Effect of Water Saturation on the Diffusion/Adsorption of ²²Na and Cesium onto the Callovo-Oxfordian Claystones

Figure 6

Evolution of the cesium concentration in the source reservoir (a and c) and cesium concentration profiles (b and d) in the two intact COx samples at full saturation and at 81% of saturation.

(a)

(b)

(c)

(d)