Mineralogy of parent rock and peaty-podzolic soil of Iremel Ridge, Southern Uralsстатья
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Дата последнего поиска статьи во внешних источниках: 20 января 2021 г.
Авторы:
Khalitov R.M.,
Perova E.N.,
Abakumov E.V.,
Suleimanov R.R.
Журнал:
Eurasian Soil Science
Том:
50
Номер:
8
Год издания:
2017
Издательство:
Maik Nauka/Interperiodica Publishing
Местоположение издательства:
Russian Federation
Первая страница:
961
Последняя страница:
970
DOI:
10.1134/S1064229317080063
Аннотация:
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. © 2017, Pleiades Publishing, Ltd.
Добавил в систему:
Сулейманов Руслан Римович