Solute transport in fractured rocks with stagnant water zone and rock matrix composed of different geological layers-Model development and simulations-Reference-Cited by-同舟云学术

Solute transport in fractured rocks with stagnant water zone and rock matrix composed of different geological layers-Model development and simulations

Published:2013-03 Issue:3 Volume:49 Page:1709-1727
ISSN:0043-1397
Container-title:Water Resources Research
language:en
Short-container-title:Water Resour. Res.

Author:

Mahmoudzadeh Batoul¹,Liu Longcheng¹,Moreno Luis¹,Neretnieks Ivars¹

Affiliation:

1. Department of Chemical Engineering and Technology; Royal Institute of Technology; S-100 44 Stockholm Sweden

Funder

Swedish Nuclear Fuel and Waste Management Company (SKB)

Publisher

American Geophysical Union (AGU)

Subject

Water Science and Technology

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1002/wrcr.20132/fullpdf

Reference39 articles.

1. Abelin H. L. Moreno S. Tunbrant J. Gidlund I. Neretnieks 1985 Flow and tracer movements in some natural fractures in the Stripa granite

2. A large scale flow and tracer experiment in granite. II. Results and interpretation;Abelin;Water Resour. Res.,1991

3. Channeling experiments in crystalline fractured rocks;Abelin;J. Contam. Hydrol.,1994

4. Linear response concept combining advection and limited rock matrix in a fracture network transport model;Barten;Water Resour. Res.,1996

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