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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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 |
work_keys_str_mv |
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