The structures of xAgI+(1-x)Ag2O . 2B(2)O(3) glasses, where 0.2 less t
han or equal to x less than or equal to 0.6, have been investigated us
ing mid- and far-infrared spectroscopy. The mid-IR spectra revealed th
at in those glasses prepared using AgNO3 as the starting material for
Ag2O, the BO4-/BO3 ratio is constant with increasing amounts of AgI as
would be expected form the proposed behavior of AgI in these glasses.
However, a survey of the literature revealed those glasses prepared f
rom pure Ag2O show a strong linear dependence of the BO4-/BO3 ratio on
AgI content. Most probably, in those glasses prepared with Ag2O the A
g2O/B2O3 ratio changes with AgI content due to the decomposition of Ag
2O during melting. This different behavior is associated with AgNO3 de
composing to Ag2O with heating followed by incorporation into the glas
sy network. For Ag2O used directly, it is proposed that it decomposes
to Ag metal and Oz(gas) with heating before it can be incorporated int
o the berate network. This latter behavior decreases with increasing A
gI in the batch composition because AgI lowers the liquidus temperatur
e of the melt considerably. The far-IR analysis of the AgI-doped silve
r diborate glasses suggests that there are three coordination environm
ents for the Ag+ ions; one with iodide anions and the other two with o
xygen ions. It is proposed that the separate oxygen coordination envir
onments for the Ag+ ions arise from one with bridging oxygens of BO4-
units, and the other with nonbridging oxygens on BO3- units. Furthermo
re, it is proposed that the Ag+ ions in the iodide-ion environments pr
ogressively agglomerate into disordered regions of AgI, but do not for
m structures similar to alpha-AgI. These results appear to support the
conduction pathway or ''microdomain'' model for ionic conduction in x
AgI+(1-x)Ag2O . 2B(2)O(3) glasses where the pathways are built up form
disordered structures of AgI.