Determination of the origin and recharge process of water resources in Salda Lake Basin by using the environmental, tritium and radiocarbon isotopes (Burdur/Turkey)

The Salda Lake basin which is in the southwestern Turkey is an important water body in view of environmental values. We used stable isotopes (δD and δ18O), δ3H and 14C composition of the water samples to understand recharge process effective in the groundwater and lake water. Water samples were coll...
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Autor*in:	Simge VAROL [verfasserIn] Ayşen DAVRAZ [verfasserIn] Fatma AKSEVER [verfasserIn] Şehnaz ŞENER [verfasserIn] Erhan ŞENER [verfasserIn] Bülent KIRKAN [verfasserIn] Ahmet TOKGÖZLÜ [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2020

Schlagwörter:	stable isotope salda lake tritium radiogenic isotope

Übergeordnetes Werk:	In: Bulletin of the Mineral Research and Exploration - General Directorate of Mineral Research and Exploration, 2018, 161(2020), 161, Seite 57-70
Übergeordnetes Werk:	volume:161 ; year:2020 ; number:161 ; pages:57-70

Links:	Link aufrufen Link aufrufen Link aufrufen Journal toc

DOI / URN:	10.19111/bulletinofmre.604352

Katalog-ID:	DOAJ033031800

Internformat


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spelling	10.19111/bulletinofmre.604352 doi (DE-627)DOAJ033031800 (DE-599)DOAJa34b9a49f30346cea1fb92664a805c38 DE-627 ger DE-627 rakwb eng QE351-399.2 Simge VAROL verfasserin aut Determination of the origin and recharge process of water resources in Salda Lake Basin by using the environmental, tritium and radiocarbon isotopes (Burdur/Turkey) 2020 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The Salda Lake basin which is in the southwestern Turkey is an important water body in view of environmental values. We used stable isotopes (δD and δ18O), δ3H and 14C composition of the water samples to understand recharge process effective in the groundwater and lake water. Water samples were collected in dry and wet periods and the stable isotope (δD and δ18O) and radiogenic isotope (14C) analysis were made in the basin. The δ18O contents of groundwater and lake water ranged from -9,94‰ to 1,18‰ in dry period and from -10,24‰ to 0,30‰, in wet period. δD contents of groundwater and lake water varied from -67,42‰ to 1,20‰ and from -64,51‰ to -2,80‰, in dry and period wet respectively. The stable isotope data of samples indicate a meteoric origin for all samples. According to stable isotope data, groundwater samples seem to be recharged from higher elevations whereas the lake water is recharged from low elevations. The tritium (δ3H) content of the water samples ranges from 1.04 to 4.49 TU and from 1.91 to 4.18 TU in the dry period and wet period respectively. Long-term δ3H observations are required to determine whether these δ3H signals are associated with young recharge or with the groundwater with long residence time. In addition, the 14C activities of the samples vary between 90 pmc and 110 pmc for Salda Lake waters and 530 pmc and 5990 pmc for the groundwater. stable isotope salda lake tritium radiogenic isotope Mineralogy Ayşen DAVRAZ verfasserin aut Fatma AKSEVER verfasserin aut Şehnaz ŞENER verfasserin aut Erhan ŞENER verfasserin aut Bülent KIRKAN verfasserin aut Ahmet TOKGÖZLÜ verfasserin aut In Bulletin of the Mineral Research and Exploration General Directorate of Mineral Research and Exploration, 2018 161(2020), 161, Seite 57-70 (DE-627)1016247400 00264563 nnns volume:161 year:2020 number:161 pages:57-70 https://doi.org/10.19111/bulletinofmre.604352 kostenfrei https://doaj.org/article/a34b9a49f30346cea1fb92664a805c38 kostenfrei http://dergipark.org.tr/tr/pub/bulletinofmre/issue/42676/604352?publisher=mta kostenfrei https://doaj.org/toc/0026-4563 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 161 2020 161 57-70
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allfieldsGer	10.19111/bulletinofmre.604352 doi (DE-627)DOAJ033031800 (DE-599)DOAJa34b9a49f30346cea1fb92664a805c38 DE-627 ger DE-627 rakwb eng QE351-399.2 Simge VAROL verfasserin aut Determination of the origin and recharge process of water resources in Salda Lake Basin by using the environmental, tritium and radiocarbon isotopes (Burdur/Turkey) 2020 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The Salda Lake basin which is in the southwestern Turkey is an important water body in view of environmental values. We used stable isotopes (δD and δ18O), δ3H and 14C composition of the water samples to understand recharge process effective in the groundwater and lake water. Water samples were collected in dry and wet periods and the stable isotope (δD and δ18O) and radiogenic isotope (14C) analysis were made in the basin. The δ18O contents of groundwater and lake water ranged from -9,94‰ to 1,18‰ in dry period and from -10,24‰ to 0,30‰, in wet period. δD contents of groundwater and lake water varied from -67,42‰ to 1,20‰ and from -64,51‰ to -2,80‰, in dry and period wet respectively. The stable isotope data of samples indicate a meteoric origin for all samples. According to stable isotope data, groundwater samples seem to be recharged from higher elevations whereas the lake water is recharged from low elevations. The tritium (δ3H) content of the water samples ranges from 1.04 to 4.49 TU and from 1.91 to 4.18 TU in the dry period and wet period respectively. Long-term δ3H observations are required to determine whether these δ3H signals are associated with young recharge or with the groundwater with long residence time. In addition, the 14C activities of the samples vary between 90 pmc and 110 pmc for Salda Lake waters and 530 pmc and 5990 pmc for the groundwater. stable isotope salda lake tritium radiogenic isotope Mineralogy Ayşen DAVRAZ verfasserin aut Fatma AKSEVER verfasserin aut Şehnaz ŞENER verfasserin aut Erhan ŞENER verfasserin aut Bülent KIRKAN verfasserin aut Ahmet TOKGÖZLÜ verfasserin aut In Bulletin of the Mineral Research and Exploration General Directorate of Mineral Research and Exploration, 2018 161(2020), 161, Seite 57-70 (DE-627)1016247400 00264563 nnns volume:161 year:2020 number:161 pages:57-70 https://doi.org/10.19111/bulletinofmre.604352 kostenfrei https://doaj.org/article/a34b9a49f30346cea1fb92664a805c38 kostenfrei http://dergipark.org.tr/tr/pub/bulletinofmre/issue/42676/604352?publisher=mta kostenfrei https://doaj.org/toc/0026-4563 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 161 2020 161 57-70
allfieldsSound	10.19111/bulletinofmre.604352 doi (DE-627)DOAJ033031800 (DE-599)DOAJa34b9a49f30346cea1fb92664a805c38 DE-627 ger DE-627 rakwb eng QE351-399.2 Simge VAROL verfasserin aut Determination of the origin and recharge process of water resources in Salda Lake Basin by using the environmental, tritium and radiocarbon isotopes (Burdur/Turkey) 2020 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The Salda Lake basin which is in the southwestern Turkey is an important water body in view of environmental values. We used stable isotopes (δD and δ18O), δ3H and 14C composition of the water samples to understand recharge process effective in the groundwater and lake water. Water samples were collected in dry and wet periods and the stable isotope (δD and δ18O) and radiogenic isotope (14C) analysis were made in the basin. The δ18O contents of groundwater and lake water ranged from -9,94‰ to 1,18‰ in dry period and from -10,24‰ to 0,30‰, in wet period. δD contents of groundwater and lake water varied from -67,42‰ to 1,20‰ and from -64,51‰ to -2,80‰, in dry and period wet respectively. The stable isotope data of samples indicate a meteoric origin for all samples. According to stable isotope data, groundwater samples seem to be recharged from higher elevations whereas the lake water is recharged from low elevations. The tritium (δ3H) content of the water samples ranges from 1.04 to 4.49 TU and from 1.91 to 4.18 TU in the dry period and wet period respectively. Long-term δ3H observations are required to determine whether these δ3H signals are associated with young recharge or with the groundwater with long residence time. In addition, the 14C activities of the samples vary between 90 pmc and 110 pmc for Salda Lake waters and 530 pmc and 5990 pmc for the groundwater. stable isotope salda lake tritium radiogenic isotope Mineralogy Ayşen DAVRAZ verfasserin aut Fatma AKSEVER verfasserin aut Şehnaz ŞENER verfasserin aut Erhan ŞENER verfasserin aut Bülent KIRKAN verfasserin aut Ahmet TOKGÖZLÜ verfasserin aut In Bulletin of the Mineral Research and Exploration General Directorate of Mineral Research and Exploration, 2018 161(2020), 161, Seite 57-70 (DE-627)1016247400 00264563 nnns volume:161 year:2020 number:161 pages:57-70 https://doi.org/10.19111/bulletinofmre.604352 kostenfrei https://doaj.org/article/a34b9a49f30346cea1fb92664a805c38 kostenfrei http://dergipark.org.tr/tr/pub/bulletinofmre/issue/42676/604352?publisher=mta kostenfrei https://doaj.org/toc/0026-4563 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 161 2020 161 57-70
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callnumber-first	Q - Science
author	Simge VAROL
spellingShingle	Simge VAROL misc QE351-399.2 misc stable isotope misc salda lake misc tritium misc radiogenic isotope misc Mineralogy Determination of the origin and recharge process of water resources in Salda Lake Basin by using the environmental, tritium and radiocarbon isotopes (Burdur/Turkey)
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topic_title	QE351-399.2 Determination of the origin and recharge process of water resources in Salda Lake Basin by using the environmental, tritium and radiocarbon isotopes (Burdur/Turkey) stable isotope salda lake tritium radiogenic isotope
topic	misc QE351-399.2 misc stable isotope misc salda lake misc tritium misc radiogenic isotope misc Mineralogy
topic_unstemmed	misc QE351-399.2 misc stable isotope misc salda lake misc tritium misc radiogenic isotope misc Mineralogy
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title	Determination of the origin and recharge process of water resources in Salda Lake Basin by using the environmental, tritium and radiocarbon isotopes (Burdur/Turkey)
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title_full	Determination of the origin and recharge process of water resources in Salda Lake Basin by using the environmental, tritium and radiocarbon isotopes (Burdur/Turkey)
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author_browse	Simge VAROL Ayşen DAVRAZ Fatma AKSEVER Şehnaz ŞENER Erhan ŞENER Bülent KIRKAN Ahmet TOKGÖZLÜ
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title_sort	determination of the origin and recharge process of water resources in salda lake basin by using the environmental, tritium and radiocarbon isotopes (burdur/turkey)
callnumber	QE351-399.2
title_auth	Determination of the origin and recharge process of water resources in Salda Lake Basin by using the environmental, tritium and radiocarbon isotopes (Burdur/Turkey)
abstract	The Salda Lake basin which is in the southwestern Turkey is an important water body in view of environmental values. We used stable isotopes (δD and δ18O), δ3H and 14C composition of the water samples to understand recharge process effective in the groundwater and lake water. Water samples were collected in dry and wet periods and the stable isotope (δD and δ18O) and radiogenic isotope (14C) analysis were made in the basin. The δ18O contents of groundwater and lake water ranged from -9,94‰ to 1,18‰ in dry period and from -10,24‰ to 0,30‰, in wet period. δD contents of groundwater and lake water varied from -67,42‰ to 1,20‰ and from -64,51‰ to -2,80‰, in dry and period wet respectively. The stable isotope data of samples indicate a meteoric origin for all samples. According to stable isotope data, groundwater samples seem to be recharged from higher elevations whereas the lake water is recharged from low elevations. The tritium (δ3H) content of the water samples ranges from 1.04 to 4.49 TU and from 1.91 to 4.18 TU in the dry period and wet period respectively. Long-term δ3H observations are required to determine whether these δ3H signals are associated with young recharge or with the groundwater with long residence time. In addition, the 14C activities of the samples vary between 90 pmc and 110 pmc for Salda Lake waters and 530 pmc and 5990 pmc for the groundwater.
abstractGer	The Salda Lake basin which is in the southwestern Turkey is an important water body in view of environmental values. We used stable isotopes (δD and δ18O), δ3H and 14C composition of the water samples to understand recharge process effective in the groundwater and lake water. Water samples were collected in dry and wet periods and the stable isotope (δD and δ18O) and radiogenic isotope (14C) analysis were made in the basin. The δ18O contents of groundwater and lake water ranged from -9,94‰ to 1,18‰ in dry period and from -10,24‰ to 0,30‰, in wet period. δD contents of groundwater and lake water varied from -67,42‰ to 1,20‰ and from -64,51‰ to -2,80‰, in dry and period wet respectively. The stable isotope data of samples indicate a meteoric origin for all samples. According to stable isotope data, groundwater samples seem to be recharged from higher elevations whereas the lake water is recharged from low elevations. The tritium (δ3H) content of the water samples ranges from 1.04 to 4.49 TU and from 1.91 to 4.18 TU in the dry period and wet period respectively. Long-term δ3H observations are required to determine whether these δ3H signals are associated with young recharge or with the groundwater with long residence time. In addition, the 14C activities of the samples vary between 90 pmc and 110 pmc for Salda Lake waters and 530 pmc and 5990 pmc for the groundwater.
abstract_unstemmed	The Salda Lake basin which is in the southwestern Turkey is an important water body in view of environmental values. We used stable isotopes (δD and δ18O), δ3H and 14C composition of the water samples to understand recharge process effective in the groundwater and lake water. Water samples were collected in dry and wet periods and the stable isotope (δD and δ18O) and radiogenic isotope (14C) analysis were made in the basin. The δ18O contents of groundwater and lake water ranged from -9,94‰ to 1,18‰ in dry period and from -10,24‰ to 0,30‰, in wet period. δD contents of groundwater and lake water varied from -67,42‰ to 1,20‰ and from -64,51‰ to -2,80‰, in dry and period wet respectively. The stable isotope data of samples indicate a meteoric origin for all samples. According to stable isotope data, groundwater samples seem to be recharged from higher elevations whereas the lake water is recharged from low elevations. The tritium (δ3H) content of the water samples ranges from 1.04 to 4.49 TU and from 1.91 to 4.18 TU in the dry period and wet period respectively. Long-term δ3H observations are required to determine whether these δ3H signals are associated with young recharge or with the groundwater with long residence time. In addition, the 14C activities of the samples vary between 90 pmc and 110 pmc for Salda Lake waters and 530 pmc and 5990 pmc for the groundwater.
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title_short	Determination of the origin and recharge process of water resources in Salda Lake Basin by using the environmental, tritium and radiocarbon isotopes (Burdur/Turkey)
url	https://doi.org/10.19111/bulletinofmre.604352 https://doaj.org/article/a34b9a49f30346cea1fb92664a805c38 http://dergipark.org.tr/tr/pub/bulletinofmre/issue/42676/604352?publisher=mta https://doaj.org/toc/0026-4563
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author2	Ayşen DAVRAZ Fatma AKSEVER Şehnaz ŞENER Erhan ŞENER Bülent KIRKAN Ahmet TOKGÖZLÜ
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up_date	2024-07-03T15:27:19.775Z
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Long-term δ3H observations are required to determine whether these δ3H signals are associated with young recharge or with the groundwater with long residence time. 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Determination of the origin and recharge process of water resources in Salda Lake Basin by using the environmental, tritium and radiocarbon isotopes (Burdur/Turkey)

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