Abstract
The Henry’s law constant (H) is an important parameter in predicting the transport, behavior and fate of organic compounds in environment. H is also required to model the air–water exchange of chemicals. Henry’s law constant of formaldehyde (HCHO) was determined at six temperatures (50, 40, 30, 20, 10, and 5°C) using a bubble-column technique. The apparent Henrys law constant (H*) values were strongly correlated to inverse of temperature (1/T, K) and the following relationship was obtained: $$\ln \;H^{{\text{*}}} = {\left( {{{\text{ - 1,641}}{\text{.3}}} \mathord{\left/ {\vphantom {{{\text{ - 1,641}}{\text{.3}}} T}} \right. \kern-\nulldelimiterspace} T} \right)} - 3.089$$ Seven concurrent ambient air and aqueous samples were also collected between October 11–17, 2005 at a sampling site located on the shoreline of Tahtali dam Lake in Izmir, Turkey to determine the magnitude and direction (deposition or gas-out) of HCHO flux. In all cases, the modeled gas-phase flux was positive (average ± SD, 3,181 ± 408 μg m−2 day−1) indicating that atmospheric HCHO deposited to the Tahtali Lake.