Optical spectroscopy measurements were performed on Al2O3-B2O3-SiO2 glasses
containing 7-25 mol% Nd2O3 (soluble). The local chemical environment of Nd
(III) in glass was systematically studied as a function of the Nd2O3 concen
tration using Judd-Ofelt (J-O) optical oscillator parameters, Omega (2) and
Omega (6), that are related to the ligand field symmetry (LFS) and the deg
ree of bond covalency (BC), respectively. Two transition points (TPs), in t
erms of Omega (lambda) versus Nd2O3 concentration, were found for Omega (2)
that is sensitive to LFS and Omega (6) that is sensitive to the degree of
BC. The first TP is defined by Nd:3(B + Al) and the second by Nd:3(B + Al Si). Below the first TP, Omega (2) and Omega (6) were nearly independent o
f Nd concentration. Between the first and the second TP, Omega (2) and Omeg
a (6) increased and then decreased above the second TP. After reviewing lit
erature data on rare earths (REs) in Na2O-B2O3, Na2O-SiO2, Na2O-B2O3-SiO2,
and Al2O3-B2O3 systems, we proposed that up to the first TP, Nd preferentia
lly dissolves in a berate-rich environment composed of two trigonal boron,
B-III, and one tetrahedral boron, B-IV, where Al-IV substitutes for B-IV. F
urther increases in Nd2O3 concentrations result in excess Nd cations, [Nd-3
(B + Al)], partitioning to a silicate-rich environment, possibly in a form
of Nd-Q(3), and above the second TP, Nd-Q(2) could form at the expense of N
d-Q(3) (Q(n) is the number of bridging oxygens per Si tetrahedron), whereas
the concentration of Nd cations in the berate sites is expected to be unch
anged. Crystallization of Nd silicate above its solubility, 25-30 mol% Nd2O
3, indirectly supports the proposed Nd dissolution mechanisms. The dissolut
ion of rare earth elements in alumino-borosilicate glasses may be best desc
ribed in terms of their partitioning to these structure groups. (C) 2000 El
sevier Science B.V. All rights reserved.