Photochemical characterization of paddy water during rice cultivation: Formation of reactive intermediates for As(III) oxidation

• Published in: Water research (Oxford) Vol. 206; p. 117721
• Main Authors: Zeng, Yu, Fang, Guodong, Fu, Qinglong, Dionysiou, Dionysios D., Wang, Xiaolei, Gao, Juan, Zhou, Dongmei, Wang, Yujun
• Format: Journal Article
• Language: English
• Published: Elsevier Ltd 01.11.2021
• Subjects: Arsenite oxidation; arsenites; Dissolved organic matter; fluorescence; humification; irradiation; mass spectrometry; molecular weight; Nitrite photochemistry; nitrites; oxidation; paddies; paddy soils; Paddy water; photochemistry; pollutants; Reactive intermediate; rice; singlet oxygen; statistical analysis; surface water; Arsenite oxidation; Dissolved organic matter; Paddy water; Reactive intermediate; Nitrite photochemistry
• ISSN: 0043-1354; 1879-2448; 1879-2448
• DOI: 10.1016/j.watres.2021.117721

•Reactive intermediates (RIs) generated from paddy water during the rice growing.•3DOM*, 1O2 and •OH were found to be the dominant RIs.•Quantum yields of 1O2 were about 2.4-6.7 times higher than those of surface water.•DOM and NO2− were main responsible for RIs generation.•3DOM* was dominant RIs for As(III) oxidation in paddy water Although the photochemical behavior of surface water and its effects on pollutant transformation have been studied extensively in recent years, the photochemistry of paddy water remains largely unknown. In this study, we examined the photochemical processes involving paddy water samples collected at four different cultivation stages of rice. Triplet dissolved organic matter (3DOM*), singlet oxygen (1O2), and hydroxyl radicals (•OH) were found to be the dominant reactive intermediates (RIs), and their apparent quantum yields and steady-state concentrations were quantified. Compared with the typical surface water, quantum yields of 3DOM* and •OH were comparable, while quantum yields of 1O2 were about 2.4-6.7 times higher than those of surface water. Fluorescence emission-excitation matrix (EEM) spectra, Fourier transform ion cyclotron resonance mass spectrometry (FTICR-MS), and statistical analysis revealed that DOM properties and nitrite concentration were the main factor influencing RIs generation. The results suggest that DOM with lower molecular weight and humification extent generated more RIs, and nitrite contributed to 23.9%–100% of •OH generation. EEM and FTICR-MS data showed that DOM with more saturated and less aromatic formulas could produce more 3DOM* under the irradiation, while the polyphenolic components of DOM inhibited the formation of RIs. Moreover, RIs significantly enhanced arsenite (As(III)) oxidation with oxidation rate increased by 1.8–4.1 times in paddy water, and •OH and 3DOM* were the main RIs responsible for As(III) oxidation. This study provides new insight into the pathways of arsenite abiotic transformation in paddy soil and water. [Display omitted]