Under hydrostatic pressure, low-silica zeolite-X exhibits a range of compression behavior depending on its cation distribution as well as the pressure transmitting medium. This pressure response appears to be a complex phenomenon involving the interplay between selective overhydration, cation relocation, as well as the intrinsic framework distortion, and indicates that the apparent compressibility of LSX can be tailored via cation exchange and the choice of pressure medium.
|Number of pages||2|
|Journal||Journal of the American Chemical Society|
|Publication status||Published - 2007 Apr 25|
All Science Journal Classification (ASJC) codes
- Colloid and Surface Chemistry