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The deep exploitation of mineral deposits is carried out in many areas around the world. However, one of its negative consequences is surface deformations. These may be discontinuous deformations (sinkholes) or continuous deformations (subsidence basins). Under specific hydrogeological conditions, these forms are inundated, and thus anthropogenic reservoirs are formed. In some post-mining areas, the number of such reservoirs is so large that they are referred to as “anthropogenic lake districts”. Depending on the geological structure of the deposit and the mining technique, these reservoirs may have different morphometric parameters. Moreover, they may show various hydrological conditions and physicochemical properties of their waters. The article describes a unique group of anthropogenic water reservoirs created due to the flooding of deep salt mines on the Solotvyno mining field. Although small in terms of the area, it includes a group of anthropogenic water reservoirs highly diverse in terms of their genetics, hydrology and hydrochemistry. Some of them represent a unique type of meromictic reservoirs. This research shows the direction in which water conditions may change in other mining areas with significant surface deformation across the globe.
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Tom
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10--16
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Bibliogr. 18 poz., fot., rys., tab., wykr.
Twórcy
autor
- University of Silesia, Faculty of Natural Sciences, Institute of Earth Sciences, 60 Będzińska St., 41-200 Sosnowiec, Poland, tadeusz.molenda@us.edu.pl
autor
- University of Silesia, Faculty of Natural Sciences, Institute of Earth Sciences, 60 Będzińska St., 41-200 Sosnowiec, Poland, ireneusz.malik@us.edu.pl
autor
- University of Silesia, Faculty of Natural Sciences, Institute of Earth Sciences, 60 Będzińska St., 41-200 Sosnowiec, Poland, joanna.kidawa@us.edu.pl
Bibliografia
- Andrejchuk, V. (2002) “Collapse above the world’s lergest potash mine (Ural, Russia),” International Journal of Speleology, 31(1/4), pp. 137–158. Available at: https://doi.org/10.5038/1827-806X.31.1.8.
- Dyakiv, V.O. (2012) “Zakonomirnosti rozvytku tekhnohenno aktyvizovanoho solyanoho karstu v protsesi zatoplennya shakht № 8 ta № 9 Solotvynsʹkoho solerudnyka [Conformities to the law of development of technogenic activated salt karst in the process of submergence of mines No. 8 and No. 9 of the “Solotvinsky Saltmine”],” in F.V. Zuzuk et al. (eds.) Pryroda Zakhidnoho Polissya ta prylehlykh terytoriy [The nature of the Western Polesia and adjacent territories], 9, Luts'k: Volyn. nats. un-t im. Lesi Ukrayinky, pp. 69–79.
- Ford, D. and Williams, P. (1989) Karst geomorphology and hydrology. London: Unvin Hyman.
- Górniak, A. and Kajak, Z. (2020) Hydrobiologia – Limnologia [Hydrobiology – Limnology]. Warszawa: Wydawnictwo Naukowe PWN.
- Gutry-Korycka, M. and Werner-Więckowska, H. (1996) Przewodnik do hydrograficznych badań terenowych [A guide to hydrographic field research]. Warszawa: Wydawnictwo Naukowe PWN.
- Hammer, U.T. (1986) Saline lake ecosystems of the world. Dordrecht: Dr W. Junk Publishers.
- Hrdinka, T. et al. (2013) “The unique environment of the most acidified permanently meromictic lake in the Czech Republic,” Limnologica – Ecology and Management of Inland Waters, 43, pp. 417–426. Available at: https://doi.org/10.1016/j.limno.2013.01.005.
- Khilchevskyi, V. et al. (2020) “Hydrographic characteristic of ponds distribution in Ukraine – Basin and regional features,” Journal of Water and Land Development, 46, pp. 140–145. Available at: https://doi.org/10.24425/jwld.2020.134206.
- Lachhab, M. et al. (2022) “Salinisation process of Lake Sidi Boughaba, Kenitra, North Western, Morocco: A statistical approach,” Journal of Water and Land Development, 54, pp. 194–200. Available at: https://doi.org/10.24425/jwld.2022.141572.
- Macioszczyk, A. and Dobrzyński, D. (2002) Hydrogeochemia [Hydro-geochemistry]. Warszawa: Wydawnictwo Naukowe PWN.
- Molenda, T. (2014) “Impact of saline mine water: Development of a meromictic reservoir in Poland,” Mine Water and the Environment, 33, pp. 327–334. Available at: https://doi.org/10.1007/s10230-014-0262-z.
- Molenda, T. (2015) “Conditions for development of anthropogenic meromictic reservoirs in the workings of crystalline rocks (based on the examples of the quarries of the Žulovská pahorkatina, NE Czech Republic),” Environmental Earth Sciences, 74, pp. 2259–2271. Available at: https://doi.org/10.1007/s12665-015-4217-x.
- Molenda, T., Ciupa, T. and Suligowski, R. (2020) “The properties of reservoir water in post-mining excavations of Cambrian and Devonian quartzite sandstones (Holy Cross Mountains),” Environmental Earth Sciences, 79, 310. Available at: https://doi.org/10.1007/s12665-020-09054-8.
- Molenda, T. and Kidawa, J. (2020) “Natural and anthropogenic conditions of the chemical composition of pit lake waters (Based on example pit lakes from Central Europe),” Mine Water and the Environment, 39(3–4), pp. 473–480. Available at: https://doi.org/10.1007/s10230-020-00660-3.
- Mycielska-Dowgiałło, E. et al. (2001) Geomorfologia dynamiczna i stosowana [Dynamic and applied geomorphology]. Warszawa: Wydział Geografii Uniwersytetu Warszawskiego.
- Pulina, M. (1999) Kras – formy i procesy [Karst – forms and processes]. Katowice: Wydawnictwo Uniwersytetu Śląskiego.
- Rzętała, M. (2008) Funkcjonowanie zbiorników wodnych oraz przebieg procesów limnicznych w warunkach zróżnicowanej antropopresji na przykładzie regionu górnośląskiego [Functioning of water reservoirs and the course of limnic processes in conditions of diverse anthropopressure on the example of the Upper Silesian region]. Katowice: Wydawnictwo Uniwersytetu Śląskiego.
- Żurek, R. et al. (2018) “Unique pit lake created in an opencast potassium salt mine (Dombrovska Pit Lake in Kalush, Ukraine),” Mine Water and the Environment, 37, pp. 456–469. Available at: https://doi.org/10.1007/s10230-018-0527-z.
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Bibliografia
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