Sorption of Cr3+ on clinoptilolite tuff: A structural investigation
Autor: | Iztok Arčon, Štefica Cerjan Stefanović, Nataša Logar, Janez Kovač, Mario Šiljeg, Venčeslav Kaučič, Nataša Novak Tušar, Anton Meden |
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Rok vydání: | 2006 |
Předmět: |
X-ray absorption spectroscopy
Clinoptilolite Extended X-ray absorption fine structure Absorption spectroscopy Chemistry Analytical chemistry chemistry.chemical_element clinoptilolite zeolite chromium-loaded Cr3+ XANES EXAFS XPS General Chemistry Condensed Matter Physics Chromium X-ray photoelectron spectroscopy Mechanics of Materials General Materials Science Zeolite |
Zdroj: | Microporous and Mesoporous Materials. 93:275-284 |
ISSN: | 1387-1811 |
DOI: | 10.1016/j.micromeso.2006.02.026 |
Popis: | A Cr 3+ -modified natural zeolite sample from the deposit of Donje Jesenje (Croatia) was structurally studied using X-ray powder diffraction (XRPD), scanning electron microscopy (SEM), energy dispersive X-ray analysis (EDXS), inductively coupled plasma mass spectrometry (ICP-MS), X-ray photoelectron spectroscopy (XPS) and X-ray absorption spectroscopy (XAS). The analyses revealed the presence of up to 0.4 wt% of chromium in the clinoptilolite crystals. The X-ray photoelectron spectroscopy depth analysis suggested a uniform distribution of chromium from the surface of the crystallites to the depth of 50(3) nm. The study of local environment of chromium by XANES (X-ray absorption near edge structure) showed that chromium cations in the sample were predominantly in the 3+ oxidation state. EXAFS (extended X-ray absorption fine structure) analysis revealed that Cr 3+ cations bond to six oxygen atoms at the distance of 1.97(2) A and two chromium atoms at the distance of 2.54(2) A suggesting that Cr 3+ cations most probably arrange in the zeolite pores in the form of small clusters of CrO 6 octahedra. The chromium could not be completely desorbed from the sample after post-treatment with NaCl or HCl solutions thus indicating mostly irreversible sorption of chromium in the zeolite. |
Databáze: | OpenAIRE |
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