The outline of my thesis is the following: In Chapter 1, I present more details related to the motivation for studying silica. In Chapter 2, I mainly discuss the force matching method which has been used to construct the force field, and some methology. In Chapter 3, I show how the performance of the potential and how it can be used to calculate infrared and Raman spectra, focusing on the the calcuation of the spectra for high-temperature phase. Based on the calculated specta and the structural analysis, more profound understanding of the silica high-temperature phase is given. I will show in Chapters 4 and 5, pressure–induced changes in oxygen packing in quartz and cristobalite can be understood based on well-known transition paths for close-packing lattices. I will present in Chapter 6, a microscopic picture of the compression mechanisms of silica glass. In order to advance the understanding of pressure-induced amorphization, in Chapter 7 I also studied one example of the silica clathrate (type I) under pressure. I will then summarise the main results of my work in Chapter 8.
Modelling structure, phase transition, and vibrational spectroscopy of silica at extreme conditions
Liang, Yunfeng
2007
Abstract
The outline of my thesis is the following: In Chapter 1, I present more details related to the motivation for studying silica. In Chapter 2, I mainly discuss the force matching method which has been used to construct the force field, and some methology. In Chapter 3, I show how the performance of the potential and how it can be used to calculate infrared and Raman spectra, focusing on the the calcuation of the spectra for high-temperature phase. Based on the calculated specta and the structural analysis, more profound understanding of the silica high-temperature phase is given. I will show in Chapters 4 and 5, pressure–induced changes in oxygen packing in quartz and cristobalite can be understood based on well-known transition paths for close-packing lattices. I will present in Chapter 6, a microscopic picture of the compression mechanisms of silica glass. In order to advance the understanding of pressure-induced amorphization, in Chapter 7 I also studied one example of the silica clathrate (type I) under pressure. I will then summarise the main results of my work in Chapter 8.File | Dimensione | Formato | |
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https://hdl.handle.net/20.500.14242/123177
URN:NBN:IT:SISSA-123177