Photo-production of excited triplet-state of dissolved organic matters in inland freshwater and coastal seawater

被引:4
作者
Guo, Zhongyu [1 ]
Wang, Tingting [2 ]
Ichiyanagi, Hidetaka [3 ]
Ateia, Mohamed [4 ]
Chen, Guo [1 ]
Wang, Jieqiong [5 ]
Fujii, Manabu [1 ]
En, Kaichii [6 ]
Li, Tiansheng [7 ]
Sohrin, Rumi [8 ]
Yoshimura, Chihiro [1 ]
机构
[1] Tokyo Inst Technol, Dept Civil & Environm Engn, Meguro Ku, Tokyo 1528552, Japan
[2] Nagoya Univ, Grad Sch Sci, Furo Cho,Chikusa Ku, Nagoya, Aichi 4648602, Japan
[3] Water Resources Environm Ctr, Tokyo 1020083, Japan
[4] Rice Univ, Dept Chem & Biomol Engn, Houston, TX USA
[5] North China Elect Power Univ, Coll Environm Sci & Engn, Beijing 102206, Peoples R China
[6] Tokai Univ, Sch Sci, Dept Chem, Hiratsuka, Kanagawa 2591292, Japan
[7] Tokyo Inst Technol, Inst Innovat Res, Lab Zero Carbon Energy, Meguro Ku, Tokyo 1528550, Japan
[8] Shizuoka Univ, Inst Geosci, 836 Oya, Shizuoka 4228529, Japan
基金
日本学术振兴会;
关键词
High-energy triplets; Modeling; Optical property; Photochemistry; Quantum yield coefficient; OPTICAL-PROPERTIES; ENERGY-TRANSFER; SINGLET OXYGEN; QUANTUM YIELDS; PHOTODEGRADATION; PHOTOREACTIVITY; CARBON; DOM; PHOTOCHEMISTRY; TRANSFORMATION;
D O I
10.1016/j.watres.2024.121260
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The excited triplet-state of dissolved organic matter ((DOM)-D-3*) is a major reactive intermediate in sunlit waters. Its quantum yield is important in understanding the fate of organic micropollutants. The degradation efficiency of its chemical probe, 2,4,6-trimeythlphenol (f(TMP)), is generally used as a proxy of the quantum yield. However, f(TMP) has been described and modelled only for freshwater systems. Therefore, this study quantified f(TMP) in inland freshwater and coastal seawater sampled in Japan by conducting steady-state photochemical experiments. Optical properties of water were then used to model f(TMP). Results indicated that the inland freshwater DOM originated mainly from terrestrial sources, while the coastal seawater DOM were microbial-dominated. On average, inland freshwater exhibited lower f(TMP) (61.2 M-1) than coastal seawater (79.7 M-1) and the coastal seawater exhibited significant variations in the proportion of high-energy (DOM)-D-3* (> 250 kJ/mol). In addition, E-2:E-3 (ratio of absorbance at 254 to 365 nm) was positively correlated with f(TMP) of inland freshwater, coastal seawater, and the overall dataset. Catchment conditions such as forest coverage also influenced the production of (DOM)-D-3* and high-energy (DOM)-D-3* in inland freshwater. Furthermore, the developed models estimated f(TMP) based on the optical properties of both freshwater and seawater, providing valuable insights about (DOM)-D-3* photochemistry in the aquatic environment.
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页数:12
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