Experiments investigating the mass transfer of several dissolved volatile o
rganic compounds (VOCs) across the air-water interface were conducted using
a single-air-channel air-sparging system. Three different porous media wer
e used in the study. Air velocities ranged from 0.2 cm s(-1) to 2.5 cm s(-1
). The tortuosity factor for each porous medium and the air-water mass tran
sfer coefficients were estimated by fitting experimental data to a one-dime
nsional diffusion model. The estimated mass transfer coefficients K-G range
d from 1.79 x 10(-3) cm min(-1) to 3.85 x 10(-2) cm min(-1). The estimated
lumped gas phase mass transfer coefficients K(G)a were found to be directly
related to the air diffusivity of the vee, air velocity, and particle size
, and inversely related to the Henry's law constant of the VOCs. Of the fou
r parameters investigated, the parameter that controlled or had a dominant
effect on the lumped gas phase mass transfer coefficient was the air diffus
ivity of the VOC. Two empirical models were developed by correlating the Da
mkohler and the modified air phase Sherwood numbers with the air phase Pecl
et number, Henry's law constant, and the reduced mean particle size of poro
us media. The correlation developed in this study may be used to obtain bet
ter predictions of mass transfer Auras for field conditions.