ru

Voir la notice de l'article

Physical characteristics of steady motion of viscous heat-conducting incompressible fluid by changes of temperature and heat flow on its daylight surface are determined in the article. The main desired characteristics are temperature and fluid velocity in the entire simulation area. The problem is formalized as an inverse boundary problem for the flow model of natural thermal convection of highly viscous incompressible fluid. The mathematical flow model of such fluid is described by a stationary Navier-Stokes equations for Newtonian rheology of a medium in Boussinesq approximation in the field of gravity, by the medium incompressibility equation, stationary equation of energy conservation with corresponding boundary conditions. Density and viscosity of the fluid have non-linear dependence on its temperature. The considered inverse problem is incorrect and does not possess the property of stability; small perturbation of initial data on the section of the boundary available for measurement leads to uncontrolled errors in determining the desired values. For numerical solution of unstable problems special methods should be developed. The goal of the article is in developing methods and algorithms of constructive sustainable numerical simulation of the considered inverse problem’s solution. In order to implement this goal, the use of variational method, which is based on reduction of the initial problem to some extremum problem on the minimum of the appropriate objective functional and its sustainable minimization by some appropriate technique, is proposed. Using this strategy, an iteration process of sequential numerical solution of boundary problems of boundary control, which are systems of differential equations with partial derivatives with completely determined boundary conditions, is organized. In order to minimize quality functional, the Polac-Ribiere conjugate gradient method is used. This functional’s gradient and the descent step are determined analytically which allows significantly decreasing the volume of calculations. The method of finite volumes is used for integrating the systems of differential equations with partial derivatives with various types of boundary conditions. The developed algorithms of numerical simulation are implemented in the OpenFOAM calculations package. Calculation of the simulated example is carried out.
Keywords: thermal convection, inverse boundary problem, variational method, numerical simulation.
Mots-clés : viscous fluid
@article{VYURM_2018_10_1_a3,
     author = {A. I. Korotkii and I. A. Tsepelev},
     title = {Recovery of flow parameters of viscous heat-conducting fluid by some changes at its surface},
     journal = {Vestnik \^U\v{z}no-Uralʹskogo gosudarstvennogo universiteta. Seri\^a, Matematika, mehanika, fizika},
     pages = {27--36},
     year = {2018},
     volume = {10},
     number = {1},
     language = {ru},
     url = {http://geodesic.mathdoc.fr/item/VYURM_2018_10_1_a3/}
}
TY  - JOUR
AU  - A. I. Korotkii
AU  - I. A. Tsepelev
TI  - Recovery of flow parameters of viscous heat-conducting fluid by some changes at its surface
JO  - Vestnik Ûžno-Uralʹskogo gosudarstvennogo universiteta. Seriâ, Matematika, mehanika, fizika
PY  - 2018
SP  - 27
EP  - 36
VL  - 10
IS  - 1
UR  - http://geodesic.mathdoc.fr/item/VYURM_2018_10_1_a3/
LA  - ru
ID  - VYURM_2018_10_1_a3
ER  - 
%0 Journal Article
%A A. I. Korotkii
%A I. A. Tsepelev
%T Recovery of flow parameters of viscous heat-conducting fluid by some changes at its surface
%J Vestnik Ûžno-Uralʹskogo gosudarstvennogo universiteta. Seriâ, Matematika, mehanika, fizika
%D 2018
%P 27-36
%V 10
%N 1
%U http://geodesic.mathdoc.fr/item/VYURM_2018_10_1_a3/
%G ru
%F VYURM_2018_10_1_a3
A. I. Korotkii; I. A. Tsepelev. Recovery of flow parameters of viscous heat-conducting fluid by some changes at its surface. Vestnik Ûžno-Uralʹskogo gosudarstvennogo universiteta. Seriâ, Matematika, mehanika, fizika, Tome 10 (2018) no. 1, pp. 27-36. http://geodesic.mathdoc.fr/item/VYURM_2018_10_1_a3/

[1] Tikhonov A. N., Arsenin V. Y., On the solution of ill-posed problems, John Wiley and Sons, New York, 1977, 258 pp. | MR

[2] Ivanov V. K., Vasin V. V., Tanana V. P., Theory of linear ill-posed problems and its applications, Nauka Publ., M., 1978, 206 pp. (in Russ.)

[3] Vasiliev F. P., Optimization methods, Faktorial Publ., M., 2002, 824 pp. (in Russ.)

[4] S. Chandrasekhar, Hydrodynamic and hydromagnetic stability, Clarendon Press, Oxford, 1961, 654 pp. | MR | Zbl

[5] Landau L. D., Lifshitz E. M., Fluid Mechanics, Pergamon, 1987, 554 pp. | MR | Zbl

[6] Korotkii A. I., Kovtunov D. A., “Reconstruction of boundary regimes in an inverse problem of thermal convection of a high viscous fluid”, Trudy Instituta Matematiki i Mehaniki UrO RAN, 12, no. 2 (2006), 88–97 (in Russ.)

[7] Korotkii A. I., Starodubtseva Yu.V., Modelling of direct and inverse problems for models of stationary heat and mass transfer, Izdatelstvo Uralskogo universiteta Publ., Yekaterinburg, 2015, 168 pp. (in Russ.)

[8] A. Ismail-Zadeh, A. Korotkii, I. Tsepelev, Data-driven numerical modelling in geodynamics: methods and applications, Springer International Publishing, Berlin, 2016, 105 pp. | DOI | MR

[9] A. Korotkii, D. Kovtunov, A. Ismail-Zadeh et al., “Quantitative reconstruction of thermal and dynamic characteristics of volcanic lava from surface thermal measurements”, Geophysical Journal International, 205:3 (2016), 1767–1779 | DOI

[10] J. Nocedal, S.J. Wright, Numerical optimization, Springer, New York, 1999, 664 pp. | MR | Zbl

[11] Korotkii A. I., Kovtunov D. A., “Optimal boundary control of a system describing thermal convection”, Proceedings of the Steklov Institute of Mathematics, 272, no. suppl. 1, Supplementary issues (2011), 74–100 | DOI | MR | Zbl

[12] http://www.openfoam.org/

[13] R.I. Issa, “Solution of implicitly discretised fluid flow equations by operator-splitting”, J. Comput. Phys., 62:1 (1986), 40–65 | DOI | MR | Zbl

[14] P. Wesseling, C.W. Oosterlee, “Geometric multigrid with applications to computational fluid dynamics”, Journal of Computational and Applied Mathematics, 128:1–2 (2001), 311–334 | DOI | MR | Zbl

[15] H.A. van der Vorst, “BI-CGSTAB: A fast and smoothly converging variant of BI-CG for the solution of nonsymmetric linear systems”, SIAM Journal on Scientific and Statistical Computing, 13:2 (1992), 631–644 | DOI | MR | Zbl

[16] P.K. Sweby, “High resolution schemes using flux limiters for hyperbolic conservation laws”, SIAM Journal on Numerical Analysis, 21:5 (1984), 995–1011 | DOI | MR | Zbl

[17] A. Costa, L. Caricchi, N. Bagdassarov, “A model for the rheology of particle-bearing suspensions and partially molten tocks”, Geochemistry, Geophysics, Geosystems, 10:3 (2009), Q03010 | DOI

[18] M. Hidaka, A. Goto, S. Umino, E. Fujita, “VTFS project: Development of the lava flow simulation code LavaSIM with a model for three-dimensional convection, spreading, and solidification”, Geochemistry, Geophysics, Geosystems, 6:7 (2005), Q07008 | DOI

[19] I.M. Navon, X. Zou, J. Derber, J. Sela, “Variational data assimilation with an adiabatic version of the NMC spectral model”, Monthly Weather Review, 120:7 (1992), 1433–1446 | 2.0.CO;2 class='badge bg-secondary rounded-pill ref-badge extid-badge'>DOI