Permeability and pore-fluid chemistry of the Bullfrog Tuff in a temperature gradient: summary of results | Zendy

J. D. Byerlee | Zendy; C. A. Morrow | Zendy; D. E. Moore | Zendy

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Permeability and pore-fluid chemistry of the Bullfrog Tuff in a temperature gradient: summary of results

Author(s) -

J. D. Byerlee,

C. A. Morrow,

D. E. Moore

Publication year - 1983

Publication title -

osti oai (u.s. department of energy office of scientific and technical information)

Language(s) - English

Resource type - Reports

DOI - 10.2172/59866

Subject(s) - bullfrog , groundwater , permeability (electromagnetism) , radioactive waste , chemistry , temperature gradient , pore water pressure , yucca , geology , geotechnical engineering , ecology , nuclear chemistry , membrane , biochemistry , biology , physics , quantum mechanics

In order to study the changes that take place with time when groundwater comes in contact with heated rock, and to determine the ease with which potential radionuclide-bearing groundwater could be carried into the environment, the permeability and fluid chemistry of the Bullfrog Tuff from Yucca Mountain were studied under conditions simulating a nuclear waste repository environment. (ACR

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