1978
DOI: 10.1007/978-3-662-12545-8
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Mössbauer Spectroscopy and Transition Metal Chemistry

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Cited by 432 publications
(382 citation statements)
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“…The experimental values of the magnetic hyperfine coupling tensors A in 1-270 (Table S1) reflect this approximation, since the A values for the two subspectra have opposite signs, resulting from the spins of the individual ions being parallel and antiparallel to the applied field. The ferric site, with the larger spin, has negative A-tensor components as expected, according to the negative intrinsic A values for isolated FeS 4 sites due to the strong negative Fermi-contact contribution [17]. In conclusion, the [2Fe-2S] ?…”
Section: Reduced 1-270 Construct Of Anamorsinsupporting
confidence: 71%
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“…The experimental values of the magnetic hyperfine coupling tensors A in 1-270 (Table S1) reflect this approximation, since the A values for the two subspectra have opposite signs, resulting from the spins of the individual ions being parallel and antiparallel to the applied field. The ferric site, with the larger spin, has negative A-tensor components as expected, according to the negative intrinsic A values for isolated FeS 4 sites due to the strong negative Fermi-contact contribution [17]. In conclusion, the [2Fe-2S] ?…”
Section: Reduced 1-270 Construct Of Anamorsinsupporting
confidence: 71%
“…The hypothesis is supported by the fact that the isomer shift of the ferric site does not decrease with temperature in the range 160-220 K (Table 3), as would be expected for any ''isolated'' iron with a localized valence state. The temperature invariance is indeed completely against the usual trend of isomer shifts to decrease with temperature owing to the increasing second-order Doppler shift [17]. The observed opposite behavior can only occur if the ferric site gains ferrous character from increasing electron delocalization, caused by either coherent resonance interaction or the onset of incoherent ''electron hopping.''…”
Section: Reduced Fl Constructmentioning
confidence: 80%
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“…[2][3][4][5][6][7] The method is based on the Mössbauer effect 1 which is the recoil emission/absorption of γ radiation from a solid sample. [2][3][4] The most well-known application of Mössbauer spectroscopy is for the determination of 57 Fe in metal complexes. However, there exist more than 40 other elements in the periodic table which possess γ-active isotopes and for which the Mössbauer spectra can be obtained.…”
Section: Introductionmentioning
confidence: 99%