“…Its mobility is also controlled by sorption reactions on the surface of clay minerals (Reinoso-Maset and Ly, 2016;Robin et al, 2017) or manganese-iron (oxy-)hydroxides (Ames et al, 1983;Nirdosh et al, 1990;Sajih et al, 2014). Furthermore, radium can be incorporated into the structure of other alkaline earth sulfate or carbonate minerals occurring in mining environments (Curie, 1911;Doerner and Hoskins, 1925;Langmuir and Reise, 1985;Gnanapragasam and Lewis, 1995;Curti, 1999;Grandia et al, 2008;Yoshida et al, 2008;McDevitt et al, 2019), such as barite, through the formation of a (Ba,Ra)SO4 solid solution (Doerner and Hoskins, 1925;Brandt et al, 2015;Ouyang et al, 2019;Besançon et al, 2020;Brandt et al, 2020). Sorption of U and 226 Ra on natural organic matter has also been documented (see Bordelet et al (2018) and references therein).…”