Title of article
Prediction of mineral scale formation in geothermal and oilfield operations using the extended UNIQUAC model: Part I. Sulfate scaling minerals
Author/Authors
Ada Villaf?fila Garc?a، نويسنده , , Kaj Thomsen، نويسنده , , Erling H. Stenby، نويسنده ,
Issue Information
روزنامه با شماره پیاپی سال 2005
Pages
37
From page
61
To page
97
Abstract
Pressure parameters are added to the Extended UNIQUAC model presented by Thomsen and Rasmussen
(Modeling of vapor–liquid–solid equilibrium in gas–aqueous electrolyte systems. Chemical
Engineering Science 54, 1787–1802, 1999). The improved model has been used for correlation and
prediction of solid–liquid equilibrium (SLE) of scaling minerals (CaSO4, CaSO4·2H2O, BaSO4 and
SrSO4) at temperatures up to 300 ◦C and pressures up to 1000 bar. The results show that the Extended
UNIQUAC model, with the proposed pressure parameters, is able to represent binary, ternary and
quaternary solubility data within the experimental accuracy in the temperature range from −20 to
300 ◦C, and the pressure range from 1 to 1000 bar.
© 2004 CNR. Published by Elsevier Ltd. All rights reserved
Keywords
gypsum , Extended UNIQUAC , Vapor–liquid–solid equilibria , Scale formation , Geothermal , celestite , Barite , Anhydrite
Journal title
Geothermics
Serial Year
2005
Journal title
Geothermics
Record number
430939
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