2020
DOI: 10.1134/s1063774520030244
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Fe3 – δO4 Nanoparticles Synthesized in the Presence of Natural Polyelectrolytes

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Cited by 21 publications
(15 citation statements)
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“…A decrease of temperature results in an insignificant decrease of the intensity of the broad middle line of the U spectrum, while the intensity of paramagnetic part (asymmetric doublet and broad middle line) of the B spectrum is practically independent of temperature. It can be concluded that asymmetry of the resonance lines of the sextets at room temperature cannot be caused only by superparamagnetism (characteristic for nano-or highly dispersed iron particles) [66], but can be resulted from locally inhomogeneous environment of Fe atoms, at least in one phase present in the samples. On the other hand, the shoulders in the low-temperature spectrum of the U sample and the resonance lines out of the base line indicate superposition of the spectra of at least two magnetically ordered phases, one of which is responsible for distortion of the background line in the middle part of the spectrum at room temperature.…”
Section: Red Mud Samples Characterizationmentioning
confidence: 99%
“…A decrease of temperature results in an insignificant decrease of the intensity of the broad middle line of the U spectrum, while the intensity of paramagnetic part (asymmetric doublet and broad middle line) of the B spectrum is practically independent of temperature. It can be concluded that asymmetry of the resonance lines of the sextets at room temperature cannot be caused only by superparamagnetism (characteristic for nano-or highly dispersed iron particles) [66], but can be resulted from locally inhomogeneous environment of Fe atoms, at least in one phase present in the samples. On the other hand, the shoulders in the low-temperature spectrum of the U sample and the resonance lines out of the base line indicate superposition of the spectra of at least two magnetically ordered phases, one of which is responsible for distortion of the background line in the middle part of the spectrum at room temperature.…”
Section: Red Mud Samples Characterizationmentioning
confidence: 99%
“…Evidently, two other sextets (##3–4, Table 8 ) are related to γ-Fe 2 O 3 [ 76 , 77 , 78 ]. The reduced values of the magnetic splitting for the sextets at room temperature and the high value of the resonance line width with a strong temperature dependence suggest that this is a poorly ordered and very defective phase [ 79 ]. It could be assumed that the group of the sextets ##1–3 also includes the group of copper ferrite sextets with ultrafine parameters close to the indicated oxides—CuFe 2 O 4 [ 80 , 81 , 82 , 83 ] or substituted analogs of copper ferrite Cu 1-x A x Fe 2-y B y O 4 , where A and B are a substituent element in the oxidation state +2 or +3, respectively, for example, Zn +2 [ 84 , 85 , 86 ], Cd +2 [ 85 ], Al +3 [ 87 ], Ga +3 [ 86 ].…”
Section: Resultsmentioning
confidence: 99%
“…A slight decrease in the magnetite content in the samples containing humic acids (Fe 3 O 4 /HA) from ~82.7 % to ~79.2 % ( Table 1 ) can be associated with phenol and quinoid units in the HA structure [ 44 ]. Notably, the Fe 3 O 4 content in the Fe 3 O 4 /HA harsh oxidation sample was almost halved, assumingly due to the oxidation of magnetite NPs during mechanical treatment (harsh oxidation).…”
Section: Resultsmentioning
confidence: 99%