Physicochemical evolution of the thermal springs over the Siwana Ring Complex, western Rajasthan.
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| Title: | Physicochemical evolution of the thermal springs over the Siwana Ring Complex, western Rajasthan. |
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| Authors: | Singh, Hemant1 hemantkrsingh25@gmail.com, Garg, G.1, Chandrasekharam, D.1, Trupti, G.1, Singh, B. |
| Source: | Journal of the Geological Society of India. Dec2014, Vol. 84 Issue 6, p668-674. 7p. |
| Subject Terms: | *Hot springs, *Ring complexes (Geology), *Surface temperature, *Granite, *Volcanic ash, tuff, etc., *Alkaline earth metals |
| Geographic Terms: | Rajasthan (India) |
| Abstract: | The chemical composition of thermal springs from Siwana Ring Complex (SRC) of Barmer district, Rajasthan, India has been investigated for the first time. These springs are near neutral to mildly alkaline (pH = 6.8 to 7.8) in nature with surface temperatures varying between 31 to 39 °C. Piper diagram suggests that these thermal springs are dominated by Ca-HCO type. Experimental results of water-rock interaction at 100 °C indicate that the thermal springs are circulating through tuff and a sedimentary formation extensively controlled by ring dykes of granites, felsic volcanics and mafic dyke and the fault systems associated with the host rock. Groundwater and thermal springs show similar characteristics. Estimated reservoir temperature suggests that Siwana area geothermal system is a low enthalpy system. Heat flow values of the area range from 83 to 205 mWm, promise a viable potential for Enhanced Geothermal System (EGS). [ABSTRACT FROM AUTHOR] |
| Database: | Energy & Power Source |
| FullText | Links: – Type: pdflink Text: Availability: 0 |
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| Header | DbId: enr DbLabel: Energy & Power Source An: 99995417 AccessLevel: 6 PubType: Academic Journal PubTypeId: academicJournal PreciseRelevancyScore: 0 |
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| Items | – Name: Title Label: Title Group: Ti Data: Physicochemical evolution of the thermal springs over the Siwana Ring Complex, western Rajasthan. – Name: Author Label: Authors Group: Au Data: <searchLink fieldCode="AR" term="%22Singh%2C+Hemant%22">Singh, Hemant</searchLink><relatesTo>1</relatesTo><i> hemantkrsingh25@gmail.com</i><br /><searchLink fieldCode="AR" term="%22Garg%2C+G%2E%22">Garg, G.</searchLink><relatesTo>1</relatesTo><br /><searchLink fieldCode="AR" term="%22Chandrasekharam%2C+D%2E%22">Chandrasekharam, D.</searchLink><relatesTo>1</relatesTo><br /><searchLink fieldCode="AR" term="%22Trupti%2C+G%2E%22">Trupti, G.</searchLink><relatesTo>1</relatesTo><br /><searchLink fieldCode="AR" term="%22Singh%2C+B%2E%22">Singh, B.</searchLink> – Name: TitleSource Label: Source Group: Src Data: <searchLink fieldCode="JN" term="%22Journal+of+the+Geological+Society+of+India%22">Journal of the Geological Society of India</searchLink>. Dec2014, Vol. 84 Issue 6, p668-674. 7p. – Name: Subject Label: Subject Terms Group: Su Data: *<searchLink fieldCode="DE" term="%22Hot+springs%22">Hot springs</searchLink><br />*<searchLink fieldCode="DE" term="%22Ring+complexes+%28Geology%29%22">Ring complexes (Geology)</searchLink><br />*<searchLink fieldCode="DE" term="%22Surface+temperature%22">Surface temperature</searchLink><br />*<searchLink fieldCode="DE" term="%22Granite%22">Granite</searchLink><br />*<searchLink fieldCode="DE" term="%22Volcanic+ash%2C+tuff%2C+etc%2E%22">Volcanic ash, tuff, etc.</searchLink><br />*<searchLink fieldCode="DE" term="%22Alkaline+earth+metals%22">Alkaline earth metals</searchLink> – Name: SubjectGeographic Label: Geographic Terms Group: Su Data: <searchLink fieldCode="DE" term="%22Rajasthan+%28India%29%22">Rajasthan (India)</searchLink> – Name: Abstract Label: Abstract Group: Ab Data: The chemical composition of thermal springs from Siwana Ring Complex (SRC) of Barmer district, Rajasthan, India has been investigated for the first time. These springs are near neutral to mildly alkaline (pH = 6.8 to 7.8) in nature with surface temperatures varying between 31 to 39 °C. Piper diagram suggests that these thermal springs are dominated by Ca-HCO type. Experimental results of water-rock interaction at 100 °C indicate that the thermal springs are circulating through tuff and a sedimentary formation extensively controlled by ring dykes of granites, felsic volcanics and mafic dyke and the fault systems associated with the host rock. Groundwater and thermal springs show similar characteristics. Estimated reservoir temperature suggests that Siwana area geothermal system is a low enthalpy system. Heat flow values of the area range from 83 to 205 mWm, promise a viable potential for Enhanced Geothermal System (EGS). [ABSTRACT FROM AUTHOR] |
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| RecordInfo | BibRecord: BibEntity: Identifiers: – Type: doi Value: 10.1007/s12594-014-0177-0 Languages: – Code: eng Text: English PhysicalDescription: Pagination: PageCount: 7 StartPage: 668 Subjects: – SubjectFull: Hot springs Type: general – SubjectFull: Ring complexes (Geology) Type: general – SubjectFull: Surface temperature Type: general – SubjectFull: Granite Type: general – SubjectFull: Volcanic ash, tuff, etc. Type: general – SubjectFull: Alkaline earth metals Type: general – SubjectFull: Rajasthan (India) Type: general Titles: – TitleFull: Physicochemical evolution of the thermal springs over the Siwana Ring Complex, western Rajasthan. Type: main BibRelationships: HasContributorRelationships: – PersonEntity: Name: NameFull: Singh, Hemant – PersonEntity: Name: NameFull: Garg, G. – PersonEntity: Name: NameFull: Chandrasekharam, D. – PersonEntity: Name: NameFull: Trupti, G. – PersonEntity: Name: NameFull: Singh, B. IsPartOfRelationships: – BibEntity: Dates: – D: 01 M: 12 Text: Dec2014 Type: published Y: 2014 Identifiers: – Type: issn-print Value: 00167622 Numbering: – Type: volume Value: 84 – Type: issue Value: 6 Titles: – TitleFull: Journal of the Geological Society of India Type: main |
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