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Scaling of thermodynamic mixing properties in garnet solid solutions

机译:石榴石固溶体中热力学混合性质的缩放

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The volumes and enthalpies of mixing, ΔV~(Mix) and ΔH~(Mix), of binary solid-solution aluminosilicate garnets have been studied by computer simulation. The use of "average atoms" to simulate solid solution was found to give results that are considerably different from those obtained by calculating and averaging over many configurations of cations at a given composition. Although we expect mineral properties calculated from model calculations to be correct only on a qualitative rather than a quantitative scale, fair agreement with experiment was obtained where carefully tested potential parameters were used. The results show that mixing behaviour in these materials controlled by local strain and relaxation effects resulting from the atomic size mismatch of the mixing divalent cations. In particular, ΔV~(Mix) and ΔH~(Mix) are shown to scale quadratically with the volume difference between the end members, and to vary essentially symmetrically with composition, with a moderate dependence on the degree and nature of cation order. We conclude that computer modelling should be useful in providing detailed qualitative information about the mixing properties of solid solutions, which can help to better constrain and interpret experimental results.
机译:通过计算机模拟研究了二元固溶硅铝酸盐石榴石的混合体积和焓ΔV〜(Mix)和ΔH〜(Mix)。发现使用“平均原子”来模拟固溶体所得到的结果与在给定的组成下对许多构型的阳离子进行计算和平均所得的结果大不相同。尽管我们期望从模型计算中得出的矿物性质仅在定性而非定量范围内是正确的,但在使用经过仔细测试的潜在参数的情况下,与实验取得了合理的协议。结果表明,这些材料的混合行为受混合二价阳离子的原子尺寸失配引起的局部应变和弛豫效应控制。特别地,ΔV_(Mix)和ΔH_(Mix)显示为随着端部构件之间的体积差成二次比例变化,并且基本上随组成对称地变化,并且对阳离子顺序的程度和性质具有中等依赖性。我们得出的结论是,计算机建模应该有助于提供有关固溶体混合特性的详细定性信息,这有助于更好地约束和解释实验结果。

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