“…In an effort to disentangle the mobility, (bio)availability, and fate of these elements in different geological settings, structural interactions of phyllomanganates with such foreign elements, and more especially with transition metals, have thus attracted the attention of the scientific community over the last few decades (Manceau et al, 1997(Manceau et al, , 2002(Manceau et al, , 2014Ohta and Kawabe, 2001;Lanson et al, 2002a;Marcus et al, 2004;Toner et al, 2006;Peacock and Sherman, 2007a,b;Peacock, 2009;Peña et al, 2010;Roque-Rosell et al, 2010;Sherman and Peacock, 2010;Yin et al, 2011a,b;Kwon et al, 2013;Yu et al, 2013;Burlet and Vanbrabant, 2015;. In most studies, foreign elements were structurally substituted for Mn(IV) in the MnO 6 octahedra or sorbed as inner-sphere complexes either at vacant layer sites and/or at particle edges (Manceau et al, 1997;Yin et al, 2011aYin et al, , 2015Yu et al, 2013;Ohnuki et al, 2015;Simanova and Pena, 2015;Qin et al, 2018). Similar to other transition metals, presence of Ni(II) forming inner-sphere complexes species at vacancy or edge sites and/or structurally incorporated in phyllomanganate layers has been extensively documented (Manceau et al, 2002(Manceau et al, , 2007aPeacock and Sherman, 2007a,b;Grangeon et al, 2008;Peña et al, 2010;Yin et al, 2012Yin et al, , 2014Kwon et al, 2013;.…”