1990
DOI: 10.1016/0144-2449(90)90080-b
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The state of iron in natural zeolites: A Mössbauer study

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Cited by 45 publications
(11 citation statements)
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“…However, this result cannot be considered conclusive, since oxidation of the ferrous species may occur on the surface of the zeolite upon contact with air at room atmosphere as observed by Weidenthaler [37], thus appearing as ferric species in the samples T + FeAs1, T + FeAs2, T + FeAs3, and T + FeAs7 in Table 4. The values gathered in this table suggest that Fe 2+ in the T + Fe(II) sample, and Fe 3+ in the T + Fe(III) samples before and after arsenite adsorption have octahedral and tetrahedral coordination, respectively, according to Roque-Malherbe [50] and Fejes [39].…”
Section: Ex Situ Solid Phase Studies Of Iron-loaded Tuffs After Arsenmentioning
confidence: 94%
“…However, this result cannot be considered conclusive, since oxidation of the ferrous species may occur on the surface of the zeolite upon contact with air at room atmosphere as observed by Weidenthaler [37], thus appearing as ferric species in the samples T + FeAs1, T + FeAs2, T + FeAs3, and T + FeAs7 in Table 4. The values gathered in this table suggest that Fe 2+ in the T + Fe(II) sample, and Fe 3+ in the T + Fe(III) samples before and after arsenite adsorption have octahedral and tetrahedral coordination, respectively, according to Roque-Malherbe [50] and Fejes [39].…”
Section: Ex Situ Solid Phase Studies Of Iron-loaded Tuffs After Arsenmentioning
confidence: 94%
“…It is reasonable to consider that Na, Mg, K and Ca are the extraframework cations that compensate for the deficiency of negative charge in the zeolite network [25,26]. A Mössbauer study [27] of iron-containing zeolitic rocks from several countries (Mexico, Cuba, Czech Republic, and the Russia) showed that iron is located as high spin Fe 3+ in framework tetrahedral sites, in extraframework octahedral sites as free Fe(H 2 O) 6 3+ , and as high spin Fe 2+ in octahedral coordination in extraframework sites or in another aluminosilicate associated with the zeolite. Iron is also located in magnetite contained in the zeolite rocks.…”
Section: Elemental Compositionmentioning
confidence: 99%
“…The fact that only 1.6 mole% of Fe 3+ ions present in the original material was extracted is probably due to the fact that Fe3 § is replacing tetrahedral AP + in the framework (Roque-Malherbe et al, 1990).…”
Section: Chemical Composition Of the Samplesmentioning
confidence: 99%
“…The natural clinoptilolite used has a degree of purity higher than 85% (Roque-Malherbe et al, 1990) mordenite, calcite, and or-quartz being the major impurities. The chemical composition of the mineral (wt%) is: SiO2 68.05; A1203 12.3; TiO2 0.40; Fe203 1.34; CaO 3.70; MgO 1.03; Na20 0.43; K20 1.70 and H20 11.06.…”
Section: Sample Preparationmentioning
confidence: 99%