Mineralogy of parent rock and peaty-podzolic soil of Iremel Ridge, Southern Urals
- Autores: Khalitov R.1, Perova E.1, Abakumov E.1,2, Suleimanov R.3
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Afiliações:
- St. Petersburg State University
- Institute of Ecology of the Volga River Basin
- Institute of Biology, Ufa Scientific Center
- Edição: Volume 50, Nº 8 (2017)
- Páginas: 961-970
- Seção: Soil Mineralogy and Micromorphology
- URL: https://journals.rcsi.science/1064-2293/article/view/224124
- DOI: https://doi.org/10.1134/S1064229317080063
- ID: 224124
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Resumo
The mineralogy of soils and parent rocks of the Iremel Ridge has been studied by the methods of micromorphology, laser diffraction, computed X-ray microtomography, and X-ray fluorescence analysis. In hard rock and soil, the major minerals have been identified: quartz, illite, and a chlorite-group mineral (Fe analogue of sudoite), as well as accessory minerals: monazite, xenotime, rutile, zircon, and florencite. It has been found that chlorite, illite, and quartz are present in all horizons of the studied peaty-podzolic soil. Insignificant amounts of mixed-layered mineral and kaolinite could be suggested in the T and EL horizons of peaty-podzolic soil. The mixed-layered mineral is most probably of soil origin, which is related to the transformation of illites inherited from the parent rock under acidic conditions.
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Sobre autores
R. Khalitov
St. Petersburg State University
Email: e_abakumov@mail.ru
Rússia, St. Petersburg, 199034
E. Perova
St. Petersburg State University
Email: e_abakumov@mail.ru
Rússia, St. Petersburg, 199034
E. Abakumov
St. Petersburg State University; Institute of Ecology of the Volga River Basin
Autor responsável pela correspondência
Email: e_abakumov@mail.ru
Rússia, St. Petersburg, 199034; Tol’yatti, 445003
R. Suleimanov
Institute of Biology, Ufa Scientific Center
Email: e_abakumov@mail.ru
Rússia, Ufa, 450054