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Języki publikacji
Abstrakty
The aim of this study is to derive flow parameters, which are permeability and Forchheimer coefficient, based on experimentally measured flow rates and pressure drops. When flow rates used in measurements exceed the limits of linear Darcy’s flow regime we discuss what needs to be taken into account while processing the measurements. The study consists of two parts. In this part we briefly recall Darcy’s and Forchheimer’s laws and address the issue of detecting transition between ranges of their applicability. Then we describe the experiment and discuss 8 different ways to process measurement data, four for Darcy’s, and four for Forchheimer’s models. The main topic of the second part is to provide recommendations for the best ways to process data, so that the results obtained with numerical models are in the best agreement with the experimental data. The results shown in the two papers belong to a larger work devoted to modeling fluid flows through porous media, with a special interest in granular beds.
Słowa kluczowe
Rocznik
Tom
Strony
321--335
Opis fizyczny
Bibliogr. 17 poz., rys., tab., wykr.
Twórcy
autor
- Department of Mechanics and Machine Design, University of Warmia and Mazury in Olsztyn
autor
- Interdisciplinary Centre for Mathematical and Computational Modeling, University of Warsaw
Bibliografia
- ALABI O.O. 2011. Validity of Darcy’s Law in Laminar Regime. The Electronic Journal of Geotechnical Engineering, 16: 27-40.
- ANDRADE J.S., COSTA U.M.S., ALMEIDA M.P., MAKSE H.A., STANLEY H.E. 1999. Inertial Effects on Fluid Flow through Disordered Porous Media. Physical Review Letters, 82(26): 5249-5252.
- BATENBURG D. VAN, MILTON-TAYLER D. 2005. Discussion on SPE 89325, Beyond beta factors: a complete model for Darcy, Forchheimer, and trans-Forchheimer flow in porous media. JPT, 57(8): 72-73.
- BEAR J. 1972. Dynamics of Fluids in Porous Media. Dover, New York.
- CATALANO E. 2012. A pore-scale coupled hydromechanical model for biphasos granular media. PhD Thesis. University of Grenoble, France.
- CHAPMAN R.E. 1981. Geology and Water - An introduction to fluid mechanics for geologists. Martinus Nijhoff & Dr. W. Junk Publishers, The Hague & Boston & London.
- EWING R., LAZAROV R., LYONS S.L., PAPAVASSILIOU D.V., PASCIAK J., QIN G.X. 1999. Numerical Well Model For Non-Darcy Flow. Computational Geosciences, 3(3-4): 185-204.
- HASSANIZADEH S.M., GRAY W.G. 1987. High Velocity Flow in Porous Media. Transport in Porous Media, 2(6): 521-531.
- HELLSTRO¨M J.G.I., LUNDSTRO¨M T.S. 2006. Flow through Porous Media at Moderate Reynolds Number. 4th International Scientific Colloquium: Modelling for Material Processing. University of Latvia, Riga, Latvia, June 8-9.
- HUANG H., AYOUB J. 2008. Applicability of the Forchheimer Equation for Non-Darcy Flow in Porous Media. SPE Journal, 13(1): 112-122.
- ORODU O.D., MAKINDE F.A., ORODU K.B. 2012. Experimental Study of Darcy and Non-Darcy Flow in Porous Media. International Journal of Engineering and Technology, 2(12): 1934-1943.
- PESZYŃSKA M., TRYKOZKO A. 2013. Pore-to-core simulations of flow with large velocities using continuum models and imaging data. Computational Geosciences, 17(4): 623-645.
- SAWICKI J., SZPAKOWSKI W., WEINEROWSKA K., WOŁOSZYN E., ZIMA P. 2004. Laboratory of Fluid Mechanics and Hydraulics. Technical University of Gdańsk Publisher, Gdańsk, Poland (in Polish).
- SOBIESKI W. 2010. Use of Numerical Models in Validating Experimental Results. Journal of Applied Computer Science, 18(1): 49-60.
- SOBIESKI W., TRYKOZKO A. 2011. Sensitivity aspects of Forchheimer’s approximation. Transport in Porous Media, 89(2): 155-164.
- SUKOP M.C., HUANG H., ALVAREZ P.F., VARIANO E.A., CUNNINGHAM K.J. 2013. Evaluation of permeability and non-Darcy flow in vuggy macroporous limestone aquifer samples with lattice Boltzmann methods. Water Resources Research, 49(1): 1-15.
- TINDALL J.A., KUNKEL J.R., ANDERSON D.E. 1998. Unsaturated Zone Hydrology for Scientist and Engineers. Pearson Education, New Jersey.
Typ dokumentu
Bibliografia
Identyfikator YADDA
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