Zoning the territory in the northwest of Moscow according to the degree of karst and suffosion hazard

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The study of karst hazard associated with the suffusion is a very relevant topic for construction sites in Moscow upon performing engineering geological survey and developing means of protecting the territory. According to archival data, a site with an area of 4.9 km² in the north-west of the city belongs to “hazardous” category. Within this area, 42 karst sinkholes were recorded in the 20th century. In the article, the authors analyze the geological conditions of the site based on the study of more than 400 wells. The work attempts to find a connection between the parameters of the geological environment structure and the appearance of sinkholes. A map of the thickness of clay deposits overlying the karst horizon has been compiled. A new approach to zoning the territory according to the degree of karst hazard has been proposed, as a result of which the area of the territory classified as “hazard” is reduced to 2.50 km².

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作者简介

E. Romanova

Sergeev Institute of Environmental Geoscience, Russian Academy of Sciences; National Research Moscow State University of Civil Engineering

编辑信件的主要联系方式.
Email: romanova.elizaveta.r@yandex.ru
俄罗斯联邦, Ulanskii per. 13, str. 2, Moscow, 101000; Yaroslavskoe Shosse 26, Moscow, 129337

F. Bufeev

Sergeev Institute of Environmental Geoscience, Russian Academy of Sciences; S.Ordzhonikidze Russian State University for Geological Prospecting

Email: fbufeev@mail.ru
俄罗斯联邦, Ulanskii per. 13, str. 2, Moscow, 101000; ul. Miklukho-Maklaya 23, Moscow, 117997

参考

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  2. Anikeev, A.V. [Collapses and sinkholes in karst areas: mechanisms of formation, forecast and risk assessment]. Moscow, RUDN Publ., 2014, 328 p. (in Russian)
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1. JATS XML
2. Fig. 1. Layout of boreholes with underground karst manifestations.

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3. Fig. 2. Histogram of void heights.

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4. Fig. 3. Types of structure of the soil mass lying above the first layer of carbonate deposits from the surface.

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5. Fig. 4. Map of territory zoning by type of structure of the overlying mass.

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6. Fig. 5. Map of territory zoning by predominant degree of fracturing of the first layer of carbonate deposits from the surface.

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7. Fig. 6. Map of thickness of screening clay deposits overlying the first layer of carbonate deposits (limestone) from the surface.

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8. Fig. 7. Maps of territory zoning by thickness of clay deposits overlying the first layer of carbonate deposits (limestone) from the surface, by isopachs: a - 3 and 10 m, b - 5 and 12 m.

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9. Fig. 8. Zoning map of the territory: a - by isopachs of clay deposits of 3 and 12 m, b - by distance from the nearest surface manifestation of the karst-suffusion process.

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10. Fig. 9. Zoning map of the area previously completely classified as dangerous according to the degree of karst-suffusion hazard [9]: a - overview, b - fragment of the map at a scale of 1: 5,000.

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