F. Farges et al., COORDINATION CHEMISTRY OF TI(IV) IN SILICATE-GLASSES AND MELTS .3. GLASSES AND MELTS FROM AMBIENT TO HIGH-TEMPERATURES, Geochimica et cosmochimica acta, 60(16), 1996, pp. 3055-3065
The local structural environment of Ti in five Na-, K-, and Ca-titanos
ilicate glass/melts with TiO2 concentrations ranging from 2.7-30.5 wt%
has been determined by in situ Ti K-edge x-ray absorption fine struct
ure (XAFS) spectroscopy at temperatures ranging from 293-1650 K. In pa
rallel, two Ti-model compounds (Ni2.6Ti0.7O4 spinel and TiO2 rutile) w
ere studied under the same conditions to better understand the effects
of temperature (anharmonicity) on the XAFS spectra. Temperature-induc
ed anharmonicity was found to vary, largely as a function of the Ti-co
ordination, and increases significantly around Ti with increasing temp
erature when present as Ti-[6]. In contrast, anharmonicity appears neg
ligible around Ti-[4] at temperatures below 1200 K. We predict that an
harmonicity should be weak around Ti-[5] as well. No clear evidence wa
s found for a significant change in the average nearest-neighbor coord
ination environment of Ti in the Na- and K-titanosilicate glasses and
melts that exhibit anomalous heat capacities variations just above the
ir glass transition temperatures, T-g (860-930 K). The small (predicte
d and measured) linear thermal expansion of the ((TiO2+)-Ti-[5])-O bon
d in these systems at high temperature is expected to have an insignif
icant effect on the local environment of Ti-[5] during the glass-to-su
percooled liquid transition. In the most dilute Ti-glass studied (KS1;
2.7 wt% TiO2), the local environment around Ti-[4] (especially the se
cond-neighbor alkalis) is relatively ordered at ambient temperature, b
ut this order decreases dramatically above T-g. Lower quench rates app
ear to favor Ti-[4] over Ti-[5]. The origin of the observed anomalous
positive variations in heat capacities of these melts may be related t
o significant changes in the medium-range environment around Ti above
T-g including the disappearance of percolation domains involving inter
faces between alkali-rich and network-former rich regions during struc
tural relaxation at T-g; these percolation domains are related to the
dual structural role of Ti in silicate glass/melts (acting simultaneou
sly as network former and network modifier).