Contributions of diffusion, dissolution, ion exchange, and leakage from low-permeability layers to confined aquifers-Reference-Cited by-同舟云学术

Contributions of diffusion, dissolution, ion exchange, and leakage from low-permeability layers to confined aquifers

Published:2005-09 Issue:9 Volume:41 Page:
ISSN:0043-1397
Container-title:Water Resources Research
language:en
Short-container-title:Water Resour. Res.

Author:

Atteia O.¹,Andre L.²,Dupuy A.¹,Franceschi M.¹

Affiliation:

1. Institut Environnement, Géo-ingénierie et Développement (EGID); Université Michel De Montaigne; Pessac France

2. Centre d’hydrogéologie de l’Université de Neuchâtel (CHYN); Neuchatel Switzerland

Publisher

American Geophysical Union (AGU)

Subject

Water Science and Technology

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1029/2003WR002593/fullpdf

Reference33 articles.

1. Beekman , H. E. 1991 Ion chromatography of fresh- and sea-water intrusion: Multicomponent dispersive and diffusive transport in groundwater Univ. Utrecht Utrecht, Netherlands

2. Paradox of groundwater age;Bethke;Geology,2002

3. Bredehoeft , J. D. C. E. Neuzil P. C. D. Milly 1983 Regional flow in the Dakota Aquifer: A study of the role of confining layers U.S. Geol. Surv. Water Supply Pap. 2237

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