A model of the liquid-vapor phase partitioning behavior of low concentratio
ns of gas tracers in water at geothermal temperatures and pressures is pres
ented. This model uses Henry's coefficient to describe the variation of the
gas tracer solubility with temperature and pressure. A new method is descr
ibed for the determination and representation of Henry's coefficients. The
method uses experimentally determined values of Henry's coefficient and a t
heoretically predicted value of behavior at the critical point of water to
provide data that can be fitted by a semi-empirical correlation. No assumpt
ions regarding ideal behavior are necessary. The semiempirical correlation
is a modified version of that presented by Harvey, A. (1996. Semiempirical
correlation for Henry's constants over large temperature ranges. American I
nstitute of Chemical Engineers Journal 42(5), 1491-1494) and better account
s for high temperature and non-ideal behavior. Sets of model coefficients a
re given for a range of possible gas tracers. The resulting phase partition
ing model is simple and may be easily implemented in a numerical geothermal
simulator. The use and behavior of the model is illustrated by its applica
tion to a number of idealised test problems. (C) 2001 CNR. Published by Els
evier Science Ltd. All rights reserved.