Murri Mara, Prencipe Mauro
Department of Earth and Environmental Sciences, University of Milano-Bicocca, Piazza della Scienza 4, I-20126 Milano, Italy.
Earth Sciences Department, University of Torino, Via Valperga Caluso 35, I-10125 Torino, Italy.
Entropy (Basel). 2021 Oct 19;23(10):1366. doi: 10.3390/e23101366.
The simple chemistry and structure of quartz together with its abundance in nature and its piezoelectric properties make convenient its employment for several applications, from engineering to Earth sciences. For these purposes, the quartz equations of state, thermoelastic and thermodynamic properties have been studied since decades. Alpha quartz is stable up to 2.5 GPa at room temperature where it converts to coesite, and at ambient pressure up to 847 K where it transforms to the beta phase. In particular, the displacive phase transition at 847 K at ambient pressure is driven by intrinsic anharmonicity effects (soft-mode phase transition) and its precise mechanism is difficult to be investigated experimentally. Therefore, we studied these anharmonic effects by means of ab initio calculations in the framework of the statistical thermodynamics approach. We determined the principal thermodynamic quantities accounting for the intrinsic anharmonicity and compared them against experimental data. Our results up to 700 K show a very good agreement with experiments. The same procedures and algorithms illustrated here can also be applied to determine the thermodynamic properties of other crystalline phases possibly affected by intrinsic anharmonic effects, that could partially invalidate the standard quasi-harmonic approach.
石英简单的化学性质和结构,加上其在自然界中的丰富储量以及压电特性,使其在从工程到地球科学的多种应用中都能方便地使用。出于这些目的,石英的状态方程、热弹性和热力学性质已经被研究了数十年。α-石英在室温下直至2.5吉帕斯卡都是稳定的,在该压力下它会转变为柯石英,而在常压下直至847开尔文它会转变为β相。特别地,常压下847 K的位移型相变是由本征非谐效应(软模相变)驱动的,其精确机制很难通过实验进行研究。因此,我们在统计热力学方法的框架内通过从头算计算研究了这些非谐效应。我们确定了描述本征非谐性的主要热力学量,并将它们与实验数据进行了比较。我们高达700 K的结果与实验结果非常吻合。这里阐述的相同程序和算法也可用于确定可能受本征非谐效应影响的其他晶相的热力学性质,这些效应可能会部分使标准准谐近似失效。