1978
DOI: 10.1016/0022-1902(78)80515-6
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The influence of chloride ions on the formation of iron(III) oxyhydroxide

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Cited by 55 publications
(48 citation statements)
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“…Even when this is accounted for, effects of other common constituents of natural waters are usually not. For example, chloride, nitrate, sulphate, silicate and phosphate anions can participate in the Fe(III) precipitation process (Dousma et al, 1978(Dousma et al, , 1979Rose et al, 1996Rose et al, , 1997aSchwertmann et al, 1999;Doelsch et al, 2003), a fact that may also contribute to the sub-optimal fit of solubility models to data.…”
Section: Glossary Of Symbols and Abbreviationsmentioning
confidence: 98%
“…Even when this is accounted for, effects of other common constituents of natural waters are usually not. For example, chloride, nitrate, sulphate, silicate and phosphate anions can participate in the Fe(III) precipitation process (Dousma et al, 1978(Dousma et al, , 1979Rose et al, 1996Rose et al, , 1997aSchwertmann et al, 1999;Doelsch et al, 2003), a fact that may also contribute to the sub-optimal fit of solubility models to data.…”
Section: Glossary Of Symbols and Abbreviationsmentioning
confidence: 98%
“…The pH evolution of hydrolyzed Fe(III) solutions was studied by numerous researchers [2,6,7,9,[11][12][13][14][15][16] and was observed to decrease with time. Tang and Stumm [2] indicated that an induction period was observed for B = 0.2-0.5 before pH decrease (relaxation).…”
Section: Studies Of Titration Curvesmentioning
confidence: 99%
“…Many researchers have used turbidity (light scattering) or light absorption to observe the change of aging PICl solutions [6,7,[9][10][11]. Fresh FeCl 3 is yellowish orange with a turbidity of 4-7 NTU.…”
Section: Evolution Of Turbiditymentioning
confidence: 99%
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