Use of isotope data (δ2H, δ18O, 234U/238U) in the study of permafrost degradation processes as a result of long-term climate variations
Authors:
About authors
- St. Petersburg Branch of the Institute of Geoecology, RAS
Abstract
Marked warming of a climate has one of the results the degradation of a permafrost. Estimation of this degradation rates are necessary for considering at studying resources and qualities of underground waters, construction of long-term constructions, a burial place of radioactive waste, reconstruction of paleoclimate, etc. In this article it is considered theoretical bases and an opportunity of use developed by the author’s technique, which is based on isotope systematics δ2Н, δ18О, 234U/238U and U/He, 3Н/3Не dating of groundwater, and also correlations between them for reconstruction of rates of the permafrost degradation.
Область исследования:
(Archived) Problems of hydrogeological and engineering-geological conditions assessment in the development of territories
Funding:
None
Similar articles
Results of magnetotelluric studies on the Batolit profile (south of the Siberian platform)
2008 A. M. Pashevin, V. A. Tupitsin, V. V. Gomulskiy
Mineral-matrix technology of polluted water treatment as one of the promising directions of modern hydrogeology
2008 E. V. Shcherbakova