Optimizing synthesis of Na2Ti2SiO7 • 2H2O (Na-CST) and ion exchange pathways for Cs0.4H1.6Ti2SiO7 • H2O (Cs-CST) determined from in situ synchrotron X-ray powder diffraction

被引:17
作者
Celestian, AJ [1 ]
Medvedev, DG
Tripathi, A
Parise, JB
Clearfield, A
机构
[1] SUNY Stony Brook, Dept Geosci, Ctr Environm & Mol Sci, Stony Brook, NY 11794 USA
[2] Texas A&M Univ, Dept Chem, College Stn, TX 77843 USA
[3] SUNY Stony Brook, Dept Chem, Stony Brook, NY 11794 USA
关键词
zeolite; real time; waste sequestration; titanium silicate;
D O I
10.1016/j.nimb.2005.06.019
中图分类号
TH7 [仪器、仪表];
学科分类号
0804 ; 080401 ; 081102 ;
摘要
Observation of wide angle diffraction data collected in situ during synthesis of Na-CST (Na2Ti2O3SiO4 (.) 2H(2)O) showed initial crystallization of a precursor phase (SNT) at 30 degrees C followed by conversion to CST after 1 h at 220 degrees C. In situ studies of Cs+ ion exchange into the H+ form of CST showed a site-by-site ion exchange pathway accompanied by a simultaneous structural transition from P4(2)/mbc (cell parameters a = 11.0690(6) angstrom, c = 11.8842(6) angstrom) to P4(2)/mcm (cell parameters a = 7.847(2) angstrom, c = 11.9100(6) angstrom). After approximately 18% Cs+ exchange into site designated Cs2 in space group P4(2)/mcm, a site designated Cs1 in space group P4(2)/mcm began to fill at the center of the 8MR windows until a maximum of approximately 22% exchange was achieved for Cs1. Bond valence sums of site Cs1 to framework O2- are 1.00 v.u., while bond valence sums of site Cs2 to framework O2- are 0.712 v.u. suggesting Cs1 to have a more stable bonding environment. (c) 2005 Elsevier B.V. All rights reserved.
引用
收藏
页码:61 / 69
页数:9
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