Resource potential of Vorob’evy Gory geosystems: history, study, and prospects for development

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Abstract

The article based on the methodology of interdisciplinary research solves the problems of retrospective analysis of the resource potential dynamics of geosystem components in the natural reserve located within the boundaries of the largest megacity of Eurasia to diversify the resource potential of the ecological-educational function of its territory. The unique experience of stable functioning of recreational territory is systematized synchronously with socio-economic development of Moscow urban industrial agglomeration based on complex studies. Additionally, some parts of its territory were studied in order to actualize scientific and educational tasks of higher school. The study is based on systematic approach to clarify the ecological state of the components of the environment. Local areas of different vector dynamics of geosystems of different genesis were identified. The role of natural and natural-anthropogenic factors (geological-geomorphological, ecological-geochemical, geodynamic, geophysical, anthropogenic, socio-economic) in the formation of geo-ecological features of the recreational potential of the conservation area of the urban environment is differentiated. The dynamics of the resource potential of the recreational cluster of the megacity occurs synchronously with the growth of the urban population of the urban-industrial complex and depends on the totality of socio-economic, cultural-historical, geo-ecological conditions and the synergetic vector of their interaction. The interdisciplinary approach based on the processing of databases, field observations and laboratory studies allowed the authors to improve the methodology of setting scientific and educational tasks within the framework of the implementation of the ecological-educational function of protected areas. Specially protected natural territories of megacity contribute significantly to the achievement of goals of stable urban development, preservation of biodiversity of territories and recreation areas, predetermining the creation of a comfortable environment for the inhabitants of large cities, contributing to the minimization of health risks for different gender groups of the population.

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About the authors

T. A. Baraboshkina

Lomonosov Moscow State University

Author for correspondence.
Email: ecolab@mail.ru
Russian Federation, Leninskie Gory, 1, Moscow, 119234

E. N. Samarin

Lomonosov Moscow State University

Email: ecolab@mail.ru
Russian Federation, Leninskie Gory, 1, Moscow, 119234

I. V. Averin

Engineering Geology LLC

Email: i.averin@mail.ru
Russian Federation, ul. Yartsevskaya, 16, Moscow, 121351

R. Yu. Zhidkov

Moscow Trust of Geological, Geophysical and Cartographic Works

Email: rzhidkov@gmail.com
Russian Federation, ul. Zorge, 1, Moscow, 123308

N. N. Rakitina

Moscow Trust of Geological, Geophysical and Cartographic Works

Email: rzhidkov@gmail.com
Russian Federation, ul. Zorge, 1, Moscow, 123308

I. A. Rod’kina

Lomonosov Moscow State University

Email: ecolab@mail.ru
Russian Federation, Leninskie Gory, 1, Moscow, 119234

V. S. Rutskina

Medbridge LLC

Email: geovera@bk.ru
Russian Federation, ul. 5-ya Magistral’naya, 20, Moscow, 123007

T. N. Lubkova

Lomonosov Moscow State University

Email: ecolab@mail.ru
Russian Federation, Leninskie Gory, 1, Moscow, 119234

O. A. Lipatnikova

Lomonosov Moscow State University

Email: ecolab@mail.ru
Russian Federation, Leninskie Gory, 1, Moscow, 119234

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Supplementary files

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2. Fig. 1. Visual retrospective of the dynamics of geosystems of protected areas in the area of ​​the Luzhnetskaya bend of the Moscow River: a - in the 19th century (based on the painting by I.K. Aivazovsky, 1848) [1], b - in the 21st century [8], c - photo recording of the slope of Vorobyovy Gory from the metro bridge (T.A. Baraboshkina, 2023).

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3. Fig. 2. Map-scheme of the thickness of technogenic deposits in the territory of Vorobyovy Gory and its environs (indicating areas of significant transformation of the resource of geological space according to data from the State Budgetary Institution Mosgorgeotrest [10]).

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4. Fig. 3. Discharge of groundwater (highlighted in red) at the foot of the slope of the Sparrow Hills.

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5. Fig. 4. Historical visual retrospective of the escalator gallery and tree stand on the territory of Vorobyovy Gory: transformation of the gallery [9] (a) and phytocenoses (b) under the influence of geodynamic processes; c - reconstruction of the escalator gallery on 23.12.2022 - optimization of the recreational cluster (Photo by T.A. Baraboshkina, 2023).

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6. Fig. 5. Integrated diagram of the location of monitoring points based on data from the State Budgetary Institution “MosEcoMonitoring” and Stiff’s diagram [31] of the macrocomponent composition of spring waters (a); the content of microelements (in Kpdk values) in the water of springs studied in 2022 (b).

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7. Fig. 6. Map-scheme of zoning of soil cover (edaphotope) of the Vorobyovy Gory territory by the value of the total indicator (Zc): acceptable category – Zc < 16; moderately hazardous – Zc = 16–32; hazardous – Zc = 32–128; extremely hazardous – Zc > 128.

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