K and Ca exchange behavior of zeolite A
K and Ca exchange behavior of zeolite A
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DOI:
10.1016/j.micromeso.2011.09.025
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发表时间:
2012-03-15
影响因子:
5.2
通讯作者:
Fischer, Reinhard X.
中科院分区:
文献类型:
--
作者:
Luehrs, Hanna;Derr, Jewgenij;Fischer, Reinhard X.
Powdered samples samples of zeolite-A ([Na11.8Al11.8Si12.2O48 center dot 26 H2O](8), LTA, Na-A) were completely Ca and K exchanged. Several compositions between the end members Na-, Ca-, and K-zeolite A were produced. Combined results from X-ray powder diffraction including lattice parameter refinements in space group F m (3) over bar c, energy dispersive X-ray spectroscopy, and thermal gravimetric analyses are presented. Rietveld refinements are performed for the three Na-rich samples in the Ca exchange series. The linear dependence of the lattice parameter a on the Ca and K contents is described as well as the relationship between water. Ca and K content. The lattice parameter a decreases with increasing Ca and K content, ranging from 24.62 to 24.46 angstrom for the Ca-exchanged forms and from 24.63 to 24.58 angstrom for the K-exchanged forms. Higher Ca content results in a higher amount of water incorporated in the zeolite, ranging from 25 (Na-A) to 28 (Ca-A) molecules per formula unit (m.p.f.u.) whereas the water content in the K-exchanged forms varies about 23.5 +/- 1.0 m.p.f.u. not directly correlated with the K contents but significantly lower than the 26 m.p.f.u. of the Na-A starting material. The Ca and K contents can be estimated from lattice parameter a by linear regression. (c) 2011 Elsevier Inc. All rights reserved.