Abstract
The diffusivity of ozone in water was determined experimentally by measuring the rate of ozone absorption into an aqueous laminar liquid jet. Penetration theory was used to interpret the results. Experiments were conducted over the temperature range of 10 °C to 45 °C. The results for diffusivity were correlated by an Arrhenius function for temperature dependence with a maximum deviation of ± 3.3%: D/m2·s-1 = 1.10 × 10-6 exp[-1896/(T/K)].
Original language | English (US) |
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Pages (from-to) | 1485-1487 |
Number of pages | 3 |
Journal | Journal of Chemical and Engineering Data |
Volume | 41 |
Issue number | 6 |
DOIs | |
State | Published - Jan 1 1996 |