Assessment of river runoff components in the Crimean Mountains. 2. Runoff of karst aquifer systems

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Abstract

For experimental basins of karst aquifer systems of Mountainous Crimea, a three-component mixing model has been adapted using geochemical tracers. On its basis, the following stable sources of supply have been established: epikarst water formed mainly in the near-surface fractured and weathered zone of karst rocks; surface-slope water differing in the formation mechanism; base flow water of including a mixture of groundwater from the aeration zones of karst massifs below the epikarst and phreatic zones, providing the base part of the runoff hydrograph. Epikarst waters make up a significant share of the supply in the runoff of karst aquifer systems (> 30%). Close empirical relationships between the shares of the runoff components and the water discharges in the closing sections have been revealed.

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About the authors

T. S. Gubareva

Institute of Water Problems, Russian Academy of Sciences

Author for correspondence.
Email: tgubareva@bk.ru
Russian Federation, Moscow, 119333

G. N. Amelichev

Institute of Water Problems, Russian Academy of Sciences; Vernadsky Crimean Federal University

Email: tgubareva@bk.ru
Russian Federation, Moscow, 119333; Simferopol, 295007

S. V. Tokarev

Institute of Water Problems, Russian Academy of Sciences; Vernadsky Crimean Federal University

Email: tgubareva@bk.ru
Russian Federation, Moscow, 119333; Simferopol, 295007

B. A. Vakhrushev

Institute of Water Problems, Russian Academy of Sciences; Vernadsky Crimean Federal University

Email: tgubareva@bk.ru
Russian Federation, Moscow, 119333; Simferopol, 295007

B. I. Gartsman

Institute of Water Problems, Russian Academy of Sciences; Institute of Natural-Technical Systems

Email: tgubareva@bk.ru
Russian Federation, Moscow, 119333; Sevastopol, 299011

V. G. Naumenko

Vernadsky Crimean Federal University

Email: tgubareva@bk.ru
Russian Federation, Simferopol, 295007

Ev. G. Amelichev

Institute of Water Problems, Russian Academy of Sciences; Vernadsky Crimean Federal University

Email: tgubareva@bk.ru
Russian Federation, Moscow, 119333; Simferopol, 295007

I. B. Vakhrushev

Institute of Water Problems, Russian Academy of Sciences; Vernadsky Crimean Federal University

Email: tgubareva@bk.ru
Russian Federation, Moscow, 119333; Simferopol, 295007

References

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Supplementary files

Supplementary Files
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1. JATS XML
2. Fig. 1. Maps of the KVS basins: a – Karst, b – Red Cave, c – Ayan. 1 – hydrological sections (I – Karst tributary – Mnogorechye village, II – Kizilkobinka river – control section; III – Ayan river – concrete bridge); 2 – weather stations (M – Mnogorechye, O – Olmeskhir, KP – Krasnopeshchernaya, Ch – Chatyrdag); springs: 3 – large, 4 – small; relief elements: 5 – karst cavities; 6 – passages of large karst caves; boundaries: 7 – distribution of Upper Jurassic carbonate rocks, 8 – basins.

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3. Fig. 2. Graphs of the relationship “E residues – measured values ​​of tracer concentration” in the basins: a – Karstovy KVS, b – Krasnaya Cave KVS, c – Ayan KVS. 1 – river samples, 2 – “deviating values”, p – probability of absence of correlation links on the graphs.

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4. Fig. 3. Water mixing diagrams in the U-space of the KVS basins: a – Karst, b – Red Cave, c – Ayan. Sources of water supply: AO, KS, EK, BK, PSK (explanation in the text). Samples: KVS – of the studied sections, KVS(P) – of the verification sample, KP – of the underground river in the Red Cave, S – of the Subotkhan River; springs: ACh – Azmenyn Chokrak, BT – Besh-Tekne, ET – Eki-Tekne, SM – Biyuk-Uzenbash, G – Griffon, Tp – Tuff site, 33 – source No. 33, 17106 – spring, VC – Veyrat-Chokrak, Yach-2 – Yarma-Chokrak-2, N – Nadezhda, Chn – Chelbash lower, EC - Yeni-Sala, BUK - Beech cordon, DC - Damchi-Chokrak, Kr - Krinichka, KA - Kurt-Air, T - Tochka, pT - spring in the Tochka cave, E (Chat) - epikarst springs from the Chatyrdag plateau; other water manifestations: Su - in the Sukhoi gully, K - well, Kap - drops in the cave. Red, s.r. - slope stream.

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5. Fig. 4. Division of KVS runoff by sources of supply on the dates of survey. KVS basins: a – Karst, b – Karst (test sample), c – Red Cave, d – Ayan. The decoding of the sources of supply is given in the text.

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6. Fig. 5. Measured and model concentrations of tracers in the KVS basin mixing models: a – Karst: calibration sample – 28.08.2021–6.03.2023, verification sample 27.02.2022–11.03.2023; b – Red Cave; c – Ayan.

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7. Fig. 6. Dependences of the shares of runoff feed sources on water flow rates Q in the closing sections and the ratio of the shares of EK/PSK and EK*/PSK* in the KVS basins: a – Karst, b – Red Cave, c – Ayan.

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