Effect of dissolved oxygen on the photodecomposition of monochloramine and dichloramine in aqueous solution by UV irradiation at 253.7 nm

Abstract

The effect of dissolved oxygen on the photodecomposition of monochloramine (7.5 < pH < 10) and dichloramine (pH = 3.7 ± 0.2) at 253.7 nm has been investigated. The kinetic study shows that the rate of photodecomposition of monochloramine is about two times faster in the absence of oxygen than in the presence of oxygen, is not significantly affected by pH and by the presence of hydroxyl radical scavengers (hydrogenocarbonate ion and tert-butanol). The apparent quantum yields of photodecomposition of monochloramine at 253.7 nm ([NH 2Cl] 0 ≈ 1.5–2 mM, ɛ 253.7 nm = 371 M −1 cm −1) were equal to 0.28 ± 0.03 and 0.54 ± 0.03 mol E −1 in oxygenated-saturated and in oxygen-free solutions, respectively. The photodecomposition rates or the apparent quantum yields of photodecomposition of dichloramine ([NHCl 2] 0 ≈ 1.5–2 mM, pH = 3.7 ± 0.2) in oxygen-free and in oxygen-saturated solutions were quite identical ( Φ = 0.82 ± 0.08 mol E −1; ɛ 253.7 nm = 126 M −1 cm −1). Under O 2 saturation, UV irradiation of NH 2Cl leads to the formation of nitrite (≈0.37 mol/mol of NH 2Cl decomposed), nitrate (≈0.073 mol/mol) and does not form ammonia (<0.01 mol/mol). In oxygen-free solutions, monochloramine decomposes to form ammonia (≈0.37 mol/mol). Photodecomposition of dichloramine did not lead to significant amounts of nitrite and nitrate in the presence and in the absence of oxygen. The nitrogen mass balances also indicate the formation of other nitrogen species (probably N 2 and/or N 2O) during the photodecomposition of monochloramine and dichloramine by UV irradiation at 253.7 nm.