Identifying watershed-scale spatiotemporal groundwater and surface water mixing function in the Yiluo River, Middle of China
Researching the watershed-scale spatiotemporal groundwater and surface water mixing function, groundwater recharge heights and age can provide important information to watershed water sources management and water pollution controlling. In this study, 20 groundwater samples, 6 precipitation samples,...
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description | Researching the watershed-scale spatiotemporal groundwater and surface water mixing function, groundwater recharge heights and age can provide important information to watershed water sources management and water pollution controlling. In this study, 20 groundwater samples, 6 precipitation samples, and 40 surface water samples in the Yiluo River watershed in middle China were collected, and the mixing function between groundwater and surface water, recharge height, and age of groundwater was studied by using hydrochemistry (Cl, DO, EC, pH), radioactive isotopes (
14
C), and stable isotopes (
13
C,
18
O,
15
N). The results showed that river and shallow groundwater had frequent interaction. Evaporation function played a major role in the groundwater recharging process. Groundwater age displayed spatial and seasonal variations, and the age ranged from 660 to 2800 years (dry season) and 560 to 1800 years (wet season) in downstream and midstream, while the age range from 12,025 to 143,600 years (dry season) and 10,560 to 12,650 years (wet season) in upstream. The average recharge height of downstream and midstream both in dry and wet seasons is about 576.00 to 908.70 m. While in upstream, both, in the dry and wet seasons, ranged from 1285 to 2680 m. The mixing function between groundwater and surface water displayed spatiotemporal variety. These results of this study can provide useful information for the watershed-scale water resources management. |
doi_str_mv | 10.1007/s11356-020-11285-y |
format | Article |
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14
C), and stable isotopes (
13
C,
18
O,
15
N). The results showed that river and shallow groundwater had frequent interaction. Evaporation function played a major role in the groundwater recharging process. Groundwater age displayed spatial and seasonal variations, and the age ranged from 660 to 2800 years (dry season) and 560 to 1800 years (wet season) in downstream and midstream, while the age range from 12,025 to 143,600 years (dry season) and 10,560 to 12,650 years (wet season) in upstream. The average recharge height of downstream and midstream both in dry and wet seasons is about 576.00 to 908.70 m. While in upstream, both, in the dry and wet seasons, ranged from 1285 to 2680 m. The mixing function between groundwater and surface water displayed spatiotemporal variety. These results of this study can provide useful information for the watershed-scale water resources management.</description><identifier>ISSN: 0944-1344</identifier><identifier>EISSN: 1614-7499</identifier><identifier>DOI: 10.1007/s11356-020-11285-y</identifier><identifier>PMID: 33111224</identifier><language>eng</language><publisher>Berlin/Heidelberg: Springer Berlin Heidelberg</publisher><subject>Age ; Aquatic Pollution ; Atmospheric Protection/Air Quality Control/Air Pollution ; China ; Downstream ; Dry season ; Earth and Environmental Science ; Ecotoxicology ; Environment ; Environmental Chemistry ; Environmental Health ; Environmental Monitoring ; Environmental science ; Evaporation ; Groundwater ; Groundwater recharge ; hydrochemistry ; Isotopes ; Pollution sources ; Radioisotopes ; Rainy season ; Research Article ; Rivers ; Seasonal variations ; Seasons ; Stable isotopes ; Surface water ; Surface-groundwater relations ; Upstream ; Waste Water Technology ; Water ; Water analysis ; Water Management ; Water mixing ; Water Pollutants, Chemical - analysis ; Water pollution ; Water Pollution Control ; Water resources ; Water resources management ; Water sampling ; Watersheds ; wet season</subject><ispartof>Environmental science and pollution research international, 2021-03, Vol.28 (9), p.11053-11065</ispartof><rights>Springer-Verlag GmbH Germany, part of Springer Nature 2020</rights><rights>Springer-Verlag GmbH Germany, part of Springer Nature 2020.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c445t-e9287c92b16b8bb8d4130f9a005f3a70639331c4a1cddb3bffaa4904db7180e83</citedby><cites>FETCH-LOGICAL-c445t-e9287c92b16b8bb8d4130f9a005f3a70639331c4a1cddb3bffaa4904db7180e83</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s11356-020-11285-y$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s11356-020-11285-y$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,776,780,27901,27902,41464,42533,51294</link.rule.ids><backlink>$$Uhttps://www.ncbi.nlm.nih.gov/pubmed/33111224$$D View this record in MEDLINE/PubMed$$Hfree_for_read</backlink></links><search><creatorcontrib>Wang, Xihua</creatorcontrib><creatorcontrib>Liu, Changli</creatorcontrib><creatorcontrib>Hou, Hongbing</creatorcontrib><creatorcontrib>Wang, Xiuyan</creatorcontrib><title>Identifying watershed-scale spatiotemporal groundwater and surface water mixing function in the Yiluo River, Middle of China</title><title>Environmental science and pollution research international</title><addtitle>Environ Sci Pollut Res</addtitle><addtitle>Environ Sci Pollut Res Int</addtitle><description>Researching the watershed-scale spatiotemporal groundwater and surface water mixing function, groundwater recharge heights and age can provide important information to watershed water sources management and water pollution controlling. In this study, 20 groundwater samples, 6 precipitation samples, and 40 surface water samples in the Yiluo River watershed in middle China were collected, and the mixing function between groundwater and surface water, recharge height, and age of groundwater was studied by using hydrochemistry (Cl, DO, EC, pH), radioactive isotopes (
14
C), and stable isotopes (
13
C,
18
O,
15
N). The results showed that river and shallow groundwater had frequent interaction. Evaporation function played a major role in the groundwater recharging process. Groundwater age displayed spatial and seasonal variations, and the age ranged from 660 to 2800 years (dry season) and 560 to 1800 years (wet season) in downstream and midstream, while the age range from 12,025 to 143,600 years (dry season) and 10,560 to 12,650 years (wet season) in upstream. The average recharge height of downstream and midstream both in dry and wet seasons is about 576.00 to 908.70 m. While in upstream, both, in the dry and wet seasons, ranged from 1285 to 2680 m. The mixing function between groundwater and surface water displayed spatiotemporal variety. These results of this study can provide useful information for the watershed-scale water resources management.</description><subject>Age</subject><subject>Aquatic Pollution</subject><subject>Atmospheric Protection/Air Quality Control/Air Pollution</subject><subject>China</subject><subject>Downstream</subject><subject>Dry season</subject><subject>Earth and Environmental Science</subject><subject>Ecotoxicology</subject><subject>Environment</subject><subject>Environmental Chemistry</subject><subject>Environmental Health</subject><subject>Environmental Monitoring</subject><subject>Environmental science</subject><subject>Evaporation</subject><subject>Groundwater</subject><subject>Groundwater recharge</subject><subject>hydrochemistry</subject><subject>Isotopes</subject><subject>Pollution sources</subject><subject>Radioisotopes</subject><subject>Rainy season</subject><subject>Research Article</subject><subject>Rivers</subject><subject>Seasonal variations</subject><subject>Seasons</subject><subject>Stable isotopes</subject><subject>Surface water</subject><subject>Surface-groundwater relations</subject><subject>Upstream</subject><subject>Waste Water Technology</subject><subject>Water</subject><subject>Water analysis</subject><subject>Water Management</subject><subject>Water mixing</subject><subject>Water Pollutants, Chemical - analysis</subject><subject>Water pollution</subject><subject>Water Pollution Control</subject><subject>Water resources</subject><subject>Water resources management</subject><subject>Water sampling</subject><subject>Watersheds</subject><subject>wet season</subject><issn>0944-1344</issn><issn>1614-7499</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2021</creationdate><recordtype>article</recordtype><sourceid>EIF</sourceid><sourceid>BENPR</sourceid><recordid>eNp9kUuPFCEURonROO3oH3BhSNy4GJQL1IOl6fiYZIyJ0YUrQvHoZlIFLVQ5duKPl54aNXHhisU957vAh9BToC-B0u5VAeBNSyijBID1DTneQxtoQZBOSHkfbagUggAX4gw9KuWaVlKy7iE64xyqwcQG_by0Ls7BH0Pc4Rs9u1z2zpJi9OhwOeg5pNlNh5T1iHc5LdHeQlhHi8uSvTZu1fAUfpwy_BJNlSIOEc97h7-GcUn4U_ju8gX-EKytucnj7T5E_Rg98Hos7sndeY6-vH3zefueXH18d7l9fUWMEM1MnGR9ZyQboB36YeitAE691JQ2nuuOtlzWBxmhwVg78MF7rYWkwg4d9NT1_By9WHMPOX1bXJnVFIpx46ijS0tRrOkEbxnvmoo-_we9TkuO9XaKiV5KoBxOFFspk1Mp2Xl1yGHS-aiAqlM3au1G1R9Xt92oY5We3UUvw-TsH-V3GRXgK1DqKO5c_rv7P7G_AEuQm7I</recordid><startdate>20210301</startdate><enddate>20210301</enddate><creator>Wang, Xihua</creator><creator>Liu, Changli</creator><creator>Hou, Hongbing</creator><creator>Wang, Xiuyan</creator><general>Springer Berlin Heidelberg</general><general>Springer Nature B.V</general><scope>CGR</scope><scope>CUY</scope><scope>CVF</scope><scope>ECM</scope><scope>EIF</scope><scope>NPM</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7QL</scope><scope>7SN</scope><scope>7T7</scope><scope>7TV</scope><scope>7U7</scope><scope>7WY</scope><scope>7WZ</scope><scope>7X7</scope><scope>7XB</scope><scope>87Z</scope><scope>88E</scope><scope>88I</scope><scope>8AO</scope><scope>8C1</scope><scope>8FD</scope><scope>8FI</scope><scope>8FJ</scope><scope>8FK</scope><scope>8FL</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BEZIV</scope><scope>BHPHI</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>FR3</scope><scope>FRNLG</scope><scope>FYUFA</scope><scope>F~G</scope><scope>GHDGH</scope><scope>GNUQQ</scope><scope>HCIFZ</scope><scope>K60</scope><scope>K6~</scope><scope>K9.</scope><scope>L.-</scope><scope>M0C</scope><scope>M0S</scope><scope>M1P</scope><scope>M2P</scope><scope>M7N</scope><scope>P64</scope><scope>PATMY</scope><scope>PQBIZ</scope><scope>PQBZA</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PYCSY</scope><scope>Q9U</scope><scope>7S9</scope><scope>L.6</scope></search><sort><creationdate>20210301</creationdate><title>Identifying watershed-scale spatiotemporal groundwater and surface water mixing function in the Yiluo River, Middle of China</title><author>Wang, Xihua ; Liu, Changli ; Hou, Hongbing ; Wang, Xiuyan</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c445t-e9287c92b16b8bb8d4130f9a005f3a70639331c4a1cddb3bffaa4904db7180e83</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2021</creationdate><topic>Age</topic><topic>Aquatic Pollution</topic><topic>Atmospheric Protection/Air Quality Control/Air Pollution</topic><topic>China</topic><topic>Downstream</topic><topic>Dry season</topic><topic>Earth and Environmental Science</topic><topic>Ecotoxicology</topic><topic>Environment</topic><topic>Environmental Chemistry</topic><topic>Environmental Health</topic><topic>Environmental Monitoring</topic><topic>Environmental science</topic><topic>Evaporation</topic><topic>Groundwater</topic><topic>Groundwater recharge</topic><topic>hydrochemistry</topic><topic>Isotopes</topic><topic>Pollution sources</topic><topic>Radioisotopes</topic><topic>Rainy season</topic><topic>Research Article</topic><topic>Rivers</topic><topic>Seasonal variations</topic><topic>Seasons</topic><topic>Stable isotopes</topic><topic>Surface water</topic><topic>Surface-groundwater relations</topic><topic>Upstream</topic><topic>Waste Water Technology</topic><topic>Water</topic><topic>Water analysis</topic><topic>Water Management</topic><topic>Water mixing</topic><topic>Water Pollutants, Chemical - analysis</topic><topic>Water pollution</topic><topic>Water Pollution Control</topic><topic>Water resources</topic><topic>Water resources management</topic><topic>Water sampling</topic><topic>Watersheds</topic><topic>wet season</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Wang, Xihua</creatorcontrib><creatorcontrib>Liu, Changli</creatorcontrib><creatorcontrib>Hou, Hongbing</creatorcontrib><creatorcontrib>Wang, Xiuyan</creatorcontrib><collection>Medline</collection><collection>MEDLINE</collection><collection>MEDLINE (Ovid)</collection><collection>MEDLINE</collection><collection>MEDLINE</collection><collection>PubMed</collection><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Bacteriology Abstracts (Microbiology B)</collection><collection>Ecology Abstracts</collection><collection>Industrial and Applied Microbiology Abstracts (Microbiology A)</collection><collection>Pollution Abstracts</collection><collection>Toxicology Abstracts</collection><collection>ABI/INFORM Collection</collection><collection>ABI/INFORM Global (PDF only)</collection><collection>Health & Medical Collection</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>ABI/INFORM Global (Alumni Edition)</collection><collection>Medical Database (Alumni Edition)</collection><collection>Science Database (Alumni Edition)</collection><collection>ProQuest Pharma Collection</collection><collection>Public Health Database</collection><collection>Technology Research Database</collection><collection>Hospital Premium Collection</collection><collection>Hospital Premium Collection (Alumni Edition)</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>ABI/INFORM Collection (Alumni Edition)</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest One Sustainability</collection><collection>ProQuest Central UK/Ireland</collection><collection>Agricultural & Environmental Science Collection</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Business Premium Collection</collection><collection>Natural Science Collection</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>Engineering Research Database</collection><collection>Business Premium Collection (Alumni)</collection><collection>Health Research Premium Collection</collection><collection>ABI/INFORM Global (Corporate)</collection><collection>Health Research Premium Collection (Alumni)</collection><collection>ProQuest Central Student</collection><collection>SciTech Premium Collection</collection><collection>ProQuest Business Collection (Alumni Edition)</collection><collection>ProQuest Business Collection</collection><collection>ProQuest Health & Medical Complete (Alumni)</collection><collection>ABI/INFORM Professional Advanced</collection><collection>ABI/INFORM Global</collection><collection>Health & Medical Collection (Alumni Edition)</collection><collection>Medical Database</collection><collection>Science Database</collection><collection>Algology Mycology and Protozoology Abstracts (Microbiology C)</collection><collection>Biotechnology and BioEngineering Abstracts</collection><collection>Environmental Science Database</collection><collection>ProQuest One Business</collection><collection>ProQuest One Business (Alumni)</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>Environmental Science Collection</collection><collection>ProQuest Central Basic</collection><collection>AGRICOLA</collection><collection>AGRICOLA - Academic</collection><jtitle>Environmental science and pollution research international</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Wang, Xihua</au><au>Liu, Changli</au><au>Hou, Hongbing</au><au>Wang, Xiuyan</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Identifying watershed-scale spatiotemporal groundwater and surface water mixing function in the Yiluo River, Middle of China</atitle><jtitle>Environmental science and pollution research international</jtitle><stitle>Environ Sci Pollut Res</stitle><addtitle>Environ Sci Pollut Res Int</addtitle><date>2021-03-01</date><risdate>2021</risdate><volume>28</volume><issue>9</issue><spage>11053</spage><epage>11065</epage><pages>11053-11065</pages><issn>0944-1344</issn><eissn>1614-7499</eissn><abstract>Researching the watershed-scale spatiotemporal groundwater and surface water mixing function, groundwater recharge heights and age can provide important information to watershed water sources management and water pollution controlling. In this study, 20 groundwater samples, 6 precipitation samples, and 40 surface water samples in the Yiluo River watershed in middle China were collected, and the mixing function between groundwater and surface water, recharge height, and age of groundwater was studied by using hydrochemistry (Cl, DO, EC, pH), radioactive isotopes (
14
C), and stable isotopes (
13
C,
18
O,
15
N). The results showed that river and shallow groundwater had frequent interaction. Evaporation function played a major role in the groundwater recharging process. Groundwater age displayed spatial and seasonal variations, and the age ranged from 660 to 2800 years (dry season) and 560 to 1800 years (wet season) in downstream and midstream, while the age range from 12,025 to 143,600 years (dry season) and 10,560 to 12,650 years (wet season) in upstream. The average recharge height of downstream and midstream both in dry and wet seasons is about 576.00 to 908.70 m. While in upstream, both, in the dry and wet seasons, ranged from 1285 to 2680 m. The mixing function between groundwater and surface water displayed spatiotemporal variety. These results of this study can provide useful information for the watershed-scale water resources management.</abstract><cop>Berlin/Heidelberg</cop><pub>Springer Berlin Heidelberg</pub><pmid>33111224</pmid><doi>10.1007/s11356-020-11285-y</doi><tpages>13</tpages></addata></record> |
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subjects | Age Aquatic Pollution Atmospheric Protection/Air Quality Control/Air Pollution China Downstream Dry season Earth and Environmental Science Ecotoxicology Environment Environmental Chemistry Environmental Health Environmental Monitoring Environmental science Evaporation Groundwater Groundwater recharge hydrochemistry Isotopes Pollution sources Radioisotopes Rainy season Research Article Rivers Seasonal variations Seasons Stable isotopes Surface water Surface-groundwater relations Upstream Waste Water Technology Water Water analysis Water Management Water mixing Water Pollutants, Chemical - analysis Water pollution Water Pollution Control Water resources Water resources management Water sampling Watersheds wet season |
title | Identifying watershed-scale spatiotemporal groundwater and surface water mixing function in the Yiluo River, Middle of China |
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