“…·OH are also ubiquitous in natural aquatic environments. They can be produced via the photolysis of nitrite, nitrate, and dissolved organic matter (DOM), photo-Fenton reactions, microbial activities, and overturn-induced aeration of anoxic bottom water. − Reactive chlorine species (RCS), like chlorine atoms (Cl·), chlorine oxide radicals (ClO·), and dichlorine radical anions (Cl 2 •– ), have attracted great attention for AOPs in recent years, − and they can be produced through ultraviolet light (UV)-activated photolysis of free chlorine and monochloramine. − Moreover, emerging technologies such as photocatalysis, electrocatalysis, and photoelectrocatalysis have been discovered to produce a high concentration of RCS for effective pollutant control. − Similar to ·OH, RCS are also ubiquitous in natural aquatic systems, especially in brines, estuaries, and seawater, and they are generated through the oxidation of chloride by ·OH, singlet oxygen ( 1 O 2 ), and photoexcited DOM. − When compared to ·OH, RCS oxidation could be less thermodynamically favorable due to their lower reduction potentials (the reduction potential of Cl·, Cl 2 •– , and ClO· is 2.5, 2.2, and 1.5–1.8 eV, respectively). ,, Moreover, RCS is more selective than ·OH: Cl· launches the electrophilic attack on aromatic rings whereas Cl 2 •– and ClO· prefer to react with aromatics with electron-donating groups through electron transfer. − However, RCS-induced oxidation is likely to form halogenated byproducts, which may raise concerns for human health and ecosystems. ,− …”