TY - JOUR
T1 - Microstructural behavior of γ-Fe2O3 formation in reactions between layered iron oxychloride and sodium n-pentoxide
AU - Shiono, Takeshi
AU - Tando, Fumiaki
AU - Nakano, Hiromi
AU - Sugahara, Yoshiyuki
N1 - Funding Information:
This work was financially supported in part by the Global COE Program “Center for Practical Chemical Wisdom” from the Ministry of Education, Culture, Sports, Science and Technology (MEXT), Japan . The authors thank Ms. Machi Ito for her assistance.
PY - 2013
Y1 - 2013
N2 - Microstructural behavior of γ-Fe2O3 formation in reactions between FeOCl and n-C5H11ONa was thoroughly investigated. Reactions were conducted at 50-150 °C for 3 days in an autoclave using n-C5H11OH as a solvent. X-ray diffraction (XRD) patterns and infrared (IR) spectra of the products suggested the crystallization of γ-Fe2O3 besides the formation of n-pentoxy derivatives of FeOCl. Scanning electron microscopic observation revealed that the FeOCl particles were divided into thin sheets upon reaction. The selected area electron diffractions (SAED) of the sheets revealed the crystallization of γ-Fe2O3 at even 80 °C, apparently due to the fact that the γ-Fe2O3 crystallization process involved a collapse from n-pentoxide derivatives with large separations between two adjacent layers. In the reaction at 150 °C, a part of the sheets was converted into highly oriented polycrystalline γ-Fe2O3 in improved crystallinity, and the SAED clearly showed that an oriented transformation with a crystallographic relationship of FeOCl (010)//γ-Fe2O3 (110) occurred. The reaction at 120 °C, on the contrary, led to the formation of randomly oriented γ-Fe2O3 crystallites within a sheet.
AB - Microstructural behavior of γ-Fe2O3 formation in reactions between FeOCl and n-C5H11ONa was thoroughly investigated. Reactions were conducted at 50-150 °C for 3 days in an autoclave using n-C5H11OH as a solvent. X-ray diffraction (XRD) patterns and infrared (IR) spectra of the products suggested the crystallization of γ-Fe2O3 besides the formation of n-pentoxy derivatives of FeOCl. Scanning electron microscopic observation revealed that the FeOCl particles were divided into thin sheets upon reaction. The selected area electron diffractions (SAED) of the sheets revealed the crystallization of γ-Fe2O3 at even 80 °C, apparently due to the fact that the γ-Fe2O3 crystallization process involved a collapse from n-pentoxide derivatives with large separations between two adjacent layers. In the reaction at 150 °C, a part of the sheets was converted into highly oriented polycrystalline γ-Fe2O3 in improved crystallinity, and the SAED clearly showed that an oriented transformation with a crystallographic relationship of FeOCl (010)//γ-Fe2O3 (110) occurred. The reaction at 120 °C, on the contrary, led to the formation of randomly oriented γ-Fe2O3 crystallites within a sheet.
KW - FeOCl
KW - Organic derivatization
KW - Transmission electron microscope
KW - γ-FeO
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U2 - 10.1016/j.solidstatesciences.2012.12.021
DO - 10.1016/j.solidstatesciences.2012.12.021
M3 - Article
AN - SCOPUS:84875453865
SN - 1293-2558
VL - 19
SP - 156
EP - 161
JO - Solid State Sciences
JF - Solid State Sciences
ER -