Using 3H as a tracer to study streamflow components in large plain catchments on temperate climate
3H enters the hydrologic cycle after oxidizing in the 3H1HO molecule and it constitutes a very useful tracer for hydrological studies. One of these applications is streamflow component separation, which provides useful information to understand the hydrological cycle. This application is based on th...
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| Veröffentlicht in: | Hydrological processes 2024-08, Vol.38 (8), p.n/a |
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| creator | Alcaraz, Emiliano Basaldúa, Alejandro Quiroz‐Londoño, Orlando Mauricio Dapeña, Cristina Ibarra, Eduardo Copia, Lorenzo Martínez, Daniel |
| description | 3H enters the hydrologic cycle after oxidizing in the 3H1HO molecule and it constitutes a very useful tracer for hydrological studies. One of these applications is streamflow component separation, which provides useful information to understand the hydrological cycle. This application is based on the fact that the contents in precipitation (runoff) tend to be markedly higher than those in groundwater (baseflow) because of decreasing activity in the last as a consequence of radioactive decay. The main objective of this paper is to test 3H for hydrograph separation in sub‐tropical South America, where it is favoured by high values in precipitation. The catchment of the Quequén Grande River, in Argentina, was selected. Total flow in surface water is a mixing between the baseflow and the event flow portion; the separation was done in three sections of the drainage network, and the proportion of baseflow were 36%, 88% and 47%.
Tritium is a powerful tool for hydrograph separation. Significant differences in tritium contents exist between precipitation and groundwater. |
| doi_str_mv | 10.1002/hyp.15264 |
| format | Article |
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Tritium is a powerful tool for hydrograph separation. Significant differences in tritium contents exist between precipitation and groundwater.</description><subject>Argentina</subject><subject>Base flow</subject><subject>Catchment area</subject><subject>Catchments</subject><subject>drainage</subject><subject>Drainage patterns</subject><subject>Groundwater</subject><subject>hydrograph</subject><subject>hydrograph separation</subject><subject>Hydrologic cycle</subject><subject>Hydrologic studies</subject><subject>Hydrological cycle</subject><subject>large catchment hydrology</subject><subject>Oxidation</subject><subject>Precipitation</subject><subject>Radioactive decay</subject><subject>rivers</subject><subject>runoff</subject><subject>Separation</subject><subject>Stream discharge</subject><subject>Stream flow</subject><subject>Surface water</subject><subject>Temperate climates</subject><subject>temperate zone of South America</subject><subject>temperate zones</subject><subject>Tracers</subject><subject>tritium</subject><subject>watersheds</subject><issn>0885-6087</issn><issn>1099-1085</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2024</creationdate><recordtype>article</recordtype><recordid>eNpdkE1PwzAMhiMEEmNw4B9E4sKlm9P0IzmiCRjSJDiwA6coTd2tU79IUk3992SDExe_lv3Ysl9C7hksGEC83E_DgqVxllyQGQMpIwYivSQzECKNMhD5Nblx7gAACQiYkWLr6m5H-ZpqRzX1Vhu01PfU-bGcQrSo26rpj9T07dB32HlH64422u6QDo0OudHe7Ntzp--ox3ZAqz1S09Rt0FtyVenG4d2fzsn25flztY42769vq6dNNDCRJVEpioTlZcGYRp5gbHKZGZNgxXJTGQEgeVEKxAyNkHGVCBEKhYwDz1MsMz4nj797B9t_j-i8amtnsGl0h_3oFGcpzyHlYW5OHv6hh360XbhOcZC5TOIcTtTylzrWDU5qsOEdOykG6mS1Clars9Vq_fVxTvgPfelzxg</recordid><startdate>202408</startdate><enddate>202408</enddate><creator>Alcaraz, Emiliano</creator><creator>Basaldúa, Alejandro</creator><creator>Quiroz‐Londoño, Orlando Mauricio</creator><creator>Dapeña, Cristina</creator><creator>Ibarra, Eduardo</creator><creator>Copia, Lorenzo</creator><creator>Martínez, Daniel</creator><general>John Wiley & Sons, Inc</general><general>Wiley Subscription Services, Inc</general><scope>7QH</scope><scope>7ST</scope><scope>7TG</scope><scope>7UA</scope><scope>8FD</scope><scope>C1K</scope><scope>F1W</scope><scope>FR3</scope><scope>H96</scope><scope>KL.</scope><scope>KR7</scope><scope>L.G</scope><scope>SOI</scope><scope>7S9</scope><scope>L.6</scope><orcidid>https://orcid.org/0000-0002-7640-1754</orcidid><orcidid>https://orcid.org/0000-0003-4781-2682</orcidid></search><sort><creationdate>202408</creationdate><title>Using 3H as a tracer to study streamflow components in large plain catchments on temperate climate</title><author>Alcaraz, Emiliano ; Basaldúa, Alejandro ; Quiroz‐Londoño, Orlando Mauricio ; Dapeña, Cristina ; Ibarra, Eduardo ; Copia, Lorenzo ; Martínez, Daniel</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-p1864-d8b417db11ae34e2c796cc4ef17cfc80093bd8ee6ec892f48893bb9211a35ed63</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2024</creationdate><topic>Argentina</topic><topic>Base flow</topic><topic>Catchment area</topic><topic>Catchments</topic><topic>drainage</topic><topic>Drainage patterns</topic><topic>Groundwater</topic><topic>hydrograph</topic><topic>hydrograph separation</topic><topic>Hydrologic cycle</topic><topic>Hydrologic studies</topic><topic>Hydrological cycle</topic><topic>large catchment hydrology</topic><topic>Oxidation</topic><topic>Precipitation</topic><topic>Radioactive decay</topic><topic>rivers</topic><topic>runoff</topic><topic>Separation</topic><topic>Stream discharge</topic><topic>Stream flow</topic><topic>Surface water</topic><topic>Temperate climates</topic><topic>temperate zone of South America</topic><topic>temperate zones</topic><topic>Tracers</topic><topic>tritium</topic><topic>watersheds</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Alcaraz, Emiliano</creatorcontrib><creatorcontrib>Basaldúa, Alejandro</creatorcontrib><creatorcontrib>Quiroz‐Londoño, Orlando Mauricio</creatorcontrib><creatorcontrib>Dapeña, Cristina</creatorcontrib><creatorcontrib>Ibarra, Eduardo</creatorcontrib><creatorcontrib>Copia, Lorenzo</creatorcontrib><creatorcontrib>Martínez, Daniel</creatorcontrib><collection>Aqualine</collection><collection>Environment Abstracts</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Technology Research Database</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Engineering Research Database</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Civil Engineering Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Environment Abstracts</collection><collection>AGRICOLA</collection><collection>AGRICOLA - Academic</collection><jtitle>Hydrological processes</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Alcaraz, Emiliano</au><au>Basaldúa, Alejandro</au><au>Quiroz‐Londoño, Orlando Mauricio</au><au>Dapeña, Cristina</au><au>Ibarra, Eduardo</au><au>Copia, Lorenzo</au><au>Martínez, Daniel</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Using 3H as a tracer to study streamflow components in large plain catchments on temperate climate</atitle><jtitle>Hydrological processes</jtitle><date>2024-08</date><risdate>2024</risdate><volume>38</volume><issue>8</issue><epage>n/a</epage><issn>0885-6087</issn><eissn>1099-1085</eissn><abstract>3H enters the hydrologic cycle after oxidizing in the 3H1HO molecule and it constitutes a very useful tracer for hydrological studies. One of these applications is streamflow component separation, which provides useful information to understand the hydrological cycle. This application is based on the fact that the contents in precipitation (runoff) tend to be markedly higher than those in groundwater (baseflow) because of decreasing activity in the last as a consequence of radioactive decay. The main objective of this paper is to test 3H for hydrograph separation in sub‐tropical South America, where it is favoured by high values in precipitation. The catchment of the Quequén Grande River, in Argentina, was selected. Total flow in surface water is a mixing between the baseflow and the event flow portion; the separation was done in three sections of the drainage network, and the proportion of baseflow were 36%, 88% and 47%.
Tritium is a powerful tool for hydrograph separation. Significant differences in tritium contents exist between precipitation and groundwater.</abstract><cop>Hoboken, USA</cop><pub>John Wiley & Sons, Inc</pub><doi>10.1002/hyp.15264</doi><tpages>13</tpages><orcidid>https://orcid.org/0000-0002-7640-1754</orcidid><orcidid>https://orcid.org/0000-0003-4781-2682</orcidid></addata></record> |
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| subjects | Argentina Base flow Catchment area Catchments drainage Drainage patterns Groundwater hydrograph hydrograph separation Hydrologic cycle Hydrologic studies Hydrological cycle large catchment hydrology Oxidation Precipitation Radioactive decay rivers runoff Separation Stream discharge Stream flow Surface water Temperate climates temperate zone of South America temperate zones Tracers tritium watersheds |
| title | Using 3H as a tracer to study streamflow components in large plain catchments on temperate climate |
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