2006
DOI: 10.1016/j.envint.2005.08.015
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The use of ultra filtration in trace metal speciation studies in sea water

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Cited by 34 publications
(20 citation statements)
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“…Based on the concentrations reported for the three colloidal fractions (i.e., 1-10 kDa, 10-100 kDa and 100 kDa to 0.22 lm), Mn and Fe concentrations were constant at all sites except sites F and A. Mn concentrations tended to increase with decreasing size fraction at site F, while the opposite held true for Fe at site A (Table 1), which was consistent with the result of Singhal et al (2006). They suggested that such behavior of Fe and Mn might be anticipated, as Mn ions generally occur as free cations and inorganic ion pairs and organic complexes have relatively low stability constants, while Fe precipitates and flocculates as colloidal Fe(III) hydroxide in well-oxygenated waters (Singhal et al, 2006).…”
Section: Group 2: Inorganic Colloidal Pool-borne Metals Mn and Fesupporting
confidence: 80%
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“…Based on the concentrations reported for the three colloidal fractions (i.e., 1-10 kDa, 10-100 kDa and 100 kDa to 0.22 lm), Mn and Fe concentrations were constant at all sites except sites F and A. Mn concentrations tended to increase with decreasing size fraction at site F, while the opposite held true for Fe at site A (Table 1), which was consistent with the result of Singhal et al (2006). They suggested that such behavior of Fe and Mn might be anticipated, as Mn ions generally occur as free cations and inorganic ion pairs and organic complexes have relatively low stability constants, while Fe precipitates and flocculates as colloidal Fe(III) hydroxide in well-oxygenated waters (Singhal et al, 2006).…”
Section: Group 2: Inorganic Colloidal Pool-borne Metals Mn and Fesupporting
confidence: 80%
“…They suggested that such behavior of Fe and Mn might be anticipated, as Mn ions generally occur as free cations and inorganic ion pairs and organic complexes have relatively low stability constants, while Fe precipitates and flocculates as colloidal Fe(III) hydroxide in well-oxygenated waters (Singhal et al, 2006). Consequently, it is not difficult to explain the reason for the much lower percentages of Fe in colloidal size classes 10-100 kDa and 100 kDa to 0.22 lm in poor-oxygenated waters of F (DO: 0.23 mg L À1 , Fig.…”
Section: Group 2: Inorganic Colloidal Pool-borne Metals Mn and Fementioning
confidence: 99%
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“…3. Comparison of Cu distribution over the colloidal size spectrum between the Penzé estuary (this study) and that found by Ingri et al (2004) and Singhal et al (2006) in the Ekhagen estuary (Sweden) and the Mumbai Bay (India), respectively. The Cu concentrations in each size fraction are normalized to a size range of 1 nm.…”
Section: Spring Cu Additions In the Lower Part Of The Systemmentioning
confidence: 96%