首页> 外文期刊>The Journal of Chemical Thermodynamics >Thermodynamic properties of mixed-layer illite-smectite by calorimetric methods: Acquisition of the enthalpies of mixing of illite and smectite layers
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Thermodynamic properties of mixed-layer illite-smectite by calorimetric methods: Acquisition of the enthalpies of mixing of illite and smectite layers

机译:热量测定方法混合层硅藻土 - 蒙脱石的热力学性质:采集伊利石和蒙脱层混合的焓

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The stability of illite-smectite interstratified with respect to discrete illite and smectite minerals was investigated by measuring their thermodynamic properties. The standard thermodynamic properties of the illite-smectite ISCz-1 mineral (G, H, S, C-p, and V) were determined between 298.15 K and 375 K by using calorimetric methods. Moreover, the enthalpies of mixing between the illite and smectite layers were measured at 298.15 K by acid solution calorimetry from a complete series of illite-smectite interstratified minerals (Shinzan area, Japan). The measured values were slightly negative, with a minimum value of -3.7 kJ.mol(-1). This contributed to the stability of the mixed-layer with respect to a mechanical mixture of illite and smectite. In addition, the model from Blanc et al. (2015) was implemented to estimate the thermodynamic properties of the interstratified illite-smectite ISCz-1 mineral. The predicted values were consistent with the experimental results. However, the estimates were slightly improved by considering the thermodynamic properties of the mixture of the illite and smectite components and then adding the terms of energies of mixing. This could be confirmed by establishing the stability domains of ISCz-1 and those of the corresponding illite and smectite end-members according to Meunier and Velde's determination of the smectite to illite reaction pathways (Meunier and Velde, 1989). (C) 2019 Elsevier Ltd.
机译:通过测量其热力学性质,研究了相对于离散伊利铁矿和蒙脱石矿物学的透射硅酸盐的稳定性。通过使用量热方法测定298.15k和375 k之间的illite-蒙脱石ISCZ-1矿物质(G,H,S,C-P和V)的标准热力学性质。此外,在298.15K通过酸溶液热量从一系列硅灰石 - 蒙霉菌矿化矿物(日本Shinzan地区)的酸溶液热量测量,在298.15k之间测量混合的焓。测量值略有阴性,最小值为-3.7kJ.mol(-1)。这有助于混合层的稳定性相对于伊利钠和蒙脱石的机械混合物。此外,来自Blanc等人的模型。 (2015)实施以估算漂白硅灰石 - 蒙脱石ISCZ-1矿物质的热力学性质。预测值与实验结果一致。然而,通过考虑伊尔石和蒙脱石组分的混合物的热力学性能,然后加入混合的能量术语,估计略有改善。这可以通过建立ISCZ-1的稳定性域以及根据Meunier和Velde确定蒙脱石对Imlite反应途径的测定(Meunier和Velde,1989)来证实这一点来证实。 (c)2019年elestvier有限公司

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