Background-Ferritin exhibits complex behavior in the ultracentrifuge due to variability in iron core size among molecules. A comprehensive study was undertaken to develop procedures for obtaining more uniform cores and assessing their homogeneity.Methods-Analytical ultracentrifugation was used to measure the mineral core size distributions obtained by adding iron under high-and low-flux conditions to horse spleen (apoHoSF) and human H-chain (apoHuHF) apoferritins.Results-More uniform core sizes are obtained with the homopolymer human H-chain ferritin than with the heteropolymer horse spleen HoSF protein in which subpopulations of HoSF molecules with varying iron content are observed. A binomial probability distribution of H-and Lsubunits among protein shells qualitatively accounts for the observed subpopulations. The addition of Fe 2+ to apoHuHF produces iron core particle size diameters from 3.8 ± 0.3 to 6.2 ± 0.3 nm. Diameters from 3.4 ± 0.6 to 6.5 ± 0.6 nm are obtained with natural HoSF after sucrose gradient fractionation. The change in the sedimentation coefficient as iron accumulates in ferritin suggests that the protein shell contracts ~10% to a more compact structure, a finding consistent with published electron micrographs. The physicochemical parameters for apoHoSF (15%/85% H/L subunits) are M = 484,120 g/mol, ν̄ = 0.735mL/g, s 20,w = 17.0 S and D 20,W = 3.21 × 10 −7 cm 2 /s; and for apoHuHF M = 506,266 g/mol, ν̄ = 0.724 mL/g, s 20,w = 18.3 S and D 20,w = 3.18 × 10 −7 cm 2 /s.Significance-The methods presented here should prove useful in the synthesis of size controlled nanoparticles of other minerals.