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This study investigated the partitioning behavior of dissolved organic matter (DOM) in liquid and ice phases,as well as the changes in the optical properties and chlorine reactivity of DOM during the freezing processes of water.DOM was rejected from the ice phase and accumulated in the remaining liquid phase during water freezing.Moreover,the decrease in freezing temperature,as well as the increase in dissolved organic carbon (DOC)concentration of feed water,caused an increase in DOM captured in the ice phase.The ultraviolet-absorbing compounds,trihalomethane precursors,as well as fulvic acid-and humic acid-like fluorescent materials,were more liable to be to be rejected from the ice phase and were more easily retained in the unfrozen liquid phase during water freezing,as compared with organics (on average) that comprise DOC.In addition,it was also found a higher accumulation of these organics in the unfrozen liquid phase during water freezing at higher temperature.The freeze/thaw processes altered the quantity,optical properties,and chlorine reactivity of DOM.The decrease in ultraviolet light at 254 nm as well as the production of aromatic protein-and soluble microbial byproduct-like fluorescent materials in DOM due to freeze/thaw were consistently observed.On the other hand,the changes in DOC,trihalomethane formation potential,and fulvic acid-and humic acid-like fluorescence caused by freeze/thaw varied significantly between samples.