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Evaporative Evolution of Carbonate-Rich Brines from Synthetic Topopah Spring Tuff Pore Water, YuccaMountain, NV

Published online by Cambridge University Press:  17 March 2011

Mark Sutton
Affiliation:
Chemistry & Material Science,Lawrence Livermore National Laboratory, 7000 East Avenue, Livermore, CA 94550
Maureen Alai
Affiliation:
Energy & Environmental Science,Lawrence Livermore National Laboratory, 7000 East Avenue, Livermore, CA 94550
Susan Carroll
Affiliation:
Energy & Environmental Science,Lawrence Livermore National Laboratory, 7000 East Avenue, Livermore, CA 94550
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Abstract

The evaporation of a range of synthetic pore water solutions representative of the potential high-level-nuclear-waste repository at Yucca Mountain, NV is being investigated. The motivation of this work is to understand and predict the range of brine compositions that may contact the wastecontainers from evaporation of pore waters, because these brines could form corrosive thin films on the containers and impact their long-term integrity. A relatively complex synthetic Topopah Spring Tuff pore water was progressively concentrated by evaporation in a closed vessel, heated to 95°C in a series of sequential experiments. Periodic samples of the evaporating solution were taken to determine the evolving water chemistry. According to chemical divide theory at 25°C and 95°C our starting solution should evolve towards a high pH carbonate brine. Results at 95°C show that this solution evolves towardsa complex brinethat contains about 99 mol% Na+for the cations, and 71 mol% Cl-, 18 mol% ΣCO2(aq), 9 mol% SO42- for the anions. Initial modeling ofthe evaporating solution indicates precipitation of aragonite, halite, silica, sulfate and fluoride phases. The experiments have been used to benchmark the use of the EQ3/6 geochemical code in predicting the evolution of carbonate-rich brines during evaporation.

Type
Research Article
Copyright
Copyright © Materials Research Society 2004

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References

1. Eugster, H. P and Hardie, L. A. (1978) In: A, Lerman. (Ed.), Lakes: Chemistry, Geology, Physics. Springer-Verlag, New York.Google Scholar
2. Wolery, T. J & Jarek, R. L. (2003) EQ3/6, A Software Package for Geochemical Modeling of Aqueous Systems, v8.0Google Scholar
3. Moller, N. (1988) Geochmicia et Cosmichimica Acta, 52, 821837.Google Scholar
4. Rard, J.A and Wijesinghe, A.M. (2003) Journal of Chemical Thermodynamics, 35, 439473.Google Scholar
5. Pitzer, K.S. (1991) Activity Coefficients in Electrolyte Solutions, 2nd edition, Chapter 3, p.75-153, CRC Press, Boca Raton, Florida.Google Scholar
6. He, S and Morse, J.W. (1993) Geochimica et Cosmichimica Acta 57, 35333554 Google Scholar