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1

XU, PENG, HAICHENG LIU, AGUS PULUNG SASMITO, SHUXIA QIU, and CUIHONG LI. "EFFECTIVE PERMEABILITY OF FRACTURED POROUS MEDIA WITH FRACTAL DUAL-POROSITY MODEL." Fractals 25, no. 04 (2017): 1740014. http://dx.doi.org/10.1142/s0218348x1740014x.

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As natural fractures show statistically fractal scaling laws, fractal geometry has been proposed and applied to model the fracture geometry and to study the hydraulic properties of fractured porous media. In this paper, a fractal dual-porosity model is developed to study the single-phase fluid flow through fractured porous media. An analytical expression for effective permeability of fractured porous media is derived, which depends on the fractal dimension and fracture aperture. The effect of fractal dimensions for fracture aperture distribution and tortuosity, the ratio of minimum to maximum
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2

Fumagalli, Alessio, and Eirik Keilegavlen. "Dual Virtual Element Methods for Discrete Fracture Matrix models." Oil & Gas Science and Technology – Revue d’IFP Energies nouvelles 74 (2019): 41. http://dx.doi.org/10.2516/ogst/2019008.

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The accurate description of fluid flow and transport in fractured porous media is of paramount importance to capture the macroscopic behavior of an oil reservoir, a geothermal system, or a CO2 sequestration site, to name few applications. The construction of accurate simulation models for flow in fractures is challenging due to the high ratio between a fracture’s length and width. In this paper, we present a mixed-dimensional Darcy problem which can represent the pressure and Darcy velocity in all the dimensions, i.e. in the rock matrix, in the fractures, and in their intersections. Moreover,
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3

XU, PENG, CUIHONG LI, SHUXIA QIU, and AGUS PULUNG SASMITO. "A FRACTAL NETWORK MODEL FOR FRACTURED POROUS MEDIA." Fractals 24, no. 02 (2016): 1650018. http://dx.doi.org/10.1142/s0218348x16500183.

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The transport properties and mechanisms of fractured porous media are very important for oil and gas reservoir engineering, hydraulics, environmental science, chemical engineering, etc. In this paper, a fractal dual-porosity model is developed to estimate the equivalent hydraulic properties of fractured porous media, where a fractal tree-like network model is used to characterize the fracture system according to its fractal scaling laws and topological structures. The analytical expressions for the effective permeability of fracture system and fractured porous media, tortuosity, fracture densi
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4

Shafabakhsh, Paiman, Marwan Fahs, Behzad Ataie-Ashtiani, and Craig T. Simmons. "Unstable Density-Driven Flow in Fractured Porous Media: The Fractured Elder Problem." Fluids 4, no. 3 (2019): 168. http://dx.doi.org/10.3390/fluids4030168.

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The Elder problem is one of the well-known examples of an unstable density-driven flow (DDF) and solute transport in porous media. The goal of this research is to investigate the influence of fracture networks on this benchmark problem due to the great importance of the fractured heterogeneity effect on unstable DDF. For this aim, the fractured Elder problem is solved using COMSOL Multiphysics, which is a finite element method simulator. Uniform and orthogonal fracture networks are embedded to analyze free convective flow and development of unstable salt plumes. The results indicate that the m
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5

Song, Jing Wen, Ming Yu Wang, and Da Wei Tang. "Experiment on Water Infiltration and Solute Migration in Porous and Fractured Media." Advanced Materials Research 955-959 (June 2014): 1993–97. http://dx.doi.org/10.4028/www.scientific.net/amr.955-959.1993.

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The experiments were performed by considering the upper loose porous media and lower fractured media as a typical structure of vadose zones, and by constructing the corresponding physical model to simulate water flow and solute transport processes in order to investigate water flow features and migration mechanism. It has been indicated that in the porous and fractured complex media, if the lower fracture structure remains unchanged, the structure and permeability of the porous media offer considerable impact on infiltration processes. Additionally, if the structure and permeability of the por
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6

ZHENG, QIAN, JINTU FAN, XIANGPENG LI, and SHIFANG WANG. "FRACTAL MODEL OF GAS DIFFUSION IN FRACTURED POROUS MEDIA." Fractals 26, no. 03 (2018): 1850035. http://dx.doi.org/10.1142/s0218348x18500354.

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Understanding gas transport behavior though fractured porous media is essential in many fields including fiber science, energy science, soil science, environmental engineering, chemical engineering, etc. In this paper, a fractal model is developed to characterize gas diffusion through fractured porous media, where a bundle of fractal-like tree branching networks is used to represent the fracture system according to fractal scaling laws. The analytical expression for relative gas diffusion coefficient of fractured porous media is derived. The proposed fractal model has been validated by the ava
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7

Novikov, Mikhail A., and Vadim V. Lisitsa. "NUMERICAL ALGORITHM OF SEISMIC ATTENUATION ESTIMATION IN ANISOTROPIC FRACTURED POROUS FLUID-SATURATED MEDIA." Interexpo GEO-Siberia 2, no. 2 (2021): 186–95. http://dx.doi.org/10.33764/2618-981x-2021-2-2-186-195.

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In our work we investigate the effect of transport and elastic properties anisotropy on seismic attenuation due to fracture-to-fracture wave-induced fluid flow using numerical algorithm of estimation of seismic wave attenuation in anisotropic fractured porous fluid-saturated media. Algorithm is based on numerical solution of anisotropic Biot equations using finite-difference scheme on staggered grid. We perform a set of numerical experiments to model wave propagation in fractured media with anisotropic fractured-filling material providing wave-induced fluid flow within interconnected fractures
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8

Schery, S. D., D. J. Holford, J. L. Wilson, and F. M. Phillips. "The Flow and Diffusion of Radon Isotopes in Fractured Porous Media: Part 1, Finite Slabs." Radiation Protection Dosimetry 24, no. 1-4 (1988): 185–89. http://dx.doi.org/10.1093/oxfordjournals.rpd.a080267.

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Abstract In the conventional equations used to describe gaseous transport of radon isotopes through fractured porous media the two processes responsible for radon movement are diffusion and pressure-driven flow (advection). Fractures in a porous medium can be especially effective for pressure-driven transport but lateral diffusion can be a strong mitigating influence. The interplay of diffusion and flow is examined for a fractured concrete slab and a fractured, high-diffusivity layer between a house and an underlying radium-rich medium. For underpressures common in houses, fractures only a fra
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9

Nair, R. N., T. M. Krishnamoorthy, and K. C. Pillai. "Radionuclede Transport Through Fractured Porous Media." Isotopenpraxis Isotopes in Environmental and Health Studies 29, no. 3 (1993): 225–36. http://dx.doi.org/10.1080/00211919308046689.

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10

Owusu, Richard, Adu Sakyi, Peter Amoako-Yirenkyi, and Isaac Kwame Dontwi. "A New Multicontinuum Model for Advection-Diffusion Process of Single-Phase Nonlinear Flow in a Multiscale Fractured Porous Media." Journal of Applied Mathematics 2022 (March 31, 2022): 1–14. http://dx.doi.org/10.1155/2022/5731988.

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Fractured porous media modeling and simulation has seen significant development in the past decade but still pose a great challenge and difficulty due to the multiscale nature of fractures, domain heterogeneity, and the nonlinear flow fields due to the high flow velocity and permeability resulting from the presence of fractures. Therefore, modeling fluid transport that is influenced by both advection and diffusion in fractured porous media studies becomes a generic problem, which this study seeks to address. In this paper, we present a study on non-Darcian fluid transport in multiscale natural
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11

Novikov, Mikhail, Vadim Lisitsa, and Tatiana Khachkova. "IMPACT OF FRACTURED-POROUS MEDIA TRANSPORT PROPERTIES CHANGE IN SEISMIC WAVEFIELDS." Interexpo GEO-Siberia 2, no. 2 (2019): 248–53. http://dx.doi.org/10.33764/2618-981x-2019-2-2-248-253.

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In this paper we research the response of carbonates dissolution when interacting with carbon dioxide in the seismic wave fields in a fractured-porous reservoir. We numerically estimate the change of limestone physical properties due to CO2 sequestration based on the analysis of samples CT-scans. Obtained estimations is then used to model a poroelastic material, which we use as fracture-filling material in statistically generated fractured porous fluid-saturated media models. A numerical modeling of wave propagation is performed to estimate a velocity dispersion and attenuation caused by a wav
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12

XU, PENG. "A DISCUSSION ON FRACTAL MODELS FOR TRANSPORT PHYSICS OF POROUS MEDIA." Fractals 23, no. 03 (2015): 1530001. http://dx.doi.org/10.1142/s0218348x15300019.

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Fractal model provides an alternative and useful means for studying the transport phenomenon in porous media and analyzing the macroscopic transport properties of porous media, as fractal geometry can successfully characterize disordered and heterogeneous geometrical microstructures of porous media on multi scales. Recently, fractal models on porous media have attracted increasing interests from many different disciplines. In this mini-review paper, a review on fractal models for number-size distribution in porous media is made, and a unified fractal model to characterize pore and particle siz
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13

Wu, Tao, Qian Wang, and Shifang Wang. "An Apparent Gas Permeability Model for Real Gas Flow in Fractured Porous Media with Roughened Surfaces." Polymers 13, no. 12 (2021): 1937. http://dx.doi.org/10.3390/polym13121937.

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The investigation of gas transport in fractured porous media is essential in most petroleum and chemical engineering. In this paper, an apparent gas permeability model for real gas flow in fractured porous media is derived with adequate consideration of real gas effect, the roughness of fracture surface, and Knudsen diffusion based on the fractal theory. The fractal apparent gas permeability model is obtained to be a function of micro-structural parameters of fractured porous media, relative roughness, the pressure, the temperature, and the properties of gas. The predictions from the apparent
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14

Sharma, Pramod Kr, Nitin Joshi, Rajesh Srivastava, and C. S. P. Ojha. "Reactive Transport in Fractured Permeable Porous Media." Journal of Hydrologic Engineering 20, no. 7 (2015): 04014078. http://dx.doi.org/10.1061/(asce)he.1943-5584.0001096.

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15

Bai, Mao, Jean-Claude Roegiers, and Hilary I. Inyang. "Contaminant Transport in Nonisothermal Fractured Porous Media." Journal of Environmental Engineering 122, no. 5 (1996): 416–23. http://dx.doi.org/10.1061/(asce)0733-9372(1996)122:5(416).

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16

YEH, LI-MING. "ON TWO-PHASE FLOW IN FRACTURED MEDIA." Mathematical Models and Methods in Applied Sciences 12, no. 08 (2002): 1075–107. http://dx.doi.org/10.1142/s0218202502002045.

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A model describing two-phase, incompressible, immiscible flow in fractured media is discussed. A fractured medium is regarded as a porous medium consisting of two superimposed continua, a continuous fracture system and a discontinuous system of medium-sized matrix blocks. Transport of fluids through the medium is primarily within the fracture system. No flow is allowed between blocks, and only matrix-fracture flow is possible. Matrix block system plays the role of a global source distributed over the entire medium. Two-phase flow in a fractured medium is strongly related to phase mobilities an
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17

Hoteit, Hussein, and Abbas Firoozabadi. "Compositional Modeling of Discrete-Fractured Media Without Transfer Functions by the Discontinuous Galerkin and Mixed Methods." SPE Journal 11, no. 03 (2006): 341–52. http://dx.doi.org/10.2118/90277-pa.

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Summary In a recent work, we introduced a numerical approach that combines the mixed-finite-element (MFE) and the discontinuous Galerkin (DG) methods for compositional modeling in homogeneous and heterogeneous porous media. In this work, we extend our numerical approach to 2D fractured media. We use the discrete-fracture model (crossflow equilibrium) to approximate the two-phase flow with mass transfer in fractured media. The discrete-fracture model is numerically superior to the single-porosity model and overcomes limitations of the dual-porosity model including the use of a shape factor. The
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18

Schery, S. D., D. J. Holford, J. L. Wilson, and F. M. Phillips. "The Flow and Diffusion of Radon Isotopes in Fractured Porous Media: Part 2, Semi-infinite Media." Radiation Protection Dosimetry 24, no. 1-4 (1988): 191–97. http://dx.doi.org/10.1093/oxfordjournals.rpd.a080268.

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Abstract The release of radon isotopes under conditions of combined diffusion and flow from a fractured, semi-infinite medium such as soil is analysed. Relations are developed to indicate when flow from fractures will dominate overall transport and when the radon released from fractures will have the concentration characteristic of great depths. The presence of pressure-driven flow from fractures can greatly enhance transport of radon, but narrow or shallow fractures are not necessarily important due to the strong diffusive exchange with the surrounding porous medium and a reduced vertical pre
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19

Říha, Jakub, and Jiřina Královcová. "GENERATION OF TRANSPORT PATHS IN FRACTURED POROUS MEDIA." Acta Polytechnica 57, no. 5 (2017): 348. http://dx.doi.org/10.14311/ap.2017.57.0348.

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In this article, a method for generation of transport paths in combined equivalent porous media / discrete fracture network computational meshes is proposed as an alternative to a particle tracking method. It is based on a computation of the functional of the velocity and concentration individually for each element of a mesh. Its functionality is demonstrated on two test cases.
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20

Fomin, Sergei A., Vladimir A. Chugunov, and Toshiyuki Hashida. "Non-Fickian mass transport in fractured porous media." Advances in Water Resources 34, no. 2 (2011): 205–14. http://dx.doi.org/10.1016/j.advwatres.2010.11.002.

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21

Natarajan, N., and G. Suresh Kumar. "Effect of fracture-skin on virus transport in fractured porous media." Geoscience Frontiers 3, no. 6 (2012): 893–900. http://dx.doi.org/10.1016/j.gsf.2012.03.004.

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22

Natarajan, N., and G. Suresh Kumar. "Numerical modelling of colloidal transport in fractured porous media with double layered fracture-skin." Journal of Geo-Engineering Sciences 1, no. 2 (2014): 83–94. http://dx.doi.org/10.3233/jgs-130016.

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A numerical model is developed for studying the transport of colloids in a coupled fracture-matrix system with double layer fracture-skin. The governing equations describing colloid transport along the fracture and diffusion into fracture-skin layers as well as rock-matrix, normal to the fracture axis are coupled with each other. The coupled non linear equations are solved numerically with fully implicit finite difference method. Sensitivity analysis is performed to investigate the effect of various colloid properties on the colloid concentration in the multiple porosity fractured system. Coll
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23

Fan, Xiaolin, Shuyu Sun, Wei Wei, and Jisheng Kou. "Numerical Simulation of Pollutant Transport in Fractured Vuggy Porous Karstic Aquifers." Journal of Applied Mathematics 2011 (2011): 1–41. http://dx.doi.org/10.1155/2011/498098.

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This paper begins with presenting a mathematical model for contaminant transport in the fractured vuggy porous media of a species of contaminant (PCP). Two phases are numerically simulated for a process of contaminant and clean water infiltrated in the fractured vuggy porous media by coupling mixed finite element (MFE) method and finite volume method (FVM), both of which are locally conservative, to approximate the model. A hybrid mixed finite element (HMFE) method is applied to approximate the velocity field for the model. The convection and diffusion terms are approached by FVM and the stand
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24

Kfoury, Moussa, Rachid Ababou, Benoît Noetinger, and Michel Quintard. "Upscaling Fractured Heterogeneous Media: Permeability and Mass Exchange Coefficient." Journal of Applied Mechanics 73, no. 1 (2005): 41–46. http://dx.doi.org/10.1115/1.1991864.

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In order to optimize oil recuperation, to secure waste storage, CO2 sequestration and describe more precisely many environmental problems in the underground, we need to improve some homogenization methods that calculate petrophysical parameters. In this paper, we discuss the upscaling of fluid transport equations in fractured heterogeneous media consisting of the fractures themselves and a heterogeneous porous matrix. Our goal is to estimate precisely the fluid flow parameters like permeability and fracture/matrix exchange coefficient at large scale. Two approaches are possible. The first appr
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25

Mikhailov, Mikhail D., M. Ungs, and Renato M. Cotta. "HYBRID SOLUTIONS FOR CONTAMINANT TRANSPORT IN FRACTURED POROUS MEDIA." Hybrid Methods in Engineering 4, no. 1-2 (2002): 27. http://dx.doi.org/10.1615/hybmetheng.v4.i1-2.40.

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26

Sharma, P. K. "Temporal moments for solute transport through fractured porous media." ISH Journal of Hydraulic Engineering 19, no. 3 (2013): 235–43. http://dx.doi.org/10.1080/09715010.2013.798908.

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27

Toran, Laura, Andrea Sjoreen, and Max Morris. "Sensitivity analysis of solute transport in fractured porous media." Geophysical Research Letters 22, no. 11 (1995): 1433–36. http://dx.doi.org/10.1029/95gl01096.

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28

Reynolds, David A., and Bernard H. Kueper. "Multiphase flow and transport through fractured heterogeneous porous media." Journal of Contaminant Hydrology 71, no. 1-4 (2004): 89–110. http://dx.doi.org/10.1016/j.jconhyd.2003.09.008.

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29

Kärger, J. "Flow and Transport in Porous Media and Fractured Rock." Zeitschrift für Physikalische Chemie 194, Part_1 (1996): 135–36. http://dx.doi.org/10.1524/zpch.1996.194.part_1.135a.

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30

Sharma, P. K., and Umang Dixit. "Contaminant transport through fractured-porous media: An experimental study." Journal of Hydro-environment Research 8, no. 3 (2014): 223–33. http://dx.doi.org/10.1016/j.jher.2013.08.003.

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31

Wu, Yu-Shu, Ming Ye, and E. A. Sudicky. "Fracture-Flow-Enhanced Matrix Diffusion in Solute Transport Through Fractured Porous Media." Transport in Porous Media 81, no. 1 (2009): 21–34. http://dx.doi.org/10.1007/s11242-009-9383-4.

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32

CAI, JIANCHAO, WEI WEI, XIANGYUN HU, RICHENG LIU, and JINJIE WANG. "FRACTAL CHARACTERIZATION OF DYNAMIC FRACTURE NETWORK EXTENSION IN POROUS MEDIA." Fractals 25, no. 02 (2017): 1750023. http://dx.doi.org/10.1142/s0218348x17500232.

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Fracture network and fractured porous media as well as their transport properties have received great attentions in many fields from engineering application and basic theoretical researches. Fracture will dynamically extend in length and aperture to form complex fracture network under some external conditions such as percussion drilling, wave propagation, desiccation and hydrofracturing. The complexity of fracture network can be well quantitatively characterized by fractal dimension. In this work, the dynamic characterization of fracture network extension in porous media under drying process i
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33

Cherubini, Claudia, Nicola Pastore, Concetta I. Giasi, and Nicoletta Maria Allegretti. "Laboratory experimental investigation of heat transport in fractured media." Nonlinear Processes in Geophysics 24, no. 1 (2017): 23–42. http://dx.doi.org/10.5194/npg-24-23-2017.

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Abstract. Low enthalpy geothermal energy is a renewable resource that is still underexploited nowadays in relation to its potential for development in society worldwide. Most of its applications have already been investigated, such as heating and cooling of private and public buildings, road defrosting, cooling of industrial processes, food drying systems or desalination. Geothermal power development is a long, risky and expensive process. It basically consists of successive development stages aimed at locating the resources (exploration), confirming the power generating capacity of the reserv
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34

Li, Liyong, and Seong H. Lee. "Efficient Field-Scale Simulation of Black Oil in a Naturally Fractured Reservoir Through Discrete Fracture Networks and Homogenized Media." SPE Reservoir Evaluation & Engineering 11, no. 04 (2008): 750–58. http://dx.doi.org/10.2118/103901-pa.

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Summary This paper describes a hybrid finite volume method, designed to simulate multiphase flow in a field-scale naturally fractured reservoir. Lee et al. (WRR 37:443-455, 2001) developed a hierarchical approach in which the permeability contribution from short fractures is derived in an analytical expression that from medium fractures is numerically solved using a boundary element method. The long fractures are modeled explicitly as major fluid conduits. Reservoirs with well-developed natural fractures include many complex fracture networks that cannot be easily modeled by simple long fractu
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35

Younes, Anis, Marwan Fahs, and Philippe Ackerer. "Modeling of Flow and Transport in Saturated and Unsaturated Porous Media." Water 13, no. 8 (2021): 1088. http://dx.doi.org/10.3390/w13081088.

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Modeling fluid flow and transport processes in porous media is a relevant topic for a wide range of applications. In water resources problems, this topic presents specific challenges related to the multiphysical processes, large time and space scales, heterogeneity and anisotropy of natural porous media, and complex mathematical models characterized by coupled nonlinear equations. This Special Issue aims at collecting papers presenting new developments in the field of flow and transport in porous media. The 25 published papers deal with different aspects of physical processes and applications
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36

Zhang, Wenjuan, Waleed Diab, Hadi Hajibeygi, and Mohammed Al Kobaisi. "A Computational Workflow for Flow and Transport in Fractured Porous Media Based on a Hierarchical Nonlinear Discrete Fracture Modeling Approach." Energies 13, no. 24 (2020): 6667. http://dx.doi.org/10.3390/en13246667.

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Modeling flow and transport in fractured porous media has been a topic of intensive research for a number of energy- and environment-related industries. The presence of multiscale fractures makes it an extremely challenging task to resolve accurately and efficiently the flow dynamics at both the local and global scales. To tackle this challenge, we developed a computational workflow that adopts a two-level hierarchical strategy based on fracture length partitioning. This was achieved by specifying a partition length to split the discrete fracture network (DFN) into small-scale fractures and la
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37

Ibaraki, M., and E. A. Sudicky. "Colloid-facilitated contaminant transport in discretely fractured porous media: 2. Fracture network examples." Water Resources Research 31, no. 12 (1995): 2961–69. http://dx.doi.org/10.1029/95wr02181.

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38

Yang, Jianwen. "Reactive silica transport in fractured porous media: Analytical solution for a single fracture." Computers & Geosciences 38, no. 1 (2012): 80–86. http://dx.doi.org/10.1016/j.cageo.2011.05.008.

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39

Formaggia, Luca, Alessio Fumagalli, and Anna Scotti. "A multi-layer reactive transport model for fractured porous media." Mathematics in Engineering 4, no. 1 (2021): 1–32. http://dx.doi.org/10.3934/mine.2022008.

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40

Hakl, J., I. Csige, I. Hunyadi, A. Várhegyi, and G. Géczy. "Radon transport in fractured porous media — Experimental study in caves." Environment International 22 (January 1996): 433–37. http://dx.doi.org/10.1016/s0160-4120(96)00143-2.

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41

Battiato, Ilenia, Daniel M. Tartakovsky, Alexandre M. Tartakovsky, and T. D. Scheibe. "Hybrid models of reactive transport in porous and fractured media." Advances in Water Resources 34, no. 9 (2011): 1140–50. http://dx.doi.org/10.1016/j.advwatres.2011.01.012.

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42

Zhang, Dongxiao, and Qinjun Kang. "Pore scale simulation of solute transport in fractured porous media." Geophysical Research Letters 31, no. 12 (2004): n/a. http://dx.doi.org/10.1029/2004gl019886.

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43

Logan, J. D., V. A. Zlotnik, and S. Cohn. "Transport in fractured porous media with time-periodic boundary conditions." Mathematical and Computer Modelling 24, no. 9 (1996): 1–9. http://dx.doi.org/10.1016/0895-7177(96)00149-5.

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44

Leo, C. J., and J. R. Booker. "Boundary element analysis of contaminant transport in fractured porous media." International Journal for Numerical and Analytical Methods in Geomechanics 17, no. 7 (1993): 471–92. http://dx.doi.org/10.1002/nag.1610170704.

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45

Valliappan, S., W. Wang, and N. Khalili. "Contaminant transport under variable density flow in fractured porous media." International Journal for Numerical and Analytical Methods in Geomechanics 22, no. 7 (1998): 575–95. http://dx.doi.org/10.1002/(sici)1096-9853(199807)22:7<575::aid-nag928>3.0.co;2-x.

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46

Faybishenko, Boris. "A Concept of Fuzzy Dual Permeability of Fractured Porous Media." Water 15, no. 21 (2023): 3752. http://dx.doi.org/10.3390/w15213752.

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The interpretation of the results of hydrogeological field observations and the modeling of fractured porous subsurface media is often conducted using dual-porosity and/or dual-permeability concepts. These concepts, however, do not consider the effects of spatial and temporal variations and uncertainties, or fuzziness, in the evaluation of the subsurface flow characteristics of fractured porous media. The goal of the paper is to introduce a concept of fuzzy dual permeability of fractured porous media based on the fuzzy system analysis of the results of ponded infiltration tests in fractured ba
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47

Blessent, Daniela, Peter R. Jørgensen, and René Therrien. "Comparing Discrete Fracture and Continuum Models to Predict Contaminant Transport in Fractured Porous Media." Groundwater 52, no. 1 (2013): 84–95. http://dx.doi.org/10.1111/gwat.12032.

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48

Ireson, A. M., A. B. Butler, and H. S. Wheater. "Evidence for the onset and persistence with depth of preferential flow in unsaturated fractured porous media." Hydrology Research 43, no. 5 (2012): 707–19. http://dx.doi.org/10.2166/nh.2012.030.

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Two distinct types of fracture flow can occur in unsaturated fractured porous media: non-preferential flow, whereby the fractures and matrix wet up in equilibrium, and preferential flow, whereby water in the fractures bypasses the matrix. This has important implications for how infiltration, recharge, groundwater flooding and contaminant transport are modelled. Taking the UK Chalk as a case study, we explore evidence for the occurrence of unsaturated preferential fracture flow, considering separately its initiation in the near surface, and persistence at 20–30 m depth. We postulate a link betw
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Natarajan, N., and G. Suresh Kumar. "Numerical modeling of bacteria facilitated contaminant transport in fractured porous media." Colloids and Surfaces A: Physicochemical and Engineering Aspects 387, no. 1-3 (2011): 104–12. http://dx.doi.org/10.1016/j.colsurfa.2011.07.037.

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Grillo, Alfio, Dmitriy Logashenko, Sabine Stichel, and Gabriel Wittum. "Forchheimer’s correction in modelling flow and transport in fractured porous media." Computing and Visualization in Science 15, no. 4 (2012): 169–90. http://dx.doi.org/10.1007/s00791-013-0208-1.

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