2021
DOI: 10.1016/j.envpol.2021.116749
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Spatial distribution and biogeochemical cycling of methyl iodide in the Yellow Sea and the East China Sea during summer

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Cited by 5 publications
(4 citation statements)
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“…Moreover, experiments show that CH3I emission under dark incubation was much lower than that under light incubation and CH3I production under visible light conditions is lower than that under natural light (Li et al, 2021). Those results indicate that ultraviolet light promotes the production 480 of CH3I (Chen et al, 2020;Li et al, 2021) as well as its photochemical oxidation. This is consistent with our observation that HIOx is only formed in the daytime (Fig.…”
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confidence: 87%
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“…Moreover, experiments show that CH3I emission under dark incubation was much lower than that under light incubation and CH3I production under visible light conditions is lower than that under natural light (Li et al, 2021). Those results indicate that ultraviolet light promotes the production 480 of CH3I (Chen et al, 2020;Li et al, 2021) as well as its photochemical oxidation. This is consistent with our observation that HIOx is only formed in the daytime (Fig.…”
mentioning
confidence: 87%
“…CH3I concentration was shown to be correlated with surface seawater temperature (SST) in marine boundary layer air at midlatitude (Yokouchi et al, 2008). Others reported the opposite results in the Yellow Sea and the East China Sea during summer (Li et al, 2021) and the reason may be that higher surface water temperature also accelerates the chemical loss of CH3I from the seawater and atmospheric CH3I is readily photolyzed. Long-term variations of atmospheric CH3I at several sites show that SST 465 near each site cannot fully explain the variation of observed CH3I concentrations (Yokouchi et al, 2012).…”
Section: Iodine Sources 420mentioning
confidence: 99%
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“…In recent years, organic iodides (such as CH 3 I) have attracted increasing attention from the atmospheric science community. 1 As a gaseous pollutant with high reactivity, CH 3 I mainly comes from the ocean, fumigants, and the spent fuel. 2 Among them, CH 3 I emitted from the reprocessing process of spent fuel is radioactive, because it is converted from radioactive isotopes 129 I (half-life, t 1/2 = 1.6 × 10 7 years) and 131 I ( t 1/2 = 8 days).…”
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confidence: 99%