Mössbauer Effect Data Index 1978
DOI: 10.1007/978-1-4757-5903-7_3
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Tables for Mössbauer Spectroscopy

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Cited by 14 publications
(15 citation statements)
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“…The presence of γ-Fe 2 O 3 was eliminated because of its thermal instability. As for Fe 3 O 4 , its Mössbauer spectrum at ambient temperature includes two sextets with an isomer shift of δ ≈ 0.27 and 0.67 mm s -1 and different hyperfine fields of ∼490 and ∼460 kG . As no sextet with δ ≈ 0.67 mm s -1 and H ≈ 460 kG (Fe 2+ ) has been observed, we can eliminate the presence of Fe 3 O 4 .…”
Section: Resultsmentioning
confidence: 86%
“…The presence of γ-Fe 2 O 3 was eliminated because of its thermal instability. As for Fe 3 O 4 , its Mössbauer spectrum at ambient temperature includes two sextets with an isomer shift of δ ≈ 0.27 and 0.67 mm s -1 and different hyperfine fields of ∼490 and ∼460 kG . As no sextet with δ ≈ 0.67 mm s -1 and H ≈ 460 kG (Fe 2+ ) has been observed, we can eliminate the presence of Fe 3 O 4 .…”
Section: Resultsmentioning
confidence: 86%
“…The small component observed at 3.7 mm.s -I in sample A (9 Li) corresponds to Sn n in a sulfide environment [11], and shows that a very small portion of tin has not been totally reduced into Sn ~ at this stage of the lithium insertion. Both components observed between 2.0 and 2.3 mm.s -1 in spectra A, B, C can be attributed to Sn ~ i.e.…”
Section: Resultsmentioning
confidence: 88%
“…15 The spectrum of the sample reduced in the field of 60 Oe is shown in Fig. 5a where two more sextets are visible, the parameters of which (the hyperfine magnetic fields 4884 and 4569 kOe) characterize the magnetite 16 remaining due to incomplete reduction. Besides there is a small doublet component (2%) corresponding to wustite.…”
Section: Resultsmentioning
confidence: 99%