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-Reference-Cited by-同舟云学术

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

Published:2003-03 Issue:3 Volume:39 Page:
ISSN:0043-1397
Container-title:Water Resources Research
language:en
Short-container-title:Water Resour. Res.

Author:

Zinn Brendan¹,Harvey Charles F.¹

Affiliation:

1. Ralph M. Parsons Laboratory, Department of Civil and Environmental Engineering; Massachusetts Institute of Technology; Cambridge Massachusetts USA

Publisher

American Geophysical Union (AGU)

Subject

Water Science and Technology

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1029/2001WR001146/fullpdf

Reference54 articles.

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4. Direct comparison of kinetic and local equilibrium formulations for solute transport affected by surface reactions;Bahr;Water Resour. Res.,1987

5. Basic concept of the theory of seepage of homogeneous liquids in fissured rocks;Barenblatt;J. Appl. Math. Mech.,1960

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