Journal articles: 'Porous media'

1

Ma, Li. "Porous media equation on locally finite graphs." Archivum Mathematicum, no. 3 (2022): 177–87. http://dx.doi.org/10.5817/am2022-3-177.

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Adler, P. M., and J. F. Thovert. "Fractal porous media." Transport in Porous Media 13, no. 1 (October 1993): 41–78. http://dx.doi.org/10.1007/bf00613270.

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Yeghiazarian, Lilit, Krishna Pillai, and Rodrigo Rosati. "Thin Porous Media." Transport in Porous Media 115, no. 3 (November 12, 2016): 407–10. http://dx.doi.org/10.1007/s11242-016-0793-9.

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4

Bejan, Adrian. "2.11.4 HEAT TRANSFER IN POROUS MEDIA: Heat exchangers as porous media." Heat Exchanger Design Updates 6, no. 2 (1999): 3. http://dx.doi.org/10.1615/heatexchdesignupd.v6.i2.40.

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5

Selim, H. M., Hannes Flühler, and Rainer Schulin. "Simultaneous Ion Transport and Exchange in Aggregated Porous Media." Zeitschrift der Deutschen Geologischen Gesellschaft 136, no. 2 (December 1, 1985): 385–96. http://dx.doi.org/10.1127/zdgg/136/1985/385.

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Jaakko, Miettinen, and Ilvonen Mikko. "ICONE15-10291 SOLVING POROUS MEDIA FLOW FOR LWR COMPONENTS." Proceedings of the International Conference on Nuclear Engineering (ICONE) 2007.15 (2007): _ICONE1510. http://dx.doi.org/10.1299/jsmeicone.2007.15._icone1510_146.

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Plecas, Ilija. "Mathematical modelling of transport phenomena in concrete porous media." Epitoanyag - Journal of Silicate Based and Composite Materials 61, no. 1 (2009): 11–13. http://dx.doi.org/10.14382/epitoanyag-jsbcm.2009.3.

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8

x, MAAlam, Akshay Chaudhry, and Janmeet Singh. "Effect of Angularity on Hydraulic Conductivity of Porous Media." International Journal of Scientific Engineering and Research 5, no. 1 (January 27, 2017): 1–6. https://doi.org/10.70729/ijser151154.

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9

Quintard, Michel. "TRANSFERS IN POROUS MEDIA." Special Topics & Reviews in Porous Media: An International Journal 6, no. 2 (2015): 91–108. http://dx.doi.org/10.1615/specialtopicsrevporousmedia.2015013158.

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10

Adler, P. "Transports in Porous Media." Materials Science Forum 123-125 (January 1993): 3–4. http://dx.doi.org/10.4028/www.scientific.net/msf.123-125.3.

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11

Dashtpour, Omid. "Transport in Porous Media." International Journal of Oil, Gas and Coal Engineering 1, no. 1 (2013): 1. http://dx.doi.org/10.11648/j.ogce.20130101.11.

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12

Bourbie, T., O. Coussy, B. Zinszner, and Miguel C. Junger. "Acoustics of Porous Media." Journal of the Acoustical Society of America 91, no. 5 (May 1992): 3080. http://dx.doi.org/10.1121/1.402899.

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13

Kamal, M. M., and A. A. Mohamad. "Combustion in Porous Media." Proceedings of the Institution of Mechanical Engineers, Part A: Journal of Power and Energy 220, no. 5 (July 11, 2006): 487–508. http://dx.doi.org/10.1243/09576509jpe169.

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14

Aït-Mokhtar, Abdelkarim, Olivier Millet, and Ouali Amiri. "Electrodiffusion in porous media." Revue Européenne de Génie Civil 11, no. 6 (June 2007): 775–85. http://dx.doi.org/10.1080/17747120.2007.9692958.

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15

BUSSCHER, WARREN. "Advances in Porous Media." Soil Science 155, no. 6 (June 1993): 425. http://dx.doi.org/10.1097/00010694-199306000-00008.

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16

Selvadurai, Patrick. "Transport in porous media." European Journal of Environmental and Civil Engineering 14, no. 8-9 (September 2010): 949–87. http://dx.doi.org/10.1080/19648189.2010.9693275.

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17

Lenormand, R. "Liquids in porous media." Journal of Physics: Condensed Matter 2, S (December 1, 1990): SA79—SA88. http://dx.doi.org/10.1088/0953-8984/2/s/008.

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18

HAMBLEY, D. F. "Mechanics of Porous Media." Environmental & Engineering Geoscience II, no. 3 (September 1, 1996): 449–50. http://dx.doi.org/10.2113/gseegeosci.ii.3.449.

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19

Bacri, L., and F. Brochard-Wyart. "Dewetting on porous media." Europhysics Letters (EPL) 56, no. 3 (November 2001): 414–19. http://dx.doi.org/10.1209/epl/i2001-00534-y.

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20

Villermaux, Emmanuel. "Mixing by porous media." Comptes Rendus Mécanique 340, no. 11-12 (November 2012): 933–43. http://dx.doi.org/10.1016/j.crme.2012.10.042.

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21

Steeb, Holger, and David Smeulders. "Waves in Porous Media." Transport in Porous Media 93, no. 2 (April 6, 2012): 241–42. http://dx.doi.org/10.1007/s11242-012-9998-8.

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22

Shokri, Nima, Dani Or, Noam Weisbrod, and Marc Prat. "Drying of Porous Media." Transport in Porous Media 110, no. 2 (September 25, 2015): 171–73. http://dx.doi.org/10.1007/s11242-015-0577-7.

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23

Blokhra, R. L., and J. Joshi. "Flow through Porous Media." Journal of Colloid and Interface Science 160, no. 1 (October 1993): 260–61. http://dx.doi.org/10.1006/jcis.1993.1393.

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24

Adler, Pierre. "Transport in Porous Media." Journal of Chemical Technology & Biotechnology 65, no. 4 (April 1996): 386–87. http://dx.doi.org/10.1002/(sici)1097-4660(199604)65:4<386::aid-jctb420>3.0.co;2-a.

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25

Békri, S., J. F. Thovert, and P. M. Adler. "Dissolution of porous media." Chemical Engineering Science 50, no. 17 (September 1995): 2765–91. http://dx.doi.org/10.1016/0009-2509(95)00121-k.

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26

Miller, Robert D. "Capillary thermomechanics in serially porous media, with implications for randomly porous media." Water Resources Research 34, no. 6 (June 1998): 1361–71. http://dx.doi.org/10.1029/98wr00728.

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27

Mota, M., J. A. Teixeira, and A. Yelshin. "Immobilized Particles in Gel Matrix-Type Porous Media. Homogeneous Porous Media Model." Biotechnology Progress 17, no. 5 (October 5, 2001): 860–65. http://dx.doi.org/10.1021/bp010064t.

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28

Liang, Yuntao, Peiyu Hu, Shugang Wang, Shuanglin Song, and Shuang Jiang. "Medial axis extraction algorithm specializing in porous media." Powder Technology 343 (February 2019): 512–20. http://dx.doi.org/10.1016/j.powtec.2018.11.061.

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29

Whitaker, Stephen. "Flow in porous media III: Deformable media." Transport in Porous Media 1, no. 2 (1986): 127–54. http://dx.doi.org/10.1007/bf00714689.

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30

ZHENG, JIAYI, XING SHI, JUAN SHI, and ZHENQIAN CHEN. "PORE STRUCTURE RECONSTRUCTION AND MOISTURE MIGRATION IN POROUS MEDIA." Fractals 22, no. 03 (September 2014): 1440007. http://dx.doi.org/10.1142/s0218348x14400076.

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Three kinds of porous media (isotropic, perpendicular anisotropic and parallel anisotropic porous media) with the same porosity, different pore size distributions and fractal spectral dimensions were reconstructed by random growth method. It was aimed to theoretically study the impact of microscopic pore structure on water vapor diffusion process in porous media. The results show that pore size distribution can only denote the static characteristics of porous media but cannot effectively reflect the dynamic transport characteristics of porous media. Fractal spectral dimension can effectively analyze and reflect pores connectivity and moisture dynamic transport properties of porous media from the microscopic perspective. The pores connectivity and water vapor diffusion performance in pores of porous media get better with the increase of fractal spectral dimension of porous media. Fractal spectral dimension of parallel anisotropic porous media is more than that of perpendicular anisotropic porous media. Fractal spectral dimension of isotropic porous media is between parallel anisotropic porous media and perpendicular anisotropic porous media. Other macroscopic parameters such as equilibrium diffusion coefficient of water vapor, water vapor concentration variation at right boundary in equilibrium, the time when water vapor diffusion process reaches a stable state also can characterize the pores connectivity and water vapor diffusion properties of porous media.

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31

Rahim, Nawzad O., Kamal A. Rasheed, and Omed Saeed Qadir. "Effect of Grain size of Porous Media on Physical Clogging." Journal of Zankoy Sulaimani - Part A 10, no. 1 (November 19, 2006): 59–72. http://dx.doi.org/10.17656/jzs.10164.

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32

Salokhe, Shivam, Mohammad Rahmati, Ryan Masoodi, and Jane Entwhistle. "NUMERICAL SIMULATION OF FLOW THROUGH ABSORBING POROUS MEDIA PART 1: RIGID POROUS MEDIA." Journal of Porous Media 25, no. 5 (2022): 53–75. http://dx.doi.org/10.1615/jpormedia.2022039973.

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33

Ahmed Janvekar, Ayub, M. Z. Abdullah, Zainal Arifin Ahmad, Aizat Abas, Ahmed A. Hussien, Musavir Bashir, Qummare Azam, and Mohammed Ziad Desai. "Assessment of porous media combustion with foam porous media for surface/submerged flame." Materials Today: Proceedings 5, no. 10 (2018): 20865–73. http://dx.doi.org/10.1016/j.matpr.2018.06.473.

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34

Frisken, B. J., Andrea J. Liu, and David S. Cannell. "Critical Fluids in Porous Media." MRS Bulletin 19, no. 5 (May 1994): 19–24. http://dx.doi.org/10.1557/s0883769400036526.

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The behavior of fluids confined in porous materials has been of interest to engineers and scientists for many decades. Among the applications driving this research are the use of porous membranes to achieve liquid-liquid separations and to deionize water, the use of porous materials as beds for catalysis, and the need to extract liquids (especially oil and water) from such media. Many of these applications depend on transport, which is governed by flow or diffusion in the imbibed fluids. Both the flow and diffusion of multiphase fluids in porous media, however, strongly depend on the morphology of phase-separated domains, and on the kinetics of domain growth. Thus, it is worthwhile to study the behavior of multiphase fluids in porous media in the absence of flow. Recently, much attention has focused on even simpler systems that still capture these essential features, namely, near-critical binary liquid mixtures and vapor-liquid systems in model porous media, such as Vycor and dilute silica gels. Although near-critical fluids may seem rather artificial as models for multiphase liquids, there are several advantages associated with them. In general, domain morphology and growth kinetics are governed primarily by competition between interfacial tension and the preferential attraction of one phase to the surface of the medium. In near-critical fluids, the relative strength of these two energy scales is sensitive to temperature, and can therefore be altered in a controlled fashion. In addition, the kinetics of domain growth are sensitive to the temperature quench depth, and can be controlled.

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35

Biswal, Bibhu, Pål-Eric Øren, Rudolf J. Held, Stig Bakke, and Rudolf Hilfer. "MODELING OF MULTISCALE POROUS MEDIA." Image Analysis & Stereology 27, no. 1 (May 3, 2011): 23. http://dx.doi.org/10.5566/ias.v28.p23-34.

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A stochastic geometrical modeling method for reconstructing three dimensional pore scale microstructures of multiscale porous media is presented. In this method the porous medium is represented by a random but spatially correlated structure of objects placed in the continuum. The model exhibits correlations with the sedimentary textures, scale dependent intergranular porosity over many decades, vuggy or dissolution porosity, a percolating pore space, a fully connected matrix space, strong resolution dependence and wide variability in the permeabilities and other properties. The continuum representation allows discretization at arbitrary resolutions providing synthetic micro-computertomographic images for resolution dependent fluid flow simulation. Model implementations for two different carbonate rocks are presented. The method can be used to generate pore scale models of a wide class of multiscale porous media.

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36

Remache, Leila, and Nacerddine Djermane. "Material Behavior of Porous Media." Advanced Materials Research 816-817 (September 2013): 42–46. http://dx.doi.org/10.4028/www.scientific.net/amr.816-817.42.

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The drying of porous media is studied in this paper by means of the continuous approach and the control volume method. Both transport phenomena inside the porous medium and overall drying kinetics are analyzed. The model utilized in this study requires a lot of physical properties. All of them have been established experimentally. The capillary pressure, which depends on the moisture content, is obtained by a mercury intrusion curve.

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37

Zhang, Guofang, Taoping Chen, Fuping Wang, Boyu Sun, Yong Wang, and Dali Hou. "Experimental determination of deviation factor of natural gas in natural gas reservoir with high CO2 content." E3S Web of Conferences 245 (2021): 01045. http://dx.doi.org/10.1051/e3sconf/202124501045.

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The deviation factor of natural gas is a coefficient to quantitatively describe the deviation degree between real gas (natural gas) and ideal gas. Generally, the deviation factor of natural gas is measured in PVT cell without considering porous media. However, when natural gas is in underground porous media reservoir, due to the adsorption of porous media, the deviation factor of natural gas in porous media deviates from that measured in conventional PVT cell. Moreover, compared with other gases, CO2 has stronger adsorption capacity. Therefore, in porous media, the deviation factor of natural gas considering the adsorption of porous media is quite different from that measured in conventional PVT cell. In this paper, simulating the isothermal mining conditions in gas reservoir,the deviation factor of natural gas with different CO2 content considering the influence of porous media under different pressure isothermal conditions is studied by using the test of designed sand filled long slim tube in series. And under the same conditions, the deviation factor is compared with that of conventional PVT. The experimental results show that under the same conditions, due to the adsorption of porous media, the deviation factor measured in porous media is smaller than that measured by PVT cell without considering porous media.

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38

Vafai, Kambiz, Weifeng Lv, Hirofumi Daiguji, and Moran Wang. "PREFACE: TRANSFERS IN POROUS MEDIA." Special Topics & Reviews in Porous Media: An International Journal 6, no. 2 (2015): v—vi. http://dx.doi.org/10.1615/specialtopicsrevporousmedia.2015015248.

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39

Amanifard, N., M. Borji, and A. K. Haghi. "Heat transfer in porous media." Brazilian Journal of Chemical Engineering 24, no. 2 (June 2007): 223–32. http://dx.doi.org/10.1590/s0104-66322007000200007.

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40

Jasti, Jay K., Ravimadhav N. Vaidya, and H. Scott Fogler. "Capacitance Effects in Porous Media." SPE Reservoir Engineering 3, no. 04 (November 1, 1988): 1207–14. http://dx.doi.org/10.2118/16707-pa.

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41

Johnson, P., V. Starov, and A. Trybala. "Foam flow through porous media." Current Opinion in Colloid & Interface Science 58 (April 2022): 101555. http://dx.doi.org/10.1016/j.cocis.2021.101555.

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42

Balcerak, Ernie. "Dynamic pressures in porous media." Eos, Transactions American Geophysical Union 93, no. 49 (December 4, 2012): 520. http://dx.doi.org/10.1029/2012eo490010.

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43

Dautov, Raphail, Konstantin Kornev, and Valerii Mourzenko. "Foam patterning in porous media." Physical Review E 56, no. 6 (December 1, 1997): 6929–44. http://dx.doi.org/10.1103/physreve.56.6929.

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44

Rojas, Sergio, and Joel Koplik. "Nonlinear flow in porous media." Physical Review E 58, no. 4 (October 1, 1998): 4776–82. http://dx.doi.org/10.1103/physreve.58.4776.

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45

Ostrovsky, Lev A. "Acoustic nonlinearities in porous media." Journal of the Acoustical Society of America 100, no. 4 (October 1996): 2766. http://dx.doi.org/10.1121/1.416374.

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46

Alcocer, F. J., V. Kumar, and P. Singh. "Permeability of periodic porous media." Physical Review E 59, no. 1 (January 1, 1999): 711–14. http://dx.doi.org/10.1103/physreve.59.711.

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47

Salvage, Karen M. "Reactive Transport in Porous Media." Eos, Transactions American Geophysical Union 80, no. 4 (1999): 39. http://dx.doi.org/10.1029/99eo00031.

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48

Groupe, Poreux P. C. "Transport in Heterogeneous Porous Media." Physica Scripta T19B (January 1, 1987): 524–30. http://dx.doi.org/10.1088/0031-8949/1987/t19b/033.

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49

Feder, Jens, and Torstein Jøssang. "Fractal Flow in Porous Media." Physica Scripta T29 (January 1, 1989): 200–205. http://dx.doi.org/10.1088/0031-8949/1989/t29/037.

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50

Hewitt, D. R. "Vigorous convection in porous media." Proceedings of the Royal Society A: Mathematical, Physical and Engineering Sciences 476, no. 2239 (July 2020): 20200111. http://dx.doi.org/10.1098/rspa.2020.0111.

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The problem of convection in a fluid-saturated porous medium is reviewed with a focus on ‘vigorous’ convective flow, when the driving buoyancy forces are large relative to any dissipative forces in the system. This limit of strong convection is applicable in numerous settings in geophysics and beyond, including geothermal circulation, thermohaline mixing in the subsurface and heat transport through the lithosphere. Its manifestations range from ‘black smoker’ chimneys at mid-ocean ridges to salt-desert patterns to astrological plumes, and it has received a great deal of recent attention because of its important role in the long-term stability of geologically sequestered CO 2 . In this review, the basic mathematical framework for convection in porous media governed by Darcy’s Law is outlined, and its validity and limitations discussed. The main focus of the review is split between ‘two-sided’ and ‘one-sided’ systems: the former mimics the classical Rayleigh–Bénard set-up of a cell heated from below and cooled from above, allowing for detailed examination of convective dynamics and fluxes; the latter involves convection from one boundary only, which evolves in time through a series of regimes. Both set-ups are reviewed, accounting for theoretical, numerical and experimental studies in each case, and studies that incorporate additional physical effects are discussed. Future research in this area and various associated modelling challenges are also discussed.

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Journal articles on the topic 'Porous media'

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