Distribution of tritium and stable isotopes in precipitation in Syria
The paper discusses aspects of the isotopic composition (tritium and stable isotopes) of precipitation, which was monitored from 2000 to 2003 at 12 stations in Syria. The seasonal variations in δ 18 O are smaller at the western stations than at the eastern ones due to low seasonal temperature variat...
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| creator | Al Charideh, Abdul Rahman Abou Zakhem, Boulos |
| description | The paper discusses aspects of the isotopic composition (tritium and stable isotopes) of precipitation, which was monitored from 2000 to 2003 at 12 stations in Syria. The seasonal variations in δ
18
O are smaller at the western stations than at the eastern ones due to low seasonal temperature variations. A good correlation between δ
2
H and δ
18
O was obtained for each station, and the slopes of the local meteoric water lines are significantly lower than the Global Meteoric Water Line. Values of d-excess decrease from 19‰ at the western stations to 13‰ at the eastern ones, indicating the influence of precipitation generated by air masses coming from the Mediterranean Sea. A reliable altitude effect represented by depletion of heavy stable isotopes (δ
18
O and δ
2
H), of about −0.21‰ and −1.47‰ per 100 m elevation, respectively, was observed. Monthly tritium contents in precipitation, and seasonal variations, are less at the western stations than at the eastern ones. The weighted mean tritium values are between 3 and 9 TU, and increase with distance from the Syrian coast by 1 TU/100 km.
Citation Al Charideh, A. R. & Abou Zakhem, B. (2010) Distribution of tritium and stable isotopes in precipitation in Syria. Hydrol. Sci. J.
55(5), 832-843. |
| doi_str_mv | 10.1080/02626667.2010.487977 |
| format | Article |
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18
O are smaller at the western stations than at the eastern ones due to low seasonal temperature variations. A good correlation between δ
2
H and δ
18
O was obtained for each station, and the slopes of the local meteoric water lines are significantly lower than the Global Meteoric Water Line. Values of d-excess decrease from 19‰ at the western stations to 13‰ at the eastern ones, indicating the influence of precipitation generated by air masses coming from the Mediterranean Sea. A reliable altitude effect represented by depletion of heavy stable isotopes (δ
18
O and δ
2
H), of about −0.21‰ and −1.47‰ per 100 m elevation, respectively, was observed. Monthly tritium contents in precipitation, and seasonal variations, are less at the western stations than at the eastern ones. The weighted mean tritium values are between 3 and 9 TU, and increase with distance from the Syrian coast by 1 TU/100 km.
Citation Al Charideh, A. R. & Abou Zakhem, B. (2010) Distribution of tritium and stable isotopes in precipitation in Syria. Hydrol. Sci. J.
55(5), 832-843.</description><identifier>ISSN: 0262-6667</identifier><identifier>EISSN: 2150-3435</identifier><identifier>DOI: 10.1080/02626667.2010.487977</identifier><identifier>CODEN: HSJODN</identifier><language>eng</language><publisher>Wallingford: Taylor & Francis</publisher><subject>Earth sciences ; Earth, ocean, space ; Exact sciences and technology ; Hydrology. Hydrogeology ; isotope stable ; precipitation ; précipitation ; stable isotope ; Syria ; Syrie ; tritium</subject><ispartof>Hydrological sciences journal, 2010-07, Vol.55 (5), p.832-843</ispartof><rights>Copyright 2010 IAHS Press 2010</rights><rights>2015 INIST-CNRS</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c411t-acb7e31b1a4594ef4f569755f24bda6fd32124ece91d0984c88d023f28c00ca43</citedby><cites>FETCH-LOGICAL-c411t-acb7e31b1a4594ef4f569755f24bda6fd32124ece91d0984c88d023f28c00ca43</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.tandfonline.com/doi/pdf/10.1080/02626667.2010.487977$$EPDF$$P50$$Ginformaworld$$H</linktopdf><linktohtml>$$Uhttps://www.tandfonline.com/doi/full/10.1080/02626667.2010.487977$$EHTML$$P50$$Ginformaworld$$H</linktohtml><link.rule.ids>314,780,784,27923,27924,59646,60435</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=23054263$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Al Charideh, Abdul Rahman</creatorcontrib><creatorcontrib>Abou Zakhem, Boulos</creatorcontrib><title>Distribution of tritium and stable isotopes in precipitation in Syria</title><title>Hydrological sciences journal</title><description>The paper discusses aspects of the isotopic composition (tritium and stable isotopes) of precipitation, which was monitored from 2000 to 2003 at 12 stations in Syria. The seasonal variations in δ
18
O are smaller at the western stations than at the eastern ones due to low seasonal temperature variations. A good correlation between δ
2
H and δ
18
O was obtained for each station, and the slopes of the local meteoric water lines are significantly lower than the Global Meteoric Water Line. Values of d-excess decrease from 19‰ at the western stations to 13‰ at the eastern ones, indicating the influence of precipitation generated by air masses coming from the Mediterranean Sea. A reliable altitude effect represented by depletion of heavy stable isotopes (δ
18
O and δ
2
H), of about −0.21‰ and −1.47‰ per 100 m elevation, respectively, was observed. Monthly tritium contents in precipitation, and seasonal variations, are less at the western stations than at the eastern ones. The weighted mean tritium values are between 3 and 9 TU, and increase with distance from the Syrian coast by 1 TU/100 km.
Citation Al Charideh, A. R. & Abou Zakhem, B. (2010) Distribution of tritium and stable isotopes in precipitation in Syria. Hydrol. Sci. J.
55(5), 832-843.</description><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>Exact sciences and technology</subject><subject>Hydrology. Hydrogeology</subject><subject>isotope stable</subject><subject>precipitation</subject><subject>précipitation</subject><subject>stable isotope</subject><subject>Syria</subject><subject>Syrie</subject><subject>tritium</subject><issn>0262-6667</issn><issn>2150-3435</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2010</creationdate><recordtype>article</recordtype><recordid>eNp9kE1LxDAURYMoOI7-AxfdiKtqvpOuRMbxAwZcqOuQpglEOk1NUmT-va2dcenq8S7nvgcHgEsEbxCU8BZijjnn4gbDMaJSVEIcgQVGDJaEEnYMFhNSTswpOEvpE0JCK04WYP3gU46-HrIPXRFcMS7ZD9tCd02Rsq5bW_gUcuhtKnxX9NEa3_usf_kxeNtFr8_BidNtshf7uQQfj-v31XO5eX16Wd1vSkMRyqU2tbAE1UhTVlHrqGO8Eow5TOtGc9cQjDC1xlaogZWkRsoGYuKwNBAaTckSXM93-xi-Bpuy2vpkbNvqzoYhKcGolAJjOJJ0Jk0MKUXrVB_9VsedQlBN0tRBmpqkqVnaWLvaP9DJ6NZF3Rmf_rqYQEYxJyN3N3O-cyFu9XeIbaOy3rUhHkrk308_7OSAVQ</recordid><startdate>20100708</startdate><enddate>20100708</enddate><creator>Al Charideh, Abdul Rahman</creator><creator>Abou Zakhem, Boulos</creator><general>Taylor & Francis</general><general>IAHS Press</general><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7QH</scope><scope>7ST</scope><scope>7TG</scope><scope>7UA</scope><scope>C1K</scope><scope>F1W</scope><scope>H96</scope><scope>KL.</scope><scope>L.G</scope><scope>SOI</scope></search><sort><creationdate>20100708</creationdate><title>Distribution of tritium and stable isotopes in precipitation in Syria</title><author>Al Charideh, Abdul Rahman ; Abou Zakhem, Boulos</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c411t-acb7e31b1a4594ef4f569755f24bda6fd32124ece91d0984c88d023f28c00ca43</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2010</creationdate><topic>Earth sciences</topic><topic>Earth, ocean, space</topic><topic>Exact sciences and technology</topic><topic>Hydrology. Hydrogeology</topic><topic>isotope stable</topic><topic>precipitation</topic><topic>précipitation</topic><topic>stable isotope</topic><topic>Syria</topic><topic>Syrie</topic><topic>tritium</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Al Charideh, Abdul Rahman</creatorcontrib><creatorcontrib>Abou Zakhem, Boulos</creatorcontrib><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Aqualine</collection><collection>Environment Abstracts</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Environment Abstracts</collection><jtitle>Hydrological sciences journal</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Al Charideh, Abdul Rahman</au><au>Abou Zakhem, Boulos</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Distribution of tritium and stable isotopes in precipitation in Syria</atitle><jtitle>Hydrological sciences journal</jtitle><date>2010-07-08</date><risdate>2010</risdate><volume>55</volume><issue>5</issue><spage>832</spage><epage>843</epage><pages>832-843</pages><issn>0262-6667</issn><eissn>2150-3435</eissn><coden>HSJODN</coden><abstract>The paper discusses aspects of the isotopic composition (tritium and stable isotopes) of precipitation, which was monitored from 2000 to 2003 at 12 stations in Syria. The seasonal variations in δ
18
O are smaller at the western stations than at the eastern ones due to low seasonal temperature variations. A good correlation between δ
2
H and δ
18
O was obtained for each station, and the slopes of the local meteoric water lines are significantly lower than the Global Meteoric Water Line. Values of d-excess decrease from 19‰ at the western stations to 13‰ at the eastern ones, indicating the influence of precipitation generated by air masses coming from the Mediterranean Sea. A reliable altitude effect represented by depletion of heavy stable isotopes (δ
18
O and δ
2
H), of about −0.21‰ and −1.47‰ per 100 m elevation, respectively, was observed. Monthly tritium contents in precipitation, and seasonal variations, are less at the western stations than at the eastern ones. The weighted mean tritium values are between 3 and 9 TU, and increase with distance from the Syrian coast by 1 TU/100 km.
Citation Al Charideh, A. R. & Abou Zakhem, B. (2010) Distribution of tritium and stable isotopes in precipitation in Syria. Hydrol. Sci. J.
55(5), 832-843.</abstract><cop>Wallingford</cop><pub>Taylor & Francis</pub><doi>10.1080/02626667.2010.487977</doi><tpages>12</tpages><oa>free_for_read</oa></addata></record> |
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| subjects | Earth sciences Earth, ocean, space Exact sciences and technology Hydrology. Hydrogeology isotope stable precipitation précipitation stable isotope Syria Syrie tritium |
| title | Distribution of tritium and stable isotopes in precipitation in Syria |
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