Abstract
Methyl chloride (CH(3)Cl) is presently understood to arise from biotic and abiotic processes in marine systems. However, the production of CH(3)Cl via photochemical processes has not been well studied. Here, we reported the production of CH(3)Cl from humic acid (HA) in sunlit saline water and the effects of the concentration of HA, chloride ions, ferric ions and pH were investigated. HA in aqueous chloride solutions or natural seawater were irradiated under an artificial light, and the amounts of CH(3)Cl were determined using a purge-and-trap and gas chromatography-mass spectrometry. CH(3)Cl was generated upon irradiation and its amount increased with increasing irradiation time and the light intensity. The formation of CH(3)Cl increased with an increase of HA concentration ranging from 2 mg L(-1) to 20 mg L(-1) and chloride ion concentration ranging from 0.02 mol L(-1) to 0.5 mol L(-1). The photochemical production of CH(3)Cl was pH-dependent, with the highest amount of CH(3)Cl generating near neutral conditions. Additionally, the generation of CH(3)Cl was inhibited by ferric ions. Finally, natural coastal seawater was irradiated under artificial light and the concentration of CH(3)Cl rose significantly. Our results suggest that the photochemical process of HA may be a source of CH(3)Cl in the marine environment.