The research touches upon marsh landscapes in the context of temperature monitoring and in connection with exogenous processes during engineering intervention. The monitoring of temperature regimes was conducted in the mid-taiga subzone of marsh landscapes for revealing the dynamics of exogenous processes. The authors used the method of recording systems for the field measurement of the temperature of the peat and underlying soils. The measurements were conducted on a territory that belongs to the middle taiga landscapes of Western Siberia. The authors of the research analyze the data obtained from thermowells 5, 5a and 6. During the observation period of 2015-2016, the average annual temperature was 8.3 ºC for thermowell 5a (technogenic area), which is 3.8 ºC and 4.2 ºC higher than the average annual values of thermowell 5 and thermowell 6 respectively. The latter belongs to natural marsh landscapes. Observations conducted in 2016-2017 confirmed this fact with a difference of 4.8 ºC and 3.7 ºC for thermowells 5 and 6 respectively. As compared to natural marsh landscapes not affected by man-made impact, a higher temperature was observed on soils, which affects the manifestation of exogenous processes.
Belyaev, V.I., Bondarovich, A. A. et al. (2017) Temperature Regime of Air and Soil According to the Meteorological and Soil-Hydrological Monitoring Network in the Kulunda Plain During the Vegetation Periods 2013-2016. Newsletter of the Altai State Agrarian University 3(149): 30-37.
Dyukarev, E. A. (2017) Partitioning of net ecosystem exchange using chamber measurements data from bare soil and vegetated areas. Agricultural and Forest Meteorology, 239: 236-248.
Dyukarev, E.A. (2017) Determining the Components of the Total Ecosystem Exchange of Carbon According to Automatic Chamber Measurements. In Lapshina, E. D., Mironycheva-Tokareva, N. P. (Eds.) Carbon Balance of the Bogs in Western Siberia in the Context of Climate Changes. Proceedings of the International Conference. Tomsk: Publishing House of Tomsk University, pp. 54-56.
Kazantsev, S. A. (2017) Digital Station of Ecological Monitoring. Interexpo Geo-Siberia 2(3): 46-49.
Konstantinov, P. Ya., Fedorov, A. N., Michimura, T., Iwahana, G., Yabuki, H., Iijima, Y., Costard F. (2011) Use of automatic recording devices (loggers) for temperature monitoring of permafrost soils. Cryosphere of the Earth XV(1): 23-32.
Korkin, S. E., Kail, E. K., Mironova, N. S. (2015) Anti-erosion organization of the territory of the Eastern part of the latitudinal segment of Ob river on the basis of monitoring data. Newsletter of Samara Scientific Center of the Russian Academy of Sciences 17(6): 104-109.
Korkin, S. E., Talyneva, O. Yu., Kail, E. K., Korkina, E. A., Isupov, V. A. (2017) Exogenous geodynamic processes of the central part West Siberia. Proceedings of the International Multidisciplinary Scientific GeoConferences SGEM, Sofia, Bulgaria, pp. 329-335.
Korkin, S. E, Korkina, E. A., Talyneva, O. Y. (2016) Risks of exogeodynamic processes in latitudinal segment of the Ob river. ARPN Journal of Engineering and Applied Sciences 11(19): 11333-11337.
Korkina, E. A. (2015) Self-Restoration of Middle Priob Soils Disturbed by Technogenesis: Monograph. Nizhnevartovsk: Publishing House of Nizhnevartovsk State University.
Lappalainen, H. K., Kerminen, V. M., Petäjä, T., Alekseychik, P., De Leeuw, G., Järvi, L., Järvinen, H., Kieloaho, A.J., Kujansuu, J., Duplissy, E.M., Mazon, S., Moisseev, D., Pihlatie, M., Sipilä, M., Vesala, T., Zilitinkevich, S., Kulmala, M., Vihma, T., Asmi, E., Laaksonen, A. et al. (2016) Pan-eurasian experiment (peex): towards a holistic understanding of the feedbacks and interactions in the land-atmosphere-ocean-society continuum in the northern Eurasian region. Atmospheric Chemistry and Physics 16(22): 14421-14461.
Liss, O. L., Abramova, L. I., Avetov, N. A. (2001) Marsh Systems of Western Siberia and Their Conservation Value. Tula: Grif and K.
Lopatina, K.I. (2012) Geoecological foundations for the use of peat bogs and forests of the Middle Ob Region. Tver: Publishing House “Triada”.
Melnikov, V.P., Drozdov, D.S., Pendin, V.V. (2016) Arctic Territories and Cryogenic Risks. Proceedings of the Scientific Congress of the 18th International Scientific and Industrial Forum. Nizhny Novgorod: Nizhny Novgorod State University of Architecture and Civil Engineering, pp. 496-502.
Orekhov, P. T. (2008) Landscape Differentiation of the Temperature Regime of Soils in the Northern Taiga of Western Siberia. Proceedings of the International Conference “Cryogenic Resources of Polar and Mountain Regions. State and Prospects of Engineering Permafrost” (Tyumen, April 21-24, 2008). Tyumen: Earth Cryosphere Institute of the Siberian Branch of the Russian Academy of Sciences, pp. 252-255.
Pavlov, A. V. (2008) Monitoring of Permafrost Zone. Novosibirsk: Academic Publishing House “Geo”.
Popov, E. Y., Romushkevich, R. A., Popov, Y. A. (2017) Measurements of the Thermal Properties of Rocks on Standard Samples as a Necessary Stage of Thermophysical Studies of Hydrocarbon Deposits. News of Higher Educational Institutions. Geology and Exploration 2: 56-70.
Prokushkin, A. S, Guggenberger, G. (2007) The Role of Climate in the Removal of Dissolved Organic Substances from the Watersheds of the Cryolithozone of Central Siberia. Meteorology and Hydrology 6: 93-105.
Sheinkman, V., Sedov, S., Shumilovskikh, L., Korkina, E., Korkin, S., Zinovyev, E., Golyeva, A. (2016) First results from the Late Pleistocene paleosols in northern Western Siberia: Implications for pedogenesis and landscape evolution at the end of MIS3. Quaternary International 418: 132-146.
Sheng, Y., Smith, L. C., MacDonald, G. M., Kremenetski, K. V., Frey, K. E., Velichko, A. A., Lee, M., Beilman, D. W., Dubinin, P. A. (2004) High-resolution GIS-based inventory of the West Siberian peat carbon pool. Global Biogeochemical Cycles 18: GB3004.
Vasiliev, A.A., Streletskaya, I.D., Oblogov, G.E., Shirokov, R.S. (2016) Dynamics of the Submarine Permafrost of the Kara Sea in Changing Climatic Conditions. Proceedings of the Fifth Conference of Russian Geocryologists / Part 5. Regional and Historical Geocryology. Part 6. Dynamic geocryology. Geocryological Processes and Phenomena. Part 7. Lithogenetic Geocryology (Cryolithogenesis). Sumy: Limited Liability Company “University Book” Publishing and Trading House, pp. 26-30.
Wisser, D., Marchenko, S. S., Talbot, J. et al. (2011) Soil temperature response to 21st century global warming: the role of and some implications for peat carbon in thawing permafrost soils in North America. Earth System Dynamics 2: 121-138.
Zang, Y., Chen, W., Smith, S. L. et al. (2005) Soil temperature in Canada during the twentieth century: Complex responses to anthropogenic climate change. Journal of Geophysical Research Journal of Geophysical. Research, 110: D03112.