2008
DOI: 10.1016/j.corsci.2007.11.029
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Formation of the Fe(II–III) hydroxysulphate green rust during marine corrosion of steel associated to molecular detection of dissimilatory sulphite-reductase

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Cited by 120 publications
(97 citation statements)
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“…5). It was reported that GRs can be oxidized by dissolved O 2 into Fe 3 O 4 , a-FeOOH, g-FeOOH or g-Fe 2 O 3 depending on pH and oxidation rate (Erbs, 2004;Pineau et al, 2008). Under the condition of this investigation, the dissolved O 2 concentration in the pipe loops was considered relatively higher than that in actual DWDS condition because oxygen could continuously dissolved into the experimental loops through the feed water tank.…”
Section: Scale Crystalline Composition Transformationmentioning
confidence: 98%
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“…5). It was reported that GRs can be oxidized by dissolved O 2 into Fe 3 O 4 , a-FeOOH, g-FeOOH or g-Fe 2 O 3 depending on pH and oxidation rate (Erbs, 2004;Pineau et al, 2008). Under the condition of this investigation, the dissolved O 2 concentration in the pipe loops was considered relatively higher than that in actual DWDS condition because oxygen could continuously dissolved into the experimental loops through the feed water tank.…”
Section: Scale Crystalline Composition Transformationmentioning
confidence: 98%
“…The higher solubility of Fe(II) oxides led to more iron released into bulk water and consequently caused the formation of red water (Lytle et al, 2005). In addition, SRB proliferation favored sulfide production and hindered the formation of Fe 3 O 4 , thus promoted iron corrosion and iron release (Lytle et al, 2005;Pineau et al, 2008). The presence of SRB is often characterized by the presence of S 0 and Fe x S y minerals, e.g.…”
Section: 4mentioning
confidence: 99%
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