The Input of the Climatic Factors in the Temperature Regime of Soils of Discontinuous Permafrost of Northern Taiga of Western Siberia
The results of the four-year study of the temperature regime of soils of three common landscapes of northern taiga in Western Siberia, located in the area of discontinuous permafrost, are presented. The soils of lumpy peatlands are characterized by mild permafrost annual regime with very cold summer...
Main Authors: | O. Yu. Goncharova, G. V. Matyshak, A. A. Bobrik, D. G. Petrov, M. O. Tarkhov, M. M. Udovenko |
---|---|
Format: | Article |
Language: | Russian |
Published: |
V.V. Dokuchaev Soil Science Institute
2017-03-01
|
Series: | Бюллетень Почвенного института им. В.В. Докучаева |
Subjects: | |
Online Access: | https://bulletin.esoil.ru/jour/article/view/255 |
Similar Items
-
Aufeises of the Siberian permafrost zone and increase of the river channel nets
by: V. R. Alekseev
Published: (2015-03-01) -
Equipment and Technology Application for Washing Highly Saline Soils
by: F. U. Zhuraev, et al.
Published: (2020-06-01) -
The use of group composition of iron compounds for diagnostics of mountain soils in the middle Urals
by: I. A. Samophalova, et al.
Published: (2015-07-01) -
Diagnostic properties and classification of forest steppe soil The Vorona-Tsna interfluve of The Provolzhskaya upland
by: E. A. Levchenko, et al.
Published: (2017-05-01) -
CHANGING PROPERTIES OF THE MESOTROPHIC PEAT SOIL IN GRAIN-ROW CROP ROTATION UNDER THE INFLUENCE OF FERTILIZERS AND LIME
by: I. I. Lytkin
Published: (2012-12-01)