Structural-adsorption characteristics of natural and аcid-modified clinoptilolite

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dc.contributor.authorKiose, Tetiana O.en
dc.contributor.authorGolubchik, Khrystyna O.en
dc.contributor.authorRakytska, Tetiana L.en
dc.contributor.authorDlubovskyi, Ruslan M.en
dc.contributor.authorKara, A. L.en
dc.contributor.authorVolkova, V. Y.en
dc.contributor.authorКіосе, Тетяна Олександрівнаuk
dc.contributor.authorРакитська, Тетяна Леонідівнаuk
dc.date.accessioned2018-04-26T08:19:08Z
dc.date.available2018-04-26T08:19:08Z
dc.date.issued2016
dc.description.abstractNatural clinoptilolite (N-CLI) is a polyphase mineral containing clinoptilolite, -quartz, mordenite, and hematite at certain ratios. We use clinoptilolite in its acid-modified forms (H-CLIs) as a support for Pd(II)-Cu(II) complexes (Pd-Cu/Н-CLIs) characterized by catalytic properties in the reaction of CO oxidation. N-CLI used in the study was provided from Sokirnitskoye deposit (Trans-Carpathian region). (0.25-3)Н-CLI-0.5H-CLI samples were prepared by N-CLI boiling for 0.5 h in nitric acid solution at its concentrations ranged from 0.25 to 3 M. Since water molecules directly participate in the formation of Pd(II)-Cu(II) surface complexes, we investigated ad/desorption of water vapor into/from N-CLI, (0.25-3)Н-CLI-0.5, and Pd-Cu/Н-CLIs using well-known McBain gravimetric method.uk
dc.identifier.citationChemistry, Physics and Technology of Surface: Ukr. Conf. with Int. Particip. (17-18 May, 2016): Book Abstr.– Kiev, 2016.uk
dc.identifier.urihttps://dspace.onu.edu.ua/handle/123456789/14075
dc.language.isootheruk
dc.subjectpolyphase mineraluk
dc.subjectmodifieduk
dc.subjectclinoptiloliteuk
dc.subjectstructural-adsorptionuk
dc.titleStructural-adsorption characteristics of natural and аcid-modified clinoptiloliteuk
dc.typeArticleuk
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