Purpose Lead contamination is ubiquitous, and much attention has been paid due to its toxicity. The phyllomanganate birnessite is the most common Mn oxide in soils. The MnO 6 octahedral layers may have significant Mn vacancies in the hexagonal birnessites. Among heavy metal ions, birnessites possess the greatest adsorption affinity and capacity for Pb 2+ . The aim of this study was to understand the relationship between vacant Mn octahedral sites and Pb 2+ adsorption. Materials and methods Birnessite synthesis was achieved by the reduction of potassium permanganate in a strong acidic medium. Synthetic birnessite was then treated with Mn 2+ or Zn 2+ at different concentrations. Isothermal Pb 2+ adsorption on birnessite before and after treatments was measured at a solid-to-liquid ratio of approximately 1.67 g/L, and Pb 2+ concentrations ranged from 0 to 10 mmol/L with an ionic strength of 0.1 mol/L NaNO 3 . The amount of Pb 2+ adsorbed and the amount of Mn 2+ or Zn 2+ released during the whole adsorption process were obtained by comparison with a control group without adding Pb 2+ . The amount of H + released was determined from the recorded additions of standard HNO 3 /NaOH solutions. Results and discussion Mn average oxidation state (AOS) and d(110)-interplanar spacings of the birnessites remained almost unchanged as the concentration of the treating Zn 2+ increased, indicating an unchanged number of vacant Mn octahedral sites, whereas the maximum Pb 2+ adsorption decreased from 3,190 to 2,030 mmol/kg due to the presence of Zn 2+ on adsorption sites. The AOS's of the Mn 2+ -treated birnessites decreased and most of the Mn 2+ ions added were oxidized to Mn 3+ ions. The d(110)-interplanar spacing of Mn 2+ -treated birnessites increased from 0.14160 to 0.14196 nm, indicative of a decreased vacant Mn octahedral sites. Moreover, the maximum Pb 2+ adsorption of Mn 2+ -treated birnessites decreased from 3,190 to 1,332 mmol/kg, the decrease being greater than that for the corresponding Zn 2+ -treated birnessites. Conclusions Most Mn 2+ was oxidized to Mn 3+ by birnessite, with a portion of Mn 3+ located above or below vacant sites, which did not affect the number of vacant sites, and the remaining Mn 3+ migrating to occupy the vacant sites. In contrast, Zn 2+ ions are adsorbed only above or below vacant sites. Birnessite Pb 2+ adsorption capacity is determined largely by the number of vacant Mn sites.