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Please be aware that this old REACH registration data factsheet is no longer maintained; it remains frozen as of 19th May 2023.

The new ECHA CHEM database has been released by ECHA, and it now contains all REACH registration data. There are more details on the transition of ECHA's published data to ECHA CHEM here.

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Environmental fate & pathways

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Chlorine is a highly reactive compound, which will react readily in the atmosphere and in soil, and with organic matter. In water, chlorine will form hypochlorous acid and hypochlorite at environmental relevant pH. Chlorine discharged to sewer will react to form chloramines. As a non-organic compound, chlorine is not biodegradable.

Photolysis in water

The photolysis half-life of aqueous chlorine in, exposed to summer noon sunlit with clear sky (47°N) at a pH 8 is 12 min when measured at the surface. The half-life

increases with decreasing pH due to the decreasing ratio of OCl-/HOCl to 60 min at pH 5. The pseudo-first-order rate constant for the photolysis of HOCl becomes 2 x 10-4/s and that of OCl-1.2 x 10-3/s. The variation of the rate of photolysis with depth was calculated for water columns exhibiting different light absorption coefficients by taking into account that, for both HOCl and OCl-, the most effective wavelength for photolysis in sunlight is approx. 330 nm. These results show that in water treatment, chlorine photolysis should be minimized whenever possible by operating at low pH, sun shielding or night-time addition of chlorine or avoiding storage in shallow reservoirs. The rate of chlorine photolysis controls the formation of OH radical which acts as a secondary highly reactive photooxidant.

On u.v. (255 nm) irradiation both HOCl and OCl- photolyze at comparable rates and slowly enough that chlorine depletion will not occur during the time of irradiation typical in UV disinfection.

Photolysis can also contribute to the depletion of chlorine in atmospheric waters whenever chlorine is formed by (slow) ozonation of chloride.