Assessing River Runoff Components in the Mountain Crimea. 1. The Runoff of Small Rivers

Water runoff components were evaluated for experimental river basins in the Mountain Crimea based on a two-tracer mixing model with three recharge sources. The identified recharge sources for river runoff in karstified catchments were found to include: epikarstic waters, soil-slope waters, and basef...

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Published in:Water resources Vol. 51; no. 6; pp. 882 - 894
Main Authors: Gubareva, T. S., Amelichev, G. N., Gartsman, B. I., Tokarev, S. V., Vakhrushev, B. A., Naumenko, V. G., Amelichev, E. G., Vakhrushev, I. B.
Format: Journal Article
Language:English
Published: Moscow Pleiades Publishing 2024
Springer Nature B.V
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Abstract Water runoff components were evaluated for experimental river basins in the Mountain Crimea based on a two-tracer mixing model with three recharge sources. The identified recharge sources for river runoff in karstified catchments were found to include: epikarstic waters, soil-slope waters, and baseflow waters, circulating at the contact with underlying impermeable rocks. Epikarstic waters account for a considerable portion of the runoff of small rivers. Their proportions in the outlet sections increase during floods and steadily increase with an increase in water discharge, obeying logarithmic relationships. The proportions of baseflow water decrease compared with those of epikarstic waters.
AbstractList Water runoff components were evaluated for experimental river basins in the Mountain Crimea based on a two-tracer mixing model with three recharge sources. The identified recharge sources for river runoff in karstified catchments were found to include: epikarstic waters, soil-slope waters, and baseflow waters, circulating at the contact with underlying impermeable rocks. Epikarstic waters account for a considerable portion of the runoff of small rivers. Their proportions in the outlet sections increase during floods and steadily increase with an increase in water discharge, obeying logarithmic relationships. The proportions of baseflow water decrease compared with those of epikarstic waters.
Author Vakhrushev, I. B.
Gubareva, T. S.
Gartsman, B. I.
Vakhrushev, B. A.
Amelichev, E. G.
Tokarev, S. V.
Naumenko, V. G.
Amelichev, G. N.
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ContentType Journal Article
Copyright Pleiades Publishing, Ltd. 2024. ISSN 0097-8078, Water Resources, 2024, Vol. 51, No. 6, pp. 882–894. © Pleiades Publishing, Ltd., 2024.
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Keywords river catchments
EMMA mixing model
recharge sources
karst
chemical tracers
Mountain Crimea
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Snippet Water runoff components were evaluated for experimental river basins in the Mountain Crimea based on a two-tracer mixing model with three recharge sources. The...
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SubjectTerms Aquatic Pollution
Base flow
Catchment area
Catchments
Components
Earth and Environmental Science
Earth Sciences
Hydrogeology
Hydrological Problems of Water-Scarce Regions
Hydrology/Water Resources
Mountains
Outlets
Recharge
River basins
River discharge
River flow
River runoff
Rivers
Runoff
Tracers
Waste Water Technology
Water discharge
Water Management
Water Pollution Control
Title Assessing River Runoff Components in the Mountain Crimea. 1. The Runoff of Small Rivers
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