1987
DOI: 10.1007/bf03155660
|View full text |Cite
|
Sign up to set email alerts
|

Catalytically important metal ion intermediates on zeolites and silica surfaces

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1
1

Citation Types

1
17
0

Year Published

1988
1988
2021
2021

Publication Types

Select...
7
2
1

Relationship

1
9

Authors

Journals

citations
Cited by 33 publications
(18 citation statements)
references
References 44 publications
1
17
0
Order By: Relevance
“…For both modes of alumina incorporation into Pd/SZ, the sample spectra collected at 300 K in Figure a,b show the presence of Pd + species indicated by the g ∥ factor of 2.3 and the g ⊥ factor of 2.13, as well as the g ∥ factors at 2.85 and 2.68. These species are likely formed as a result of the partial transformation of Pd 2+ species through an interaction with Pd 0 . , Zr 3+ species were also observed in the samples based on the g ⊥ factor at 1.975 and the g ∥ factor at 1.96 …”
Section: Results and Discussionmentioning
confidence: 72%
“…For both modes of alumina incorporation into Pd/SZ, the sample spectra collected at 300 K in Figure a,b show the presence of Pd + species indicated by the g ∥ factor of 2.3 and the g ⊥ factor of 2.13, as well as the g ∥ factors at 2.85 and 2.68. These species are likely formed as a result of the partial transformation of Pd 2+ species through an interaction with Pd 0 . , Zr 3+ species were also observed in the samples based on the g ⊥ factor at 1.975 and the g ∥ factor at 1.96 …”
Section: Results and Discussionmentioning
confidence: 72%
“…5,6,[8][9][10] On the basis of the absence of deuterium modulation from D 2 O and a weak interaction between Cu 2+ and adsorbed ethylene (C 2 D 4 ) in the ESEEM studies, 5, 23 Kevan's group suggested that Cu 2+ was located at site II′ displaced 0.12 nm from the six-ring plane into the cage and coordinated to three O(3) atoms. 11,23 On the other hand, Schoonheydt located Cu 2+ in the dehydrated species at site II on the basis of the diffuse reflectance spectrum. 8 When Cu 2+ is in a trigonal plane, the plane of maximum probability amplitude of the singly occupied 3d orbital coincides with the trigonal plane and the g z direction invariably is perpendicular to this plane.…”
Section: Discussionmentioning
confidence: 99%
“…1, faujasite) the g 8 and A 8 (Cu) values have usually been interpreted based on the well established distinct cation sites within the faujasite structure. 69,70 However, based on earlier suggestion derived from 27 Al electronspin echo envelope modulation (ESEEM) spectroscopy, 71 an extensive theoretical analysis of the g-tensor and the optical spectra of Cu 21 in dehydrated zeolites A, ZK-4 and Y challenged this traditional assignment proposing that the EPR parameters are instead related to the number of Al atoms in the six-membered ring. 72 This study has also shown that in the dehydrated zeolites Cu 21 adapts a tetragonal coordination sphere by coordinating four zeolite oxygens and not three as previously believed.…”
Section: Exchanged Transition Metal Ionsmentioning
confidence: 99%