Testing and parameterizing a conceptual model for solute transport in a fractured granite using multiple tracers in a forced-gradient test

Author:

Reimus Paul1,Pohll Greg2,Mihevc Todd2,Chapman Jenny3,Haga Marc1,Lyles Brad2,Kosinski Sean2,Niswonger Rich2,Sanders Peter4

Affiliation:

1. Los Alamos National Laboratory; Los Alamos New Mexico USA

2. Desert Research Institute; Reno Nevada USA

3. Desert Research Institute; Las Vegas Nevada USA

4. Department of Energy; Nevada Operations Office; Las Vegas Nevada USA

Publisher

American Geophysical Union (AGU)

Subject

Water Science and Technology

Reference37 articles.

1. Lithium sorption to Yucca Mountain tuffs;Anghel;Appl. Geochem.,2002

2. Becker , M. W. Tracer tests in a fractured rock and their first passage time mathematical models Univ. of Tex. Austin 1996

3. First-passage-time transfer functions for groundwater tracer tests conducted in radially convergent flow;Becker;J. Contam. Hydrol.,2000

4. Tracer transport in fractured crystalline rock: Evidence of non-diffusive breakthrough tailing;Becker;Water Resour. Res.,2000

5. Tri- and tetrafluorobenzoates as nonreactive tracers in soil and groundwater;Benson;Soil Sci. Soc. Am. J.,1994

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