2015
DOI: 10.1016/j.jssc.2014.10.006
|View full text |Cite
|
Sign up to set email alerts
|

Synthesis, structural and electronic properties of monodispersed self-organized single crystalline nanobricks of isocubanite CuFe2S3

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1
1
1

Citation Types

0
5
0

Year Published

2016
2016
2024
2024

Publication Types

Select...
8

Relationship

0
8

Authors

Journals

citations
Cited by 12 publications
(5 citation statements)
references
References 34 publications
0
5
0
Order By: Relevance
“…Literature data for isocubanite Mößbauer parameters vary. Lyubutin et al 65 showed different models for possible fitting procedures. Due to the small amount of isocubanite in the synthesised samples, parameters for this phase could not be refined freely.…”
Section: Resultsmentioning
confidence: 99%
“…Literature data for isocubanite Mößbauer parameters vary. Lyubutin et al 65 showed different models for possible fitting procedures. Due to the small amount of isocubanite in the synthesised samples, parameters for this phase could not be refined freely.…”
Section: Resultsmentioning
confidence: 99%
“…can be helpful in phase identification. Isomer shift values determined from the Mo ¨ssbauer spectra of the B2 and B3 nanocrystals are very high for Fe(III) and very low for Fe(II), 41 implying an intermediate iron oxidation state, which can be achieved though the fast electron exchange between these two form of iron. 40 Very similar Mo ¨ssbauer parameters were recently reported for nanocrystals of isocubanite (known as non-magnetic but never magnetically tested at very low temperatures).…”
Section: Magnetic Properties and Mossbauer Spectroscopymentioning
confidence: 97%
“…Among the different forms of Cu-Fe-S nanocrystals, one can distinguish antiferromagnetic a-CuFeS 2 (tetragonal), [36][37][38] ferromagnetic b-CuFeS 2 (cubic) 36,39 and non-magnetic (down to 78 K) g-CuFeS 2 (tetragonal) 36 phases of chalcopyrite, ferromagnetic CuFe 2 S 3 (cubanite; orthorhombic) 40 and non-magnetic cubic form of cubanite, namely, isocubanite. 41 The point is how to distinguish between chalcopyrite (and its different phases) and cubanite (and its different phases). The diffraction method fails since, for instance, ferromagnetic chalcopyrite and non-magnetic isocubanite yield essentially the same set of Bragg reflections and only Mo ¨ssbauer spectroscopy can help in distinguishing between these phases.…”
Section: Magnetic Properties and Mossbauer Spectroscopymentioning
confidence: 99%
“…Furthermore, as above discussed, S4 and S5 with more Fe 2+ produced by stronger reduction would accelerate atomic exchange and varied ratio of two valences stated iron ions, resulting in stronger magnetism. Another reason for the producing of magnetization is the presence of Fe–S type of magnetism impurities in the CuFe 2 S 3 crystals [ 42 ]. It has been discussed above, more S 2- produced and reduction of Fe 3+ to Fe 2+ by DT and thiourea, hence, some non-stoichiometric precipitates might be produced and resulted in some Fe–S type of magnetism impurities in S4 and S5.…”
Section: Discussionmentioning
confidence: 99%