“…-3 - 90 Sr and 137 Cs are well known to have a low mobility in soils (Han et al, 2016;Mishra et al, 2016) due to their strong interactions with clay minerals (Adeleye et al, 1994;Baborova et al, 2018;Durrant et al, 2018;Dyer et al, 2000;Sawhney, 1970;Semenkova et al, 2018), out of which illite and vermiculite are known to be the most selective adsorbents for Cs + (Durrant et al, 2018;Dzene et al, 2015). This high adsorption is due to the weak hydration energy of Cs + (Marcus, 1985) and mainly attributed to the existence of low concentration high affinity sites, usually referred as frayed edge sites (FES) on illite (Cornell, 1993;Sawhney, 1972).…”