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RESEARCH PRODUCT
Iron-containing phases in metallurgical and coke dusts as well as in bog iron ore
Marzena RachwałTadeusz MagieraKatarzyna BrzózkaM. GawrońskiJoanna Kyzioł-komosińskaM. Gzik-szumiataB. GórkaTadeusz Szumiatasubject
Nuclear and High Energy PhysicsBog ironSciencebog ore02 engineering and technology010501 environmental sciences01 natural sciencesSafety Risk Reliability and QualityWaste Management and DisposalInstrumentation0105 earth and related environmental sciencesMossbauer spectrometrycoke dustsQMetallurgybog ore; phase analysisCoke021001 nanoscience & nanotechnologyCondensed Matter PhysicsMagnetic susceptibilityMössbauer spectrometryphase analysisNuclear Energy and Engineeringmetallurgical dusts0210 nano-technologyPhase analysismagnetic susceptibilitydescription
Abstract Several samples of dusts from steel and coke plants (collected mostly with electro filters) were subjected to the investigation of content of mineral phases in their particles. Additionally, sample of bog iron ore and metallurgical slurry was studied. Next, the magnetic susceptibility of all the samples was determined, and investigations of iron-containing phases were performed using transmission Mössbauer spectrometry. The values of mass-specific magnetic susceptibility χ varied in a wide range: from 59 to above 7000 × 10−8 m-3·kg−1. The low values are determined for bog iron ore, metallurgical slurry, and coke dusts. The extremely high χ was obtained for metallurgical dusts. The Mössbauer spectra and X-ray diffraction patterns point to the presence of the following phases containing iron: hematite and oxidized magnetite (in coke and metallurgical dusts as well as metallurgical slurry), traces of magnetite fine grains fraction (in metallurgical dusts), amorphous glassy silicates with paramagnetic Fe3+ and Fe2+ ions, traces of pyrrhotite (in coke dusts), α-Fe and nonstoichiometric wüstite (in metallurgical slurry), as well as ferrihydrite nanoparticles (in bog iron ore). For individual samples of metallurgical dusts, the relative contributions of Fe2+/3+ ions in octahedral B sites and Fe2+ ions in tetrahedral A sites in magnetite spinel structure differs considerably.
year | journal | country | edition | language |
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2017-06-09 | Nukleonika |