Evaluation of water source origin around Kerman tunnel, Iran: water transfer tunnel path using 2H, 3H, 18O, and 34S isotopes
Abstract Safa Dam Tunnel to Golzar makes it possible to transfer water from Dam Safa to Kerman City. The tunnel, which is approximately 40 km long, is located in the Kerman Cenozoic magmatic arc as a part of the Dehaj-Sarduiyeh belt. The aim of this study was to investigate and identify the source o...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Ahmadi, Farshad [verfasserIn] Eilbeigy, Mehdi [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2021 |
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| Schlagwörter: |
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| Anmerkung: |
© Saudi Society for Geosciences 2021 |
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| Übergeordnetes Werk: |
Enthalten in: Arabian journal of geosciences - Berlin : Springer, 2008, 14(2021), 11 vom: 26. Mai |
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| Übergeordnetes Werk: |
volume:14 ; year:2021 ; number:11 ; day:26 ; month:05 |
| Links: |
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| DOI / URN: |
10.1007/s12517-021-07323-9 |
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| Katalog-ID: |
SPR044148526 |
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| 520 | |a Abstract Safa Dam Tunnel to Golzar makes it possible to transfer water from Dam Safa to Kerman City. The tunnel, which is approximately 40 km long, is located in the Kerman Cenozoic magmatic arc as a part of the Dehaj-Sarduiyeh belt. The aim of this study was to investigate and identify the source of water resources around the tunnel path as well as the source of water entering the northern and southern parts of the tunnel. In this study, isotopes of oxygen, hydrogen (deuterium and tritium), and sulfur have been used. The values of these isotopes are first interpreted analytically on the reference graphs displayed in the next step. As a whole, 13 samples were taken for isotopic analysis from different parts of water resources around the tunnel path. In all samples, %$ {}{}^{18}O %$ and %$ {}{}^2H %$ were measured, and in addition, in 5 samples of %$ {}{}^{34}S %$ isotope and in seven samples %$ {}{}^3H %$ isotope values were measured as well. According to the isotopic composition, age of the samples, and hydrogeological conditions of the region, four types of water sources have been identified, which include the following: (1) meteoric waters (water samples of Chari and Dizin Mah Rivers, Mubarak Shah salt spring, Sarzeh and Ashkan, BH5 and artesian Shirink well), (2) hydrothermal waters (sample of Shirink hot spring water), (3) ancient waters (sample of water in the northern part of the tunnel), (4) ancient waters of snowmelt origin (southern part of the tunnel and BH4). The BH9 water sample is the result of mixing ancient water with ancient water from the source of snowmelt. Sulfur originates from water samples in the northern part of the tunnel and in the southern part of Thenardite sulfate (Na2SO4) mineral. In the source of sulfur, the samples of Shirink hot spring water and BH9, in addition to the extraction of Thenardite, also have some oxidation and reduction processes. The source of water sulfur of Ashkan spring was mainly fossil fuels and air currents. The results stated that the age of water samples shows a direct relationship with their depth. | ||
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10.1007/s12517-021-07323-9 doi (DE-627)SPR044148526 (SPR)s12517-021-07323-9-e DE-627 ger DE-627 rakwb eng 550 ASE Ahmadi, Farshad verfasserin aut Evaluation of water source origin around Kerman tunnel, Iran: water transfer tunnel path using 2H, 3H, 18O, and 34S isotopes 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Saudi Society for Geosciences 2021 Abstract Safa Dam Tunnel to Golzar makes it possible to transfer water from Dam Safa to Kerman City. The tunnel, which is approximately 40 km long, is located in the Kerman Cenozoic magmatic arc as a part of the Dehaj-Sarduiyeh belt. The aim of this study was to investigate and identify the source of water resources around the tunnel path as well as the source of water entering the northern and southern parts of the tunnel. In this study, isotopes of oxygen, hydrogen (deuterium and tritium), and sulfur have been used. The values of these isotopes are first interpreted analytically on the reference graphs displayed in the next step. As a whole, 13 samples were taken for isotopic analysis from different parts of water resources around the tunnel path. In all samples, %$ {}{}^{18}O %$ and %$ {}{}^2H %$ were measured, and in addition, in 5 samples of %$ {}{}^{34}S %$ isotope and in seven samples %$ {}{}^3H %$ isotope values were measured as well. According to the isotopic composition, age of the samples, and hydrogeological conditions of the region, four types of water sources have been identified, which include the following: (1) meteoric waters (water samples of Chari and Dizin Mah Rivers, Mubarak Shah salt spring, Sarzeh and Ashkan, BH5 and artesian Shirink well), (2) hydrothermal waters (sample of Shirink hot spring water), (3) ancient waters (sample of water in the northern part of the tunnel), (4) ancient waters of snowmelt origin (southern part of the tunnel and BH4). The BH9 water sample is the result of mixing ancient water with ancient water from the source of snowmelt. Sulfur originates from water samples in the northern part of the tunnel and in the southern part of Thenardite sulfate (Na2SO4) mineral. In the source of sulfur, the samples of Shirink hot spring water and BH9, in addition to the extraction of Thenardite, also have some oxidation and reduction processes. The source of water sulfur of Ashkan spring was mainly fossil fuels and air currents. The results stated that the age of water samples shows a direct relationship with their depth. Kerman tunnel (dpeaa)DE-He213 Isotopic tracking (dpeaa)DE-He213 Groundwater (dpeaa)DE-He213 Oxygen isotopes (dpeaa)DE-He213 Hydrogen (dpeaa)DE-He213 Sulfur (dpeaa)DE-He213 Eilbeigy, Mehdi verfasserin aut Enthalten in Arabian journal of geosciences Berlin : Springer, 2008 14(2021), 11 vom: 26. Mai (DE-627)572421877 (DE-600)2438771-X 1866-7538 nnns volume:14 year:2021 number:11 day:26 month:05 https://dx.doi.org/10.1007/s12517-021-07323-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 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_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 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_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 14 2021 11 26 05 |
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10.1007/s12517-021-07323-9 doi (DE-627)SPR044148526 (SPR)s12517-021-07323-9-e DE-627 ger DE-627 rakwb eng 550 ASE Ahmadi, Farshad verfasserin aut Evaluation of water source origin around Kerman tunnel, Iran: water transfer tunnel path using 2H, 3H, 18O, and 34S isotopes 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Saudi Society for Geosciences 2021 Abstract Safa Dam Tunnel to Golzar makes it possible to transfer water from Dam Safa to Kerman City. The tunnel, which is approximately 40 km long, is located in the Kerman Cenozoic magmatic arc as a part of the Dehaj-Sarduiyeh belt. The aim of this study was to investigate and identify the source of water resources around the tunnel path as well as the source of water entering the northern and southern parts of the tunnel. In this study, isotopes of oxygen, hydrogen (deuterium and tritium), and sulfur have been used. The values of these isotopes are first interpreted analytically on the reference graphs displayed in the next step. As a whole, 13 samples were taken for isotopic analysis from different parts of water resources around the tunnel path. In all samples, %$ {}{}^{18}O %$ and %$ {}{}^2H %$ were measured, and in addition, in 5 samples of %$ {}{}^{34}S %$ isotope and in seven samples %$ {}{}^3H %$ isotope values were measured as well. According to the isotopic composition, age of the samples, and hydrogeological conditions of the region, four types of water sources have been identified, which include the following: (1) meteoric waters (water samples of Chari and Dizin Mah Rivers, Mubarak Shah salt spring, Sarzeh and Ashkan, BH5 and artesian Shirink well), (2) hydrothermal waters (sample of Shirink hot spring water), (3) ancient waters (sample of water in the northern part of the tunnel), (4) ancient waters of snowmelt origin (southern part of the tunnel and BH4). The BH9 water sample is the result of mixing ancient water with ancient water from the source of snowmelt. Sulfur originates from water samples in the northern part of the tunnel and in the southern part of Thenardite sulfate (Na2SO4) mineral. In the source of sulfur, the samples of Shirink hot spring water and BH9, in addition to the extraction of Thenardite, also have some oxidation and reduction processes. The source of water sulfur of Ashkan spring was mainly fossil fuels and air currents. The results stated that the age of water samples shows a direct relationship with their depth. Kerman tunnel (dpeaa)DE-He213 Isotopic tracking (dpeaa)DE-He213 Groundwater (dpeaa)DE-He213 Oxygen isotopes (dpeaa)DE-He213 Hydrogen (dpeaa)DE-He213 Sulfur (dpeaa)DE-He213 Eilbeigy, Mehdi verfasserin aut Enthalten in Arabian journal of geosciences Berlin : Springer, 2008 14(2021), 11 vom: 26. Mai (DE-627)572421877 (DE-600)2438771-X 1866-7538 nnns volume:14 year:2021 number:11 day:26 month:05 https://dx.doi.org/10.1007/s12517-021-07323-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 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_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 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_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 14 2021 11 26 05 |
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10.1007/s12517-021-07323-9 doi (DE-627)SPR044148526 (SPR)s12517-021-07323-9-e DE-627 ger DE-627 rakwb eng 550 ASE Ahmadi, Farshad verfasserin aut Evaluation of water source origin around Kerman tunnel, Iran: water transfer tunnel path using 2H, 3H, 18O, and 34S isotopes 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Saudi Society for Geosciences 2021 Abstract Safa Dam Tunnel to Golzar makes it possible to transfer water from Dam Safa to Kerman City. The tunnel, which is approximately 40 km long, is located in the Kerman Cenozoic magmatic arc as a part of the Dehaj-Sarduiyeh belt. The aim of this study was to investigate and identify the source of water resources around the tunnel path as well as the source of water entering the northern and southern parts of the tunnel. In this study, isotopes of oxygen, hydrogen (deuterium and tritium), and sulfur have been used. The values of these isotopes are first interpreted analytically on the reference graphs displayed in the next step. As a whole, 13 samples were taken for isotopic analysis from different parts of water resources around the tunnel path. In all samples, %$ {}{}^{18}O %$ and %$ {}{}^2H %$ were measured, and in addition, in 5 samples of %$ {}{}^{34}S %$ isotope and in seven samples %$ {}{}^3H %$ isotope values were measured as well. According to the isotopic composition, age of the samples, and hydrogeological conditions of the region, four types of water sources have been identified, which include the following: (1) meteoric waters (water samples of Chari and Dizin Mah Rivers, Mubarak Shah salt spring, Sarzeh and Ashkan, BH5 and artesian Shirink well), (2) hydrothermal waters (sample of Shirink hot spring water), (3) ancient waters (sample of water in the northern part of the tunnel), (4) ancient waters of snowmelt origin (southern part of the tunnel and BH4). The BH9 water sample is the result of mixing ancient water with ancient water from the source of snowmelt. Sulfur originates from water samples in the northern part of the tunnel and in the southern part of Thenardite sulfate (Na2SO4) mineral. In the source of sulfur, the samples of Shirink hot spring water and BH9, in addition to the extraction of Thenardite, also have some oxidation and reduction processes. The source of water sulfur of Ashkan spring was mainly fossil fuels and air currents. The results stated that the age of water samples shows a direct relationship with their depth. Kerman tunnel (dpeaa)DE-He213 Isotopic tracking (dpeaa)DE-He213 Groundwater (dpeaa)DE-He213 Oxygen isotopes (dpeaa)DE-He213 Hydrogen (dpeaa)DE-He213 Sulfur (dpeaa)DE-He213 Eilbeigy, Mehdi verfasserin aut Enthalten in Arabian journal of geosciences Berlin : Springer, 2008 14(2021), 11 vom: 26. Mai (DE-627)572421877 (DE-600)2438771-X 1866-7538 nnns volume:14 year:2021 number:11 day:26 month:05 https://dx.doi.org/10.1007/s12517-021-07323-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 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_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 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_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 14 2021 11 26 05 |
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10.1007/s12517-021-07323-9 doi (DE-627)SPR044148526 (SPR)s12517-021-07323-9-e DE-627 ger DE-627 rakwb eng 550 ASE Ahmadi, Farshad verfasserin aut Evaluation of water source origin around Kerman tunnel, Iran: water transfer tunnel path using 2H, 3H, 18O, and 34S isotopes 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Saudi Society for Geosciences 2021 Abstract Safa Dam Tunnel to Golzar makes it possible to transfer water from Dam Safa to Kerman City. The tunnel, which is approximately 40 km long, is located in the Kerman Cenozoic magmatic arc as a part of the Dehaj-Sarduiyeh belt. The aim of this study was to investigate and identify the source of water resources around the tunnel path as well as the source of water entering the northern and southern parts of the tunnel. In this study, isotopes of oxygen, hydrogen (deuterium and tritium), and sulfur have been used. The values of these isotopes are first interpreted analytically on the reference graphs displayed in the next step. As a whole, 13 samples were taken for isotopic analysis from different parts of water resources around the tunnel path. In all samples, %$ {}{}^{18}O %$ and %$ {}{}^2H %$ were measured, and in addition, in 5 samples of %$ {}{}^{34}S %$ isotope and in seven samples %$ {}{}^3H %$ isotope values were measured as well. According to the isotopic composition, age of the samples, and hydrogeological conditions of the region, four types of water sources have been identified, which include the following: (1) meteoric waters (water samples of Chari and Dizin Mah Rivers, Mubarak Shah salt spring, Sarzeh and Ashkan, BH5 and artesian Shirink well), (2) hydrothermal waters (sample of Shirink hot spring water), (3) ancient waters (sample of water in the northern part of the tunnel), (4) ancient waters of snowmelt origin (southern part of the tunnel and BH4). The BH9 water sample is the result of mixing ancient water with ancient water from the source of snowmelt. Sulfur originates from water samples in the northern part of the tunnel and in the southern part of Thenardite sulfate (Na2SO4) mineral. In the source of sulfur, the samples of Shirink hot spring water and BH9, in addition to the extraction of Thenardite, also have some oxidation and reduction processes. The source of water sulfur of Ashkan spring was mainly fossil fuels and air currents. The results stated that the age of water samples shows a direct relationship with their depth. Kerman tunnel (dpeaa)DE-He213 Isotopic tracking (dpeaa)DE-He213 Groundwater (dpeaa)DE-He213 Oxygen isotopes (dpeaa)DE-He213 Hydrogen (dpeaa)DE-He213 Sulfur (dpeaa)DE-He213 Eilbeigy, Mehdi verfasserin aut Enthalten in Arabian journal of geosciences Berlin : Springer, 2008 14(2021), 11 vom: 26. Mai (DE-627)572421877 (DE-600)2438771-X 1866-7538 nnns volume:14 year:2021 number:11 day:26 month:05 https://dx.doi.org/10.1007/s12517-021-07323-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 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_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 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_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 14 2021 11 26 05 |
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10.1007/s12517-021-07323-9 doi (DE-627)SPR044148526 (SPR)s12517-021-07323-9-e DE-627 ger DE-627 rakwb eng 550 ASE Ahmadi, Farshad verfasserin aut Evaluation of water source origin around Kerman tunnel, Iran: water transfer tunnel path using 2H, 3H, 18O, and 34S isotopes 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Saudi Society for Geosciences 2021 Abstract Safa Dam Tunnel to Golzar makes it possible to transfer water from Dam Safa to Kerman City. The tunnel, which is approximately 40 km long, is located in the Kerman Cenozoic magmatic arc as a part of the Dehaj-Sarduiyeh belt. The aim of this study was to investigate and identify the source of water resources around the tunnel path as well as the source of water entering the northern and southern parts of the tunnel. In this study, isotopes of oxygen, hydrogen (deuterium and tritium), and sulfur have been used. The values of these isotopes are first interpreted analytically on the reference graphs displayed in the next step. As a whole, 13 samples were taken for isotopic analysis from different parts of water resources around the tunnel path. In all samples, %$ {}{}^{18}O %$ and %$ {}{}^2H %$ were measured, and in addition, in 5 samples of %$ {}{}^{34}S %$ isotope and in seven samples %$ {}{}^3H %$ isotope values were measured as well. According to the isotopic composition, age of the samples, and hydrogeological conditions of the region, four types of water sources have been identified, which include the following: (1) meteoric waters (water samples of Chari and Dizin Mah Rivers, Mubarak Shah salt spring, Sarzeh and Ashkan, BH5 and artesian Shirink well), (2) hydrothermal waters (sample of Shirink hot spring water), (3) ancient waters (sample of water in the northern part of the tunnel), (4) ancient waters of snowmelt origin (southern part of the tunnel and BH4). The BH9 water sample is the result of mixing ancient water with ancient water from the source of snowmelt. Sulfur originates from water samples in the northern part of the tunnel and in the southern part of Thenardite sulfate (Na2SO4) mineral. In the source of sulfur, the samples of Shirink hot spring water and BH9, in addition to the extraction of Thenardite, also have some oxidation and reduction processes. The source of water sulfur of Ashkan spring was mainly fossil fuels and air currents. The results stated that the age of water samples shows a direct relationship with their depth. Kerman tunnel (dpeaa)DE-He213 Isotopic tracking (dpeaa)DE-He213 Groundwater (dpeaa)DE-He213 Oxygen isotopes (dpeaa)DE-He213 Hydrogen (dpeaa)DE-He213 Sulfur (dpeaa)DE-He213 Eilbeigy, Mehdi verfasserin aut Enthalten in Arabian journal of geosciences Berlin : Springer, 2008 14(2021), 11 vom: 26. Mai (DE-627)572421877 (DE-600)2438771-X 1866-7538 nnns volume:14 year:2021 number:11 day:26 month:05 https://dx.doi.org/10.1007/s12517-021-07323-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 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_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 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_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 14 2021 11 26 05 |
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Enthalten in Arabian journal of geosciences 14(2021), 11 vom: 26. Mai volume:14 year:2021 number:11 day:26 month:05 |
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Enthalten in Arabian journal of geosciences 14(2021), 11 vom: 26. Mai volume:14 year:2021 number:11 day:26 month:05 |
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Ahmadi, Farshad @@aut@@ Eilbeigy, Mehdi @@aut@@ |
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The tunnel, which is approximately 40 km long, is located in the Kerman Cenozoic magmatic arc as a part of the Dehaj-Sarduiyeh belt. The aim of this study was to investigate and identify the source of water resources around the tunnel path as well as the source of water entering the northern and southern parts of the tunnel. In this study, isotopes of oxygen, hydrogen (deuterium and tritium), and sulfur have been used. The values of these isotopes are first interpreted analytically on the reference graphs displayed in the next step. As a whole, 13 samples were taken for isotopic analysis from different parts of water resources around the tunnel path. In all samples, %$ {}{}^{18}O %$ and %$ {}{}^2H %$ were measured, and in addition, in 5 samples of %$ {}{}^{34}S %$ isotope and in seven samples %$ {}{}^3H %$ isotope values were measured as well. According to the isotopic composition, age of the samples, and hydrogeological conditions of the region, four types of water sources have been identified, which include the following: (1) meteoric waters (water samples of Chari and Dizin Mah Rivers, Mubarak Shah salt spring, Sarzeh and Ashkan, BH5 and artesian Shirink well), (2) hydrothermal waters (sample of Shirink hot spring water), (3) ancient waters (sample of water in the northern part of the tunnel), (4) ancient waters of snowmelt origin (southern part of the tunnel and BH4). The BH9 water sample is the result of mixing ancient water with ancient water from the source of snowmelt. Sulfur originates from water samples in the northern part of the tunnel and in the southern part of Thenardite sulfate (Na2SO4) mineral. In the source of sulfur, the samples of Shirink hot spring water and BH9, in addition to the extraction of Thenardite, also have some oxidation and reduction processes. The source of water sulfur of Ashkan spring was mainly fossil fuels and air currents. 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|
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Ahmadi, Farshad |
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Ahmadi, Farshad ddc 550 misc Kerman tunnel misc Isotopic tracking misc Groundwater misc Oxygen isotopes misc Hydrogen misc Sulfur Evaluation of water source origin around Kerman tunnel, Iran: water transfer tunnel path using 2H, 3H, 18O, and 34S isotopes |
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550 ASE Evaluation of water source origin around Kerman tunnel, Iran: water transfer tunnel path using 2H, 3H, 18O, and 34S isotopes Kerman tunnel (dpeaa)DE-He213 Isotopic tracking (dpeaa)DE-He213 Groundwater (dpeaa)DE-He213 Oxygen isotopes (dpeaa)DE-He213 Hydrogen (dpeaa)DE-He213 Sulfur (dpeaa)DE-He213 |
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ddc 550 misc Kerman tunnel misc Isotopic tracking misc Groundwater misc Oxygen isotopes misc Hydrogen misc Sulfur |
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ddc 550 misc Kerman tunnel misc Isotopic tracking misc Groundwater misc Oxygen isotopes misc Hydrogen misc Sulfur |
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Evaluation of water source origin around Kerman tunnel, Iran: water transfer tunnel path using 2H, 3H, 18O, and 34S isotopes |
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Evaluation of water source origin around Kerman tunnel, Iran: water transfer tunnel path using 2H, 3H, 18O, and 34S isotopes |
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Ahmadi, Farshad Eilbeigy, Mehdi |
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evaluation of water source origin around kerman tunnel, iran: water transfer tunnel path using 2h, 3h, 18o, and 34s isotopes |
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Evaluation of water source origin around Kerman tunnel, Iran: water transfer tunnel path using 2H, 3H, 18O, and 34S isotopes |
| abstract |
Abstract Safa Dam Tunnel to Golzar makes it possible to transfer water from Dam Safa to Kerman City. The tunnel, which is approximately 40 km long, is located in the Kerman Cenozoic magmatic arc as a part of the Dehaj-Sarduiyeh belt. The aim of this study was to investigate and identify the source of water resources around the tunnel path as well as the source of water entering the northern and southern parts of the tunnel. In this study, isotopes of oxygen, hydrogen (deuterium and tritium), and sulfur have been used. The values of these isotopes are first interpreted analytically on the reference graphs displayed in the next step. As a whole, 13 samples were taken for isotopic analysis from different parts of water resources around the tunnel path. In all samples, %$ {}{}^{18}O %$ and %$ {}{}^2H %$ were measured, and in addition, in 5 samples of %$ {}{}^{34}S %$ isotope and in seven samples %$ {}{}^3H %$ isotope values were measured as well. According to the isotopic composition, age of the samples, and hydrogeological conditions of the region, four types of water sources have been identified, which include the following: (1) meteoric waters (water samples of Chari and Dizin Mah Rivers, Mubarak Shah salt spring, Sarzeh and Ashkan, BH5 and artesian Shirink well), (2) hydrothermal waters (sample of Shirink hot spring water), (3) ancient waters (sample of water in the northern part of the tunnel), (4) ancient waters of snowmelt origin (southern part of the tunnel and BH4). The BH9 water sample is the result of mixing ancient water with ancient water from the source of snowmelt. Sulfur originates from water samples in the northern part of the tunnel and in the southern part of Thenardite sulfate (Na2SO4) mineral. In the source of sulfur, the samples of Shirink hot spring water and BH9, in addition to the extraction of Thenardite, also have some oxidation and reduction processes. The source of water sulfur of Ashkan spring was mainly fossil fuels and air currents. The results stated that the age of water samples shows a direct relationship with their depth. © Saudi Society for Geosciences 2021 |
| abstractGer |
Abstract Safa Dam Tunnel to Golzar makes it possible to transfer water from Dam Safa to Kerman City. The tunnel, which is approximately 40 km long, is located in the Kerman Cenozoic magmatic arc as a part of the Dehaj-Sarduiyeh belt. The aim of this study was to investigate and identify the source of water resources around the tunnel path as well as the source of water entering the northern and southern parts of the tunnel. In this study, isotopes of oxygen, hydrogen (deuterium and tritium), and sulfur have been used. The values of these isotopes are first interpreted analytically on the reference graphs displayed in the next step. As a whole, 13 samples were taken for isotopic analysis from different parts of water resources around the tunnel path. In all samples, %$ {}{}^{18}O %$ and %$ {}{}^2H %$ were measured, and in addition, in 5 samples of %$ {}{}^{34}S %$ isotope and in seven samples %$ {}{}^3H %$ isotope values were measured as well. According to the isotopic composition, age of the samples, and hydrogeological conditions of the region, four types of water sources have been identified, which include the following: (1) meteoric waters (water samples of Chari and Dizin Mah Rivers, Mubarak Shah salt spring, Sarzeh and Ashkan, BH5 and artesian Shirink well), (2) hydrothermal waters (sample of Shirink hot spring water), (3) ancient waters (sample of water in the northern part of the tunnel), (4) ancient waters of snowmelt origin (southern part of the tunnel and BH4). The BH9 water sample is the result of mixing ancient water with ancient water from the source of snowmelt. Sulfur originates from water samples in the northern part of the tunnel and in the southern part of Thenardite sulfate (Na2SO4) mineral. In the source of sulfur, the samples of Shirink hot spring water and BH9, in addition to the extraction of Thenardite, also have some oxidation and reduction processes. The source of water sulfur of Ashkan spring was mainly fossil fuels and air currents. The results stated that the age of water samples shows a direct relationship with their depth. © Saudi Society for Geosciences 2021 |
| abstract_unstemmed |
Abstract Safa Dam Tunnel to Golzar makes it possible to transfer water from Dam Safa to Kerman City. The tunnel, which is approximately 40 km long, is located in the Kerman Cenozoic magmatic arc as a part of the Dehaj-Sarduiyeh belt. The aim of this study was to investigate and identify the source of water resources around the tunnel path as well as the source of water entering the northern and southern parts of the tunnel. In this study, isotopes of oxygen, hydrogen (deuterium and tritium), and sulfur have been used. The values of these isotopes are first interpreted analytically on the reference graphs displayed in the next step. As a whole, 13 samples were taken for isotopic analysis from different parts of water resources around the tunnel path. In all samples, %$ {}{}^{18}O %$ and %$ {}{}^2H %$ were measured, and in addition, in 5 samples of %$ {}{}^{34}S %$ isotope and in seven samples %$ {}{}^3H %$ isotope values were measured as well. According to the isotopic composition, age of the samples, and hydrogeological conditions of the region, four types of water sources have been identified, which include the following: (1) meteoric waters (water samples of Chari and Dizin Mah Rivers, Mubarak Shah salt spring, Sarzeh and Ashkan, BH5 and artesian Shirink well), (2) hydrothermal waters (sample of Shirink hot spring water), (3) ancient waters (sample of water in the northern part of the tunnel), (4) ancient waters of snowmelt origin (southern part of the tunnel and BH4). The BH9 water sample is the result of mixing ancient water with ancient water from the source of snowmelt. Sulfur originates from water samples in the northern part of the tunnel and in the southern part of Thenardite sulfate (Na2SO4) mineral. In the source of sulfur, the samples of Shirink hot spring water and BH9, in addition to the extraction of Thenardite, also have some oxidation and reduction processes. The source of water sulfur of Ashkan spring was mainly fossil fuels and air currents. The results stated that the age of water samples shows a direct relationship with their depth. © Saudi Society for Geosciences 2021 |
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| container_issue |
11 |
| title_short |
Evaluation of water source origin around Kerman tunnel, Iran: water transfer tunnel path using 2H, 3H, 18O, and 34S isotopes |
| url |
https://dx.doi.org/10.1007/s12517-021-07323-9 |
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Eilbeigy, Mehdi |
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| doi_str |
10.1007/s12517-021-07323-9 |
| up_date |
2024-07-03T23:10:55.231Z |
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|
| score |
7.4000654 |