CRYSTAL-STRUCTURE OF FULLY DEHYDRATED, PARTIALLY AG+-EXCHANGED ZEOLITE-4A, AG7.6NA4.4-A - AG+ IONS PREFER 6-RING SITES - ONE AG+ ION IS REDUCED

被引：26

作者：

KIM, Y

SEFF, K

机构：

[1] UNIV HAWAII,DEPT CHEM,HONOLULU,HI 96822

[2] PUSAN NATL UNIV,DEPT CHEM,PUSAN 607,SOUTH KOREA

来源：

JOURNAL OF PHYSICAL CHEMISTRY | 1987年 / 91卷 / 03期

关键词：

D O I：

10.1021/j100287a035

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：

引用

页码：671 / 674

页数：4

共 32 条

[11] JOHNSON CK, 1965, ORTEP ORNL3794 REP
[12] STRUCTURE OF A VERY SMALL PIECE OF SILVER METAL - OCTAHEDRAL AG6 MOLECULE, 2 CRYSTAL-STRUCTURES OF PARTIALLY DECOMPOSED VACUUM-DEHYDRATED FULLY AG+-EXCHANGED ZEOLITE-A
KIM, Y
SEFF, K
[J]. JOURNAL OF THE AMERICAN CHEMICAL SOCIETY, 1977, 99 (21) : 7055 - 7057
[13] CRYSTAL-STRUCTURE OF A BROMINE SORPTION COMPLEX OF DEHYDRATED FULLY AG+-EXCHANGED ZEOLITE-A
KIM, Y
SEFF, K
[J]. JOURNAL OF PHYSICAL CHEMISTRY, 1978, 82 (08) : 925 - 929
[14] OCTAHEDRAL HEXASILVER MOLECULE - 7 CRYSTAL-STRUCTURES OF VARIOUSLY VACUUM-DEHYDRATED FULLY AG+-EXCHANGED ZEOLITE-A
KIM, Y
SEFF, K
[J]. JOURNAL OF THE AMERICAN CHEMICAL SOCIETY, 1978, 100 (22) : 6989 - 6997
[15] HEXA-SILVER MOLECULE STABILIZED BY COORDINATION TO 6 SILVER IONS - STRUCTURE OF (AG+)6(AG6) - CRYSTAL-STRUCTURE OF AN ETHYLENE SORPTION COMPLEX OF PARTIALLY DECOMPOSED FULLY AG+-EXCHANGED ZEOLITE-A
KIM, Y
SEFF, K
[J]. JOURNAL OF THE AMERICAN CHEMICAL SOCIETY, 1978, 100 (01) : 175 - 180
[16] KIM Y, 1985, B KOR CHEM SOC, V6, P202
[17] CRYSTAL-STRUCTURE OF DEHYDRATED FULLY AG+-EXCHANGED ZEOLITE-A REDUCED BY HYDROGEN AND REOXIDIZED BY OXYGEN, BOTH AT 330-DEGREES-C - LOSS OF LONG-RANGE ORDER AND ITS SUBSEQUENT RETURN
KIM, Y
SEFF, K
[J]. JOURNAL OF PHYSICAL CHEMISTRY, 1978, 82 (08) : 921 - 924
[18] EVIDENCE FOR NEAR ZERO COORDINATE SILVER(I) - CRYSTAL-STRUCTURES OF FULLY AND PARTIALLY HYDRATED FULLY AG+-EXCHANGED ZEOLITE A
KIM, Y
SEFF, K
[J]. JOURNAL OF PHYSICAL CHEMISTRY, 1978, 82 (09) : 1071 - 1077
[19] KIM Y, 1984, B KOR CHEM SOC, V5, P135
[20] CRYSTAL-STRUCTURE OF ZEOLITE-A EXCHANGED WITH AG+ AND TL+, AG6.5TL5.5-A, EVACUATED AT 400-DEGREES-C - PARTIAL MECHANISM FOR INTRAZEOLITIC REDUCTION OF AG+ TO FORM HEXASILVER
KIM, Y
SEFF, K
[J]. JOURNAL OF PHYSICAL CHEMISTRY, 1978, 82 (11) : 1307 - 1311

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