Np. Lower et al., Physical properties of alkaline-earth and alkali borate glasses prepared over an extended range of compositions, J NON-CRYST, 293, 2001, pp. 669-675
By using rapid cooling we have greatly extended the reported glass-forming
ranges in the binary magnesium, calcium, strontium, and barium borate syste
ms. We observed phase separation for low alkaline-earth oxide contents, typ
ically below about 15 mol% alkaline-earth oxide, but we have been able to i
ncrease the alkaline-earth oxide limit of glass formation to approximately
60-65 mol%. We have determined the density and the glass transition tempera
ture for a large number of glasses within each of these systems. We compare
these data with atomic arrangement studies based on spectroscopy. Using a
model derived from the NMR data of Greenblatt and Bray [Phys. Chem. Glasses
8 (5) (1967) 190-193] we have determined the associated volumes of the fou
r basic borate structural units thought to be present in each system. These
groups include trigonal borons with three (f(1)), two (f(3)), and one brid
ging oxygens (f(4)) as well as the tetrahedral boron unit (f(2)). We compar
e these volumes with those obtained from the binary alkali borates. In addi
tion, we have calculated the volumes of the borate groups using Shannon and
Prewitt radii. This allowed us to determine and compare the packing fracti
ons of each borate arrangement in the alkaline-earth and alkali borate syst
ems. The T, data display two distinct regions, a high temperature region fo
r the alkaline-earth borates and one for the alkali borates. These regions
are separated by approximately 150 degreesC. (C) 2001 Elsevier Science B.V.
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