Complex cementitious matrices undergo weathering with environmental exchange and can release metallic pollutants during alteration. The molecular mechanisms responsible for metal release are difficult to identify, though this is necessary if such processes are to be controlled.The present study determines and models the molecular mechanisms of Pb release during Portland cement leaching. Since Pb release is strongly related to its speciation (i.e. atomic environment and nature of bearing phases), the first objective of the present work is to investigate the evolution of Pb retention sites together with the evolution of the cement mineralogy during leaching. Complementary and efficient investigation tools were used, namely XRD, µ-XRF and XAFS. The second goal is to reproduce our results with a reactive transport code (CHESS/HYTEC) in order to test the proposed speciation model of Pb.Combined results indicate that both in the unaltered core and altered layer of the leached cement, Pb(II) would be retained through C-S-H "nano-structure", probably linked to a Q 1 or Q 2P silicate tetrahedra. Moreover in the altered layer, the presence of Fe atoms in the atomic environment of Pb is highly probable. Unfortunately little is known about Fe phases in cement, making the interpretation difficult. Can Fe-substituted hydrogranet (C 3 AH 6 ) be responsible for Pb retention? Modelling results are consistent with Pb retention through C-S-H in layers and also in an additional, possibly Fe-containing, Pb-retention phase in the altered layer.