“…Q nÀ1 Si conversion [2,4,[84][85][86]. Although early 27 Al NMR studies on crystalline aluminate phases indicated the absence of any correlation between δ iso [4] and the number of BO atoms (n) at the Q Al n tetrahedron [87,88], the data-bank of 27 Al isotropic chemical shifts from phyllosilicate minerals, which comprise sheets of interconnected Q Al 3 (3Si) groups, reveal about 10 ppm higher shifts (typically $ 65-75 ppm) than those of Q Al 4 (4Si) groups ($ 55-70 ppm) in 3D framework structures, such as zeolites [38,41]. Moreover, several MAS NMR studies of Al-bearing aluminate and aluminosilicate glasses manifest weak but consistent 27 Al deshielding effects for increasing network-modifier content of the glass [6,49,60,89].…”