“…The interactions, however, between water and soil play a key role in the terrestrial iodine cycle and, unfortunately, this is the most complex, and least studied part of the cycle (Muramatsu et al, 1990;Sheppard et al, 1995;Moran et al, 2002;Snyder and Fehn, 2004). Although the 129 I concentration in soils was not determined in this study, the few published data (Hou et al, 2003b;Englund et al, 2005) indicate relatively higher 129 I (about 2 Â 10 9 atoms g ÿ1 ) concentrations in the soils of southern Sweden compared to central Sweden (about 5 Â 10 8 atoms g ÿ1 ). This is an interesting observation and would mean that rivers draining soils with higher 129 I concentrations may acquire a higher input of soluble iodine.…”