TY - JOUR
T1 - Influence of waves on air-water gas transfer
AU - Daniil, Ekaterini I.
AU - Gulliver, John S.
PY - 1991/9
Y1 - 1991/9
N2 - Experiments on air-water gas transfer were performed in a flume with a mechanical wave maker for the determination of the gas-transfer coefficient with waves. Oxygen was used as the transferred gas. The experiments indicate that nonbreaking deep-water gravity waves significantly influence air-water gas transfer. The gas-transfer coefficient was correlated with the wave characteristics. A renewal model was used for the analysis of the data, and the renewal rate was dependent on a wave Reynolds number. The gas-transfer coefficient was linearly dependent upon the product of wave height and wave frequency. This is also equivalent to the gas-transfer coefficient being directly proportional to the wave velocity at the water surface. Comparison with data reported in the literature indicates that a significant portion of the observed gas transfer in wind-wave flume experiments can be attributed to nonbreaking waves. The presence of bubbles or bubble-entraining breaking waves enhances the gas-transfer coefficient considerably. Visual correlation between breaking intensity and the transfer coefficient was good, although the relation has not been quantified.
AB - Experiments on air-water gas transfer were performed in a flume with a mechanical wave maker for the determination of the gas-transfer coefficient with waves. Oxygen was used as the transferred gas. The experiments indicate that nonbreaking deep-water gravity waves significantly influence air-water gas transfer. The gas-transfer coefficient was correlated with the wave characteristics. A renewal model was used for the analysis of the data, and the renewal rate was dependent on a wave Reynolds number. The gas-transfer coefficient was linearly dependent upon the product of wave height and wave frequency. This is also equivalent to the gas-transfer coefficient being directly proportional to the wave velocity at the water surface. Comparison with data reported in the literature indicates that a significant portion of the observed gas transfer in wind-wave flume experiments can be attributed to nonbreaking waves. The presence of bubbles or bubble-entraining breaking waves enhances the gas-transfer coefficient considerably. Visual correlation between breaking intensity and the transfer coefficient was good, although the relation has not been quantified.
UR - http://www.scopus.com/inward/record.url?scp=0026228531&partnerID=8YFLogxK
UR - http://www.scopus.com/inward/citedby.url?scp=0026228531&partnerID=8YFLogxK
U2 - 10.1061/(ASCE)0733-9372(1991)117:5(522)
DO - 10.1061/(ASCE)0733-9372(1991)117:5(522)
M3 - Article
AN - SCOPUS:0026228531
SN - 0733-9372
VL - 117
SP - 522
EP - 540
JO - Journal of Environmental Engineering (United States)
JF - Journal of Environmental Engineering (United States)
IS - 5
ER -