scholarly journals Surface charge and growth of sulphate and carbonate green rust in aqueous media

2013 ◽  
Vol 108 ◽  
pp. 141-153 ◽  
Author(s):  
Romain Guilbaud ◽  
Maggie L. White ◽  
Simon W. Poulton
1964 ◽  
Vol 47 (10) ◽  
pp. 516-520 ◽  
Author(s):  
McDONALD ROBINSON ◽  
J. A. PASK ◽  
D. W. FUERSTENAU
Keyword(s):  

2016 ◽  
Vol 17 (4) ◽  
pp. 1404-1413 ◽  
Author(s):  
Justin O. Zoppe ◽  
Xingyu Xu ◽  
Cindy Känel ◽  
Paola Orsolini ◽  
Gilberto Siqueira ◽  
...  

2015 ◽  
Vol 3 (5) ◽  
pp. 2120-2127 ◽  
Author(s):  
Fangyuan Gai ◽  
Tianlei Zhou ◽  
Yunling Liu ◽  
Qisheng Huo

This work demonstrates that a series of electron transfer-based fluorescent chemosensors have been designed by using surface negatively charged silica cross-linked micellar nanoparticles as scaffolds to encapsulate FTA for improving the quantitative Fe3+ sensing ability in aqueous media.


Materials ◽  
2020 ◽  
Vol 13 (17) ◽  
pp. 3777
Author(s):  
Amira Doggaz ◽  
Romain Coustel ◽  
Pierrick Durand ◽  
François Humbert ◽  
Christian Ruby

Iron and manganese are ubiquitous in the natural environment. FeII-FeIII layered double hydroxide, commonly called green rust (GR), and MnIII-MnIV birnessite (Bir) are also well known to be reactive solid compounds. Therefore, studying the chemical interactions between Fe and Mn species could contribute to understanding the interactions between their respective biogeochemical cycles. Moreover, ferromanganese solid compounds are potentially interesting materials for water treatment. Here, a {Fe(OH)2, FeIIaq} mixture was oxidized by Bir in sulphated aqueous media in the presence or absence of dissolved O2. In oxic conditions for an initial FeII/OH− ratio of 0.6, a single GR phase was obtained in a first step; the oxidation kinetics being faster than without Bir. In a second step, GR was oxidised into various final products, mainly in a spinel structure. A partial substitution of Fe by Mn species was suspected in both GR and the spinel. In anoxic condition, GR was also observed but other by-products were concomitantly formed. All the oxidation products were characterized by XRD, XPS, and Mössbauer spectroscopy. Hence, oxidation of FeII species by Bir can be considered as a new chemical pathway for producing ferromanganese spinels. Furthermore, these results suggest that Bir may participate in the formation of GR minerals.


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