2020
DOI: 10.1016/j.apgeochem.2019.104460
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Fe(III) uptake by calcium silicate hydrates

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Cited by 38 publications
(33 citation statements)
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“…The K d values of ≈ 600 m 3 /kg for Al in the absence of alkali are comparable to the K d values of ≈ 700 m 3 /kg for Fe(III) on C–S–H reported in [ 76 ]. However, they are considerably higher than the K d values in the range of 0.1 m 3 /kg to 6 m 3 /kg observed for bivalent cations such as Fe(II), Ba(II) or Sr(II) [ 78 80 ].…”
Section: Resultssupporting
confidence: 86%
See 1 more Smart Citation
“…The K d values of ≈ 600 m 3 /kg for Al in the absence of alkali are comparable to the K d values of ≈ 700 m 3 /kg for Fe(III) on C–S–H reported in [ 76 ]. However, they are considerably higher than the K d values in the range of 0.1 m 3 /kg to 6 m 3 /kg observed for bivalent cations such as Fe(II), Ba(II) or Sr(II) [ 78 80 ].…”
Section: Resultssupporting
confidence: 86%
“…The decrease of Al uptake by C-S–H with increasing the pH value (Fig. 11 ) is comparable to the decrease of Fe(III) uptake by titanium dioxide (TiO 2 ) with increasing the pH value [ 76 ], which is present mainly as negatively charged hydroxide complex (Fe(OH) 4 − ) at pH values above 10. The aqueous aluminum speciation depends on pH; negatively charged Al(OH) 4 − dominates at pH > 7 as explained in [ 35 , 77 ].…”
Section: Resultsmentioning
confidence: 52%
“…In these experiments, the precipitation of Fe(OH) 3 (s) is commonly observed in addition to Fe(III)-containing hydrate phases, such as hydrogarnet 1 [36] and carbonate containing AFm phases [37,38]. This observation underlines that the sparingly soluble Fe(OH) 3 (s) marks the upper solubility limit for Fe(III) in cementitious systems [46,47].…”
Section: Review Of Empirical Data On Iron Phases In Cementitious Systemsmentioning
confidence: 77%
“…It can also exist as ferrihydrite (Fe(OH) 3 (s)) during the first hours of hydration or bind to siliceous hydrogarnet (C 3 (A,F)S y H 6− 2y and C 3 FS y H 6− 2y ) at longer hydration times [42]. In addition, some Fe(III) might also be present in the form of Fe-hydrotalcite (M 3 F 0.5 c 0.5 H 6 ), partially replace Al(III) in ettringite (Ca 6 [Al 1− x Fe x (OH) 6 ] 2 (SO 4 ) 3 ⋅26H 2 O) and/or monosulfate (Ca 4 [Al 1− x Fe x (OH) 6 ] 2 (SO 4 )⋅6H 2 O), or be taken up both by C-S-H in the form of Fe(II) or Fe(III) [32,36,37,42,47,79,80]. The ferrihydrite formation during the first hours of hydration [42] indicates the importance of 2-line ferrihydrite (2l-Fe(OH) 3 (s)) as a solubility limiting iron bearing phase in accordance with a maximum aqueous iron concentration at early hydration times [35,39,40,42,81].…”
Section: Iron-bearing Cementitious Phasesmentioning
confidence: 99%
“…Due to this large amount found in the waste, some works are reported in literature trying to recover iron from the bauxite residue [26], [27], but the process is not yet economically viable, and the remaining waste (with a low amount of iron) is still discarded. Other works are purposed to understand the mechanisms of iron interaction with cementitious materials for predicting the service life and design of reinforced concrete structures [28].…”
Section: Materials Characterizationmentioning
confidence: 99%