Prediction of mineral scale formation in geothermal and oilfield operations using the extended UNIQUAC model Part I.: Sulfate scaling minerals

被引:52
作者
García, AV [1 ]
Thomsen, K [1 ]
Stenby, EH [1 ]
机构
[1] Tech Univ Denmark, Dept Chem Engn, IVC SEP, DK-2800 Lyngby, Denmark
关键词
extended UNIQUAC; vapor-liquid-solid equilibria; scale formation; geothermal; barite; celestite; anhydrite; gypsum;
D O I
10.1016/j.geothermics.2004.11.002
中图分类号
TE [石油、天然气工业]; TK [能源与动力工程];
学科分类号
0807 ; 0820 ;
摘要
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, CaSO(4)(.)2H(2)O, BaSO4 and SrSO4) at temperatures up to 300degreesC 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 300degreesC, and the pressure range from 1 to 1000 bar. (C) 2004 CNR. Published by Elsevier Ltd. All rights reserved.
引用
收藏
页码:61 / 97
页数:37
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