Reaction paths and equilibrium end-points in solid-solution systems; discussion and reply

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doi: 10.1016/0016-7037(92)90209-2
Authors:Stoessell, Ronald K.; Glynn, Pierre D.; Reardon, Eric J.; Plummer, L. Niel; Busenberg, Eurybiades
Author Affiliations:Primary:
Univ. New Orleans, Dep. Geol. and Geophys., New Orleans, LA, United States
U. S. Geol. Surv., United States
Univ. Waterloo, Canada
Volume Title:Geochimica et Cosmochimica Acta
Source:Geochimica et Cosmochimica Acta, 56(6), p.2555-2572. Publisher: Pergamon, Oxford, International. ISSN: 0016-7037
Publication Date:1992
Note:In English. For reference to original see Glynn, P. D., Reardon, E. J., Plummer, L. N. and Busenberg, E., Geochim. Cosmochim. Acta, Vol. 54, p. 267-279, 1990. 57 refs.; illus.
Summary:The author answers questions raised by Glynn et al. about the general use of stoichiometric saturation as a control on SSAS (solid-solution aqueous-solution) reactions during precipitation, about the limiting activity coefficients of NaBr in halite, and on the limitation of a Lippmann phase diagram in determining if a solution composition follows stoichiometric saturation for a trace component in a binary solid solution. [R.K.H.]
Subjects:Aqueous solutions; Brines; Chlorides; Geochemistry; Halides; Halite; Partitioning; Phase equilibria; Precipitation; Processes; Saturation; Solid phase; Solid solution; Stoichiometry; Sylvite; Europe; United Kingdom; Western Europe; Reactions
Abstract Numbers:93M/571
Record ID:1992054781
Copyright Information:GeoRef, Copyright 2019 American Geosciences Institute. Reference includes data from Mineralogical Abstracts, United Kingdom, Twickenham, United Kingdom
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