2020
DOI: 10.1016/j.scitotenv.2020.140922
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Mechanistic insights into iodine enrichment in groundwater during the transformation of iron minerals in aquifer sediments

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Cited by 33 publications
(30 citation statements)
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“…With increasing PVs through the aquifers, the concentrations of organic I were elevated for the entire depth profile (Figure G-I). Likewise, the rate of organic I accumulation was higher at the early stage due to the faster degradation of organic matter and the formation of iodinated organic compounds . Decreasing the production rate of organic I has led its concentration to approach a maximum that is constrained by the vertical flow velocity.…”
Section: Resultsmentioning
confidence: 99%
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“…With increasing PVs through the aquifers, the concentrations of organic I were elevated for the entire depth profile (Figure G-I). Likewise, the rate of organic I accumulation was higher at the early stage due to the faster degradation of organic matter and the formation of iodinated organic compounds . Decreasing the production rate of organic I has led its concentration to approach a maximum that is constrained by the vertical flow velocity.…”
Section: Resultsmentioning
confidence: 99%
“…Likewise, the rate of organic I accumulation was higher at the early stage due to the faster degradation of organic matter and the formation of iodinated organic compounds. 5 Decreasing the production rate of organic I has led its concentration to approach a maximum that is constrained by the vertical flow velocity. The maximum was lower owing to greater dilution at faster groundwater flow and thus required fewer PVs to approach (e.g., 0.26 vs 0.41 μmol/L at 33 m depth, Figure 6I vs 6G).…”
Section: Prediction Of Iodine Spatiotemporal Variabilitymentioning
confidence: 99%
“…Oxidation iodine species (IO 3 − and organo-iodine) more occur in oxidizing and organic rich environments 2 , 17 . The stronger absorption capacity of oxidation iodine onto mineral surfaces 20 than I − makes the species to be dominant (contributing 64.30% ± 26.40% to total iodine content) in iodine-deficient areas (TI < 10 μg/L). The dispersed distribution of high iodate groundwater under varying geo-environmental zones is reflected by a poor correlation between IO 3 − and TI (R 2 = 0.19, P < 0.001) (Supplementary Fig.…”
Section: Spatial Distribution Of Iodine Speciationmentioning
confidence: 99%
“…Oxidation iodine (IO 3 − and organo-iodine), which often appear in a non-steady state, are more likely to exist under weak oxidizing thermodynamic conditions 16 commonly found in low-iodine groundwater. IO 3 − is more likely to bond with sediment rather than enrich groundwater 20 , and thus groundwater IO 3 − rarely exceeds the threshold at which oxidative damage occurs 21 . Different organo-iodine compounds can also comprise a significant fraction of TI 16 .…”
Section: Introductionmentioning
confidence: 99%
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