“…In a large number of experiments, the pH at the interface (which is difficult to measure in integrated experiments), or the pH of solutions in batch experiments, is slightly alkaline as a result of the corrosion process, with values increasing up to about 9e10 (Wilson et al, 2006b;De Combarieu et al, 2007: Perronnet et al, 2007Ishidera et al, 2008;Perronnet et al, 2008). This pH perturbation is responsible for the presence of a transformed clay mineral layer showing systematic dissolution of primary clay minerals: in experiments with clay-rocks, illite, and I-Sm (Jodin-Caumon et al, 2012) tend to dissolve preferentially along with the occasional destabilization of quartz and dolomite (Bourdelle et al, 2014).…”