2007
DOI: 10.1016/j.jallcom.2006.08.208
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The thermal stability of maghemite-silica nanocomposites: An investigation using X-ray diffraction and Raman spectroscopy

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Cited by 50 publications
(45 citation statements)
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“…In the XRD patterns, only a few very broad peaks are recognizable (Figs. 7-9), which is consistent with other works [e.g., 65,68]. The formation of nanomaghemite results in substantial increase in magnetic susceptibility (Fig.…”
Section: Pure Ferrihydritesupporting
confidence: 92%
See 1 more Smart Citation
“…In the XRD patterns, only a few very broad peaks are recognizable (Figs. 7-9), which is consistent with other works [e.g., 65,68]. The formation of nanomaghemite results in substantial increase in magnetic susceptibility (Fig.…”
Section: Pure Ferrihydritesupporting
confidence: 92%
“…600 cm -1 at 850°C. Similar FTIR features were reported for e-Fe 2 O 3 [68]. Therefore, between 800 and 885°C, two Fe 2 O 3 polymorphs (alpha and epsilon) coexist in the sample.…”
Section: Pure Ferrihydritesupporting
confidence: 82%
“…In nature, both hematite and maghemite can be found in minerals as well as in nanoparticle form, but it is generally accepted that a nanoparticle sizedependent transition from maghemite to hematite occurs around 10 nm 43 . Furthermore, the stabilization of maghemite nanoparticles has been observed at maghemite silica-based supports 44 . We believe that the N-rGOx sheets in our study have a similar role in stabilizing the maghemite nanoparticles by providing sufficient and suitable adsorption sites, thus inhibiting their transformation to hematite particles.…”
Section: Resultsmentioning
confidence: 95%
“…A região II, de 145 a 355 °C corresponde à zona de oxidação da matéria carbônica ligada as partículas magnéticas, sejam estas o oxalato (a), o lauril sulfato (b) e a enzima palatase (c). A região III, de 355 a 900 °C corresponde à zona de oxidação de algum carbono residual que não tenha sido oxidado na região II e nesta região a maghemita passa da fase γ-Fe 2 O 3 para α-Fe 2 O 3 (comumente ocorrem as duas fases entre 500 e 700 °C (Sartoratto et al, 2007), ou seja, não ocorre variação de massa, apenas uma mudança na estrutura cristalina do material suporte. Na Tabela 2, encontra-se o percentual de perda de massa ocorrido em cada região referente a cada amostra analisada.…”
Section: Resultsunclassified