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  • Articles  (5)
  • homogenization  (5)
  • Springer  (5)
  • American Geophysical Union
  • Annual Reviews
  • Blackwell Publishing Ltd
  • 2020-2024
  • 2005-2009
  • 1990-1994  (5)
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  • 1993  (5)
  • Geosciences  (5)
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  • Articles  (5)
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  • Springer  (5)
  • American Geophysical Union
  • Annual Reviews
  • Blackwell Publishing Ltd
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  • 2020-2024
  • 2005-2009
  • 1990-1994  (5)
  • 1980-1984
  • 1975-1979
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  • 1
    Electronic Resource
    Electronic Resource
    Springer
    Transport in porous media 13 (1993), S. 205-220 
    ISSN: 1573-1634
    Keywords: Dual-porosity ; fractures ; gravitational forces ; homogenization ; modeling ; validation
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Technology
    Notes: Abstract Three models are considered for single component, single phase flow in naturally fractured porous media. The microscopic model holds on the Darcy scale, and it is considered to govern the system. The macroscopic, dual-porosity model was derived in Part I of this work from the microscopic model by two-scale mathematical homogenization. In this paper, we show that the dual-porosity model predicts well the behavior of the microscopic model by comparing their computed solutions in certain reasonable test cases. Homogenization gives a complex formula for a key parameter in the dual-porosity model; herein a simple approximation to this formula is presented. The third model considered is a single-porosity model with averaged parameters. It is shown that this type of model cannot predict the behavior of the microscopic flow.
    Type of Medium: Electronic Resource
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  • 2
    Electronic Resource
    Electronic Resource
    Springer
    Transport in porous media 10 (1993), S. 197-202 
    ISSN: 1573-1634
    Keywords: Constitutive equation ; consolidation ; homogenization ; two-phase medium
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Technology
    Notes: Abstract A set of equations governing the consolidation of a two-phase medium consisting of a porous elastic skeleton saturated with a highly compressible liquid (gas), is described. The homogenization method was utilized to deduce the equations. For the equivalent macroscopic medium, mass and momentum conservation equations and the flow equation of pore liquid are presented. Sample material constants were calculated using laboratory test results which were carried out at the Institute of Geotechnics, Technical University of Wroclaw.
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  • 3
    Electronic Resource
    Electronic Resource
    Springer
    Transport in porous media 12 (1993), S. 73-106 
    ISSN: 1573-1634
    Keywords: Naturally fractured ; dual-porosity ; immiscible displacement ; homogenization
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Technology
    Notes: Abstract A dual-porosity model is defined for saturated, two-phase, compressible, immiscible flow in a vertically fractured reservoir or aquifer. This model allows detailed simulation of the matrix-fracture interaction as well as the matrix flow itself. This is accomplished by directly coupling the matrix and fracture systems along the vertical faces of the matrix blocks, incorporating gravitational effects directly, and simulating flow inside the block. Thus fluid segregation due to gravitational effects and heterogeneities can be simulated. We show that our model can be derived via homogenization techniques. The model (in incompressible form for simplicity of exposition) is then approximated by a computationally efficient finite difference scheme. Calculations are presented to show the convergence of the scheme and to indicate the behavior of the model as a function of several parameters.
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  • 4
    Electronic Resource
    Electronic Resource
    Springer
    Transport in porous media 12 (1993), S. 161-183 
    ISSN: 1573-1634
    Keywords: Heterogeneous porous media ; homogenization ; upscaling ; numerical simulation ; stochastic modeling ; effective conductivity
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Technology
    Notes: Abstract The numerical simulation of flow through heterogeneous formations requires the assignment of the conductivity value to each numerical block. The conductivity is subjected to uncertainty and is modeled as a stationary random space function. In this study a methodology is proposed to relate the statistical moments of the block conductivity to the given moments of the continuously distributed conductivity and to the size of the numerical blocks. After formulating the necessary conditions to be satisfied by the flow in the upscaled medium, it is found that they are obeyed if the mean and the two-point covariance of the space averaged energy disspation function over numerical elements in the two media, of point value and of upscaled conductivity, are identical. This general approach leads to a systematic upscaling procedure for uniform average flow in an unbounded domain. It yields the statistical moments of upscaled logconductivity that depend only on those of the original one and on the size and shape of the numerical elements. The approach is applied to formations of isotropic heterogeneity and to isotropic partition elements. After a general discussion based on dimensional analysis, the procedure is illustrated by using a first-order approximation in the logconductivity variance. The upscaled logconductivity moments (mean, two-point covariance) are computed for two and three dimensional flows, isotropic heterogeneous media and elements of circular or spherical shape. The asymptotic cases of elements of small size, which preserve the point value conductivity structure on one hand, and of large blocks for which the medium can be replaced by one of deterministic effective properties, on the other hand, are analyzed in detail. The results can be used in order to generate the conductivity of numerical elements in Monte Carlo simulations.
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  • 5
    Electronic Resource
    Electronic Resource
    Springer
    Transport in porous media 13 (1993), S. 179-203 
    ISSN: 1573-1634
    Keywords: Dual-porosity ; fractures ; gravitational forces ; homogenization ; modeling
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Technology
    Notes: Abstract We consider the problem of modeling flow through naturally fractured porous media. In this type of media, various physical phenomena occur on disparate length scales, so it is difficult to properly average their effects. In particular, gravitational forces pose special problems. In this paper we develop a general understanding of how to incorporate gravitational forces into the dual-porosity concept. We accomplish this through the mathematical technique of formal two-scale homogenization. This technique enables us to average the single-porosity, Darcy equations that govern the flow on the finest (fracture thickness) scale. The resulting homogenized equations are of dual-porosity type. We consider three flow situations, the flow of a single component in a single phase, the flow of two fluid components in two completely immiscible phases, and the completely miscible flow of two components.
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