Tracing sources of stormflow and groundwater recharge in an urban, semi-arid watershed using stable isotopes

Study region: In this study, we use stable isotopes of water to quantify the flow pathways delivering water to the tributaries, mainstem river and groundwater basin underlying urban San Diego. Information about sources of stormflow and recharge are necessary to maintain the health of waterways and a...

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Main Authors: Sierra Wallace, Trent Biggs, Chun-Ta Lai, Hilary McMillan
Format: Article
Language:English
Published: Elsevier 2021-04-01
Series:Journal of Hydrology: Regional Studies
Subjects:
Online Access:http://www.sciencedirect.com/science/article/pii/S2214581821000355
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spelling doaj-e5f7bf94bee547b7a5c56d104420a77e2021-03-27T04:27:42ZengElsevierJournal of Hydrology: Regional Studies2214-58182021-04-0134100806Tracing sources of stormflow and groundwater recharge in an urban, semi-arid watershed using stable isotopesSierra Wallace0Trent Biggs1Chun-Ta Lai2Hilary McMillan3Department of Geography, San Diego State University, San Diego, United StatesDepartment of Geography, San Diego State University, San Diego, United StatesDepartment of Biology, San Diego State University, San Diego, United StatesDepartment of Geography, San Diego State University, San Diego, United States; Corresponding author.Study region: In this study, we use stable isotopes of water to quantify the flow pathways delivering water to the tributaries, mainstem river and groundwater basin underlying urban San Diego. Information about sources of stormflow and recharge are necessary to maintain the health of waterways and aquifers, but studies of these processes are scarce in urban, semi-arid regions. Study focus: Isotopic methods have been used in experimental or natural watersheds, but also have potential to quantify urban water cycling behaviour and water sources. We sampled baseflow, precipitation, and hourly stormflow from eight events with a range of antecedent conditions, and used end member mixing analysis to determine stormflow and groundwater sources. New hydrological insights for the region: Our results show that hydrologic connectivity controls stormflow sources. After a dry summer, and early in storm events, connectivity of pre-event water with the channel is low, so only new precipitation reaches the river. In wetter conditions, connectivity is higher and pre-event surface water mixes with infiltration-origin groundwater. Deeper groundwater composition mimics stormflow, a mix of stagnated river water and infiltration-origin water. The close connection between streamflow and groundwater implies that improving groundwater quality requires improvements to surface water quality. Average uncertainty in source fractions was ±8.0 %, suggesting that despite complex water pathways in urban, semi-arid environments, isotopic sampling is valuable for quantifying water sources.http://www.sciencedirect.com/science/article/pii/S2214581821000355Stable isotopesEnd member mixing analysisUrbanSemi-aridAquiferWatershed
collection DOAJ
language English
format Article
sources DOAJ
author Sierra Wallace
Trent Biggs
Chun-Ta Lai
Hilary McMillan
spellingShingle Sierra Wallace
Trent Biggs
Chun-Ta Lai
Hilary McMillan
Tracing sources of stormflow and groundwater recharge in an urban, semi-arid watershed using stable isotopes
Journal of Hydrology: Regional Studies
Stable isotopes
End member mixing analysis
Urban
Semi-arid
Aquifer
Watershed
author_facet Sierra Wallace
Trent Biggs
Chun-Ta Lai
Hilary McMillan
author_sort Sierra Wallace
title Tracing sources of stormflow and groundwater recharge in an urban, semi-arid watershed using stable isotopes
title_short Tracing sources of stormflow and groundwater recharge in an urban, semi-arid watershed using stable isotopes
title_full Tracing sources of stormflow and groundwater recharge in an urban, semi-arid watershed using stable isotopes
title_fullStr Tracing sources of stormflow and groundwater recharge in an urban, semi-arid watershed using stable isotopes
title_full_unstemmed Tracing sources of stormflow and groundwater recharge in an urban, semi-arid watershed using stable isotopes
title_sort tracing sources of stormflow and groundwater recharge in an urban, semi-arid watershed using stable isotopes
publisher Elsevier
series Journal of Hydrology: Regional Studies
issn 2214-5818
publishDate 2021-04-01
description Study region: In this study, we use stable isotopes of water to quantify the flow pathways delivering water to the tributaries, mainstem river and groundwater basin underlying urban San Diego. Information about sources of stormflow and recharge are necessary to maintain the health of waterways and aquifers, but studies of these processes are scarce in urban, semi-arid regions. Study focus: Isotopic methods have been used in experimental or natural watersheds, but also have potential to quantify urban water cycling behaviour and water sources. We sampled baseflow, precipitation, and hourly stormflow from eight events with a range of antecedent conditions, and used end member mixing analysis to determine stormflow and groundwater sources. New hydrological insights for the region: Our results show that hydrologic connectivity controls stormflow sources. After a dry summer, and early in storm events, connectivity of pre-event water with the channel is low, so only new precipitation reaches the river. In wetter conditions, connectivity is higher and pre-event surface water mixes with infiltration-origin groundwater. Deeper groundwater composition mimics stormflow, a mix of stagnated river water and infiltration-origin water. The close connection between streamflow and groundwater implies that improving groundwater quality requires improvements to surface water quality. Average uncertainty in source fractions was ±8.0 %, suggesting that despite complex water pathways in urban, semi-arid environments, isotopic sampling is valuable for quantifying water sources.
topic Stable isotopes
End member mixing analysis
Urban
Semi-arid
Aquifer
Watershed
url http://www.sciencedirect.com/science/article/pii/S2214581821000355
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