Gamma-ray resonance study of adsorbed Femonolayers
- 1 September 1976
- journal article
- research article
- Published by American Physical Society (APS) in Physical Review B
- Vol. 14 (5) , 1876-1886
- https://doi.org/10.1103/physrevb.14.1876
Abstract
A Mössbauer resonance study of Fe monolayers deposited on oriented basal planes of graphite (Grafoil) is reported. Samples with fractional monolayer coverages between 0.2 and 0.9 were studied between 300 and 80°K. The spectra show two distinct quadrupole doublets; one with a room-temperature splitting of ∼ 2 mm/sec (designated ) and the other ∼ 0.8 mm/sec (), which is identical to the splitting of bulk Fe and has the same shift. There is a marked difference between the intensities of the two lines of each doublet: For each sample, the ratio depends on the orientation of the planes of the Grafoil sheets relative to . The intensity ratio for normal to the plane of the foils progresses from to with reduction of coverage. The total intensity of the doublet relative to is reduced with decreasing coverage. The velocity shift of and the temperature dependence of the intensity of both and doublets differ markedly from those of bulk Fe and other known compounds. The results suggest the existence of at least two distinct phases of Fe in the film samples, and that the Fe-graphite samples involve monolayer surface states rather than bulk Fe aggregates. A calculation of the adsorption binding energy from the temperature dependence of the Debye-Waller factor yields about 80 kcal/mole for and about 60 kcal/mole for the phase; both values are larger than the heats of fusion (10 kcal/mole) and evaporation (30 kcal/mole) of bulk Fe, and are comparable with the heat of formation (80 kcal/mole). Possible models for surface arrangements of ferrous chloride molecules are discussed.
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