“…In natural waters, trace elements including radionuclides can be distributed into three fractions distinguished by their difference in size (Figure 1): the particulate fraction greater than 0.45 µm (corresponding to the water filtration threshold usually adopted for environmental monitoring), the truly dissolved fraction lower than 1 nm and the colloidal fraction with a size between these two fractions (Stumm, 1997;Missana et al, 2004;Aiken et al, 2011). Colloids are mainly composed of minerals exhibiting retention properties towards trace elements such as Fe-Ti-Al oxy-hydroxides, phosphates, carbonates, sulfates, silica, and aluminosilicate phases found in oxidizing contexts, and sulfides under reducing conditions (Kaplan et al, 1994;Turrero et al, 1995;Porcelli et al, 2001;Nordstrom, 2011;Nordstrom et al, 2015;Husson et al, 2019;Javed et al, 2020;Equeenuddin et al, 2020;Silva et al, 2021). They can also be a mix of organic substances and minerals (Kretzschmar and Schäfer, 2005;Wang et al, 2013;Wang et al, 2014;Novotnik et al, 2018).…”