Miscibility in the CaSO4-2H2O-CaSeO4-2H2Osystem:: Implications for the crystallisation and dehydration behaviour

被引:31
作者
Fernández-González, A
Andara, A
Alía, JM
Prieto, M
机构
[1] Univ Oviedo, Dept Geol, Oviedo 33005, Spain
[2] Univ Los Andes, Escuela Ingn Geol, Merida 5101A, Venezuela
[3] Univ Castilla La Mancha, Dept Quim Fis, E-13071 Ciudad Real, Spain
关键词
solid solution; gypsum; calcium selenate;
D O I
10.1016/j.chemgeo.2005.08.019
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
SeO42- ions solid ions can substitute for sulphate in the gypsum structure. In this work crystals of different Ca(SO4, SeO4). 2H(2)O solid solutions were precipitated by mixing a CaCl2 solution with solutions containing different ratios of Na2SO4 and Na2SeO4. The compositions of the precipitates were analysed by EDS and the cell parameters were determined by X-ray powder diffraction. Moreover, a comparative study on dehydration behaviour of selenate rich and sulfate rich Ca(SO4,SeO4) (.) 2H(2)O solid solutions was carried out by thermogravimetry. The experimental results show that the Ca(SO4,SeO4) - 2H(2)O solid solution presents a symmetric miscibility gap for compositions ranging from X-CaSO4 - (2H2O) = 0.23 to X-CaSO4 (- 2H2O) = 0.77. By considering a regular solution model a Guggenheim parameter a(0)=2.238 was calculated. The solid phase activity coefficients obtained with this parameter were used to calculate a Lippmann diagram for the system Ca(SO4,SeO4) (.) 2H(2)O -H2O (c) 2005 Elsevier B.V. All rights reserved.
引用
收藏
页码:256 / 265
页数:10
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