2013
DOI: 10.1063/1.4799153
|View full text |Cite
|
Sign up to set email alerts
|

Mössbauer analysis of silicate Li2FeSiO4 and delithiated Li2−xFeSiO4 (x = 0.66) compounds

Abstract: Lithium iron silicate compounds of Li2FeSiO4 and partially delithiated Li2−xFeSiO4 (x = 0.66) were synthesized by vacuum-sealed solid-state and chemical delithiation reactions, and their magnetic properties were characterized based on Mössbauer analysis. Crystal structures of both Li2FeSiO4 and Li2−xFeSiO4 (x = 0.66) compounds are found to be γs-type (P21/n) monoclinic structures with difference in the lattice parameters due to lithium delithiation. Mössbauer spectrum of Li2FeSiO4 below TN1 = 20 K exhibits eig… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
3
2

Citation Types

3
7
0

Year Published

2013
2013
2024
2024

Publication Types

Select...
9

Relationship

0
9

Authors

Journals

citations
Cited by 11 publications
(10 citation statements)
references
References 12 publications
3
7
0
Order By: Relevance
“…The presence of ferric Fe is most likely originating from surface oxidation as after etching with the argon ion under 1000 V for 2 min, a standard ferrous Fe XPS signal is only detected (Fe p 2/3 locating at 709.30 eV). This confirms that the ferrous Fe signal comes from the Li 2 FeSiO 4 material itself41. Therefore it is inferred that the as-prepared LFS@400 and LFS@700 samples is covered with thin ferric Fe contained silicates in addition to the N-doped carbon coating layer as identified by the XPS studies.…”
Section: Resultssupporting
confidence: 72%
“…The presence of ferric Fe is most likely originating from surface oxidation as after etching with the argon ion under 1000 V for 2 min, a standard ferrous Fe XPS signal is only detected (Fe p 2/3 locating at 709.30 eV). This confirms that the ferrous Fe signal comes from the Li 2 FeSiO 4 material itself41. Therefore it is inferred that the as-prepared LFS@400 and LFS@700 samples is covered with thin ferric Fe contained silicates in addition to the N-doped carbon coating layer as identified by the XPS studies.…”
Section: Resultssupporting
confidence: 72%
“…Then, a clear correlation cannot be found between polymorphism and magnetic features of Li 2 FeSiO 4 . Rather, the T N value of the lithium iron silicates can be influenced by the coexistence between Fe ions with different oxidation states32. Also the results shown above for the Li-Mn silicates are in agreement with these hypotheses: the small T N shift from 12 K ( i.e.…”
Section: Discussionsupporting
confidence: 75%
“…A higher μ eff value has instead been obtained for Fe-900 (μ eff ≅ 5.15), which could imply, for example, the contribution, in addition to the one of divalent iron ions, from Fe ions with higher oxidation state. Nevertheless, this should not be the case because a T N value of 20 K in this compound is related to magnetic interactions between Fe 2+ spins only, while the coexistence of Fe 2+ and Fe 3+ ions should give rise to AF ordering with a T N value higher than 20 K32. On this basis, an extrinsic contribution can be instead invoked to explain the higher estimated μ eff value for Fe-900, as, for example, the one due to the small amount in the sample of the ferrimagnetic Li 3 Fe 5 O 8 phase not fully saturated in the whole temperature range considered to estimate Curie and Weiss constants.…”
Section: Resultsmentioning
confidence: 95%
“…This value is indeed compatible with the presence of Fe 3+ ions on the Fe 2+ sites. In fact, a T N higher than 20 K for Li 2 FeSiO 4 was already related to a consistent amount of Fe 3+ in the orthosilicate phase by Mössbauer measurements performed at low temperature onto de-lithiated samples41. The authors reported a T N  = 20K for Li 2 FeSiO 4 , containing only Fe 2+ , and a T N  = 28 K for a de-lithiated sample with Li 1.34 Fe 2+ 0.33 Fe 3+ 0.66 SiO 4 composition, suggesting that stronger AF interactions take place when Fe 2+ ions are partially substituted by Fe 3+ ions.…”
Section: Discussionmentioning
confidence: 87%