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Evolution of the unsaturated zone testing at Yucca Mountain
1Earth Sciences Division, Lawrence Berkeley National Laboratory, MS 90-1116, One Cyclotron Road, CA 94720, USA. jswang@lbl.gov
Journal of Contaminant Hydrology
|April 26, 2003
Summary
Site characterization at Yucca Mountain has progressed from surface studies to underground drift testing, focusing on the unsaturated zone (UZ). Key findings inform future quantification of water flow and contaminant transport processes.
Area of Science:
- Geology
- Hydrogeology
- Environmental Science
Background:
- Yucca Mountain site evaluation has transitioned from surface investigations to underground drift testing.
- Characterization efforts address key issues within the unsaturated zone (UZ).
Purpose of the Study:
- To summarize the evolution of site characterization activities and prominent issues concerning the unsaturated zone (UZ) at Yucca Mountain.
- To highlight lessons learned from underground testing for future process quantification.
Main Methods:
- Evolved data collection from mapping faults and fractures to estimating percolation and quantifying seepage.
- Conducted fracture-matrix interaction, matrix diffusion, and thermal tests at various scales.
- Evaluated tuff interfaces and local faults in different geological units.
Main Results:
- Demonstrated evolution in data collection from qualitative mapping to quantitative seepage measurements.
- Quantified fracture-matrix interaction and matrix diffusion effects.
- Measured water mobilization and moisture redistribution during thermal tests.
Conclusions:
- Underground testing has refined understanding of hydrological processes in the unsaturated zone.
- Further quantification is needed for migration through the drift shadow zone and liquid flow through faults.