“…Because Al and O can form an Al 2 O 3 structure inside the Al domain, the negative charge is considered to localize at the boundary. The tetracoordinated Al is ubiquitous in zeolite (aluminosilicate), , and its [AlO 4 ] − sites are negatively charged. Furthermore, for the SiO 2 –Al 2 O 3 system, Al atoms were reported to be tetrahedrally coordinated when the Al concentration is less than about 20%. − Therefore, the emergence of the negative charge especially at an Al concentration of 6–13% is reasonable.…”