Skip to main content
Log in

Isotope-Hydrochemical Study of Natural Waters on the Western Border of the Ufa Plateau

  • HYDROCHEMISTRY, HYDROBIOLOGY, ENVIRONMENTAL ASPECTS
  • Published:
Water Resources Aims and scope Submit manuscript

Abstract

Based on studies conducted in 2017, the features of formation and changes in the isotopic (δ18O and δ2H) and chemical composition of natural waters on the western border of the Ufa plateau were revealed. Within the Ufa plateau, waters were tested in three hydrodynamic zones of the Orda cave and the adjacent territory. Changes in the isotope-hydrochemical parameters in the horizontal and vertical directions are noted. Data from isotope-hydrochemical monitoring allowed us to establish that the replenishment of groundwater reserves on the western border of the Ufa plateau occurs mainly due to isotopically light winter precipitation, which is explained by the speed of water exchange in the karst system and the time of atmospheric precipitation in the aquifer. According to isotope data, the time of water inflow from the basin of aquifer into the aquifer was determined, which is approximately equal to six months. The latter indicates that there is some delay in the transfer of isotopic signal from the precipitation to the groundwater. The use of Spearman’s rank correlation coefficient made it possible to clarify the relationship of surface waters with waters in different hydrodynamic zones. No connection was found between the isotopic compositions of atmospheric precipitation and the waters of the vertical downward circulation zone, the connection with the composition of the waters of the horizontal circulation zone was also not established, and with the waters of the siphon circulation zone was partially established for one source. This correlation suggests that the groundwater on the western border of the Ufa plateau has a predominantly mixed aquifer recharge.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Fig. 1.
Fig. 2.
Fig. 3.
Fig. 4.
Fig. 5.
Fig. 6.
Fig. 7.
Fig. 8.
Fig. 9.
Fig. 10.

Similar content being viewed by others

REFERENCES

  1. Gorbunova, K.A., Kostarev, V.P., Andreychouk, V.N., et al., Karst i pescheri Permskoi oblasti (Karst and Caves of Perm region), Perm: Publ. House Perm State Univ., 1992.

    Google Scholar 

  2. Kadebskaya, O.I. and Maksimovich, N.G., Geologicheskie, gidrogeologicheskie i gidrogeokhimicheskie predposylki formirovaniya Ordinskoj peshchery (Geological, Hydrogeological and Hydrogeochemical Prerequisites for the Formation of the Orda Cave), Caves: Interuniversity Collection of Sci. Papers Perm Univ., 2009, pp. 12–21.

  3. Kadebskaya, O.I. and Maksimovich, N.G., Orda cave as a geographical phenomenon of global importance, Geogr. Bull., 2016, pp. 17–28.

  4. Kataev, V.N., Metodologiya i praktika sravnitel’no-ocenochnogo karstologicheskogo rajonirovaniya (Methodology and Practice of Comparative-Evaluative Karstological Zoning), Perm, 2001.

    Google Scholar 

  5. Lavrova, N.V., Regularities of distribution and formation of karst breccias (on the example of the Perm Kama region), Cand. Sci. Disser., Perm, 2005.

  6. Maksimovich, N.G. and Lavrov, I.A., Ordinskaya peshchera. Dlinneishaya podvodnaya peshchera Rossii (Ordinskaya cave. The longest underwater cave in Russia), Perm, 2006.

  7. Mihajlov, G.K., Buldakov, B.A., and Ivanov, M.I., Rezhim karstovyh rodnikov v central’noj chasti Ufimskogo plato (Regime of karst springs in the central part of the Ufa plateau), Karst studies, Perm, 1969, pp. 63–69.

  8. Turyshev, A.V., Karstovye yavleniya i podzemnye vody severnoj chasti Ufimskogo plato (Karst Phenomena and Groundwaters of the Northern Part of the Ufa Plateau), Kungur, 1960.

  9. Tchaikovsky, I.I., Kadebskaya, O.I., and Kalinina, T.A., Kazakovskaya gora: tektonika, geologiya, gidrogeologiya, karst i mineralogiya (Kazakovskaya Mountain: Tectonics, Geology, Hydrogeology, Karst, and Mineralogy), Perm, 2015.

  10. Shimanovskij, L.A., Grondwaters of the Ufa plateau (zone of active water exchange), Cand. Sci. Dissertation, Perm, 1964.

Download references

Funding

This work was financially supported by the Russian Foundation for Basic Research in the framework of scientific projects no. 17-45-590369 “Research the formation of the isotopic and chemical composition of natural waters in the Perm region” (2017); no. 16-55-14002 “Migration of the permafrost border at the Europe—Asia border in the Pleistocene” (2016) and the Austrian Foundation FWF no. I 2707-N28 “Pleistocene permafrost boundary shifts at the Europe-Asia border.”

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to A. S. Kazantseva.

Ethics declarations

The authors declare that they have no conflicts of interest.

Rights and permissions

Reprints and permissions

About this article

Check for updates. Verify currency and authenticity via CrossMark

Cite this article

Kazantseva, A.S., Kadebskaya, O.I., Dublyansky, Y.V. et al. Isotope-Hydrochemical Study of Natural Waters on the Western Border of the Ufa Plateau. Water Resour 49, 142–153 (2022). https://doi.org/10.1134/S0097807822010080

Download citation

  • Received:

  • Revised:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1134/S0097807822010080

Keywords:

Navigation