Models for Air–Water Gas Transfer
Tellus (1984), 36B, 92-100 Models for air-water gas transfer: an experimental investigation By KIM HOLMEN, Department of Meteorology,' University of Stockholm, Arrhenius Laboratory, S-106 91 Stockholm, Sweden and PETER LISS, School of Environmental Sciences, University of East Anglia, Norwich, NR4 7TJ, England (Manuscript received August 16; in final form November 14, 1983) ABSTRACT The air-water transfer velocities for H,, He and Xe have been measured simultaneously in laboratory-tank experiments. Using average values from the existing literature data for the molecular diffusivities of the gases, the transfer velocities are found to vary with the diffusivity raised to the power 0.57. This exponent is in reasonable agreement with the findings from other laboratories, as well as field studies, provided average diffusivities are used consistently. Although interpretation is limited by uncertainties in presently available diffusion coefficients, the results may be interpreted as supportive of both the surface-renewal and boundary-layer models of air-water gas exchange, but they provide little evidence for the appropriateness of the film model. 1. Introduction In it, the main body of the fluid (liquid or gaseous) is assumed to be well mixed, the rate of interfacial The air-water transfer of gases which are transfer being determined by molecular diffusion of sparingly soluble in water and do not react rapidly the gas molecules across a stagnant layer (or film) in the aqueous phase is controlled by processes in of fluid (thickness z) adjacent to the surface. In this the near-surface water (Liss, 1973). Gases for model, the rate of gas exchange, expressed in terms which this applies include 0,, CO,, the inert gases, of a transfer velocity k, (defined as the flux of gas CO, CH,, CHJ, (CH,),S, freons and other low 'x' per unit of concentration gradient driving its molecular weight halocarbons.
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