2018
DOI: 10.1016/j.chemgeo.2018.05.044
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Effect of Zn coprecipitation on the structure of layered Mn oxides

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Cited by 23 publications
(37 citation statements)
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“…Based on previous studies and our recent study [37], when Zn is added during δ-MnO 2 formation, it exists as surface sorbed species, but can introduce significant structural modification. In order to compare the effects of Zn-coprecipitation-induced structural modification on δ-MnO 2 sorptive reactivity, we also conducted parallel experiments where pure δ-MnO 2 with Zn sorption (i.e., Zn-sorbed δ-MnO 2 , with Zn concentrations comparable to the coprecipitation system) were used as the sorbent, with the subsequent addition of Cd 2+ , phosphate, and arsenate as sorbate.…”
Section: Cation and Anion Sorption On Zn-sorbed δ-Mnomentioning
confidence: 91%
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“…Based on previous studies and our recent study [37], when Zn is added during δ-MnO 2 formation, it exists as surface sorbed species, but can introduce significant structural modification. In order to compare the effects of Zn-coprecipitation-induced structural modification on δ-MnO 2 sorptive reactivity, we also conducted parallel experiments where pure δ-MnO 2 with Zn sorption (i.e., Zn-sorbed δ-MnO 2 , with Zn concentrations comparable to the coprecipitation system) were used as the sorbent, with the subsequent addition of Cd 2+ , phosphate, and arsenate as sorbate.…”
Section: Cation and Anion Sorption On Zn-sorbed δ-Mnomentioning
confidence: 91%
“…When Zn 2+ was added during the formation of biogenic MnO x , it was found to interrupt the mineral layer stacking [36]. Our recent study showed that the presence of Zn 2+ during abiotic δ-MnO 2 formation has more significant impacts on δ-MnO 2 structure compared to Zn sorption on pure δ-MnO 2 [37]. These studies demonstrate the significant effects of Zn 2+ treatment (either sorption or coprecipitation) on δ-MnO 2 structure, which can potentially affect the sorptive reactivity of δ-MnO 2 .…”
Section: Introductionmentioning
confidence: 98%
“…These spectral differences were previously interpreted from the different AOS of Mn and the disparate symmetry of MnO 6 layers in the crystalline structures of δ-MnO 2 and triclinic birnessite. 8,28,29 The δ-MnO 2 phase has a hexagonal MnO 6 symmetry with a certain amount of vacant sites as well as an extremely low content and low ordering of Mn(III). 28,29 Triclinic birnessite possesses an orthogonal MnO 6 symmetry with no vacant sites as well as a relatively high content (∼33%) and high ordering of Mn(III).…”
Section: Acs Earth and Space Chemistrymentioning
confidence: 99%
“…8,28,29 The δ-MnO 2 phase has a hexagonal MnO 6 symmetry with a certain amount of vacant sites as well as an extremely low content and low ordering of Mn(III). 28,29 Triclinic birnessite possesses an orthogonal MnO 6 symmetry with no vacant sites as well as a relatively high content (∼33%) and high ordering of Mn(III). 30 Under such circumstances, the enrichment and ordering of Mn(III) in triclinic birnessite lead to the peak splitting, broadening, and shifting in the k 3 χ(k) spectrum.…”
Section: Acs Earth and Space Chemistrymentioning
confidence: 99%
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