Cryogenesis of lithogenic basis of landscapes in the North-East of Russia and prevention of its negative manifestations
Authors:
About authors
- North-Eastern Permafrost Research Station IPF SB RAS
Abstract
Ameliorative development of the territories formed by permafrost is accompanied by changes in the conditions of external heat exchange and, as a result, increase in the depth of seasonal thawing with manifestation of thermal subsidence, thermal erosion and other phenomena, as well as the phenomenon of waterlogging. Prevention of negative processes is achieved by eliminating barriers of drainage surfaces and creating slopes of frozen water table, increasing the depth of thawing and drainage channels.
Similar articles
Features of karst processes by the example of the Urals
2003 A. Ya. Gaev, Yu. A. Kilin, S. G. Dubeikovskii, V. P. Semakin
Assessment of the probability of involvement in the development of mineral reserves with different levels of availability
2003 K. N. Trubetskoi, A. A. Peshkov, N. A. Matsko