کد مقاله | کد نشریه | سال انتشار | مقاله انگلیسی | نسخه تمام متن |
---|---|---|---|---|
1695379 | 1011857 | 2011 | 6 صفحه PDF | دانلود رایگان |
Samples of Araucária area soil from Paraná state, Brazil, were separated by particle size fractionation and investigated by electron paramagnetic resonance (EPR) in X-Band of 9.5 GHz at room temperature and 77 K, infra-red spectroscopy and X-ray diffractometry. The paramagnetic species in the soil samples were identified by comparison with EPR spectra of some minerals studied recently by our group, several soil types and/or soil components investigated in the literature. The value of g = 2.1 (ΔH = 85 mT) indicated the presence of ferrihydrite. Hematite was identified by g = 2.1 (ΔH = 100 mT) and g = 4.3 for Fe3+ lines of the concentrated dominium and diluted dominium. Kaolinite was identified by IR and EPR with the resonance at g = 4.3 attributed to Fe3+ ions in isolated sites of tetrahedral and octahedral symmetry with rhombic distortion. The resonances at g = 3.7 and g = 4.9 were attributed to Fe3+ in more highly symmetrical environment than rhombic symmetry, but not in axial symmetry. Three signals around g = 2 were attributed to radiation defects, plus additional resonances at g = 2.8 and 9.0. Signals less intense than those at g = 2.1, 3.7, and 6.5, observed for clear grains of soil, were attributed to presence of Fe3+ in quartz which was identified by IR and XDR.
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► The investigated Brazilian soils presented the EPR signals of ferrihydrite and hematite.
► Kaolinite was identified by IR and EPR.
► Defects in the kaolinite structure were detected by the EPR spectra.
► Less intense EPR signals were attributed to presence of Fe3+ in quartz.
Journal: Applied Clay Science - Volume 53, Issue 1, July 2011, Pages 42–47