1994
DOI: 10.2475/ajs.294.4.449
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A chemical and thermodynamic model of aluminous dioctahedral 2:1 layer clay minerals in diagenetic processes; regular solution representation of interlayer dehydration in smectite

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Cited by 62 publications
(87 citation statements)
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“…As the standard entropy of hydration is assumed constant in [66] and [68] models, the integral hydration enthalpies provided by these two previous models are nearly linear. Those obtained by [68] exhibit three sections of curves corresponding to the three states of hydration (1, 2 and 3 water layers).…”
Section: Zeolite Mineralsmentioning
confidence: 99%
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“…As the standard entropy of hydration is assumed constant in [66] and [68] models, the integral hydration enthalpies provided by these two previous models are nearly linear. Those obtained by [68] exhibit three sections of curves corresponding to the three states of hydration (1, 2 and 3 water layers).…”
Section: Zeolite Mineralsmentioning
confidence: 99%
“…As indicated in the enthalpy section, integral hydration entropies modelled by [66] (yellow dotted line, N°1) and [68] (green dotted line, N°2a, 2b and 2c corresponding to 1 st , 2 nd and 3 rd layer) are linear and merge together. In the model proposed by Vieillard et al [63], three calculated integral entropies of SWy1-Na -water system were plotted in Figure 5A and correspond to the adsorption (red line), the desorption (blue line) and the theoretical equilibrium water -Swy1-Na (black line, N° 3), whose equation is given: …”
Section: Zeolitesmentioning
confidence: 99%
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