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Mechanisms for the Formation of a Perched Water Zone in Fractured Tuff: a Natural Analogue Study

Published online by Cambridge University Press:  03 September 2012

E. G. Woodhouse
Affiliation:
Department of Hydrology and Water Resources, P.O. Box 210011, University of Arizona, Tucson, AZ 85721–0011, betsy@hwr.arizona.edu
R. L. Bassett
Affiliation:
Department of Hydrology and Water Resources, P.O. Box 210011, University of Arizona, Tucson, AZ 85721–0011, betsy@hwr.arizona.edu
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Abstract

Perched water zones have been identified in the fractured, welded tuff in the semi-arid to arid environments of Yucca Mountain, Nevada and near Superior, Arizona. An understanding of the formation of such zones is necessary in order to predict where future perched water might form at Yucca Mountain, the proposed site of a high-level nuclear waste repository. The formation or growth of a perched zone near a repository is one of the factors to be considered in the risk assessment of the Yucca Mountain site.

The Apache Leap Research Site near Superior, Arizona is a natural analog to the Yucca Mountain site in terms of geology, hydrology, and climate. Information used to study possible mechanisms for the formation of the perched zone included data regarding isotopie and geochemical properties of the waters in and above the perched water zone; measured hydrologie parameters of the perched zone; geophysical and measured parameters of the tuff; megascopic and microscopic observations of the tuff, including mineralogical, alteration, and structural features; and the lateral and vertical extent of perched water in the region.

Aquifer test, geophysical, geochemical, and radioisotopic data show that fractures are the means by which water is recharging the perched zone. The reduced hydraulic conductivity of the formation in the perched zone appears to result from both a severe reduction in matrix porosity and permeability caused by welding, devitrification, and vapor phase crystallization; and by an increase in fracture filling which restricts the pathways for flow.

Type
Research Article
Copyright
Copyright © Materials Research Society 1997

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References

REFERENCES

1. Wu, Y. S., Chen, G., and Bodvarsson, G. S., Perched water analysis, in Bodvarsson, G. S. and Bandurraga, T. M., eds., Development and Calibration of the Three-Dimensional Site-Scale Unsaturated Zone Model of Yucca Mountain Nevada, ch.7, Lawrence Berkeley Laboratory, Berkeley, CA, 1996.Google Scholar
2. Bassett, R. L., Neuman, S. P., Rasmussen, T. C., Guzman, A., Davidson, G. R., and Lohrstorfer, C. F., Validation Studies for Assessing Unsaturated Flow and Transport Through Fractured Rock, NUREG/CR-6203, U. S. Nuclear Regulatory Commission, Washington, DC, 1994.10.2172/145606Google Scholar
3. Peterson, D. W., Dacitic ash-flow sheet near Superior and Globe. Arizona, Ph.D. thesis, Stanford University; U.S. Geological Survey Open-File Report 130, 1961.10.3133/ofr61119Google Scholar
4. Hardin, E. L., Ph.D. dissertation, University of Arizona, Tucson, 1996.Google Scholar
5. Davidson, G. R., Bassett, R. L., Hardin, E. L., and Thompson, D. L., Geochemical evidence of preferential flow of water through fractures in unsaturated tuff, Apache Leap, Arizona, Applied Geochemistry, accepted for publication.Google Scholar
6. Sample Management Facility, Geologic summary of borehole USW UZP-4 phase le prototype drilling, Apache Leap, Arizona, prepared for U.S. Department of Energy Yucca Mountain Project, 1990.Google Scholar
7. Hardin, E. L., Bassett, R. L. and Murrell, M. T., 234U/238U fractionation in vadose zone pore waters of the Apache Leap Tuff, Waste Management '96: Proceedings on Waste Management. Tucson, AZ, 1996, CD-ROM.Google Scholar
8. Woodhouse, E. G., Ph.D. dissertation, University of Arizona, Tucson, in preparation.Google Scholar
9. Gringarten, A. C. and Ramey, H. J. Jr., The use of source and Green's functions in solving unsteady-flow problems in reservoirs, Soc. Pet. Eng. J., 1973, pp. 285296.10.2118/3818-PAGoogle Scholar