Published date:Feb 11 2022

Journal Title: KnE Social Sciences

Issue title: Integration Processes in the Russian and International Research Domain: Experience and Prospects

Pages:93–97

DOI: 10.18502/kss.v7i3.10428

Olga BakhmetDepartment of Multidisciplinary Scientific Research of Karelian Research Centre of the RAS

Maria Medvedevamariamed@mail.ruForest Research Institute of Karelian Research Centre Russian Academy of Sciences

Gulnara AkhmetovaForest Research Institute of Karelian Research Centre Russian Academy of Sciences

The article discusses the methodology of organizing soil monitoring in the territory of Eastern Fennoscandia. The history of developing monitoring studies of soils is presented. The main stages of monitoring are shown. Soil monitoring requires an adequate selection of indicators to match the type of impact and the mission of the monitoring. The importance of complex studies in soil monitoring is shown. It is noted that it is possible to change the monitoring objects in response to the increase in anthropogenic impact. The need for international cooperation in monitoring the natural environment in connection with global climate change is discussed. Continuous and consistent observations based on integrated research are what enable a reliable assessment of the current state of the natural environment in protected areas. This particularly applies to soil monitoring in valuable UNESCO heritage sites (e.g., rock art – White Sea and Lake Onega petroglyphs).

Keywords: natural environment, protected areas, soil monitoring

[1] Tevini M, Teramura AH. UV-B effects on terrestrial plants. Photochemistry and Photobiology. 1989; 50:479-487.
[2] Mironov VL, Kondratev AY, Mironova AV. Sphagnum growth as an indicator of wavelength-specific UV-B penetration through the ozone layer. Ecological Indicators. 2020; 116:106430.
[3] Mironov VL, Grabovik SI, Ignashov PA, Kantserova LV. Geotropic curvatures of Sphagnum: Environmental features of their genesis and trial application for estimation shoot length increment. Arctoa. 2016; 25:353–363.
[4] Mironov VL, Kondratev AY, Mironova AV. Growth of Sphagnum is strongly rhythmic: Contribution of the seasonal, circalunar and third components. Physiologia Plantarum. 2020; 168:765-776.
[5] Field guide for identification of Russian soils. Moscow: Dokuchaev Soil Science Institute; 2008. [in Russian]
[6] Israel YA. Global observing system. Forecast and assessment of environmental changes. Basics of monitoring. Journal of Meteorology and Hydrology. 1974;7:3-8.
[7] Page-Dumroese, Deborah S.; Sanchez, Felipe G.; Udawatta, Ranjith P.; Perry, Charles (Hobie); Gonzalez, Grizelle. 2021. Soil health assessment of forest soils [Chapter 6]. In: Karlen D.L., Stott D.E., Mikha M.M. Approaches to Soil Health Analysis (First Edition, Vol. 1). Soil Health Series, Soils Science Society of America. USA: Set. John Wiley & Sons. p. 100-138. 2021.
[8] Shishov LL, Tonkonogov VD, Lebedeva II, Gerasimova MI. Classification and diagnostic system of Russian soils. Smolensk: Oikumena; 2004.
[9] World reference base for soil resources. International soil classification system for naming soils and creating legends for soil maps. Update 2015. World soil resources reports. International Union of Soil Sciences Working Group World Reference Base for Soil Resources 2014;106:1-192.