1966
DOI: 10.1007/bf01000961
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A M�ssbauer study of some ferrocene derivatives

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1973
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Cited by 16 publications
(12 citation statements)
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“…In the case of the Fctpy, a wide doublet peak with QS (quadrupole splitting) = 2.33 mm s −1 and IS = 0.45 mm s −1 was observed; these values correspond to those reported for (diamagnetic) pristine ferrocene. 29 We observed similar wide doublet peaks for 1 (QS = 1.92 mm s −1 , IS = 0.39 mm s −1 ) and 5 (QS = 1.86 mm s −1 , IS = 0.38 mm s −1 ), respectively, demonstrating that the ferrocene substituent remained intact after the oxidation of the cobalt(II) to cobalt(III) had occurred in 1.…”
Section: Dalton Transactions Papersupporting
confidence: 59%
“…In the case of the Fctpy, a wide doublet peak with QS (quadrupole splitting) = 2.33 mm s −1 and IS = 0.45 mm s −1 was observed; these values correspond to those reported for (diamagnetic) pristine ferrocene. 29 We observed similar wide doublet peaks for 1 (QS = 1.92 mm s −1 , IS = 0.39 mm s −1 ) and 5 (QS = 1.86 mm s −1 , IS = 0.38 mm s −1 ), respectively, demonstrating that the ferrocene substituent remained intact after the oxidation of the cobalt(II) to cobalt(III) had occurred in 1.…”
Section: Dalton Transactions Papersupporting
confidence: 59%
“…In the case of the 57 Fe Mössbauer data both spectra could be reproduced well with single signals at isomer shifts of δ = 0.48(1) mms –1 ( 1 ) and δ = 0.45(1) mms –1 ( 2 ), the typical doublet spectra for diamagnetic low-spin Fe­(II), S = 0. The isomer shifts and quadrupole splitting values of 1 and 2 are almost equal, indicating comparable 4s electron densities at the iron nuclei and lie in the range typical for substituted and unsubstituted ferrocene-based coordination compounds. …”
Section: Resultsmentioning
confidence: 89%
“…The isomer shift quantifies electron density at the 57 Fe nuclei, and hence can be used to identify oxidation state; unfortunately, the isomer shifts in ferrocene (δ≈ 0.45-0.6) 39 , 40 and associated cations (δ≈ 0.51 – 0.62 for 1+ 41 , δ≈ 0.59 mm/sec for 2+ 10 ) are similar. The isomer shift range of previously reported formally Fe 1+ sandwich complexes (~0.52 – 0.73 at 77 K) 23 , 24 , 38 , 42 are smaller than that observed for 5 , but these literature examples almost exclusively exhibit low spin ground states; herein, we propose that 5 has a formal 4s 0 3d 7 high spin ground state with a reduced Fe spin population of +2.82 (see below).…”
Section: Resultsmentioning
confidence: 99%