2002
DOI: 10.1007/s002690100200
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Crystal orbital contributions to the pyrrhotite valence band with XPS evidence for weak Fe-Fe ? bond formation

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Cited by 16 publications
(8 citation statements)
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“…Recently Nesbitt et al (2002) investigated the valence band structure of hexagonal pyrrhotite (Fe 10 S 11 ) using synchrotron radiation XPS (SXPS) and demonstrated the existence of Fe 3d peak contributions in the upper valence band consistent with the model of Tossell (1977). They also suggested that, due to the similarity of their structure, these contributions should be evident in monoclinic pyrrhotite (Fe 7 S 8 ) and troilite (FeS).…”
Section: Introductionmentioning
confidence: 87%
“…Recently Nesbitt et al (2002) investigated the valence band structure of hexagonal pyrrhotite (Fe 10 S 11 ) using synchrotron radiation XPS (SXPS) and demonstrated the existence of Fe 3d peak contributions in the upper valence band consistent with the model of Tossell (1977). They also suggested that, due to the similarity of their structure, these contributions should be evident in monoclinic pyrrhotite (Fe 7 S 8 ) and troilite (FeS).…”
Section: Introductionmentioning
confidence: 87%
“…For Fe 2+ in the [FeS 6 ] octahedra with a 3d 6 electron configuration, the energy levels are split into two e g and three t 2g orbitals [15,16]. It is assumed that the overlap between the t 2g orbitals of the interlayer Fe-Fe bonds causes the spin-orbital coupling (SOC), which is responsible for a strong anisotropy with the hard axis in the c-direction and the spin rotation out of the c-plane at T < 200 K [17][18][19]. According to Goodenough [20], the critical value of an Fe-Fe bond length for the overlap of d electrons in NiAs-type monosulfides is 3.0 Å.…”
Section: Introductionmentioning
confidence: 99%
“…The much stronger peak intensity of Fe 2+ to that of Fe 3+ suggested a larger portion of Fe 2+ in Fe 1– x S. Generally, the valence of Fe was supposed to exhibit the single bivalence to balance the valance of S 2– in stoichiometric FeS. However, the previous reports showed that though the molar ratio of Fe/S was near-stoichiometric in FeS, the defects were still present in the phase at ambient temperature because of the entropic considerations . Moreover, Goodenough pointed out that a very limited deficiency of iron (Fe 1– x S, 0 < x < 0.055) is possible for FeS (troilite) .…”
Section: Resultsmentioning
confidence: 99%
“…However, the previous reports showed that though the molar ratio of Fe/S was near-stoichiometric in FeS, the defects were still present in the phase at ambient temperature because of the entropic considerations. 61 Moreover, Goodenough pointed out that a very limited deficiency of iron (Fe 1−x S, 0 < x < 0.055) is possible for FeS (troilite). 21 Thus, a certain amount of Fe vacancies was supposed to be formed in Fe 1−x S, as the Fe valence has partially varied from +2 to +3.…”
Section: Resultsmentioning
confidence: 99%