In‐Situ Evaluations of Linear and Nonlinear Shear Moduli of Cemented Alluvium at Yucca Mountain

2011 ◽  
Author(s):  
Kwangsoo Park ◽  
Kenneth Stokoe ◽  
Wonseok Seo ◽  
Michael Schuhen
Author(s):  
A. K. Keene ◽  
H. Jaffal ◽  
K. H. Stokoe ◽  
C. S. El Mohtar ◽  
A. Reyes ◽  
...  

2016 ◽  
Vol 49 (4) ◽  
pp. 1444-1453 ◽  
Author(s):  
Zhi-Chao Yan ◽  
Salvatore Costanzo ◽  
Youncheol Jeong ◽  
Taihyun Chang ◽  
Dimitris Vlassopoulos

1995 ◽  
Vol 412 ◽  
Author(s):  
John J. Nitao ◽  
Thomas A. Buscheck

AbstractAn in situ heater test was performed at G-Tunnel, Nevada Nuclear Test Site, to investigate the thermal-hydrological response of unsaturated, fractured volcanic tuff under conditions similar to those at Yucca Mountain. The NUFT flow and transport code was used to model the test using discrete-fracture and equivalent-continuum approaches. Nonequilibrium fracture flow and thermal buoyant gas-phase convection were found to be the likely causes for observed lack of condensate imbibition into the matrix. The potential repository at Yucca Mountain was also modeled. Disequilibrium fracture flow is predicted to occur for less than a hundred years after emplacement followed by a period of fracture-matrix equilibrium, during which the equivalent-continuum and discrete-fracture models give almost identical results.


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