1985
DOI: 10.1021/j100267a028
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Studies of the interaction of palladium(3+) and palladium(1+) with organic adsorbates, water, and molecular oxygen in palladium-Ca-X zeolite by electron spin resonance and electron spin-echo modulation spectroscopy

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Cited by 49 publications
(30 citation statements)
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“…Kasai et al suggested that the reduction of Cu(II) ions in Cu-exchanged mordenite observed when heating in a vacuum is due to reduction by residual water. Michalik et al also showed that retained water in PdCa−X zeolite plays a significant role in the reduction of Pd upon heating in a vacuum. However, in our case, dehydration generates a framework defect and a much stronger Ni(I) signal in the ion-exchanged sample, whereas in the synthesized sample, the Ni(I) signal is weaker and is produced along with a free radical.…”
Section: Discussionmentioning
confidence: 99%
“…Kasai et al suggested that the reduction of Cu(II) ions in Cu-exchanged mordenite observed when heating in a vacuum is due to reduction by residual water. Michalik et al also showed that retained water in PdCa−X zeolite plays a significant role in the reduction of Pd upon heating in a vacuum. However, in our case, dehydration generates a framework defect and a much stronger Ni(I) signal in the ion-exchanged sample, whereas in the synthesized sample, the Ni(I) signal is weaker and is produced along with a free radical.…”
Section: Discussionmentioning
confidence: 99%
“…Kasai et al suggested that the reduction of Cu(II) ions in Cu(II)-exchanged modenite zeolite that occurs upon heating in a vacuum is due to reduction by residual water . Michalik et al suggested that water in PdCa-X zeolite plays a role in the reduction of Pd(II) upon heating in a vacuum …”
Section: Discussionmentioning
confidence: 99%
“…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%