Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
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.
Язык оригинала | английский |
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Страницы (с-по) | 961-970 |
Число страниц | 10 |
Журнал | Eurasian Soil Science |
Том | 50 |
Номер выпуска | 8 |
DOI | |
Состояние | Опубликовано - 1 авг 2017 |
ID: 9156847