The volumes and expansivities of four hydrous phonolite glasses and liquids
have been measured by dilatometry from 300 K up to the glass transition an
d over a 50 K interval just above the glass transition. The partial molar v
olume of water is independent of the water content for the glass and liquid
phases, with values of about 11.0 +/- 0.5 and 17.1 +/- 0.9 cm(3)/mol at 30
0 and 800 K, respectively. The partial molar thermal expansivity of water i
n phonolite glasses is about 8x10(-5) K-1, a result similar to recently pub
lished values for different silicate compositions, and about 36.5x10(-5) K-
1 in phonolite liquids. The implications for melt density and water dissolu
tion are discussed.