“…The heavier transuranic elements (Am, Bk, and Cf) show more lanthanide-like characteristics and, thus, prefer having a trivalent oxidation state. − The trivalent oxidation would result in different ionic radii and preferred coordination chemistry. , For such trivalent cations to be introduced into the zircon structure, a charge-coupled substitution would be required. Nonetheless, the tetravalent states of the majority of the aforementioned elements are possible through either a transient state as a result of radiation-induced radiolysis − or a steady state being stabilized by either ligands or electrochemical methods. ,− Both, transient-state and steady-state conditions can be achieved in the unlikely event of a failure of the geological repository and breach in radiological waste canister. Each of these states could be observed under such a hypothetical scenario, if said geological repository is located in a geologic setting where the host lithology is also rich with mineral halides (i.e., halite), such as what is observed at the Waste Isolation Pilot Plant (WIPP) located in New Mexico, , and then there would be a supply of radiation, heat, high-ionic strength aqueous solutions, and the silica source from the natural barriers .…”