Highly ordered Ge-incorporated akaganeite (β-FeOOH): a tunnel-type nanorod
A highly ordered Ge-incorporated akaganeite with the atomic ratio of Ge/Fe = 0.14 and Cl/Fe = 0.11 was firstly synthesized through hydrolysis and acidification of a mixed solution of FeCl 3 ·6H 2 O and TEOGe (Ge(OC 2 H 5 ) 4 ) under the α-Fe 2 O 3 synthesis conditions. The newly synthesized Ge-akaga...
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Veröffentlicht in: | CrystEngComm 2011-01, Vol.13 (1), p.287-292 |
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Sprache: | eng |
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Zusammenfassung: | A highly ordered Ge-incorporated akaganeite with the atomic ratio of Ge/Fe = 0.14 and Cl/Fe = 0.11 was firstly synthesized through hydrolysis and acidification of a mixed solution of FeCl
3
·6H
2
O and TEOGe (Ge(OC
2
H
5
)
4
) under the α-Fe
2
O
3
synthesis conditions. The newly synthesized Ge-akaganeite shows a monodisperse nanorod with 15-17 nm in width and ∼200 nm in length, the distinctly enhanced structural ordering and stability, and substantial differences in crystallographic and magnetic features. Here we propose a hypothetical akaganeite model with Ge occupying the tunnel sites as Ge(OH)
4
0
based on crystallographic and chemical analyses.
A highly ordered Ge-incorporated akaganeite was first synthesized through hydrolysis and acidification of a mixed solution of FeCl
3
·6H
2
O and TEOGe (Ge(OC
2
H
5
)
4
) under the α-Fe
2
O
3
synthesis conditions. The newly synthesized Ge-akaganeite shows a monodisperse nanorod with 15-17 nm in width and ∼200 nm in length, and distinctly enhanced structural ordering and stability. |
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ISSN: | 1466-8033 1466-8033 |
DOI: | 10.1039/c0ce00276c |