IGGCAS OpenIR  > 岩石圈演化国家重点实验室
A new model for transformation of ferrihydrite to hematite in soils and sediments
Jiang, Zhaoxia1,2,3; Liu, Qingsong3,4; Roberts, Andrew P.5; Barron, Vidal6; Torrents, Jose6; Zhang, Qiang7
2018-11-01
Source PublicationGEOLOGY
ISSN0091-7613
Volume46Issue:11Pages:987-990
AbstractFerrihydrite is among the most common precursors for iron-oxide formation in soils and sediments. Previous studies proposed a three-stage process for ferrihydrite transformation to hematite via an intermediate ferrimagnetic phase, which provides the basis for interpreting iron-oxide formation and its paleoenvironmental significance. From our new results, we identified two extra stages in this transformation, which fundamentally change the conventional model. The revised five-stage model is: (I) magnetically ordered (or core-shell structured) superparamagnetic (SP) ferrihydrite formation, (II) rapid hematite formation from SP ferrihydrite, (III) relative hematite stabilization, (IV) maghemite nanoparticle neoformation, and (V) completion of the transformation from maghemite to hematite. Unlike the previous model, in which pedogenic maghemite and hematite were formed mainly in stages I and II, we conclude that they are formed dominantly in stages IV and V, respectively. Thus, our work provides a new framework for interpreting pedogenic iron oxides and their paleoclimatic implications in natural environments.
DOI10.1130/G45386.1
Funding OrganizationNational Key Research and Development Program of China ; National Key Research and Development Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Australian Research Council ; Australian Research Council ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Australian Research Council ; Australian Research Council ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Australian Research Council ; Australian Research Council ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Australian Research Council ; Australian Research Council
WOS KeywordMAGNETIC ENHANCEMENT ; 2-LINE FERRIHYDRITE ; IRON OXYHYDROXIDE ; CHINESE LOESS ; SUSCEPTIBILITY ; PALEOPRECIPITATION ; AGGREGATION ; MAGHEMITE ; OXIDES ; FE2O3
Language英语
Funding ProjectNational Key Research and Development Program of China[2016YFA0601903] ; National Natural Science Foundation of China[41504055] ; National Natural Science Foundation of China[41430962] ; Australian Research Council[DP110105419] ; Australian Research Council[DP120103952]
Funding OrganizationNational Key Research and Development Program of China ; National Key Research and Development Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Australian Research Council ; Australian Research Council ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Australian Research Council ; Australian Research Council ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Australian Research Council ; Australian Research Council ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Australian Research Council ; Australian Research Council
WOS Research AreaGeology
WOS SubjectGeology
WOS IDWOS:000449047800015
PublisherGEOLOGICAL SOC AMER, INC
Citation statistics
Document Type期刊论文
Identifierhttp://ir.iggcas.ac.cn/handle/132A11/89159
Collection岩石圈演化国家重点实验室
Corresponding AuthorLiu, Qingsong
Affiliation1.Ocean Univ China, Minist Educ, Key Lab Submarine Geosci & Prospecting Tech, Qingdao 266100, Peoples R China
2.Ocean Univ China, Coll Marine Geosci, Qingdao 266100, Peoples R China
3.Qingdao Natl Oceanog Lab Marine Sci & Technol, Lab Marine Geol, Qingdao 266237, Peoples R China
4.Southern Univ Sci & Technol, Shenzhen 518055, Peoples R China
5.Australian Natl Univ, Res Sch Earth Sci, Canberra, ACT 2601, Australia
6.Univ Cordoba, Dept Agron, Edificio C4,Campus Rabanales, E-14071 Cordoba, Spain
7.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
Recommended Citation
GB/T 7714
Jiang, Zhaoxia,Liu, Qingsong,Roberts, Andrew P.,et al. A new model for transformation of ferrihydrite to hematite in soils and sediments[J]. GEOLOGY,2018,46(11):987-990.
APA Jiang, Zhaoxia,Liu, Qingsong,Roberts, Andrew P.,Barron, Vidal,Torrents, Jose,&Zhang, Qiang.(2018).A new model for transformation of ferrihydrite to hematite in soils and sediments.GEOLOGY,46(11),987-990.
MLA Jiang, Zhaoxia,et al."A new model for transformation of ferrihydrite to hematite in soils and sediments".GEOLOGY 46.11(2018):987-990.
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