Interaction of groundwater with Lake Urmia in Iran
Being a large hyper‐saline water body, Lake Urmia in north‐western Iran deals with a gradual decline in its water level. Most of the studies on Lake Urmia have neglected the groundwater issue. In this study, as a direct approach, the interaction between the groundwater level and the lake water level...
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| Veröffentlicht in: | Hydrological processes 2018-10, Vol.32 (21), p.3283-3295 |
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| container_title | Hydrological processes |
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| creator | Vaheddoost, Babak Aksoy, Hafzullah |
| description | Being a large hyper‐saline water body, Lake Urmia in north‐western Iran deals with a gradual decline in its water level. Most of the studies on Lake Urmia have neglected the groundwater issue. In this study, as a direct approach, the interaction between the groundwater level and the lake water level is investigated both in time and space by analysing the groundwater data compiled from observation wells surrounding the lake. Baseflow separation is considered as an indirect approach to understand the groundwater contribution to the river network flowing into the lake. It is determined that about 70% of run‐off in the rivers draining into the lake is born in the form of baseflow. An interaction between the lake and the groundwater storage is clearly seen from the analysis to conclude that groundwater has a potential to recharge the lake. Thus, the shrinkage of water level in Lake Urmia could be expected to accelerate with the drastic use of groundwater, which will be a disaster with no return. |
| doi_str_mv | 10.1002/hyp.13263 |
| format | Article |
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Thus, the shrinkage of water level in Lake Urmia could be expected to accelerate with the drastic use of groundwater, which will be a disaster with no return.</description><subject>Base flow</subject><subject>baseflow separation</subject><subject>Data processing</subject><subject>Drainage</subject><subject>Groundwater</subject><subject>Groundwater data</subject><subject>Groundwater levels</subject><subject>Groundwater storage</subject><subject>groundwater–surface water interaction</subject><subject>Hydrologic data</subject><subject>hyper‐saline lake</subject><subject>Lake Urmia</subject><subject>Lakes</subject><subject>Observation wells</subject><subject>River networks</subject><subject>Rivers</subject><subject>Saline water</subject><subject>shallow lake</subject><subject>Shrinkage</subject><subject>Water bodies</subject><subject>Water levels</subject><issn>0885-6087</issn><issn>1099-1085</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2018</creationdate><recordtype>article</recordtype><recordid>eNp1kD1PwzAQhi0EEqEw8A8sMTGkvbPzYY-oAhqpEgx0YLLsxKEprROcRFH-PYGwMp306rl7dQ8htwhLBGCr_dgskbOEn5EAQcoQQcTnJAAh4jABkV6Sq7Y9AEAEAgLCMtdZr_Ouqh2tS_rh694Vg55COlTdnm71p6U7f6o0rRzNvHbX5KLUx9be_M0F2T09vq034fblOVs_bEPNGfBQxMgiQFkYjanUBRotMBJpLq2AgufGGgF5jiaSWjBMWVlyMCxKCyMLaWK-IHfz3cbXX71tO3Woe--mSsUQpxfTJIaJup-p3Ndt622pGl-dtB8VgvpRoiYl6lfJxK5mdqiOdvwfVJv313njG4hLYQI</recordid><startdate>20181015</startdate><enddate>20181015</enddate><creator>Vaheddoost, Babak</creator><creator>Aksoy, Hafzullah</creator><general>Wiley Subscription Services, Inc</general><scope>AAYXX</scope><scope>CITATION</scope><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><orcidid>https://orcid.org/0000-0002-4767-6660</orcidid><orcidid>https://orcid.org/0000-0001-5807-5660</orcidid></search><sort><creationdate>20181015</creationdate><title>Interaction of groundwater with Lake Urmia in Iran</title><author>Vaheddoost, Babak ; Aksoy, Hafzullah</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a3203-85124019dba179ad1ba81487c9e80d3cbeb80cc1b49a82172ff30b247db9d9b53</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2018</creationdate><topic>Base flow</topic><topic>baseflow separation</topic><topic>Data processing</topic><topic>Drainage</topic><topic>Groundwater</topic><topic>Groundwater data</topic><topic>Groundwater levels</topic><topic>Groundwater storage</topic><topic>groundwater–surface water interaction</topic><topic>Hydrologic data</topic><topic>hyper‐saline lake</topic><topic>Lake Urmia</topic><topic>Lakes</topic><topic>Observation wells</topic><topic>River networks</topic><topic>Rivers</topic><topic>Saline water</topic><topic>shallow lake</topic><topic>Shrinkage</topic><topic>Water bodies</topic><topic>Water levels</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Vaheddoost, Babak</creatorcontrib><creatorcontrib>Aksoy, Hafzullah</creatorcontrib><collection>CrossRef</collection><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><jtitle>Hydrological processes</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Vaheddoost, Babak</au><au>Aksoy, Hafzullah</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Interaction of groundwater with Lake Urmia in Iran</atitle><jtitle>Hydrological processes</jtitle><date>2018-10-15</date><risdate>2018</risdate><volume>32</volume><issue>21</issue><spage>3283</spage><epage>3295</epage><pages>3283-3295</pages><issn>0885-6087</issn><eissn>1099-1085</eissn><abstract>Being a large hyper‐saline water body, Lake Urmia in north‐western Iran deals with a gradual decline in its water level. Most of the studies on Lake Urmia have neglected the groundwater issue. In this study, as a direct approach, the interaction between the groundwater level and the lake water level is investigated both in time and space by analysing the groundwater data compiled from observation wells surrounding the lake. Baseflow separation is considered as an indirect approach to understand the groundwater contribution to the river network flowing into the lake. It is determined that about 70% of run‐off in the rivers draining into the lake is born in the form of baseflow. An interaction between the lake and the groundwater storage is clearly seen from the analysis to conclude that groundwater has a potential to recharge the lake. 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| ispartof | Hydrological processes, 2018-10, Vol.32 (21), p.3283-3295 |
| issn | 0885-6087 1099-1085 |
| language | eng |
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| source | Wiley Online Library Journals Frontfile Complete |
| subjects | Base flow baseflow separation Data processing Drainage Groundwater Groundwater data Groundwater levels Groundwater storage groundwater–surface water interaction Hydrologic data hyper‐saline lake Lake Urmia Lakes Observation wells River networks Rivers Saline water shallow lake Shrinkage Water bodies Water levels |
| title | Interaction of groundwater with Lake Urmia in Iran |
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