Unsaturated flow through fracture networks: Evolution of liquid phase structure, dynamics, and the critical importance of fracture intersections-Reference-Cited by-同舟云学术

Unsaturated flow through fracture networks: Evolution of liquid phase structure, dynamics, and the critical importance of fracture intersections

Published:2003-12 Issue:12 Volume:39 Page:
ISSN:0043-1397
Container-title:Water Resources Research
language:en
Short-container-title:Water Resour. Res.

Author:

Glass Robert J.¹,Nicholl Michael J.²,Rajaram Harihar³,Wood Thomas R.⁴

Affiliation:

1. Flow Visualization and Processes Laboratory; Sandia National Laboratories; Albuquerque New Mexico USA

2. Mining and Geological Engineering; University of Idaho; Moscow Idaho USA

3. Department of Civil, Environmental, and Architectural Engineering; University of Colorado; Boulder Colorado USA

4. Idaho National Engineering and Environmental Laboratory; Idaho Falls Idaho USA

Publisher

American Geophysical Union (AGU)

Subject

Water Science and Technology

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1029/2003WR002015/fullpdf

Reference24 articles.

1. Slow two-phase flow in artificial fractures: Experiments and simulations;Amundsen;Water Resour. Res.,1999

2. Field observation of flow in a fracture intersecting unsaturated chalk;Dahan;Water Resour. Res.,1999

3. Geochemical evidence of preferential flow of water through fractures in unsaturated tuff, Apache Leap, Arizona;Davidson;Appl. Geochem.,1998

4. Implications of environmental isotopes for flow and transport in the unsaturated zone at Yucca Mountain, Nevada;Fabryka-Martin;Geol. Soc. Am. Abstr. Programs,1996

5. Conceptual model of the geometry and physics of water flow in a fractured basalt vadose zone;Faybishenko;Water Resour. Res.,2000

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