“…Double carbonates with the composition M1M2(CO 3 ) 2 (M = Ca, Mg, Mn, Zn, Ba, Sr) are an interesting group of materials, where, for example, dolomite [CaMg(CO 3 ) 2 ] has attracted attention as it is a geologically relevant model system in which to study cation order-disorder processes (Vinograd et al, 2009;Burton & Van de Walle, 2003). The double carbonate BaCa(CO 3 ) 2 has recently been investigated with respect to its suitability for the immobilisation of radioactive isotopes (Grandjean & Leturcq, 2005;Massoni et al, 2013Massoni et al, , 2014Massoni et al, , 2015Massoni & Le Gallet, 2016), where the incorporation of 14 C was explored as an alternative to the incorporation of 14 C in CaCO 3 (Brooks et al, 1974;Croff, 1976).…”