Pressure-induced hydration at 0.6 GPa in a synthetic gallosilicate zeolite.
The onset of pressure-induced hydration and volume expansion is lowered to 0.6 GPa via the increased flexibility of the host lattice using isomorphous substitution of Al by larger Ga in a sodium aluminosilicate natrolite.
Lee
Yongjae
Y
Physics Department, Brookhaven National Laboratory, Upton, New York 11973, USA. yollee@bnl.gov
Hriljac
Joseph A
JA
Kim
Sun Jin
SJ
Hanson
Jonathan C
JC
Vogt
Thomas
T