dc.creator | Solt, Hanna | |
dc.creator | Lónyi, Ferenc | |
dc.creator | Mihályi, R. Magdolna | |
dc.creator | Valyon, József | |
dc.creator | Gutierrez, Laura Beatriz | |
dc.creator | Miro, Eduardo Ernesto | |
dc.date.accessioned | 2018-08-27T16:09:21Z | |
dc.date.accessioned | 2018-11-06T15:59:39Z | |
dc.date.available | 2018-08-27T16:09:21Z | |
dc.date.available | 2018-11-06T15:59:39Z | |
dc.date.created | 2018-08-27T16:09:21Z | |
dc.date.issued | 2008-12 | |
dc.identifier | Solt, Hanna; Lónyi, Ferenc; Mihályi, R. Magdolna; Valyon, József; Gutierrez, Laura Beatriz; et al.; A mechanistic study of the solid-state reactions of H-Mordenite with Indium(0) and Indium(III)oxide; American Chemical Society; Journal of Physical Chemistry C; 112; 12-2008; 19423-19436 | |
dc.identifier | 1932-7447 | |
dc.identifier | http://hdl.handle.net/11336/57192 | |
dc.identifier | CONICET Digital | |
dc.identifier | CONICET | |
dc.identifier.uri | http://repositorioslatinoamericanos.uchile.cl/handle/2250/1903306 | |
dc.description.abstract | Solid-state reactions of In2O3/H-mordenite and In0/H-mordenite mixtures (Al/In = 3) were studied using an atmospheric flow-through microreactor, diffuse reflectance Fourier-transform spectroscopy (DRIFTS), and X-ray powder diffractometry (XRD). The indium(III)oxide/H-mordenite mixture was heated in a flow of 2% H2/N2 gas mixture or pure N2 to 873 and 973 K, respectively. The indium(0)/H-mordenite mixture was heated in a dry and wet N2 stream to 673−973 K. The reactions were monitored by analyzing the effluent gas, using mass spectroscopy (MS). The protons of H-mordenite were exchanged for In+ cations, indicating that In3+ was reduced and In0 was oxidized in the exchange processes. In the process of reductive solid-state ion exchange (RSSIE), the indium was reduced by H2. In the oxidative solid-state ion exchange (OSSIE) process, the indium was oxidized by H2O. Results substantiate that the ion exchange proceeds through a volatile InOH intermediate. Formation of InOH and its rapid transport within the zeolite crystals requires the presence of water vapor. The In+ in the zeolite lattice can be oxidized by O2 or H2O to indium oxycations, most probably to InO+, while the obtained oxycations can be reduced in hydrogen back to In+. | |
dc.language | eng | |
dc.publisher | American Chemical Society | |
dc.relation | info:eu-repo/semantics/altIdentifier/doi/http://dx.doi.org/10.1021/jp804110d | |
dc.relation | info:eu-repo/semantics/altIdentifier/url/https://pubs.acs.org/doi/10.1021/jp804110d | |
dc.rights | https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ | |
dc.rights | info:eu-repo/semantics/restrictedAccess | |
dc.subject | SOLID STATE REACTIO | |
dc.subject | InHMORDENITE | |
dc.subject | OSSIE | |
dc.subject | RSSIE | |
dc.title | A mechanistic study of the solid-state reactions of H-Mordenite with Indium(0) and Indium(III)oxide | |
dc.type | Artículos de revistas | |
dc.type | Artículos de revistas | |
dc.type | Artículos de revistas | |