Statistical characteristics of flow as indicators of channeling in heterogeneous porous and fractured media

被引:45
作者
Le Goc, R. [1 ,2 ]
de Dreuzy, J. -R. [1 ]
Davy, P. [1 ]
机构
[1] Univ Rennes 1, CNRS, UMR 6118, CS 74205, F-35042 Rennes, France
[2] Itasca Consultants SAS, F-69134 Ecully, France
关键词
Flow channels; Heterogeneous media; Connectivity; Fracture network; Channeling indicators; HYDRAULIC CONDUCTIVITY; CONNECTIVITY; TRANSPORT; SYSTEMS;
D O I
10.1016/j.advwatres.2009.12.002
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
We introduce two new channeling indicators D-ic and D-cc based on the Lagrangian distribution of flow rates. On the basis of the participation ratio, these indicators characterize the extremes of both the flow-tube width distribution and the flow rate variation along flow lines. The participation ratio is an indicator biased toward the larger values of a distribution and is equal to the normalized ratio of the square of the first-order moment to the second-order moment. Compared with other existing indicators, they advantageously provide additional information on the flow channel geometry, are consistently applicable to both porous and fractured media, and are generally less variable for media generated using the same parameters than other indicators. Based on their computation for a broad range of porous and fracture permeability fields, we show that they consistently characterize two different geometric properties of channels. D-ic gives a characteristic scale of low-flow zones in porous media and a characteristic distance between effectively flowing structures in fractured cases. D-cc gives a characteristic scale of the extension of high-flow zones in porous media and a characteristic channel length in fractured media. D-ic is mostly determined by channel density and permeability variability. D-cc is, however, more affected by the nature of the correlation structure like the presence of permeability channels or fractures in porous media and the length distribution in fracture networks. (C) 2009 Elsevier Ltd. All rights reserved.
引用
收藏
页码:257 / 269
页数:13
相关论文
共 44 条
  • [1] [Anonymous], 1967, Elements pour une theorie des milieux poreux
  • [2] BEAUDOIN A, 2007, EUROPAR 2007 PARALLE
  • [3] Scaling of fracture systems in geological media
    Bonnet, E
    Bour, O
    Odling, NE
    Davy, P
    Main, I
    Cowie, P
    Berkowitz, B
    [J]. REVIEWS OF GEOPHYSICS, 2001, 39 (03) : 347 - 383
  • [4] Relating flow channelling to tracer dispersion in heterogeneous networks
    Bruderer-Weng, C
    Cowie, P
    Bernabé, Y
    Main, I
    [J]. ADVANCES IN WATER RESOURCES, 2004, 27 (08) : 843 - 855
  • [5] Algorithm 832: UMFPACK V4.3 - An unsymmetric-pattern multifrontal method
    Davis, TA
    [J]. ACM TRANSACTIONS ON MATHEMATICAL SOFTWARE, 2004, 30 (02): : 196 - 199
  • [6] LOCALIZATION AND FAULT GROWTH IN LAYERED BRITTLE-DUCTILE SYSTEMS - IMPLICATIONS FOR DEFORMATIONS OF THE CONTINENTAL LITHOSPHERE
    DAVY, P
    HANSEN, A
    BONNET, E
    ZHANG, SZ
    [J]. JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH, 1995, 100 (B4) : 6281 - 6294
  • [7] Hydraulic properties of two-dimensional random fracture networks following a power law length distribution 2. Permeability of networks based on lognormal distribution of apertures
    de Dreuzy, JR
    Davy, P
    Bour, O
    [J]. WATER RESOURCES RESEARCH, 2001, 37 (08) : 2079 - 2095
  • [8] Dealing with spatial heterogeneity
    de Marsily, G
    Delay, F
    Gonçalvès, J
    Renard, P
    Teles, V
    Violette, S
    [J]. HYDROGEOLOGY JOURNAL, 2005, 13 (01) : 161 - 183
  • [9] DEDREUZY JR, 2007, WATER RESOUR RES, V43, P13
  • [10] SPATIAL AVERAGING OF HYDRAULIC CONDUCTIVITY IN 3-DIMENSIONAL HETEROGENEOUS POROUS-MEDIA
    DESBARATS, AJ
    [J]. MATHEMATICAL GEOLOGY, 1992, 24 (03): : 249 - 267