Correlations between soil geochemical properties and Fe(III) reduction suggest microbial reducibility of iron in different soils from Southern China
Chen, Manjia1; Liu, Chengshuai1; Li, Fangbai1; Zhai, Guangshu2,3; Liu, Hong4; Liu, Chuanping1; Yu, Weimin1
刊名CATENA
2014-12-01
卷号123页码:176-187
关键词Soil iron reduction Weathering index Soil chemical property Soil group Soil parent materials
ISSN号0341-8162
DOI10.1016/j.catena.2014.08.005
通讯作者Liu, CS (reprint author), Guangdong Inst Ecoenvironm & Soil Sci, Guangzhou 510650, Guangdong, Peoples R China.
英文摘要Fe(II) species are a group of active compounds during the soil geochemical processes. Various iron compounds show the different reducibility, solubility and extractability in soil, leading to the greatly different contribution of the iron compounds to Fe(II) concentrations. Therefore, it is very important to study the correlation of the total reducibility of iron and the soil geochemical properties in different soils for evaluating the activities of geochemical reactions. In this study, the Fe(III) reducibilities were investigated in 23 iron-rich soils with the different geochemical properties from Southern China. The results showed that the microbial reducibilities of Fe(III) in different soils with the same iron-reducing bacteria of Shewanella decolorationis S12 varied greatly. The soils derived from the same parent material had the similar microbial iron reduction rates. Furthermore, the soil Fe(III) reducibilities did not correlate well with any of the iron species in the soils except for Fe2O3. However, the soil weathering degree was found to be the most important factor in the microbial reducibilities,of soil iron. All the weathering indices of studied soils were linearly correlated with Fe(III) reduction rate constants. The results illustrated the unique importance of soil geochemical properties on soil Fe(III) reduction susceptibilities and helped define the soil types to exhibit similar degrees of Fe(III) reduction under controlled lab conditions. In conclusion, the geochemical property of soil weathering degree was conducive to identify the iron reducibility and could become a powerful tool for characterizing the iron reducibilities in soils. (C) 2014 Elsevier B.V. All rights reserved.
资助项目National Natural Science Foundations of China[41025003] ; National Natural Science Foundations of China[41301538] ; National Natural Science Foundations of China[41171364] ; Natural Science Foundation of Guangdong Province, China[S2011030002882] ; Natural Science Foundation of Guangdong Province, China[S2013050014266] ; Science and Technology Planning Project of Guangdong Province, China[2012A030700011] ; Science and Technology Planning Project of Guangdong Province, China[2011B030900005]
WOS研究方向Geology ; Agriculture ; Water Resources
语种英语
出版者ELSEVIER SCIENCE BV
WOS记录号WOS:000343358600019
内容类型期刊论文
源URL[http://119.78.100.138/handle/2HOD01W0/1046]  
专题水污染过程与治理研究中心
通讯作者Liu, Chengshuai
作者单位1.Guangdong Inst Ecoenvironm & Soil Sci, Guangdong Key Lab Agr Environm Pollut Integrated, Guangzhou 510650, Guangdong, Peoples R China
2.Univ Iowa, Dept Civil & Environm Engn, Iowa City, IA 52242 USA
3.Univ Iowa, IIHR Hydrosci & Engn, Iowa City, IA 52242 USA
4.Chinese Acad Sci, Chongqing Inst Green & Intelligent Technol, Res Ctr Pollut Proc & Treatment Wastewater, Chongqing 400714, Peoples R China
推荐引用方式
GB/T 7714
Chen, Manjia,Liu, Chengshuai,Li, Fangbai,et al. Correlations between soil geochemical properties and Fe(III) reduction suggest microbial reducibility of iron in different soils from Southern China[J]. CATENA,2014,123:176-187.
APA Chen, Manjia.,Liu, Chengshuai.,Li, Fangbai.,Zhai, Guangshu.,Liu, Hong.,...&Yu, Weimin.(2014).Correlations between soil geochemical properties and Fe(III) reduction suggest microbial reducibility of iron in different soils from Southern China.CATENA,123,176-187.
MLA Chen, Manjia,et al."Correlations between soil geochemical properties and Fe(III) reduction suggest microbial reducibility of iron in different soils from Southern China".CATENA 123(2014):176-187.
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