Measurements of the apparent selfdiffusion coefficients of, poly(vinyl pyrrolidone) mol. wt. 40 000, poly(ethy1ene glycol) mol. wt. 4000, and chloride ion, were used to determine the effect of molecular size on diffusion characteristics in soil. The measurements were carried out on the same soil, at a range of moisture contents, and indicated that the mobility of large molecules in soils depends, to a large degree, on the inter-aggregate pores. Any drop in moisture content which caused these pores to drain, produad a sharp decrease in the apparent selfdiffusion coefficient of the poly(viny1 pyrrolidone) 40 000. Neither poly(ethy1ene glycol) 4000 nor chloride, which exhibited similar diffusion characteristics, wcre as sensitive to variation in moisture content. The results are interpreted in terms of certain parts of the pore volume being inaccessible to the diffusing molecule. Possible reasons are outlined.