Iron oxyhydroxide polytype (γ-, δ- and β-FeOOH) structures govern Zn mobility
Authors:
- Biyun HuBHBiyun Hu
- Xinran YanXYXinran Yan
- Wentao WangWWWentao Wang
- Yan LiYLYan Li
- Hui LiHLHui Li
- Mei HongMHMei Hong
- Fan LiuFLFan Liu
- Hui YinHYHui Yin
- 14 October 2022
- journal article
- research article
- Published by Elsevier in Chemical Geology
- Vol. 614
Abstract
No abstract availableKeywords
This publication has 55 references indexed in Scilit:
- An in situ quick-EXAFS and redox potential study of the Fe(II)-catalysed transformation of ferrihydriteColloids and Surfaces A: Physicochemical and Engineering Aspects, 2013
- Iron hydroxides in soils: A review of publicationsEurasian Soil Science, 2010
- A comparative study of As(III) and As(V) in aqueous solutions and adsorbed on iron oxy-hydroxides by Raman spectroscopyWater Research, 2010
- Dissolution of Cr, Zn, Cd, and Pb Single- and Multi-Metal-Substituted Goethite: Relationship to Structural, Morphological, and Dehydroxylation PropertiesClays and Clay Minerals, 2010
- Copper substitution alone and in the presence of chromium, zinc, cadmium and lead in goethite (α-FeOOH)Clay Minerals, 2009
- Simultaneous incorporation of Cr, Zn, Cd, and Pb in the goethite structureClays and Clay Minerals, 2009
- Akaganéite-type β-FeO(OH) nanocrystals: preparation and characterizationMicroporous and Mesoporous Materials, 2001
- Acid dissolution of synthetic aluminous goethite before and after transformation to hematite by heatingClay Minerals, 1995
- Transformation of γ-FeO(OH) to Fe 3 O 4 by adsorption of iron( II ) ion on γ-FeO(OH)J. Chem. Soc., Dalton Trans., 1983
- Natural Occurrence of Feroxyhite (δ′-FeOOH)Clays and Clay Minerals, 1980