Variation of tap-water isotope ratios and municipal water sources across Kyiv city, Ukraine

Abstract Stable isotopes of water allow researchers to examine water pathways and better understand spatial and temporal variability in mixtures of municipal water sources. In regions such as Kyiv (Ukraine), with a water supply that is vulnerable to the effects of climate change, pollution, and geop...

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Main Authors: Elizabeth Avery, Olena Samonina, Iryna Vyshenska, Alan E. Fryar, Andrea M. Erhardt
Format: Article
Language:English
Published: Springer 2022-11-01
Series:Discover Water
Subjects:
Online Access:https://doi.org/10.1007/s43832-022-00021-x
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author Elizabeth Avery
Olena Samonina
Iryna Vyshenska
Alan E. Fryar
Andrea M. Erhardt
author_facet Elizabeth Avery
Olena Samonina
Iryna Vyshenska
Alan E. Fryar
Andrea M. Erhardt
author_sort Elizabeth Avery
collection DOAJ
description Abstract Stable isotopes of water allow researchers to examine water pathways and better understand spatial and temporal variability in mixtures of municipal water sources. In regions such as Kyiv (Ukraine), with a water supply that is vulnerable to the effects of climate change, pollution, and geopolitical conflict, such understanding is critical for effective water management. Trends in stable isotope values and water sources can function as a confirmation of municipal data. Additionally, these data can provide an early signal for the effects of climate change on these sources, reducing uncertainty from physical measurements. For this study, tap water, surface water, and groundwater were collected over 14 months in Kyiv and nearby Boryspil, Brovary, and Boyarka and measured for hydrogen (δ2H) and oxygen (δ18O) stable isotopes. The stable isotope values from the tap water for each district show a general seasonal trend in water sources, with more groundwater used in the supply in the winter for most districts. Spatially, groundwater use increases from south to north in the left-bank districts in Kyiv city and groundwater use generally decreases from south to north in the right-bank districts. As precipitation patterns shift and temperatures increase, the reliance on particular water sources may need to shift as well. Overall, δ2H and δ18O data provide a baseline expectancy for current water use throughout the year and, from this, deviations can be assessed early.
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spelling doaj.art-108cc81550124ed2bd9c390a758a00bb2022-12-22T04:35:37ZengSpringerDiscover Water2730-647X2022-11-012111610.1007/s43832-022-00021-xVariation of tap-water isotope ratios and municipal water sources across Kyiv city, UkraineElizabeth Avery0Olena Samonina1Iryna Vyshenska2Alan E. Fryar3Andrea M. Erhardt4Department of Earth and Environmental Sciences, University of KentuckyDepartment of Environmental Sciences, National University Kyiv-Mohyla AcademyDepartment of Environmental Sciences, National University Kyiv-Mohyla AcademyDepartment of Earth and Environmental Sciences, University of KentuckyDepartment of Earth and Environmental Sciences, University of KentuckyAbstract Stable isotopes of water allow researchers to examine water pathways and better understand spatial and temporal variability in mixtures of municipal water sources. In regions such as Kyiv (Ukraine), with a water supply that is vulnerable to the effects of climate change, pollution, and geopolitical conflict, such understanding is critical for effective water management. Trends in stable isotope values and water sources can function as a confirmation of municipal data. Additionally, these data can provide an early signal for the effects of climate change on these sources, reducing uncertainty from physical measurements. For this study, tap water, surface water, and groundwater were collected over 14 months in Kyiv and nearby Boryspil, Brovary, and Boyarka and measured for hydrogen (δ2H) and oxygen (δ18O) stable isotopes. The stable isotope values from the tap water for each district show a general seasonal trend in water sources, with more groundwater used in the supply in the winter for most districts. Spatially, groundwater use increases from south to north in the left-bank districts in Kyiv city and groundwater use generally decreases from south to north in the right-bank districts. As precipitation patterns shift and temperatures increase, the reliance on particular water sources may need to shift as well. Overall, δ2H and δ18O data provide a baseline expectancy for current water use throughout the year and, from this, deviations can be assessed early.https://doi.org/10.1007/s43832-022-00021-xIsotopesHydrogen-2Oxygen-18Tap waterClimate changeUkraine
spellingShingle Elizabeth Avery
Olena Samonina
Iryna Vyshenska
Alan E. Fryar
Andrea M. Erhardt
Variation of tap-water isotope ratios and municipal water sources across Kyiv city, Ukraine
Discover Water
Isotopes
Hydrogen-2
Oxygen-18
Tap water
Climate change
Ukraine
title Variation of tap-water isotope ratios and municipal water sources across Kyiv city, Ukraine
title_full Variation of tap-water isotope ratios and municipal water sources across Kyiv city, Ukraine
title_fullStr Variation of tap-water isotope ratios and municipal water sources across Kyiv city, Ukraine
title_full_unstemmed Variation of tap-water isotope ratios and municipal water sources across Kyiv city, Ukraine
title_short Variation of tap-water isotope ratios and municipal water sources across Kyiv city, Ukraine
title_sort variation of tap water isotope ratios and municipal water sources across kyiv city ukraine
topic Isotopes
Hydrogen-2
Oxygen-18
Tap water
Climate change
Ukraine
url https://doi.org/10.1007/s43832-022-00021-x
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AT olenasamonina variationoftapwaterisotoperatiosandmunicipalwatersourcesacrosskyivcityukraine
AT irynavyshenska variationoftapwaterisotoperatiosandmunicipalwatersourcesacrosskyivcityukraine
AT alanefryar variationoftapwaterisotoperatiosandmunicipalwatersourcesacrosskyivcityukraine
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