2018
DOI: 10.1016/j.chemgeo.2018.05.031
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Effect of Zn(II) coprecipitation on Mn(II)-induced reductive transformation of birnessite

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Cited by 17 publications
(3 citation statements)
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“…Feitknechtite has been synthesized in the reaction of nanocrystalline vernadite (δ-MnO 2 ) with aqueous solutions containing Mn 2+ cations, at a pH below 9 [41]. It was shown [37] that in the presence of Mn 2+ cations, transformation of a birnessite-type MnO 2 compound into manganite (Mng) proceeds via the intermediate unstable feitknechtite (Ftk) phase in accordance with the scheme Mn 2+ (aq) + MnO 2 + 2H 2 O → 2Ftk + 2H + (aq); Ftk → Mng. The formation of the intermediate feitknechtite phase was faster for Zncoprecipitated birnessite than for pure birnessite.…”
Section: Discussionmentioning
confidence: 99%
See 1 more Smart Citation
“…Feitknechtite has been synthesized in the reaction of nanocrystalline vernadite (δ-MnO 2 ) with aqueous solutions containing Mn 2+ cations, at a pH below 9 [41]. It was shown [37] that in the presence of Mn 2+ cations, transformation of a birnessite-type MnO 2 compound into manganite (Mng) proceeds via the intermediate unstable feitknechtite (Ftk) phase in accordance with the scheme Mn 2+ (aq) + MnO 2 + 2H 2 O → 2Ftk + 2H + (aq); Ftk → Mng. The formation of the intermediate feitknechtite phase was faster for Zncoprecipitated birnessite than for pure birnessite.…”
Section: Discussionmentioning
confidence: 99%
“…The broad absorption bands at 2010 and 2600 cm −1 correspond to stretching vibrations of OH groups forming strong hydrogen bonds. The distinct narrow bands at 1085, 1114, and 1150 cm −1 are due to Mn 3+ •••O-H bending vibrations and are considered to be characteristic bands of manganite [37]. The absorptions in the range of 400-600 cm −1 correspond to Mn 3+ -O stretching modes, and the shoulder at 950 is an overtone or a Mn 3+ -O stretching combination mode.…”
Section: Manganitementioning
confidence: 99%
“…For instance, reproducing todorokite under low temperatures and neutral environmental conditions in the lab is difficult. The current methods for synthesizing todorokite from layered Mn oxides typically require conditions that significantly differ from those in nature, such as elevated pH levels [ 18 , 105 , 255 , 256 ]. The aforementioned observation outcome exhibits a notable disparity from the prevailing occurrence of todorokite in naturally occurring low-temperature settings [ 18 ].…”
Section: Factors Affecting the Sorption And Oxidation Of Metals On Mn...mentioning
confidence: 99%