“…In principle it may be present in the form of crystalline or amorphous SiO 2 -or Si-containing minerals. Both crystalline and amorphous forms of SiO 2 have been widely studied (Iler, 1979;Bergna and Roberts, 2005) and have also been studied with interfacial behavior including the silicawater interface under static conditions using nonlinear spectroscopy techniques (Ong et al, 1992;Ostroverkhov et al, 2004Ostroverkhov et al, , 2005Jena and Hore, 2009;Jena et al, 2011;Azam et al, 2012Azam et al, , 2013Dalstein et al, 2017;Darlington et al, 2017;DeWalt-Kerian et al, 2017;Schaefer et al, 2017Schaefer et al, , 2018Boamah et al, 2018), potentiometric titration (Karlsson et al, 2001;Dove and Craven, 2005), atomic force microscopy (Morag et al, 2013), or X-ray photoelectron spectroscopy (Brown et al, 2016). However, studies under non-equilibrium conditions are rare (Gibbs-Davis et al, 2008;Lis et al, 2014;Schaefer et al, 2018).…”