Skip to main content
U.S. Department of Energy
Office of Scientific and Technical Information

Phase transition upon K{sup +} ion exchange into Na-low silica X: Combined NMR and synchrotron X-ray powder diffraction study

Journal Article · · Chemistry of Materials
DOI:https://doi.org/10.1021/cm980342s· OSTI ID:669768
;  [1];  [2]
  1. State Univ. of New York, Stony Brook, NY (United States)
  2. ANSTO, Menai (Australia)

The mechanism by which K{sup +} ions exchange into zeolite Na-low silica X (LSX) (Na{sub 96}Al{sub 96}Si{sub 96}O{sub 384}{center_dot}nH{sub 2}O) has ben determined by studying structures of the Na-LSX and K-LSX end members in the Na-K LSX solid solution series as well as samples exchanged at the 20%, 42% and 80% K{sup +} levels. A preliminary investigation using {sup 29}Si MAS NMR spectroscopy revealed a two-phase region in the solid solution near 80% K{sup +} exchange. Rietveld analysis of the powder diffraction data collected from hydrated samples showed that, up to 42% of K{sup +} exchange, K{sup +} ions were located preferentially at site I{prime}, just outside the double 6-ring (D6R) in the sodalite age, and at site II, above the single 6-ring (S6R) in the supercage. Introduction of K{sup +} ions into site I{prime} repositioned Na{sup +} ions into site I, at the center of the D6R. An abrupt change in the cubic lattice parameter from 25.0389(5) to 25.2086(5) {angstrom} marked the formation of a second phase at the 80% K{sup +}-exchange level as K{sup +} ions began to occupy site I. No coexistence of phases was observed for the fully K{sup +}-exchanged sample (a = 25.2486(2) {angstrom}), where sites I and II were fully occupied by K{sup +} ions.

Sponsoring Organization:
USDOE, Washington, DC (United States); National Science Foundation, Washington, DC (United States)
OSTI ID:
669768
Journal Information:
Chemistry of Materials, Journal Name: Chemistry of Materials Journal Issue: 9 Vol. 10; ISSN CMATEX; ISSN 0897-4756
Country of Publication:
United States
Language:
English

Similar Records

Hydronium ions in zeolites. 1. Structures of partially and fully dehydrated Na, H{sub 3}O-X by X-ray and neutron diffraction
Journal Article · Wed Nov 24 23:00:00 EST 1999 · Journal of Physical Chemistry B: Materials, Surfaces, Interfaces, amp Biophysical · OSTI ID:20013641

Crystal structure of partially Pd{sup 2+}-exchanged zeolite X dehydrated in oxygen at 400 C. Formation of linear Pd{sub 2}O{sub 3} clusters proposed to be HO-Pd{sup IV}-O-Pd{sup IV}-OH in (Pd{sup 2+}){sub 14}(HOPdOPdOH{sup 4+}){sub 8}(Na{sup +}){sub 32}-Si{sub 100}Al{sub 92}O{sub 384}
Journal Article · Wed Mar 22 23:00:00 EST 2000 · Journal of Physical Chemistry B: Materials, Surfaces, Interfaces, amp Biophysical · OSTI ID:20026922

Neutron diffraction determination of full structures of anhydrous Li-X and Li-Y zeolites
Journal Article · Fri Sep 01 00:00:00 EDT 1989 · Journal of Solid State Chemistry; (USA) · OSTI ID:6838680