Citation: Liu Chengshuai, Li Fangbai, Chen Manjia, Liao Changzhong, Tong Hui, Hua Jian. Adsorption and Stabilization of Lead during Fe(Ⅱ)-catalyzed Phase Transformation of Ferrihydrite[J]. Acta Chimica Sinica, ;2017, 75(6): 621-628. doi: 10.6023/A17030093 shu

Adsorption and Stabilization of Lead during Fe(Ⅱ)-catalyzed Phase Transformation of Ferrihydrite

Liu Chengshuai ^a,b ,
Li Fangbai ^a,*,, ,
Chen Manjia ^a ,
Liao Changzhong ^a ,
Tong Hui ^b ,
Hua Jian ^a

a.
Guangdong Key Laboratory of Integrated Agro-Environmental Pollution Control and Management, Guangdong Institute of Eco-Environmental Science & Technology, Guangzhou 510650, China
b.
State Key Laboratory of Environmental Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550081, China

Corresponding author: Li Fangbai, cefbli@soil.gd.cn
Received Date: 6 March 2017

Fund Project: the Science and Technology Project of Guangdong Province S2013050014266the National Natural Science Foundation of China 41420104007the Science and Technology Project of Guangdong Province 2015A030313752the National Natural Science Foundation of China 41671240the National Natural Science Foundation of China 41673135the Science and Technology Project of Guangdong Province 2016B020242006the Science and Technology Project of Guangdong Province 2016A030313780

Figures(8)

Aqueous Fe(Ⅱ) (Fe(Ⅱ)_aq)-catalyzed recrystallization of iron (hydr)oxides is the important chemical reaction of iron cycle in anaerobic environments, which poses significant effects on the environmental behavior of heavy metals in soils and sediments. Ferrihydrite is the initial iron mineral phase during the ferrous mineralization and has relatively unstable crystal structure. The structure transformation behavior of ferrihydrite is active and also poses important effects on environmental behavior of soil heavy metals. However, the Fe(Ⅱ)_aq-catalyzed phase transformation of ferrihydrite has been rarely reported, especially with the coexisting metal ions. In the present study, the effects of coexisting heavy metal of Pb(Ⅱ) on the Fe(Ⅱ)_aq-catalyzed phase transformation of ferrihydrite coupling the environmental behavior of Pb(Ⅱ) were systematically studied. The results show that ferrihydrite underwent efficient phase transformation rates when catalyzed by Fe(Ⅱ)_aq whenever with or without the effect of Pb(Ⅱ). Compared with the reaction system that without Pb(Ⅱ), the adsorption of Fe(Ⅱ) on the surface of ferrihydrite was inhibited due to the competition of Pb(Ⅱ) when with the coexistence of Pb(Ⅱ), which further decreased the rates of Fe atom exchange between Fe(Ⅱ)_aq and structural Fe(Ⅲ) of ferrihydrite. With the inhibited Fe atom exchange reaction, the phase transformation rates were relatively decreased and transformation products were changed during the Fe(Ⅱ)_aq-catalyzed phase transformation of ferrihydrite. Goethite and magnetite were found to be the final transformed products of iron (hydr)oxides when without Pb(Ⅱ), while lepidocrocite was determined to be the main transformed product with little goethite and magnetite as the other transformed products when with Pb(Ⅱ). During the Fe(Ⅱ)_aq-catalyzed phase transformation of ferrihydrite with the coexistence of Pb(Ⅱ), some Pb were stabilized through being incorporated into the structure of ferrihydrite transformed products with the possible mechanisms of occlusion by the crystal lattice and structural incorporation, so as to decrease the activity of the polluted heavy metal of Pb. The obtained results in the present study are expected to provide further insights for understanding the iron cycle coupling with the environmental behavior of heavy metals in soils and sediments.
- iron oxide,
- Fe atom exchange,
- heavy metal,
- stable isotope tracing,
- isomorphous replacement
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