The deposition properties of gaseous elemental iodine on water were studied in a small, Plexiglas wind tunnel. The amounts of stable iodine deposited in the water and collected from the air on charcoal were determined using activation analysis, allowing values of deposition velocity to be calculated under various controlled conditions. Deposition velocity on water was found to increase linearly with increasing wind velocities over a range of wind speeds typical of most environments. Both the pH and water temperature had a pronounced effect on the deposition rate. Water with a slightly basic pH was about three times better as a collection surface than water with a slightly acidic pH. Measured values of the deposition velocity increased almost linearly with increasing water temperature. Differences in the deposition rate due to pH and water temperature variations were attributed to the changes they caused in the iodine solubility in water.