Silicon Self-Diffusion in Stishovite: Calculations of Point Defect Parameters Based on the cBΩ Thermodynamic Model

V. Saltas, F. Vallianatos
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引用次数: 2

Abstract

In the present work we apply the so-called cBΩ thermodynamic model to study the diffusion of Si in stishovite crystal at high pressure and over a wide temperature range. According to this model [1,2], the point defect activation Gibbs free energy is expressed as a function of the bulk properties of the material, i.e. gact=cBΩ, where B is the isothermal bulk modulus, Ω is the mean atomic volume and c is a dimensionless constant. In this way, other important point defect parameters, such as the activation volume Vact, the activation entropy Sact and the activation enthalpy hact may be estimated, if the thermoelastic properties of the material are known over a wide temperature and pressure range. Our calculations are based on previously reported self-diffusion coefficients in stishovite single crystals measured at 14 GPa and at temperatures from 1400 to 1800 oC, in the [110] and [001] directions, by Shatskiy et al. [3]. Furthermore, the EoS of stishovite, proposed by Wang et al. [4] has been used for the accurate implementation of the cBΩ model. Our results suggest that the aforementioned point defect parameters exhibit considerable temperature dependence over the studied temperature range (1000-2000 oC). The estimated activation volumes (4.8-5.8 cm3/mol, in the range 1400-1800 oC) are in agreement with the experimental results reported by Xu et al. [5]. Our study confirms the potential of the cBΩ model for the theoretical investigation of diffusion processes in minerals, in order to overcome the experimental difficulties and the lack of experimental data in mantle conditions. REFERENCES Varotsos P. and Alexopoulos K. Thermodynamics of Point Defects and their Relation with the Bulk Properties, North-Holland, Amsterdam, 1986. Vallianatos, F., Saltas, V. Application of the cBΩ model to the calculation of diffusion parameters of He in olivine, Chem. Miner. 2014, 41, 181-188, Doi: 10.1007/s00269-013-0636-y. Shatskiy, A., Yamazaki, D., Borzdov, Y.M., Matsuzaki, T., Litasov, K.D., Cooray, T., Ferot, A., Ito, E., Katsura, T. Stishovite single-crystal growth and application to silicon self-diffusion measurements, Mineral. 2010, 95, 135–43, Doi: 10.2138/am.2010.3255. Wang, F., Tange, Y., Irifune, T., and Funakoshi, K. P‐V‐T equation of state of stishovite up to mid‐lower mantle conditions, Geophys. Res. 2012, 117, B06209, doi:10.1029/2011JB009100. Xu, F., Yamazaki, D., Sakamoto, N., Sun, W., Fei, H., Yurimoto, H. Silicon and oxygen self-diffusion in stishovite: Implications for stability of SiO2-rich seismic reflectors in the mid-mantle, Earth Planet. Sci. Lett. 2017, 459, 332–9, Doi: 10.1016/j.epsl.2016.11.044.
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硅在锑云母中的自扩散:基于cBΩ热力学模型的点缺陷参数计算
在本工作中,我们应用cBΩ热力学模型来研究Si在高压力和宽温度范围内在辉石晶体中的扩散。根据该模型[1,2],点缺陷激活吉布斯自由能表示为材料体积性质的函数,即gact=cBΩ,其中B为等温体积模量,Ω为平均原子体积,c为无因次常数。通过这种方法,如果材料的热弹性性质在一个较宽的温度和压力范围内已知,则可以估计其他重要的点缺陷参数,如活化体积Vact、活化熵Sact和活化焓hact。我们的计算是基于Shatskiy等人先前报道的在14gpa和1400 ~ 1800℃温度下,在[110]和[001]方向上测量的辉石单晶的自扩散系数。此外,Wang et al.[4]提出的stishovite的EoS已被用于cBΩ模型的精确实现。我们的研究结果表明,上述点缺陷参数在研究的温度范围内(1000-2000℃)表现出相当大的温度依赖性。估计的活化体积(4.8-5.8 cm3/mol,在1400-1800℃范围内)与Xu等人报道的实验结果一致。我们的研究证实了cBΩ模型在理论研究矿物扩散过程方面的潜力,从而克服了地幔条件下实验困难和缺乏实验数据的问题。参考文献Varotsos P.和Alexopoulos K.点缺陷的热力学及其与体性质的关系,北荷兰,阿姆斯特丹,1986。Vallianatos, F., Saltas, V. cBΩ模型在橄榄石中He扩散参数计算中的应用,化学。矿业学报,2014,41,181-188,Doi: 10.1007/s00269-013-0636-y。shattskiy, A, Yamazaki, D, Borzdov, Y.M, Matsuzaki, T, Litasov, K.D, Cooray, T., Ferot, A, Ito, E., Katsura ., T.硅单晶生长及其在硅自扩散测量中的应用,矿物学报,2010,95,135-43,Doi: 10.2138/am.2010.3255。王峰,唐勇,王志强,王志强,王志强,王志强,王志强。中-下地幔条件下辉石岩的P - V - T状态方程,地球物理学报。Res. 2012, 117, B06209, doi:10.1029/2011JB009100。许峰,Yamazaki, D, Sakamoto, N., Sun, W., Fei, H., Yurimoto, H.硅和氧在辉长石中的自扩散:地球中地幔富sio2地震反射体稳定性的意义。科学。通讯学报,2017,459,332-9,Doi: 10.1016/ j.p epsl.2016.11.044。
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