1977 Volume 85 Issue 982 Pages 299-305
The chemical shifts of AlKα1, 2 X-ray fluorescence lines of germanate, borate and phosphate glasses have been determined in order to investigate the coordination number of Al3+ ions in glasses.
In Na2O-Al2O3-GeO2 glasses with 60 and 70mol% GeO2 and the Al2O3/Na2O ratios ranging from 0.5 to 1.5, the chemical shifts were nearly equal with each other and with that for orthoclase crystal, indicating that the Al3+ ions are fourfold-coordinated in the glasses.
The chemical shifts for CaO-Al2O3-B2O3 glasses largely depended on the B2O3 content of glass and not on the Al2O3/CaO ratio. The chemical shift increased from the value nearly equaling that for the orthoclase towards that for α-Al2O3 as the B2O3 content increased, indicating that the average coordination number of the Al3+ ions increases with increasing B2O3 content.
A wide variety of phosphate glasses with varying P/O ratio were melted from the batches containing various constituents besides Al2O3 and P2O5, and subjected to measurement of the AlKα1, 2 spectra, assuming that the P/O ratio of 0.333 would correspond to the metaphosphate and the ratio of 0.25 to the orthophosphate. It was found from the chemical shifts that glasses with the ratio near 0.333 contain a considerable fraction of six-coordinated Al3+ ions, while those with the ratio near or below 0.25 contain almost all Al3+ ions in four-coordination.