In this work, we present first principle density functional theory calculations on hydroxycarbonate and hydroxychloride green rust. Green rust is a layered mineral, with brucitelike layers of Fe(OH) 2 . It is an important corrosion product of iron present in the near field of a nuclear waste disposal site. Substitution of a part of the Fe 2+ by Fe 3+ creates a layer charge, which is compensated by interlayer anions (e.g., carbonate or chloride). The simultaneous presence of Fe 2+ /Fe 3+ in the brucite layer of green rust is a considerable theoretical challenge due to the open shell ground states of Fe 2+ /Fe 3+ . We fully characterized the lattice parameters and the internal coordinates of pure hydroxycarbonate and hydroxychloride green rust and reproduced the available experimental structural data to a very high accuracy. Based on these results, we investigated the incorporation of trivalent lanthanides and actinides into the brucite layer of green rust by replacing Fe 3+ and obtained internuclear distances in agreement with available experimental results. We show that the incorporation in all investigated green rust variants is structurally possible. The Am 3+ −O distances are in good agreement with experimental data [Finck, N.; Nedel, S.; Dideriksen, K.; Schlegel, M. L. Trivalent Actinide Uptake by Iron (Hydr)oxides. Environ. Sci. Technol. 2016, 50, 10428], whereas the agreement of the calculated and measured Am 3+ −Fe distances is less satisfactory. We demonstrated that DFT+U is a very reliable theoretical method for the theoretical investigation of hydroxycarbonate and hydroxychloride green rust and the incorporation of trivalent lanthanides and actinides into these layered double hydroxides.