Study of rock-water-nuclear waste interactions in the Pasco Basin, Washington [electronic resource] : Part II. Preliminary equilibrium-step simulations of basalt diagenesis.

Interactions between a large number of complex chemical and physical processes have resulted in significant changes in the Pasco Basin hydrochemical system since emplacement of the first basalt flow. In order to perform preliminary simulations of the chemical evolution of this system, certain simpli...

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Bibliographic Details
Online Access: Online Access
Corporate Authors: Lawrence Berkeley Laboratory (Researcher), Lawrence Berkeley National Laboratory (Researcher)
Format: Government Document Electronic eBook
Language:English
Published: Berkeley, Calif. : Oak Ridge, Tenn. : Lawrence Berkeley National Laboratory ; distributed by the Office of Scientific and Technical Information, U.S. Dept. of Energy, 1980.
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MARC

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245 0 0 |a Study of rock-water-nuclear waste interactions in the Pasco Basin, Washington  |h [electronic resource] :  |b Part II. Preliminary equilibrium-step simulations of basalt diagenesis. 
260 |a Berkeley, Calif. :  |b Lawrence Berkeley National Laboratory ;  |a Oak Ridge, Tenn. :  |b distributed by the Office of Scientific and Technical Information, U.S. Dept. of Energy,  |c 1980. 
300 |a Pages: 31 :  |b digital, PDF file. 
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500 |a 08/01/1980. 
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500 |a Carnahan, C.L.; Benson, L.V.; Che, M. 
520 3 |a Interactions between a large number of complex chemical and physical processes have resulted in significant changes in the Pasco Basin hydrochemical system since emplacement of the first basalt flow. In order to perform preliminary simulations of the chemical evolution of this system, certain simplifying assumptions and procedures were adopted and a computer model which operates on the principal of local equilibrium was used for the mass transfer calculations. Significant uncertainties exist in both the thermodynamic and reaction rate data which were input to the computer model. In addition, the compositional characteristics of the evolving hydrochemical system remain largely unknown, especially as a function of distance along the flow path. Given these uncertainties, it remains difficult to assess the applicability of the equilibrium-step approach even though reasonable matches between observed and simulated hydrochemical data were obtained. Given the uncertainties mentioned, the predictive abilities of EQ6 are difficult, if not impossible to evaluate; our simulations produced, at best, only qualitative agreement with observed product mineral assemblages and sequences, and fluid compositions. 
536 |b W-7405-ENG-48. 
650 7 |a Mass Transfer.  |2 local. 
650 7 |a Volcanic Rocks.  |2 local. 
650 7 |a Chemical Composition.  |2 local. 
650 7 |a Mathematical Models.  |2 local. 
650 7 |a Rocks.  |2 local. 
650 7 |a Fluid Flow.  |2 local. 
650 7 |a Simulation.  |2 local. 
650 7 |a Ground Water.  |2 local. 
650 7 |a Radioactive Waste Disposal.  |2 local. 
650 7 |a Basalt.  |2 local. 
650 7 |a Water.  |2 local. 
650 7 |a Waste Disposal.  |2 local. 
650 7 |a Oxygen Compounds.  |2 local. 
650 7 |a Pacific Northwest Region.  |2 local. 
650 7 |a Minerals.  |2 local. 
650 7 |a Washington.  |2 local. 
650 7 |a Diagenesis.  |2 local. 
650 7 |a Igneous Rocks.  |2 local. 
650 7 |a Underground Disposal.  |2 local. 
650 7 |a Management.  |2 local. 
650 7 |a Water Chemistry.  |2 local. 
650 7 |a Waste Management.  |2 local. 
650 7 |a Usa.  |2 local. 
650 7 |a Dissolution.  |2 local. 
650 7 |a North America.  |2 local. 
650 7 |a Hydrogen Compounds.  |2 local. 
650 7 |a Rock-fluid Interactions.  |2 local. 
650 7 |a Geosciences.  |2 edbsc. 
710 2 |a Lawrence Berkeley Laboratory.  |4 res. 
710 2 |a Lawrence Berkeley National Laboratory.  |4 res. 
710 1 |a United States.  |b Department of Energy.  |b Office of Scientific and Technical Information.  |4 dst. 
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