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
On the upward migration of nickel and copper in the formation of salt halos in moraine sediments
1969 N. F. Mayorov
Stability of the roof near karst disturbances at the Leningrad shale deposit based on density γ-γ- logging data
1969 E. P. Popov
Use of vertical zonality of primary halos in estimation of erosional cut of tin ore bodies of Primorye region
1969 N. V. Nikitin