2018
DOI: 10.1016/j.jmmm.2018.04.044
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Magnetic granulometry and Mössbauer spectroscopy of Fe m O n –SiO 2 colloidal nanoparticles

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Cited by 18 publications
(12 citation statements)
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“…The presence of sextet with IS of 0.61 is unequivocal evidence of Fe +2 coming from magnetite phase. The third sextet (IS of 0.47 mm s −1 , H eff of 460 kOe) suggests the presence of maghemite (γ‐Fe 2 O 3 ), which commonly occurs in magnetite materials due to the natural oxidation of magnetite when exposed to air . Fe 3+ in tetrahedral site is shared between magnetite and maghemite phases.…”
Section: Resultsmentioning
confidence: 99%
“…The presence of sextet with IS of 0.61 is unequivocal evidence of Fe +2 coming from magnetite phase. The third sextet (IS of 0.47 mm s −1 , H eff of 460 kOe) suggests the presence of maghemite (γ‐Fe 2 O 3 ), which commonly occurs in magnetite materials due to the natural oxidation of magnetite when exposed to air . Fe 3+ in tetrahedral site is shared between magnetite and maghemite phases.…”
Section: Resultsmentioning
confidence: 99%
“…The method of magnetic granulometry [168,169], along with other approaches in rock magnetism [88,89,116,165], confirms that the shape and size of bacterial magnetite crystals correspond to a single-domain [170] or pseudo-single-domain [82] (metastable singledomain [167]) state, with the aspect ratio and particle length varying over a wide range, up to one order of magnitude, depending on magnetofossil geography [171], and differs little for cultivated and non-cultivated MTB strains when taking into consideration statistical data [172]. Exceptionally, multi-domain [173] and superparamagnetic [117] magnetite grains originating from magnetofossils have been found in natural conditions.…”
Section: Magnetofossils and Their Propertiesmentioning
confidence: 99%
“…При 1.8 K приобретается довольно большой магнитный момент, который, однако, спадает почти до нуля по мере приближения к комнатной температуре. Ненулевое, хотя и малое, значение магнитного момента при 300 K можно объяснить эффектом взаимодействия между суперпарамагнитными частицами [9]. Излом на кривой RT-SIRM(T) около 240 K может быть проявлением перехода Морина [10,11] в гематите, некоторое количество которого присутствует в образце согласно данным рентгеновской дифрактометрии.…”
Section: результаты и обсуждениеunclassified
“…Теоретические значения остаточной намагниченности насыщения исследуемых образцов были рассчитаны с помощью модифицированного метода моментов для системы диполь-дипольно-взаимодействующих одноосных частиц, как в работах [9,13].…”
Section: результаты и обсуждениеunclassified
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