TY - JOUR
T1 - Density-driven structural transformations in network forming glasses
T2 - A high-pressure neutron diffraction study of GeO 2 glass up to 17.5GPa
AU - Salmon, Philip S.
AU - Drewitt, James W.E.
AU - Whittaker, Dean A.J.
AU - Zeidler, Anita
AU - Wezka, Kamil
AU - Bull, Craig L.
AU - Tucker, Matthew G.
AU - Wilding, Martin C.
AU - Guthrie, Malcolm
AU - Marrocchelli, Dario
PY - 2012/10/17
Y1 - 2012/10/17
N2 - 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 5GPa, is associated with a reorganization of GeO 4 units. The second, extending over the range from 5 to 10GPa, corresponds to a regime where GeO 4 units are replaced predominantly by GeO 5 units. In the third, as the pressure increases beyond 10GPa, 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 30GPa, 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 24GPa where SiO 4 units are replaced predominantly by SiO 5 units, and a regime beyond 24GPa where appreciable concentrations of SiO 6 units begin to form.
AB - 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 5GPa, is associated with a reorganization of GeO 4 units. The second, extending over the range from 5 to 10GPa, corresponds to a regime where GeO 4 units are replaced predominantly by GeO 5 units. In the third, as the pressure increases beyond 10GPa, 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 30GPa, 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 24GPa where SiO 4 units are replaced predominantly by SiO 5 units, and a regime beyond 24GPa where appreciable concentrations of SiO 6 units begin to form.
UR - http://www.scopus.com/inward/record.url?scp=84866865849&partnerID=8YFLogxK
U2 - 10.1088/0953-8984/24/41/415102
DO - 10.1088/0953-8984/24/41/415102
M3 - Article
AN - SCOPUS:84866865849
SN - 0953-8984
VL - 24
JO - Journal of Physics Condensed Matter
JF - Journal of Physics Condensed Matter
IS - 41
M1 - 415102
ER -