Formation of temperature regime of permafrost soils of the bases of buildings at the territory of multi-storey housing development of the city of Yakutsk
The results of long-term observations of the temperature regime of soils in the territory of the Yakutsk, as the largest city, built under the conditions of permafrost soils are presented. The process of forming the temperature regime of permafrost soils of bases of buildings and structures is considered. The main factors and regularities of the process are analyzed. The dynamics of temperature changes in permafrost soils at a depth of 10 meters over the entire observation period is presented. The results are compared with the data of other researchers. Measures are proposed to improve the monitoring of thermal regime of the foundations of capital buildings under the conditions of preservation of permafrost soils. The tendencies and regularities of the formation of the temperature regime of the soils of the foundations of buildings and structures in the territory of capital construction under the conditions of the cryolithozone are revealed. Relationship with climatic and technogenic impacts, as well as with problems arising during the operation of buildings and structures, has been established. The research results can be taken into account when designing and constructing buildings and structures in other areas of permafrost with similar geocryological conditions. Recommendations on the technical regulation of temperature regime monitoring of permafrost soils of the cryolithozone have been developed.