Crystal Structures of Fully La3+-Exchanged Zeolite X: an Intrazeolitic La2O3 Continuum, Hexagonal Planar and Trigonally Monocapped Trigonal Prismatic Coordination
Crystal Structures of Fully La3+-Exchanged Zeolite X: an Intrazeolitic La2O3 Continuum, Hexagonal Planar and Trigonally Monocapped Trigonal Prismatic Coordination
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DOI:
10.1021/jp992153i
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发表时间:
2000-02
影响因子:
3.3
通讯作者:
Hyun Sook Park and;K. Seff
中科院分区:
文献类型:
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作者:
Hyun Sook Park and;K. Seff
Three single crystals of sodium zeolite X were fully La3+-exchanged at 90 °C from aqueous solution (pH = 7.45, 7.45, and 6.89 at 22 °C, respectively). One was vacuum dehydrated at 400 °C (crystal 1), another at 22 °C (crystal 2), and the third remained fully hydrated (crystal 3). Their structures at 22 °C were determined by single-crystal X-ray crystallography in the cubic space groups Fd3m (a = 24.999(4) and 25.059(4) A) and Fd3 (a = 25.154 (3) A), respectively. They were refined to the final error indices R1 = 0.076, 0.091, and 0.078 with 471, 374, and 725 reflections, respectively, for which Fo > 4σ(Fo). The number of La3+, H3O+, and OH- ions found in the three structures are about 38, 0, 18; 38, 28, 50; and 33, 16, 24, respectively, per unit cell. Crystal 1 also has 48 nonframework oxide ions and 92 H+ ions per unit cell. In all cases overexchange occurred. In crystal 1, 32 La3+ ions per unit cell fill site I‘, with the remaining six at 12-ring centers (site V). Each of these six coordinates to thre...