2001
DOI: 10.1016/s0304-4203(00)00097-9
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Iron speciation in coastal rainwater: concentration and deposition to seawater

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Cited by 91 publications
(117 citation statements)
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“…Thus, our results suggest that the initial dissolved iron is mainly Fe(II)-organic complex under dark conditions. These Fe(II) ratings are in the same order of magnitude as those reported in the literature, where DFe(II)/DFe T mean ratios higher than 50 % are observed in the atmospheric waters (Behra and Sigg, 1990;Özsoy and Saydam, 2001;Kieber et al, 2001). It is known that iron redox species are involved in numerous (photo)chemical reactions in cloud-and raindrops, such as the oxidation of S(IV), the budget of H 2 O 2 , the formation of free radicals (OH, HO 2 /O − 2 ) and the oxidation of ozone Deguillaume et al, 2004;Ben'ko and Lunin, 2010).…”
Section: Iron Solubility and Redox Speciationsupporting
confidence: 84%
See 1 more Smart Citation
“…Thus, our results suggest that the initial dissolved iron is mainly Fe(II)-organic complex under dark conditions. These Fe(II) ratings are in the same order of magnitude as those reported in the literature, where DFe(II)/DFe T mean ratios higher than 50 % are observed in the atmospheric waters (Behra and Sigg, 1990;Özsoy and Saydam, 2001;Kieber et al, 2001). It is known that iron redox species are involved in numerous (photo)chemical reactions in cloud-and raindrops, such as the oxidation of S(IV), the budget of H 2 O 2 , the formation of free radicals (OH, HO 2 /O − 2 ) and the oxidation of ozone Deguillaume et al, 2004;Ben'ko and Lunin, 2010).…”
Section: Iron Solubility and Redox Speciationsupporting
confidence: 84%
“…It is known that iron redox species are involved in numerous (photo)chemical reactions in cloud-and raindrops, such as the oxidation of S(IV), the budget of H 2 O 2 , the formation of free radicals (OH, HO 2 /O − 2 ) and the oxidation of ozone Deguillaume et al, 2004;Ben'ko and Lunin, 2010). This modifies the redox cycling between Fe(II) and Fe(III) and implies a temporal pattern of Fe(II) and Fe(III) ratio with predominance of Fe(II) throughout the day (Zhu et al, 1997;Siefert et al, 1998;Kieber et al, 2001, Deutsch et al, 2001). Thus, the organic Fe(II)-complexes released by dissolution could be not stable.…”
Section: Iron Solubility and Redox Speciationmentioning
confidence: 99%
“…The most likely mechanism for this pattern is stabilization as an organic-Fe(II) complex. Kieber et al (2001) found that Fe(II) accounted for more than 80% of total dissolved Fe in rainwater collected in coastal areas of North Carolina and New Zealand.…”
Section: Relation Of Iron Chemistry To Dissolved Organic Carbon Ph mentioning
confidence: 99%
“…20 phf) in these experiments and considered the concentrations of materials in previous work. For example, Fe(lI1) concentrations used here were outside the range of Fe(III) concentrations observed in rainwater (up to 1 and seawater (21), although readily observable in some rivers (e.g. the Satilla River, Georgia) (22).…”
Section: Methodsmentioning
confidence: 79%