Abstract:We h~ve measured the ionization potentials of gaseous ferrocene and the symmetrically ~ub~tlt~ted chlor~fe?"ocenes, F~( CsHs _ NCI N h (O..;;N";;5) by electron impact techniques. The lOntzatlOn potentIal IS found to mcrease in direct proportion to the number of chlorine substit~tions. !hese results indicate that chlorine ring substitutions result in greater overlap of the 11"-nng orbItals and the metal d orbitals. The binding energies of the unoccupied orbitals of ferrocene and 1,I'-dichloroferrocene have bee… Show more
“…The assignment of the photoabsorption features to one-electron transitions depends crucially upon the assumed level ordering of the ferrocene molecular orbitals-a matter of considerable controversy (ref 2 and the references therein). There are advocates for an orbital ordering (in terms of increasing binding energy) alg(d) < e^d) < ß1 ( ) < elg(x).…”
Section: One-electron Transitionsmentioning
confidence: 99%
“…This is in agreement with simple expectations for molecular orbital theory and optical absorption data. [12][13][14][15][16] If we assume that the B and C Racah electron repulsion parameters are related according to 4B = C,13 the difference of the electronic transitions energies is given by E(5elg(b)-8alg) -S(5elg(a)-8alg) = ( !2 + 12 + 420B2)1/2 (2) and the sum of the electronic transition energies £(5elg(b)-8alg) + £(5elg(a)-8alg) = 2 2 -, + 4B (3) The repulsion parameters are assumed to be unaltered as a result of the disubstitutions to ferrocene. The appropriate electronic transition energies if not measured and reported in Table I can be estimated from Table II.…”
Section: Ligand Field Splittingmentioning
confidence: 99%
“…There exist a considerable number of photoabsorption spectra for a variety of metallocenes, however, the assignment of the absorption features remains far from satisfactory. Even in the case of ferrocene,1 for which the assignment of absorption features is better established, there is considerable controversy as to the level ordering of some of the molecular orbitals and one-electron transitions (ref 2 and the references therein) as a result of the photoemission data. The existence of photoelectron spectra of ferrocene,3-9 , -dimethylferrocene,3,6 l,l'-dibromoferrocene,5 and , '-dichloroferrocene3 '5,6 together with photoabsorption data make the investigation of the effect of symmetric substitutions on the ferrocene molecular orbitals possible for both occupied and unoccupied orbitals, assuming one particular level ordering for ferrocene.…”
“…The assignment of the photoabsorption features to one-electron transitions depends crucially upon the assumed level ordering of the ferrocene molecular orbitals-a matter of considerable controversy (ref 2 and the references therein). There are advocates for an orbital ordering (in terms of increasing binding energy) alg(d) < e^d) < ß1 ( ) < elg(x).…”
Section: One-electron Transitionsmentioning
confidence: 99%
“…This is in agreement with simple expectations for molecular orbital theory and optical absorption data. [12][13][14][15][16] If we assume that the B and C Racah electron repulsion parameters are related according to 4B = C,13 the difference of the electronic transitions energies is given by E(5elg(b)-8alg) -S(5elg(a)-8alg) = ( !2 + 12 + 420B2)1/2 (2) and the sum of the electronic transition energies £(5elg(b)-8alg) + £(5elg(a)-8alg) = 2 2 -, + 4B (3) The repulsion parameters are assumed to be unaltered as a result of the disubstitutions to ferrocene. The appropriate electronic transition energies if not measured and reported in Table I can be estimated from Table II.…”
Section: Ligand Field Splittingmentioning
confidence: 99%
“…There exist a considerable number of photoabsorption spectra for a variety of metallocenes, however, the assignment of the absorption features remains far from satisfactory. Even in the case of ferrocene,1 for which the assignment of absorption features is better established, there is considerable controversy as to the level ordering of some of the molecular orbitals and one-electron transitions (ref 2 and the references therein) as a result of the photoemission data. The existence of photoelectron spectra of ferrocene,3-9 , -dimethylferrocene,3,6 l,l'-dibromoferrocene,5 and , '-dichloroferrocene3 '5,6 together with photoabsorption data make the investigation of the effect of symmetric substitutions on the ferrocene molecular orbitals possible for both occupied and unoccupied orbitals, assuming one particular level ordering for ferrocene.…”
“…The spectra for ferrocene on Cu(100) are qualitatively similar to those obtained on the Ag(100) surface. Again, on the basis of theoretical calculations of the ground-state molecular orbitals of ferrocene [16][17][18][19][20][21][22] and gas-phase photoemission and ionization potential studies, [23][24][25][26][27] we can assign these photoemission features of the adsorbed species (Table 2, Figure 5). The ferrocene 8a 1g and 4e 2g molecular orbitals induce the 4.2 eV feature that overlaps with the Cu 3d bands.…”
Section: Theorymentioning
confidence: 99%
“…There exists a strong similarity between the gas-phase photoemission spectra of ferrocene and condensed ferrocene, 5 although the molecule to substrate and intermolecular interactions have been observed to shift, split, or broaden the observed energies of the molecular orbitals. On the basis of theoretical calculations of the ground-state molecular orbitals of ferrocene [16][17][18][19][20][21][22] as well as gas-phase photoemission and ionization potential studies, [23][24][25][26][27] we can assign the adsorbed ferrocene-induced photoemission features to the molecular orbitals of ferrocene ( Table 2, Figures 2 and 3). The features at 5.4 and 4.1 eV arise from the ferrocene 8a 1g and 4e 2g Figure 2.…”
We have measured the molecular orientation and bonding of adsorbed ferrocene on Ag(100) and Cu(100) using angle-resolved photoemission spectroscopy (ARPES). The results for molecular adsorption on Ag(100) are complemented by high-resolution electron energy loss spectroscopy (HREELS) measurments and ab initio calculations for the ferrocene vibrational modes. The measurements indicate that ferrocene adsorbs on Ag(100) with the molecular axis perpendicular to the surface. In contrast, as indicated using ARPES and scanning tunneling microscopy, ferrocene adsorbed on the Cu(100) surface is oriented with the molecular axis parallel with the surface. Model calculations allow us to assign all of the observed vibrational modes for the weakly bound molecular ferrocene on Ag(100)-both dipole and impact scattering modes have been observed.
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