Two anhydrous zeolite X crystal structures, Cd46Si100Al92O384 and Cd24.5Tl43Si100Al92O384

被引:54
作者
Kwon, JH
Jang, SB
Kim, Y
Seff, K
机构
[1] PUSAN NATL UNIV,DEPT CHEM,PUSAN 609735,SOUTH KOREA
[2] UNIV HAWAII,DEPT CHEM,HONOLULU,HI 96822
关键词
D O I
10.1021/jp9603647
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
The structures of fully dehydrated, fully Cd2+-exchanged zeolite X, Cd46Si100Al92O384 (Cd-IB-X; a = 24.935(8) Angstrom), and that of fully dehydrated Cd2+- and Tl+-exchanged zeolite X, Cd24.5Tl43Si100Al92O384 (Cd24.5Tl43-X; a = 2 4.858(9) Angstrom), have been determined by single-crystal X-ray diffraction methods in the cubic space group Fd (3) over bar at 21(1) degrees C. Cd-46-X was prepared by ion exchange in a flowing stream of 0.05 M aqueous Cd(NO3)(2) for 2 days. Cd24.5Tl43-X was prepared similarly using a solution 0.025 M each in Cd(NO3)(2) and TlNO3. Each crystal was then dehydrated at 450 degrees C and 2 x 10(-6) Torr for 2 days, Their structures were refined to the final error indices R(1) = 0.055 and R(2) = 0.077 with 544 reflections for Cd-46-X, and R(1) = 0.054 and R(2) = 0.051 with 272 reflections for Cd24.5Tl43-X; I > 3 sigma(1). In the structure of dehydrated Cd-46-X, Cd2+ ions are located at two different crystallographic sites. Sixteen Cd2+ ions fill site I, at the centers of the double six-rings; each Cd2+ ion is octahedrally coordinated by framework oxygens, all at 2.35(1) Angstrom. The remaining 30 Cd2+ ions nearly fill the 32-fold site II in the single six-rings; each is three-coordinate planar to framework oxygens at 2.16(1) Angstrom. The fractional occupancies in dehydrated Cd Tl-24.5(43)-X are most easily explained with two types of unit cell: half have 14 Cd2+ ions at site I and four Tl+ ions at site I'. The remaining half have 15 Cd2+ ions at site I and Tl+ ions at site I'. The remaining ten Cd2+ ions occupy site II; 22 Tl+ ions extend 1.52 Angstrom into the supercage from their three oxygen planes to complete the filling of site II. The remaining 18 Tl+ ions are statistically distributed over site III, a 48-fold equipoint in the supercages on twofold axes; Tl-O = 2.79(2) Angstrom. It appears that Cd2+ ions prefer sites I and II in that order, and that Tl+ ions occupy the remaining sites, except that they are too large to be stable at site I.
引用
收藏
页码:13720 / 13724
页数:5
相关论文
共 25 条
[1]   GROWTH OF NA-X ZEOLITE MONOCRYSTALS UP TO 0.5 MM [J].
BOGOMOLOV, VN ;
PETRANOVSKY, VP .
ZEOLITES, 1986, 6 (06) :418-419
[2]   CRYSTAL-STRUCTURE OF A NATURAL AND A PARTIALLY SILVER-EXCHANGED HEULANDITE [J].
BRESCIANIPAHOR, N ;
CALLIGARIS, M ;
NARDIN, G ;
RANDACCIO, L ;
RUSSO, E ;
COMINCHIARAMONTI, P .
JOURNAL OF THE CHEMICAL SOCIETY-DALTON TRANSACTIONS, 1980, (09) :1511-1514
[3]   CRYSTAL-STRUCTURES OF THE HYDRATED AND PARTIALLY DEHYDRATED FORMS OF CD-X EXCHANGED ZEOLITES [J].
CALLIGARIS, M ;
NARDIN, G ;
RANDACCIO, L ;
ZANGRANDO, E .
ZEOLITES, 1986, 6 (06) :439-444
[4]   CRYSTAL-STRUCTURES OF THE HYDRATED AND DEHYDRATED FORMS OF A PARTIALLY CESIUM-EXCHANGED CHABAZITE [J].
CALLIGARIS, M ;
MEZZETTI, A ;
NARDIN, G ;
RANDACCIO, L .
ZEOLITES, 1986, 6 (02) :137-141
[5]   CRYSTAL-STRUCTURES OF HYDRATED AND DEHYDRATED FORMS OF A MN(II)-EXCHANGED CHABAZITE [J].
CALLIGARIS, M ;
MEZZETTI, A ;
NARDIN, G ;
RANDACCIO, L .
ZEOLITES, 1985, 5 (05) :317-319
[6]  
*CHEM RUBB CO, 1989, HDB CHEM PHYS, pF187
[8]   ADSORPTION OF CARBON MONOXIDE BY CALCIUM-EXCHANGED ZEOLITE Y [J].
EGERTON, TA ;
STONE, FS .
TRANSACTIONS OF THE FARADAY SOCIETY, 1970, 66 (573) :2364-&
[9]  
*ENR, 1990, CAL WER PERF STRUCT
[10]  
HERDEN H, 1981, INORG NUCL CHEM, V43, P2533