“…15,34−37 According to the literature, X-ray diffractograms of CVL present peaks at 0.150 nm, common for dioctahedral montmorillonite smectite, at 0.334 nm, related to the presence of quartz, and at 0.447 nm, characteristic of montmorillonite. 15,35,37 Moreover, studies performed by Oliveira et al 36 and Antonelli et al 15,35 observed, employing thermogravimetric analysis, that CVL is thermally stable up to 1000 °C. The authors verified loss of water in the range of 76− 81 °C and loss of hydroxyls in the range of 478−483 °C.…”