On the geochemistry of uranium in channel sediments of the hydrosystem of mountain taiga area
Authors:
Abstract
The studied areas of mountainous taiga terrain are developed mainly by eruptive rocks of granitoid series. All sites are located in a typically humid zone. The valleys of rivers and springs are forested, often swamped, channel sediments contain abundance of organic matter in the form of fallen leaves, needles, etc. The relief is medium-sized, but rather strongly indented. Exposedness is poor, eluvial-deluvial deposits 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 swamped.
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. Geochemistry, No. 4, 1956.
- Basic features of uranium geochemistry. PH AS USSR, M., 1963.
- Strakhov N. M. et al. Formation of sediments in modern reservoirs. PH AS USSR, 1954.
- Towson L. V. Geochemistry of Rare Elements in Granitoids. PH AS USSR. М., 1961.
Similar articles
Use of vertical zonality of primary halos in estimation of erosional cut of tin ore bodies of Primorye region
1969 N. V. Nikitin
Stability of the roof near karst disturbances at the Leningrad shale deposit based on density y-y logging data
1969 E. P. Popov
Influence of climatic factors on the formation of secondary halos of lead and zinc in Eastern Transbaikalia
1969 I. N. Kritsuk