Géosciences Montpellier

Partenaires

CNRS
Logo UM2

Géosciences Montpellier
UMR 5243 - CC 60
Université Montpellier 2
Place E. Bataillon
34095 Montpellier cedex 5

Tél +33 (0) 4 67 14 36 43
Fax +33 (0) 4 67 14 36 42

Rechercher

Sur ce site

Sur le Web du CNRS

Accueil du site > Grand public & Presse > Ressources documentaires > Anciens thèmes de recherche > Réservoirs > Hydrodynamique souterraine > Références citées

Références citées

Bonnet, E., O. Bour, N. Odling, I. , Main, B. Berkowitz, P. Davy, and P. Cowie (2001). Scaling of Fracture Systems in Geological Media. Rev. of Geophys., 39, 347-383.

Gautier S. and Gibert D., (2005), Inversion of roughness parameters of self-affine surfaces from backscattered waves, GJInt, doi : 10.1111/j.1365-246x-2005.02500.

Gelhar, L. W. 1993. Stochastic Subsurface Hydrology, Engelwood Cliffs, New Jersey.

Hornby B.E., Johnson D.L., Winkler K.H., and Plumb R.A. (1989), Fracture evaluation using reflected Stonley-wave arrivals, Geophysics, 54, 1274-1288.

Le Borgne, T., O. Bour, J.-R. De Dreuzy, P. Davy, and F. Touchard (2004). Equivalent mean flow models for fractured aquifers : Insights from a pumping tests scaling interpretation. Water Resources Research, 40, doi:10.1029/2003WR002436.

Tang X.M. and Cheng A. (2004), Quantitative borehole acoustic methods, Handbook of geophysical exploration, seismic exploration, volume 24, Elsevier, p255.

Tsang, C.-F., and I. Neretnieks (1998). Flow Channeling in Heterogeneous Fractured Rocks. Reviews of Geophysics, 36, 257-298.

Winkler K.W., Liu H.L. and Johnson D.L. (1989), Permeability and borehole Stoneley waves : comparison between experiment and theory, Geophysics, 54, 66-75.

Zinn, B., and C. F. Harvey (2003). When good statistical models of aquifer heterogeneity go bad : A comparison of flow, dispersion, and mass transfer in connected and multivariate Gaussian hydraulic conductivity fields. Water Resources Research, 39, 1051, doi:10.1029/2001WR001146.

Dans la même rubrique :