Ion probe measurements offer the advantage of in situ determination of
water content with a few micrometres spatial resolution. After a brie
f review of ion microprobe procedures used for the determination of wa
ter concentration in silicates, we examine three important effects on
analytical precision: (1) the effect of energy filtering an the backgr
ound; (2) the variation of the H/Si ratio with time; and (3) the depen
dence of the H/S1 ratio on the composition of the matrix, which requir
es the use of standards close in chemical composition to the unknowns.
, Finally, applications of this method to the determination of water i
n glasses quenched from water-saturated melts, to experimental product
s consisting of a mixture of glass and crystals, and to natural melt i
nclusions illustrate the advantages and the limitations of the ion mic
roprobe.