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MAIN PAGE > Journal "Arctic and Antarctica" > Rubric "Grounds of Cold Regios"
Grounds of Cold Regios
Maslakov A. - The assessment of geocryological threats to the developed territories of Eastern Chukotka pp. 57-72


Abstract:  This article presents and tests the method of assessment of the various geocriological threats to the developed territories of Eastern Chukotka. The research is based on the complex of field geodesic, geophysical, and geocryological measurements conducted in the core settlement of the indicated region (Lorino), as well as archival data of the engineering surveys of previous years. Based on the acquired materials using the calculation methods, the author was able to determine the current geocryological situation in subsoil of the settlement along with the development level of the negative cryogenic processes and phenomena. In the course of this war was performed the assessment of threats associated with the changes in cryogenic situation and development of the negative cryogenic processes. As a result of this research, the author allocated the sections of settlement within which is traced the low level of natural sustainability of lithocryogenic ground in terms of technogenic disturbance, as well as high level of threat pertaining to decline in the carrying capacity of refrigerated piles and increase of tangential forces of frost heaving of soil.
Efimov V.M., Stepanov A.V., Tappyrova N.I., Kravtsova O.N., Stepanov A.A. - Impact of the freeze-thaw cycles upon the heat and mass transfer properties of the technogenic cryogenic soil of the northeastern regions of the cryolithozone pp. 73-79


Abstract: This article concentrates on the experimental research of the heat and mass transfer properties of the technogenic soil of Yakutia that are subject to freeze-thaw cycles. Definition is given to the technogenic soils according to the GOST 25100-95. The work cites the established fact of significant difference in the coefficient of filtration of naturally located soils of seasonal layer of thaw from indexes acquired in controlled conditions. It is substantiated that there is a need to research the heat and mass transfer properties of the technogenic soils with consideration of the cyclic impact of the low temperatures and changes in the cryogenic structure for a more complete correspondence with the northern conditions. The authors analyze  the acquired data, approximate the experimental data via the methods of statistical processing and compare it with the data from other sources. The conducted research allowed determining the dependence of the thermophysical properties of the technogenic soils upon their moisture, temperature and loam content.
Efimov V.M., Kravtsova O.N., Stepanov A.V., Timofeev A.V., Vasil'chuk Y.K., Tappyrova N.I. - Research on the impact of the surface active agents upon the strength of the frozen soil of the cryolithozone of the Sakha Republic (Yakutia) pp. 80-85


Abstract: This article focuses on the experimental research of the impact of additives of surface active agents upon the strength of the frozen dispersed soils. The work touches on the problem of finding new theoretical approaches towards mechanical properties of dispersed soils accounting for presence of free surface energy and impact of the physical chemistry factors upon the behavior and properties of the soils. Substantiation is made on the physical chemistry approach as the most promising one in this area. Pyotr Rebinder’s mechanism for strengthening thawed soils through the effects of the surface active agents is presented in this research. Experimental research was conducted on the strength characteristics of the frozen dispersed soils with use of surfactants and without additives. The conducted research yielded experimental curve relationship of the maximal strength from time for frozen sand and loam with surfactants and without.
Efimov V.M., Vasil'chuk Y.K., Rozhin I.I., Popenko F.E., Stepanov A.V. - Modeling of the temperature schedule of the soil foundations with thermal stabilizers in the cryolithozone of the Sakha Republic (Yakutia) pp. 86-97


Abstract: This article examines the issue of numerical modeling of the soil freezing-thaw process for projection of thermal stabilization system of soil building foundations in the cryolithozone of the Sakha Republic (Yakutia). The goal of this work consists in studying the process of formation of the temperature field of the massif of the soils under the effect of thermal stabilizers. Research is conducted on the process of formation of ice wall as the result of thermal exchange of the soil with the thermal stabilizers and external cool air during clearing of the snow cover from the construction site. The main conclusions of the conducted research include the need for development of mathematical models that would account for the mass exchange processes in the zones of effect of the thermal stabilizers with consideration of the conditions of formation of the cryogenic textures in the process of forced freezing of the soils. There is also a need for mathematical explanation of the phenomena of condensation and evaporation of Freon taking place inside the thermal stabilizers.
Efimov V.M., Popenko F.E., Rozhin I.I., Stepanov A.V., Bol'shev K.N. - Formation of the temperature of foundation soils during usage of thermal stabilizers in the conditions of the cryolithozone of the central Yakutia pp. 98-105


Abstract: The subject of this research is the interaction of the seasonal thermal stabilizers with the soils, processes of thermal and mass transfer and formation of cryotextures. The thermal stabilizers found broad implementation in northern construction for strengthening foundations of buildings formed with plastic and thawed dispersed soils with installation of Anti-filtration screens and ice walls. The efficiency of the work of thermal stabilizers is assessed based on the rate of formation of the calculated temperature schedule in foundations of engineering structures. The presented data of formation of temperatures of the soil foundations cooled by the liquid-vapor thermal stabilizers reflect regularities characteristic for dispersed soils of all types with various indexes of moisture and salinization for buildings with ventilated crawl spaces.  
Kotelevets D.V., Skobelev A.D. - The ice content and the porosity of frozen grounds of the Kharasavey gas field according to electrical sounding data pp. 116-125


Abstract: The research object is the frozen grounds of the Kharasavey gas field (the Yamal peninsula), occurring at a depth of 50 m. The purpose of the paper is to study the electrophysical characteristics of frozen grounds, depending on such factors as lithology, thawed and frozen state, water salinity, humidity and porosity. At a temperature higher than the congelation temperature, the electric characteristics almost don’t depend on the temperature, but upon getting beyond this temperature point, significant changes of characteristics can be observed – a part of interstitial water freezes and turns into dielectric ice. The research was carried out in summer 2015 and was based on the electrical resistivity tomography method with the diversity from 7,5 to 221,5 m, helping achieve the desired depth. The research was carried out using the electrical resistivity tomography station “Omega-48”. The electromagnetic survey of vertical electric sounding in the modification of electrical resistivity tomography helps detect electrical characteristics of massive materials and their spacing. On the obtained electrical resistivity tomography profile the authors extract the layer of frozen sand, but its freezing within the studied area is not solid – in the eastern part the sand freezing zone decreases due to the presence of lakes, hampering sand freezing. The authors have found the geocryological structure, resembling cryopeg in its form and structure, in the studied profile. 
Maslakov A. - The results of active layer studies near Lorino settlement, Eastern Chukotka pp. 127-139


Abstract: The paper contains the results of active layer studies in Lorino monitoring site (Eastern Chukotka, Russia), conducted in framework of the Circumpolar Active Layer Monitoring (CALM) program during 2010-2015. The study site includes tundra landscapes of Eastern Chukotka coastal lowlands. The main purpose of the paper is to obtain spatial and temporal patterns of seasonal melting distribution and reveal the main natural factors defining active layer depth within study site. The author demonstrates the predominance of thermal forcing in active layer development, which was strongly complicated by local (microrelief, vegetation, soil moisture, etc.) conditions. These factors determined high spatial and temporal variability of active layer thickness within single grid (100×100 m). The study also reveals the lack of statistical data on natural characteristics and the need for further detailed studies of seasonal melting process.
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