Dissolution of CO2 droplets in the ocean has been studied. Owing to hy
drogen bonding and supersaturation with CO2, seawater at the surface o
f the CO2 droplets becomes highly structured. Since this quasi-crystal
line structure is similar to that of hydrate crystal elements, hydrate
formation on the droplets will not cause a dramatic decrease in the d
issolution rate as reported in the literature. Mass transfer of a buoy
ant CO2 droplet in Stokes flow in the ocean is analysed. Based on the
derived mass-transfer coefficients, shrinkage rates for CO2 droplets w
ithout and with a hydrate shell are predicted. Good agreement is obser
ved between predictions and experimental data. (C) 1997 Elsevier Scien
ce Ltd.