Department of Physics, University of Bath, Bath, UK.
J Phys Condens Matter. 2012 Oct 17;24(41):415102. doi: 10.1088/0953-8984/24/41/415102. Epub 2012 Sep 6.
The structure of GeO(2) glass was investigated at pressures up to 17.5(5) GPa using in situ time-of-flight neutron diffraction with a Paris-Edinburgh press employing sintered diamond anvils. A new methodology and data correction procedure were developed, enabling a reliable measurement of structure factors that are largely free from diamond Bragg peaks. Calibration curves, which are important for neutron diffraction work on disordered materials, were constructed for pressure as a function of applied load for both single and double toroid anvil geometries. The diffraction data are compared to new molecular-dynamics simulations made using transferrable interaction potentials that include dipole-polarization effects. The results, when taken together with those from other experimental methods, are consistent with four densification mechanisms. The first, at pressures up to approximately equal 5 GPa, is associated with a reorganization of GeO(4) units. The second, extending over the range from approximately equal 5 to 10 GPa, corresponds to a regime where GeO(4) units are replaced predominantly by GeO(5) units. In the third, as the pressure increases beyond ~10 GPa, appreciable concentrations of GeO(6) units begin to form and there is a decrease in the rate of change of the intermediate-range order as measured by the pressure dependence of the position of the first sharp diffraction peak. In the fourth, at about 30 GPa, the transformation to a predominantly octahedral glass is achieved and further densification proceeds via compression of the Ge-O bonds. The observed changes in the measured diffraction patterns for GeO(2) occur at similar dimensionless number densities to those found for SiO(2), indicating similar densification mechanisms for both glasses. This implies a regime from about 15 to 24 GPa where SiO(4) units are replaced predominantly by SiO(5) units, and a regime beyond ~24 GPa where appreciable concentrations of SiO(6) units begin to form.
采用烧结金刚石压砧的巴黎-爱丁堡压力机对 GeO(2)玻璃在高达 17.5(5) GPa 的压力下的结构进行了原位飞行时间中子衍射研究。开发了一种新的方法和数据校正程序,能够可靠地测量结构因子,这些结构因子在很大程度上不受金刚石布拉格峰的影响。构建了压力作为施加负载函数的校准曲线,这些校准曲线对于无序材料的中子衍射工作非常重要,适用于单环和双环环压砧几何形状。将衍射数据与使用包括偶极极化效应的可转移相互作用势进行的新分子动力学模拟进行了比较。将这些结果与其他实验方法的结果结合在一起,与四种致密化机制一致。第一种机制在压力高达约 5 GPa 左右,与 GeO(4)单元的重新组织有关。第二种机制在约 5 到 10 GPa 的范围内,对应于 GeO(4)单元主要被 GeO(5)单元取代的区域。在第三种机制中,随着压力的增加超过约 10 GPa,GeO(6)单元的浓度开始显著增加,并且中间范围有序度的变化率降低,这可以通过第一尖锐衍射峰的位置随压力的变化来测量。在第四种机制中,在约 30 GPa 时,实现了主要为八面体玻璃的转变,并且进一步的致密化通过 Ge-O 键的压缩进行。在 GeO(2)的测量衍射图案中观察到的变化发生在与 SiO(2)相似的无量纲数密度处,表明两种玻璃具有相似的致密化机制。这意味着在约 15 到 24 GPa 的范围内,SiO(4)单元主要被 SiO(5)单元取代,在约 24 GPa 以上的范围内,SiO(6)单元的浓度开始显著增加。