Thermodynamic properties of anhydrous smectite MX-80, illite IMt-2 and mixed-layer illite-smectite ISCz-1 as determined by calorimetric methods. Part I: Heat capacities, heat contents and entropies

被引:48
作者
Gailhanou, H.
van Miltenburg, J. C.
Rogez, J.
Olives, J.
Amouric, M.
Gaucher, E. C.
Blanc, P.
机构
[1] CNRS, CRMCN, F-13288 Marseille, France
[2] Bur Rech Geol & Minieres, F-45060 Orleans, France
[3] Univ Utrecht, Chem Thermodynam Grp, NL-3508 TB Utrecht, Netherlands
[4] Fac Sci & Tech St Jerome, CNRS, TECSEN, F-13397 Marseille, France
[5] ANDRA, F-92298 Chatenay Malabry, France
关键词
D O I
10.1016/j.gca.2007.09.020
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
The heat capacities of the anhydrous international reference clay minerals, smectite MX-80, illite IMt-2 and mixed-layer illite-smectite ISCz-1, were measured by low temperature adiabatic calorimetry and differential scanning calorimetry, from 6 to 520 K (at I bar). The samples were chemically purified and Na-saturated. Dehydrated clay fractions < 2 mu m were studied. The structural formulae of the corresponding clay minerals, obtained after subtracting the remaining impurities, are K0.026Na0.435Ca0.010(Si3.612Al0.388) (Al1.593Fe0.1843+ Mg-0.228 Fe0.0382+Ti0.011)O-10(OH)(2) for smectite MX-80, K0.762Na0.044(Si3.387Al0.613) (Al-1.427 Fe-0.292(3+) Mg-0.241 Fe2+ (0.084))O-10(OH)(2) for illite IMt-2 and K0.530Na0.135(Si3.565Al0.435)(Al-1.709 Fe0.0513+Mg0.218Fe0.0172+Ti0.005)O-10(OH)(2) for mixed-layer ISCz-1. From the heat capacity values, we determined the molar entropies, standard entropies of formation and heat contents of these minerals. The following values were obtained at 298.15 K and 1 bar [GRAPHICS] (c) 2007 Elsevier Ltd. All rights reserved.
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页码:5463 / 5473
页数:11
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