The effects of porosity in carbon supports and the impregnation solvent on the dispersion and stability of iron was examined, and the influence of porosity on the catalytic behavior for CO hydrogenation was studied. The porosity was varied by using carbonized olive pits activated in C02 or steam and by using a commercial carbon black. The carbons were characterized by N2 adsorption at 77 K and C02 adsorption a t 273 K while H2 and CO chemisorption was used to measure iron particle size in the Fe/C catalysts prepared from Fe3(C0)12 clusters. With the exception of the use of benzene as the solvent with the carbon containing the narrowest microporosity, high initial dispersions of iron were achieved in all cases after decomposition of these clusters in H2 at 673 K. Optimum resistance to sintering under CO hydrogenation reaction conditions or in H2 at higher temperatures was obtained by using tetrahydrofuran as the solvent and a carbon with a wide pore size distribution containing a large fraction of large micropores. In these systems, iron particle sizes remained close to 2 nm. Consistent with previous studies, turnover frequencies were low and increased with crystallite size, olefii/paraffin ratios were around 1 for the as-prepared samples and frequently approached 2 after a more thorough reduction in H2, and activation energies for both hydrocarbon formation and methanation were lower than on large iron crystallites. At the standard space velocity used for these catalysts (3600 h-l), external mass transfer was not a limitation and the variation in pore size distribution among these four carbons did not appear to have a significant effect on activity or selectivity based on the kinetic parameters and the Weisz criterion. However, at lower space velocities the influence of external mass transport limitations became apparent. In general, there was no significant effect of porosity on catalytic behavior. Heats of adsorption of CO (Q) were measured on the four carbons, on two unsupported Fe powders, and on the carbon-supported iron crystallites. Q,,, values were near 2-3 kcal mol-' for the carbons, Qirrev values were near 43 kcal mol-' on the unsupported Fe powder and agreed well with ultra-high-vacuum results, but QheV values were lower on the carbon-supported iron, with one group clustered around 15 kcal mol-' and a second group giving even lower values of 5-10 kcal mol-l.