Gamma-ray resonance study of adsorbed FeCl2monolayers

Abstract
A Mössbauer resonance study of FeCl2 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 L) and the other ∼ 0.8 mm/sec (B), which is identical to the splitting of bulk FeCl2 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 I+I depends on the orientation of the planes of the Grafoil sheets relative to kγ. The intensity ratio for kγ normal to the plane of the foils progresses from I+I>1 to I+I<1 with reduction of coverage. The total intensity of the B doublet relative to L is reduced with decreasing coverage. The velocity shift of L and the temperature dependence of the intensity of both L and B doublets differ markedly from those of bulk FeCl2 and other known Fe++ compounds. The results suggest the existence of at least two distinct phases of FeCl2 in the film samples, and that the FeCl2-graphite samples involve monolayer surface states rather than bulk FeCl2 aggregates. A calculation of the adsorption binding energy from the temperature dependence of the Debye-Waller factor yields about 80 kcal/mole for B and about 60 kcal/mole for the L phase; both values are larger than the heats of fusion (10 kcal/mole) and evaporation (30 kcal/mole) of bulk FeCl2, and are comparable with the heat of formation (80 kcal/mole). Possible models for surface arrangements of ferrous chloride molecules are discussed.