“…Of relevance here is XAFS spectroscopy, because it is well suited for molecular-level studies of adsorption complexes at mineral-water interfaces (Section 5 .2) . A number of other synchrotron-based methods can provide complementary information about mineral-water interfaces and these include X-ray fluorescence microprobe imaging (e.g ., Bertsch and Hunter, 2001), scanning transmission X-ray microscopy imaging and nanospectroscopy (e.g ., Benzerara et al ., 2004Benzerara et al ., , 2005Benzerara et al ., , 2006aBenzerara et al ., ,b, 2008Benzerara et al ., , 2010Benzerara et al ., , 2011aBernard et al ., 2007Bernard et al ., , 2009Bernard et al ., , 2010Couradeau et al ., 2012); X-ray photoelectron spectroscopy (e.g ., Liu et al ., 1998a,d), X-ray standing wave fluorescent yield spectroscopy (e.g ., Fenter et al ., 2000aFenter et al ., ,b, 2003aTempleton et al ., 2001Templeton et al ., , 2003aCatalano et al ., 2006), surface X-ray scattering (crystal truncation rod, CTR, diffraction;e.g ., Eng et al ., 2000;Trainor et al ., 2004); X-ray reflectivity and resonant anomalous X-ray reflectivity (RAXR; e.g ., Teng et al ., 2001;Catalano et al ., 2008;Fenter et al ., 2007Fenter et al ., , 2008, and high energy total X-ray scattering and pair distribution function analysis (Michel et al ., 2007a,b; . All of these new methods have also led to new understanding of Earth materials, particularly those consisting of complex mixtures of solids, liquids, and microbial organisms .…”