On the geochemistry of uranium in channel sediments of the hydrosystem of mountain taiga area
Authors:
Abstract
The studied areas of mountain-taiga terrain are developed mainly by igneous rocks of the granitoid series. All sites are located in a typically humid zone. The valleys of rivers and streams are forested, often swampy; stream channel sediments contain an abundance of organic matter in the form of fallen leaves, needles, etc. The relief is medium-mountain, but rather strongly dissected. Exposure is poor; eluvial‑deluvial deposits are of medium‑clastic character with a small (up to 20 cm) soil layer. The thickness of loose formations usually does not exceed 2‑3 m. Flat tops are often swampy.
Область исследования:
(Archived) Without section
Funding:
None
References
- Manskaya S. M., Drozdova G. V., Emelyanova M. P. Binding of uranium by humic acids and melanoidins. Geokhimiya, No. 4, 1956.
- Basic features of uranium geochemistry. Izd-vo AN SSSR, M., 1963.
- Strakhov N. M. et al. Formation of sediments in modern reservoirs. Izd-vo AN SSSR, 1954.
- Tauson L. V. Geochemistry of Rare Elements in Granitoids. Izd-vo AN SSSR, M., 1961.
Similar articles
Some features of secondary gamma spectra in line-of-sight geometry and their use in X-ray radiometric method
1969 V. N. Mitov, Yu. P. Yanshevskiy, E. P. Leman
Determination of ore density and heavy element content from two conjugate measurements of scattered u γ-γ-radiation
1969 V. A. Artsybashev, G. A. Ivanyukovich