首页> 外文期刊>Geochimica et Cosmochimica Acta: Journal of the Geochemical Society and the Meteoritical Society >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
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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

机译:通过量热法测定无水蒙脱石MX-80,伊利石IMt-2和混合层伊利石-蒙脱石ISCz-1的热力学性质。第一部分:热容量,热含量和熵

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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.
机译:通过低温绝热量热法和差示扫描量热法测量了国际上无水国际参考粘土矿物,蒙脱石MX-80,伊利石IMt-2和伊利石-蒙脱石混合层ISCz-1的热容量,其热容量为6至520 K(at我吧)。将样品化学纯化并用Na饱和。研究了小于2微米的脱水粘土级分。减去剩余杂质后获得的相应粘土矿物的结构式为K0.026Na0.435Ca0.010(Si3.612Al0.388)(Al1.593Fe0.1843 + Mg-0.228 Fe0.0382 + Ti0.011)O蒙脱石MX-80,-10(OH)(2),K0.762Na0.044(Si3.387Al0.613)(Al-1.427 Fe-0.292(3+)Mg-0.241 Fe2 +(0.084))O-10(OH )(2)用于伊利石IMt-2和K0.530Na0.135(Si3.565Al0.435)(Al-1.709 Fe0.0513 + Mg0.218Fe0.0172 + Ti0.005)O-10(OH)(2)混合层ISCz-1。从热容值,我们确定了这些矿物的摩尔熵,地层标准熵和热含量。在298.15 K和1 bar下获得以下值。[GRAPHICS](c)2007 ElsevierLtd。保留所有权利。

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