1994
DOI: 10.1016/0016-7037(94)90236-4
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The temperature dependence of the solubility product constant of vivianite

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Cited by 105 publications
(59 citation statements)
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“…Estimating the thermodynamic properties of phosphate minerals 115 Wagman et al (1982), (2) Vieillard & Tardy (1984), (3) Wagman (1968), (4) Latimer (1952), (5) Parker et al (1971), (6) Naumov et al (1971), (7) Duff (1971a), (8) Rossini et al (1952), (9) Duff (1972), (10) Robie et al (1979), (11) Duff (1971b), (12) Tacker & Stormer (1989), (13) Al-Borno & Tomson (1994), (14) Woods & Garrels (1987). -3,783.85 -3,781.27 -3,708.57 -3,700.27 -3,633.63 -3,619.27 -3,559.16 -3,538.27 Ca 5 (P0 4 ) [3][4][5][6]928.26 Ca 5 (P0 4 ) 3 0H 763.91 (1) Robie et al (1979); (2) Calculated using values of Table 3.…”
Section: Resultsmentioning
confidence: 99%
“…Estimating the thermodynamic properties of phosphate minerals 115 Wagman et al (1982), (2) Vieillard & Tardy (1984), (3) Wagman (1968), (4) Latimer (1952), (5) Parker et al (1971), (6) Naumov et al (1971), (7) Duff (1971a), (8) Rossini et al (1952), (9) Duff (1972), (10) Robie et al (1979), (11) Duff (1971b), (12) Tacker & Stormer (1989), (13) Al-Borno & Tomson (1994), (14) Woods & Garrels (1987). -3,783.85 -3,781.27 -3,708.57 -3,700.27 -3,633.63 -3,619.27 -3,559.16 -3,538.27 Ca 5 (P0 4 ) [3][4][5][6]928.26 Ca 5 (P0 4 ) 3 0H 763.91 (1) Robie et al (1979); (2) Calculated using values of Table 3.…”
Section: Resultsmentioning
confidence: 99%
“…First, the layer may have been disrupted under single bacteria or biofilm patches as a result of oxygen depletion, possibly enhanced by excretion products. Once small holes in the oxide layer were formed, corrosion of the underlying iron, according to the equation Fe ϩ 1 2 O 2 ϩ H 2 O3Fe(OH) 2 , could have added to the consumption of oxygen (28). The steel surface would now have consisted of two electrochemically different types of areas: a large area without biofilm coverage where E was still high and a smaller area with few biofilmcovered spots where E was already at E min .…”
Section: Discussionmentioning
confidence: 99%
“…In phosphate-rich reducing environments, vivianite (Fe 3 (PO 4 ) 2 Á8H 2 O) is an important sink for dissolved Fe(II) and is considered a stable mineral due to its low solubility at neutral pH (Nriagu and Dell, 1974;Buffle et al, 1989;Manning et al, 1991;Al-Borno and Tomson, 1994;Viollier et al, 1997;Sapota et al, 2006). Under anoxic conditions, vivianite is very stable (K sp = 10 À36 ; (Nriagu, 1972)) and can exert significant control over the geochemical cycles of Fe and P. Vivianite has also been reported as an end product of bacterial Fe(III) reduction Zachara et al, 1998;Roh et al, 2007;Peretyazhko et al, 2010).…”
Section: Introductionmentioning
confidence: 99%