scholarly journals Appraisal of nuclear waste isolation in the vadose zone in arid and semiarid regions (with emphasis on the Nevada Test Site)

10.2172/60301 ◽  
1983 ◽  
Author(s):  
H.A. Wollenberg ◽  
J.S.Y. Wang ◽  
G. Korbin
Keyword(s):  
Nuclear Waste ◽  
Vadose Zone ◽  
Test Site ◽  
Nevada Test Site ◽  
Semiarid Regions ◽  
Arid And Semiarid

scholarly journals Tracing long-term vadose zone processes at the Nevada Test Site, USA

2005 ◽  
Vol 19 (17) ◽  
pp. 3383-3394 ◽  
Author(s):  
James R. Hunt ◽  
Andrew F. B. Tompson
Keyword(s):  
Vadose Zone ◽  
Test Site ◽  
Nevada Test Site

Permeability and Pore-Fluid Chemistry of the Topopah Spring Member of the Paintbrush Tuff, Nevada Test Site, in a Temperature Gradient – Application to Nuclear Waste Storage

1983 ◽  
Vol 26 ◽  
Author(s):  
C. A. Morrow ◽  
D. E. Moore ◽  
J. D. Byerlee
Keyword(s):  
Temperature Gradient ◽  
Nuclear Waste ◽  
Test Site ◽  
Pore Fluid ◽  
Nuclear Waste Repository ◽  
Nevada Test Site ◽  
Nuclear Waste Storage ◽  
Fluid Chemistry ◽  
Waste Storage ◽  
Pore Fluid Chemistry

ABSTRACTThe Topopah Spring Member of the Paintbrush Tuff from the Nevada Test Site is being investigated by the Nevada Nuclear Waste Storage Investigations project (NNWSI) as a possible nuclear waste repository host rock. Changes with time of the permeability and fluid chemistry of the Topopah Spring Member have been measured in samples subjected to a temperature gradient. Maximum temperatures of the imposed gradients ranged from 90° to 250°C; minimum temperatures were 36° to 83°C. Confining and pore pressures simulated a depth of about 1.2 km, which is greater than the proposed repository depth, but chosen for comparison with previous studies at these pressures. Pore fluid used in the experiments was groundwater from the Nevada Test Site; the direction of pore-fluid flow was from the high- to the low-temperature side of the tuffs.Initial permeabilities of the tuff samples ranged from 3 to 65 μdarcys, the wide range in values resulting from differences in the void and fracture geometries of the samples. Heating the tuffs produced no change in permeability in tne lowest temperature experiment and only small changes at higher temperatures. The fluids discharged from the tuffs were dilute waters of nearneutral pH that differed only slightly from the original groundwater composition.Since proposed burial in the Topopah Spring Member would be in the unsaturated zone, the high initial permeabilities and the absence of permeability change with heating may be desirable, because downward-percolating waters would be able to drain into deeper formations and not collect at the repository level. in addition, any fluids that may come in contact with waste canisters wlll not have acquired any potentially corrosive characteristics through interaction with the tuff.

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