The crystal structure of zeolite A exchanged with silver(1+) and thallium(1+), Ag6.5Tl5.5-A, evacuated at 400.degree.C. A partial mechanism for the intrazeolitic reduction of silver(1+) ion to form hexasilver
1978 ◽
Vol 82
(11)
◽
pp. 1307-1311
◽
1996 ◽
Vol 100
(20)
◽
pp. 8373-8377
◽
1979 ◽
Vol 83
(16)
◽
pp. 2166-2169
◽
1992 ◽
Vol 96
(26)
◽
pp. 10937-10941
◽
2008 ◽
Vol 112
(30)
◽
pp. 11181-11193
◽