SEASONAL DYNAMICS OF GROUNDWATER MINERAL COMPOSITION AT THE TERRITORY OF THE CRIMEAN PALEOVOLCANO
https://doi.org/10.36305/0513-1634-2022-142-129-140
Abstract
Seasonal dynamics of 25 elements concentrations in Karadag groundwater was evaluated. Increased levels of B, Li and Se were recorded, along with negative correlations between water mineralization and both flow rate of springs and the distance from the seashore (r = -0.840 and r = -0.945), as well as high seasonal variations of P and K levels (78-130% and 80-118% respectively). Positive correlations were found between Ca, Mg, Sr (r = 0.82-0.96); Li, B, Na (r = 0.72-0.90); Li, Na, mineralization (r = 0.80-0.90) and Se, Na (r = 0.551). The highest concentrations of P, K, Si, Na were registered in spring, B, Zn, Fe, Se, F in autumn; Са, Se, F, Cl, I in winter, and Sr in spring and autumn. Ca, K, Mg, Na, B, Fe, Li, mineralization and water hardness of Bio-station well water demonstrated high seasonal variations and maximum permissible concentrations excess.
About the Authors
Nadezhda Golubkina
Federal Scientific Vegetable Center
Russian Federation
Russian Federation
Vladimir Lapchenko
Т.I. Vyazemsky Karadag Scientific Station- Nature Reserve RAS - Branch of A. O. Kovalevsky Institute of Biology of the Southern Seas of RAS
Russian Federation
Russian Federation
Helene Lapchenko
Т.I. Vyazemsky Karadag Scientific Station- Nature Reserve RAS - Branch of A. O. Kovalevsky Institute of Biology of the Southern Seas of RAS
Russian Federation
Russian Federation
Alexander Zuev
Т.I. Vyazemsky Karadag Scientific Station- Nature Reserve RAS - Branch of A. O. Kovalevsky Institute of Biology of the Southern Seas of RAS
Russian Federation
Russian Federation
Gianluca Caruso
University of Naples Federico II
Russian Federation
Russian Federation
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Review
For citations:
Golubkina N., Lapchenko V., Lapchenko H., Zuev A., Caruso G. SEASONAL DYNAMICS OF GROUNDWATER MINERAL COMPOSITION AT THE TERRITORY OF THE CRIMEAN PALEOVOLCANO. Bulletin of the State Nikitsky Botanical Gardens. 2022;(142):129-140. (In Russ.) https://doi.org/10.36305/0513-1634-2022-142-129-140
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