Geochemical characterization of geothermal spring waters occurring in Gujarat, India
Abstract Geothermal waters are valuable natural resources for direct uses, societal benefits, and industrial uses. Geochemical classification of physicochemical parameters of seven geothermal sources at Gujarat was evaluated in order to improve and identify their possible applications. The analysis...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Yadav, K. [verfasserIn] Sircar, A. [verfasserIn] Jani, D. [verfasserIn] Bist, N. [verfasserIn] Nirantare, A. [verfasserIn] Mali, N. [verfasserIn] Singh, S. [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: |
© Islamic Azad University (IAU) 2021 |
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| Übergeordnetes Werk: |
Enthalten in: International journal of energy and water resources - [Cham] : Springer International Publishing, 2018, 5(2021), 4 vom: 04. Jan., Seite 391-404 |
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| Übergeordnetes Werk: |
volume:5 ; year:2021 ; number:4 ; day:04 ; month:01 ; pages:391-404 |
| Links: |
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| DOI / URN: |
10.1007/s42108-020-00111-3 |
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SPR045407967 |
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| 520 | |a Abstract Geothermal waters are valuable natural resources for direct uses, societal benefits, and industrial uses. Geochemical classification of physicochemical parameters of seven geothermal sources at Gujarat was evaluated in order to improve and identify their possible applications. The analysis of geothermal spring water was performed using standard methods. Metal elements were determined by atomic absorption spectroscopy (AAS). The waters were categorized as Na + K and Cl + $ SO_{4} $ based on results obtained from Piper, Durov, and Stiff analysis. The Tuwa, Dholera, and Lasundra thermal waters had relatively high salinity values exceeding 5000 mg/l. This study gave an insight into the origin of water which could be due to the interaction of underground water with granitic basement/plutons. Due to high total dissolved solvent (TDS) values in places like Dholera, Tuwa, and Lasundra, the water cannot be used for daily life purposes like bathing, drinking, irrigation, etc. while in places like Tulsishyam, Savarkundala, Unai and Lalpur the TDS content was such that it can be used for daily uses. | ||
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10.1007/s42108-020-00111-3 doi (DE-627)SPR045407967 (SPR)s42108-020-00111-3-e DE-627 ger DE-627 rakwb eng 333.7 ASE 333.7 ASE Yadav, K. verfasserin aut Geochemical characterization of geothermal spring waters occurring in Gujarat, India 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Islamic Azad University (IAU) 2021 Abstract Geothermal waters are valuable natural resources for direct uses, societal benefits, and industrial uses. Geochemical classification of physicochemical parameters of seven geothermal sources at Gujarat was evaluated in order to improve and identify their possible applications. The analysis of geothermal spring water was performed using standard methods. Metal elements were determined by atomic absorption spectroscopy (AAS). The waters were categorized as Na + K and Cl + $ SO_{4} $ based on results obtained from Piper, Durov, and Stiff analysis. The Tuwa, Dholera, and Lasundra thermal waters had relatively high salinity values exceeding 5000 mg/l. This study gave an insight into the origin of water which could be due to the interaction of underground water with granitic basement/plutons. Due to high total dissolved solvent (TDS) values in places like Dholera, Tuwa, and Lasundra, the water cannot be used for daily life purposes like bathing, drinking, irrigation, etc. while in places like Tulsishyam, Savarkundala, Unai and Lalpur the TDS content was such that it can be used for daily uses. Geochemical (dpeaa)DE-He213 Thermal spring (dpeaa)DE-He213 Salinity (dpeaa)DE-He213 Cations (dpeaa)DE-He213 Anions (dpeaa)DE-He213 Sircar, A. verfasserin aut Jani, D. verfasserin aut Bist, N. verfasserin aut Nirantare, A. verfasserin aut Mali, N. verfasserin aut Singh, S. verfasserin aut Enthalten in International journal of energy and water resources [Cham] : Springer International Publishing, 2018 5(2021), 4 vom: 04. Jan., Seite 391-404 (DE-627)1041147686 (DE-600)2951257-8 2522-0101 nnns volume:5 year:2021 number:4 day:04 month:01 pages:391-404 https://dx.doi.org/10.1007/s42108-020-00111-3 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_266 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 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 5 2021 4 04 01 391-404 |
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10.1007/s42108-020-00111-3 doi (DE-627)SPR045407967 (SPR)s42108-020-00111-3-e DE-627 ger DE-627 rakwb eng 333.7 ASE 333.7 ASE Yadav, K. verfasserin aut Geochemical characterization of geothermal spring waters occurring in Gujarat, India 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Islamic Azad University (IAU) 2021 Abstract Geothermal waters are valuable natural resources for direct uses, societal benefits, and industrial uses. Geochemical classification of physicochemical parameters of seven geothermal sources at Gujarat was evaluated in order to improve and identify their possible applications. The analysis of geothermal spring water was performed using standard methods. Metal elements were determined by atomic absorption spectroscopy (AAS). The waters were categorized as Na + K and Cl + $ SO_{4} $ based on results obtained from Piper, Durov, and Stiff analysis. The Tuwa, Dholera, and Lasundra thermal waters had relatively high salinity values exceeding 5000 mg/l. This study gave an insight into the origin of water which could be due to the interaction of underground water with granitic basement/plutons. Due to high total dissolved solvent (TDS) values in places like Dholera, Tuwa, and Lasundra, the water cannot be used for daily life purposes like bathing, drinking, irrigation, etc. while in places like Tulsishyam, Savarkundala, Unai and Lalpur the TDS content was such that it can be used for daily uses. Geochemical (dpeaa)DE-He213 Thermal spring (dpeaa)DE-He213 Salinity (dpeaa)DE-He213 Cations (dpeaa)DE-He213 Anions (dpeaa)DE-He213 Sircar, A. verfasserin aut Jani, D. verfasserin aut Bist, N. verfasserin aut Nirantare, A. verfasserin aut Mali, N. verfasserin aut Singh, S. verfasserin aut Enthalten in International journal of energy and water resources [Cham] : Springer International Publishing, 2018 5(2021), 4 vom: 04. Jan., Seite 391-404 (DE-627)1041147686 (DE-600)2951257-8 2522-0101 nnns volume:5 year:2021 number:4 day:04 month:01 pages:391-404 https://dx.doi.org/10.1007/s42108-020-00111-3 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_266 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 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 5 2021 4 04 01 391-404 |
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10.1007/s42108-020-00111-3 doi (DE-627)SPR045407967 (SPR)s42108-020-00111-3-e DE-627 ger DE-627 rakwb eng 333.7 ASE 333.7 ASE Yadav, K. verfasserin aut Geochemical characterization of geothermal spring waters occurring in Gujarat, India 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Islamic Azad University (IAU) 2021 Abstract Geothermal waters are valuable natural resources for direct uses, societal benefits, and industrial uses. Geochemical classification of physicochemical parameters of seven geothermal sources at Gujarat was evaluated in order to improve and identify their possible applications. The analysis of geothermal spring water was performed using standard methods. Metal elements were determined by atomic absorption spectroscopy (AAS). The waters were categorized as Na + K and Cl + $ SO_{4} $ based on results obtained from Piper, Durov, and Stiff analysis. The Tuwa, Dholera, and Lasundra thermal waters had relatively high salinity values exceeding 5000 mg/l. This study gave an insight into the origin of water which could be due to the interaction of underground water with granitic basement/plutons. Due to high total dissolved solvent (TDS) values in places like Dholera, Tuwa, and Lasundra, the water cannot be used for daily life purposes like bathing, drinking, irrigation, etc. while in places like Tulsishyam, Savarkundala, Unai and Lalpur the TDS content was such that it can be used for daily uses. Geochemical (dpeaa)DE-He213 Thermal spring (dpeaa)DE-He213 Salinity (dpeaa)DE-He213 Cations (dpeaa)DE-He213 Anions (dpeaa)DE-He213 Sircar, A. verfasserin aut Jani, D. verfasserin aut Bist, N. verfasserin aut Nirantare, A. verfasserin aut Mali, N. verfasserin aut Singh, S. verfasserin aut Enthalten in International journal of energy and water resources [Cham] : Springer International Publishing, 2018 5(2021), 4 vom: 04. Jan., Seite 391-404 (DE-627)1041147686 (DE-600)2951257-8 2522-0101 nnns volume:5 year:2021 number:4 day:04 month:01 pages:391-404 https://dx.doi.org/10.1007/s42108-020-00111-3 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_266 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 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 5 2021 4 04 01 391-404 |
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Geochemical classification of physicochemical parameters of seven geothermal sources at Gujarat was evaluated in order to improve and identify their possible applications. The analysis of geothermal spring water was performed using standard methods. Metal elements were determined by atomic absorption spectroscopy (AAS). The waters were categorized as Na + K and Cl + $ SO_{4} $ based on results obtained from Piper, Durov, and Stiff analysis. The Tuwa, Dholera, and Lasundra thermal waters had relatively high salinity values exceeding 5000 mg/l. This study gave an insight into the origin of water which could be due to the interaction of underground water with granitic basement/plutons. Due to high total dissolved solvent (TDS) values in places like Dholera, Tuwa, and Lasundra, the water cannot be used for daily life purposes like bathing, drinking, irrigation, etc. while in places like Tulsishyam, Savarkundala, Unai and Lalpur the TDS content was such that it can be used for daily uses.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Geochemical</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Thermal spring</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Salinity</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Cations</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Anions</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Sircar, A.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Jani, D.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Bist, N.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Nirantare, A.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Mali, N.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Singh, S.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">International journal of energy and water resources</subfield><subfield code="d">[Cham] : Springer International Publishing, 2018</subfield><subfield code="g">5(2021), 4 vom: 04. 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Yadav, K. |
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Yadav, K. ddc 333.7 misc Geochemical misc Thermal spring misc Salinity misc Cations misc Anions Geochemical characterization of geothermal spring waters occurring in Gujarat, India |
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333.7 ASE Geochemical characterization of geothermal spring waters occurring in Gujarat, India Geochemical (dpeaa)DE-He213 Thermal spring (dpeaa)DE-He213 Salinity (dpeaa)DE-He213 Cations (dpeaa)DE-He213 Anions (dpeaa)DE-He213 |
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ddc 333.7 misc Geochemical misc Thermal spring misc Salinity misc Cations misc Anions |
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ddc 333.7 misc Geochemical misc Thermal spring misc Salinity misc Cations misc Anions |
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ddc 333.7 misc Geochemical misc Thermal spring misc Salinity misc Cations misc Anions |
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Geochemical characterization of geothermal spring waters occurring in Gujarat, India |
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Geochemical characterization of geothermal spring waters occurring in Gujarat, India |
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Yadav, K. |
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International journal of energy and water resources |
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Yadav, K. Sircar, A. Jani, D. Bist, N. Nirantare, A. Mali, N. Singh, S. |
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geochemical characterization of geothermal spring waters occurring in gujarat, india |
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Geochemical characterization of geothermal spring waters occurring in Gujarat, India |
| abstract |
Abstract Geothermal waters are valuable natural resources for direct uses, societal benefits, and industrial uses. Geochemical classification of physicochemical parameters of seven geothermal sources at Gujarat was evaluated in order to improve and identify their possible applications. The analysis of geothermal spring water was performed using standard methods. Metal elements were determined by atomic absorption spectroscopy (AAS). The waters were categorized as Na + K and Cl + $ SO_{4} $ based on results obtained from Piper, Durov, and Stiff analysis. The Tuwa, Dholera, and Lasundra thermal waters had relatively high salinity values exceeding 5000 mg/l. This study gave an insight into the origin of water which could be due to the interaction of underground water with granitic basement/plutons. Due to high total dissolved solvent (TDS) values in places like Dholera, Tuwa, and Lasundra, the water cannot be used for daily life purposes like bathing, drinking, irrigation, etc. while in places like Tulsishyam, Savarkundala, Unai and Lalpur the TDS content was such that it can be used for daily uses. © Islamic Azad University (IAU) 2021 |
| abstractGer |
Abstract Geothermal waters are valuable natural resources for direct uses, societal benefits, and industrial uses. Geochemical classification of physicochemical parameters of seven geothermal sources at Gujarat was evaluated in order to improve and identify their possible applications. The analysis of geothermal spring water was performed using standard methods. Metal elements were determined by atomic absorption spectroscopy (AAS). The waters were categorized as Na + K and Cl + $ SO_{4} $ based on results obtained from Piper, Durov, and Stiff analysis. The Tuwa, Dholera, and Lasundra thermal waters had relatively high salinity values exceeding 5000 mg/l. This study gave an insight into the origin of water which could be due to the interaction of underground water with granitic basement/plutons. Due to high total dissolved solvent (TDS) values in places like Dholera, Tuwa, and Lasundra, the water cannot be used for daily life purposes like bathing, drinking, irrigation, etc. while in places like Tulsishyam, Savarkundala, Unai and Lalpur the TDS content was such that it can be used for daily uses. © Islamic Azad University (IAU) 2021 |
| abstract_unstemmed |
Abstract Geothermal waters are valuable natural resources for direct uses, societal benefits, and industrial uses. Geochemical classification of physicochemical parameters of seven geothermal sources at Gujarat was evaluated in order to improve and identify their possible applications. The analysis of geothermal spring water was performed using standard methods. Metal elements were determined by atomic absorption spectroscopy (AAS). The waters were categorized as Na + K and Cl + $ SO_{4} $ based on results obtained from Piper, Durov, and Stiff analysis. The Tuwa, Dholera, and Lasundra thermal waters had relatively high salinity values exceeding 5000 mg/l. This study gave an insight into the origin of water which could be due to the interaction of underground water with granitic basement/plutons. Due to high total dissolved solvent (TDS) values in places like Dholera, Tuwa, and Lasundra, the water cannot be used for daily life purposes like bathing, drinking, irrigation, etc. while in places like Tulsishyam, Savarkundala, Unai and Lalpur the TDS content was such that it can be used for daily uses. © Islamic Azad University (IAU) 2021 |
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4 |
| title_short |
Geochemical characterization of geothermal spring waters occurring in Gujarat, India |
| url |
https://dx.doi.org/10.1007/s42108-020-00111-3 |
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| author2 |
Sircar, A. Jani, D. Bist, N. Nirantare, A. Mali, N. Singh, S. |
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Sircar, A. Jani, D. Bist, N. Nirantare, A. Mali, N. Singh, S. |
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| doi_str |
10.1007/s42108-020-00111-3 |
| up_date |
2024-07-03T15:48:20.414Z |
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| score |
7.399665 |