Characterizing hydrochemical properties of springs in Taiwan based on their geological origins
Abstract This study was performed to characterize hydrochemical properties of springs based on their geological origins in Taiwan. Stepwise discriminant analysis (DA) was used to establish a linear classification model of springs using hydrochemical parameters. Two hydrochemical datasets—ion concent...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Jang, Cheng-Shin [verfasserIn] |
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| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2011 |
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| Schlagwörter: |
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| Anmerkung: |
© Springer Science+Business Media B.V. 2011 |
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| Übergeordnetes Werk: |
Enthalten in: Environmental monitoring and assessment - Springer Netherlands, 1981, 184(2011), 1 vom: 05. März, Seite 63-75 |
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| Übergeordnetes Werk: |
volume:184 ; year:2011 ; number:1 ; day:05 ; month:03 ; pages:63-75 |
| Links: |
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| DOI / URN: |
10.1007/s10661-011-1947-4 |
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OLC2073746632 |
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| 520 | |a Abstract This study was performed to characterize hydrochemical properties of springs based on their geological origins in Taiwan. Stepwise discriminant analysis (DA) was used to establish a linear classification model of springs using hydrochemical parameters. Two hydrochemical datasets—ion concentrations and relative proportions of equivalents per liter of major ions—were included to perform prediction of the geological origins of springs. Analyzed results reveal that DA using relative proportions of equivalents per liter of major ions yields a 95.6% right assignation, which is superior to DA using ion concentrations. This result indicates that relative proportions of equivalents of major hydrochemical parameters in spring water are more highly associated with the geological origins than ion concentrations do. Low percentages of $ Na^{ + } $ equivalents are common properties of springs emerging from acid-sulfate and neutral-sulfate igneous rock. Springs emerging from metamorphic rock show low percentages of $ Cl^{ − } $ equivalents and high percentages of HCO$_{3}^{-}$ equivalents, and springs emerging from sedimentary rock exhibit high $ Cl^{ − } $/SO$_{4}^{2-}$ ratios. | ||
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| 650 | 4 | |a Discriminant analysis | |
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| 700 | 1 | |a Lin, Yun-Bin |4 aut | |
| 700 | 1 | |a Liu, Chen-Wuing |4 aut | |
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10.1007/s10661-011-1947-4 doi (DE-627)OLC2073746632 (DE-He213)s10661-011-1947-4-p DE-627 ger DE-627 rakwb eng 333.7 VZ Jang, Cheng-Shin verfasserin aut Characterizing hydrochemical properties of springs in Taiwan based on their geological origins 2011 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer Science+Business Media B.V. 2011 Abstract This study was performed to characterize hydrochemical properties of springs based on their geological origins in Taiwan. Stepwise discriminant analysis (DA) was used to establish a linear classification model of springs using hydrochemical parameters. Two hydrochemical datasets—ion concentrations and relative proportions of equivalents per liter of major ions—were included to perform prediction of the geological origins of springs. Analyzed results reveal that DA using relative proportions of equivalents per liter of major ions yields a 95.6% right assignation, which is superior to DA using ion concentrations. This result indicates that relative proportions of equivalents of major hydrochemical parameters in spring water are more highly associated with the geological origins than ion concentrations do. Low percentages of $ Na^{ + } $ equivalents are common properties of springs emerging from acid-sulfate and neutral-sulfate igneous rock. Springs emerging from metamorphic rock show low percentages of $ Cl^{ − } $ equivalents and high percentages of HCO$_{3}^{-}$ equivalents, and springs emerging from sedimentary rock exhibit high $ Cl^{ − } $/SO$_{4}^{2-}$ ratios. Spring Taiwan Discriminant analysis Igneous rock Metamorphic rock Sedimentary rock Chen, Jui-Sheng aut Lin, Yun-Bin aut Liu, Chen-Wuing aut Enthalten in Environmental monitoring and assessment Springer Netherlands, 1981 184(2011), 1 vom: 05. März, Seite 63-75 (DE-627)130549649 (DE-600)782621-7 (DE-576)476125413 0167-6369 nnns volume:184 year:2011 number:1 day:05 month:03 pages:63-75 https://doi.org/10.1007/s10661-011-1947-4 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-UMW SSG-OLC-FOR SSG-OLC-IBL GBV_ILN_22 GBV_ILN_70 GBV_ILN_4012 GBV_ILN_4219 AR 184 2011 1 05 03 63-75 |
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10.1007/s10661-011-1947-4 doi (DE-627)OLC2073746632 (DE-He213)s10661-011-1947-4-p DE-627 ger DE-627 rakwb eng 333.7 VZ Jang, Cheng-Shin verfasserin aut Characterizing hydrochemical properties of springs in Taiwan based on their geological origins 2011 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer Science+Business Media B.V. 2011 Abstract This study was performed to characterize hydrochemical properties of springs based on their geological origins in Taiwan. Stepwise discriminant analysis (DA) was used to establish a linear classification model of springs using hydrochemical parameters. Two hydrochemical datasets—ion concentrations and relative proportions of equivalents per liter of major ions—were included to perform prediction of the geological origins of springs. Analyzed results reveal that DA using relative proportions of equivalents per liter of major ions yields a 95.6% right assignation, which is superior to DA using ion concentrations. This result indicates that relative proportions of equivalents of major hydrochemical parameters in spring water are more highly associated with the geological origins than ion concentrations do. Low percentages of $ Na^{ + } $ equivalents are common properties of springs emerging from acid-sulfate and neutral-sulfate igneous rock. Springs emerging from metamorphic rock show low percentages of $ Cl^{ − } $ equivalents and high percentages of HCO$_{3}^{-}$ equivalents, and springs emerging from sedimentary rock exhibit high $ Cl^{ − } $/SO$_{4}^{2-}$ ratios. Spring Taiwan Discriminant analysis Igneous rock Metamorphic rock Sedimentary rock Chen, Jui-Sheng aut Lin, Yun-Bin aut Liu, Chen-Wuing aut Enthalten in Environmental monitoring and assessment Springer Netherlands, 1981 184(2011), 1 vom: 05. März, Seite 63-75 (DE-627)130549649 (DE-600)782621-7 (DE-576)476125413 0167-6369 nnns volume:184 year:2011 number:1 day:05 month:03 pages:63-75 https://doi.org/10.1007/s10661-011-1947-4 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-UMW SSG-OLC-FOR SSG-OLC-IBL GBV_ILN_22 GBV_ILN_70 GBV_ILN_4012 GBV_ILN_4219 AR 184 2011 1 05 03 63-75 |
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10.1007/s10661-011-1947-4 doi (DE-627)OLC2073746632 (DE-He213)s10661-011-1947-4-p DE-627 ger DE-627 rakwb eng 333.7 VZ Jang, Cheng-Shin verfasserin aut Characterizing hydrochemical properties of springs in Taiwan based on their geological origins 2011 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer Science+Business Media B.V. 2011 Abstract This study was performed to characterize hydrochemical properties of springs based on their geological origins in Taiwan. Stepwise discriminant analysis (DA) was used to establish a linear classification model of springs using hydrochemical parameters. Two hydrochemical datasets—ion concentrations and relative proportions of equivalents per liter of major ions—were included to perform prediction of the geological origins of springs. Analyzed results reveal that DA using relative proportions of equivalents per liter of major ions yields a 95.6% right assignation, which is superior to DA using ion concentrations. This result indicates that relative proportions of equivalents of major hydrochemical parameters in spring water are more highly associated with the geological origins than ion concentrations do. Low percentages of $ Na^{ + } $ equivalents are common properties of springs emerging from acid-sulfate and neutral-sulfate igneous rock. Springs emerging from metamorphic rock show low percentages of $ Cl^{ − } $ equivalents and high percentages of HCO$_{3}^{-}$ equivalents, and springs emerging from sedimentary rock exhibit high $ Cl^{ − } $/SO$_{4}^{2-}$ ratios. Spring Taiwan Discriminant analysis Igneous rock Metamorphic rock Sedimentary rock Chen, Jui-Sheng aut Lin, Yun-Bin aut Liu, Chen-Wuing aut Enthalten in Environmental monitoring and assessment Springer Netherlands, 1981 184(2011), 1 vom: 05. März, Seite 63-75 (DE-627)130549649 (DE-600)782621-7 (DE-576)476125413 0167-6369 nnns volume:184 year:2011 number:1 day:05 month:03 pages:63-75 https://doi.org/10.1007/s10661-011-1947-4 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-UMW SSG-OLC-FOR SSG-OLC-IBL GBV_ILN_22 GBV_ILN_70 GBV_ILN_4012 GBV_ILN_4219 AR 184 2011 1 05 03 63-75 |
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10.1007/s10661-011-1947-4 doi (DE-627)OLC2073746632 (DE-He213)s10661-011-1947-4-p DE-627 ger DE-627 rakwb eng 333.7 VZ Jang, Cheng-Shin verfasserin aut Characterizing hydrochemical properties of springs in Taiwan based on their geological origins 2011 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer Science+Business Media B.V. 2011 Abstract This study was performed to characterize hydrochemical properties of springs based on their geological origins in Taiwan. Stepwise discriminant analysis (DA) was used to establish a linear classification model of springs using hydrochemical parameters. Two hydrochemical datasets—ion concentrations and relative proportions of equivalents per liter of major ions—were included to perform prediction of the geological origins of springs. Analyzed results reveal that DA using relative proportions of equivalents per liter of major ions yields a 95.6% right assignation, which is superior to DA using ion concentrations. This result indicates that relative proportions of equivalents of major hydrochemical parameters in spring water are more highly associated with the geological origins than ion concentrations do. Low percentages of $ Na^{ + } $ equivalents are common properties of springs emerging from acid-sulfate and neutral-sulfate igneous rock. Springs emerging from metamorphic rock show low percentages of $ Cl^{ − } $ equivalents and high percentages of HCO$_{3}^{-}$ equivalents, and springs emerging from sedimentary rock exhibit high $ Cl^{ − } $/SO$_{4}^{2-}$ ratios. Spring Taiwan Discriminant analysis Igneous rock Metamorphic rock Sedimentary rock Chen, Jui-Sheng aut Lin, Yun-Bin aut Liu, Chen-Wuing aut Enthalten in Environmental monitoring and assessment Springer Netherlands, 1981 184(2011), 1 vom: 05. März, Seite 63-75 (DE-627)130549649 (DE-600)782621-7 (DE-576)476125413 0167-6369 nnns volume:184 year:2011 number:1 day:05 month:03 pages:63-75 https://doi.org/10.1007/s10661-011-1947-4 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-UMW SSG-OLC-FOR SSG-OLC-IBL GBV_ILN_22 GBV_ILN_70 GBV_ILN_4012 GBV_ILN_4219 AR 184 2011 1 05 03 63-75 |
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10.1007/s10661-011-1947-4 doi (DE-627)OLC2073746632 (DE-He213)s10661-011-1947-4-p DE-627 ger DE-627 rakwb eng 333.7 VZ Jang, Cheng-Shin verfasserin aut Characterizing hydrochemical properties of springs in Taiwan based on their geological origins 2011 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer Science+Business Media B.V. 2011 Abstract This study was performed to characterize hydrochemical properties of springs based on their geological origins in Taiwan. Stepwise discriminant analysis (DA) was used to establish a linear classification model of springs using hydrochemical parameters. Two hydrochemical datasets—ion concentrations and relative proportions of equivalents per liter of major ions—were included to perform prediction of the geological origins of springs. Analyzed results reveal that DA using relative proportions of equivalents per liter of major ions yields a 95.6% right assignation, which is superior to DA using ion concentrations. This result indicates that relative proportions of equivalents of major hydrochemical parameters in spring water are more highly associated with the geological origins than ion concentrations do. Low percentages of $ Na^{ + } $ equivalents are common properties of springs emerging from acid-sulfate and neutral-sulfate igneous rock. Springs emerging from metamorphic rock show low percentages of $ Cl^{ − } $ equivalents and high percentages of HCO$_{3}^{-}$ equivalents, and springs emerging from sedimentary rock exhibit high $ Cl^{ − } $/SO$_{4}^{2-}$ ratios. Spring Taiwan Discriminant analysis Igneous rock Metamorphic rock Sedimentary rock Chen, Jui-Sheng aut Lin, Yun-Bin aut Liu, Chen-Wuing aut Enthalten in Environmental monitoring and assessment Springer Netherlands, 1981 184(2011), 1 vom: 05. März, Seite 63-75 (DE-627)130549649 (DE-600)782621-7 (DE-576)476125413 0167-6369 nnns volume:184 year:2011 number:1 day:05 month:03 pages:63-75 https://doi.org/10.1007/s10661-011-1947-4 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-UMW SSG-OLC-FOR SSG-OLC-IBL GBV_ILN_22 GBV_ILN_70 GBV_ILN_4012 GBV_ILN_4219 AR 184 2011 1 05 03 63-75 |
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Characterizing hydrochemical properties of springs in Taiwan based on their geological origins |
| abstract |
Abstract This study was performed to characterize hydrochemical properties of springs based on their geological origins in Taiwan. Stepwise discriminant analysis (DA) was used to establish a linear classification model of springs using hydrochemical parameters. Two hydrochemical datasets—ion concentrations and relative proportions of equivalents per liter of major ions—were included to perform prediction of the geological origins of springs. Analyzed results reveal that DA using relative proportions of equivalents per liter of major ions yields a 95.6% right assignation, which is superior to DA using ion concentrations. This result indicates that relative proportions of equivalents of major hydrochemical parameters in spring water are more highly associated with the geological origins than ion concentrations do. Low percentages of $ Na^{ + } $ equivalents are common properties of springs emerging from acid-sulfate and neutral-sulfate igneous rock. Springs emerging from metamorphic rock show low percentages of $ Cl^{ − } $ equivalents and high percentages of HCO$_{3}^{-}$ equivalents, and springs emerging from sedimentary rock exhibit high $ Cl^{ − } $/SO$_{4}^{2-}$ ratios. © Springer Science+Business Media B.V. 2011 |
| abstractGer |
Abstract This study was performed to characterize hydrochemical properties of springs based on their geological origins in Taiwan. Stepwise discriminant analysis (DA) was used to establish a linear classification model of springs using hydrochemical parameters. Two hydrochemical datasets—ion concentrations and relative proportions of equivalents per liter of major ions—were included to perform prediction of the geological origins of springs. Analyzed results reveal that DA using relative proportions of equivalents per liter of major ions yields a 95.6% right assignation, which is superior to DA using ion concentrations. This result indicates that relative proportions of equivalents of major hydrochemical parameters in spring water are more highly associated with the geological origins than ion concentrations do. Low percentages of $ Na^{ + } $ equivalents are common properties of springs emerging from acid-sulfate and neutral-sulfate igneous rock. Springs emerging from metamorphic rock show low percentages of $ Cl^{ − } $ equivalents and high percentages of HCO$_{3}^{-}$ equivalents, and springs emerging from sedimentary rock exhibit high $ Cl^{ − } $/SO$_{4}^{2-}$ ratios. © Springer Science+Business Media B.V. 2011 |
| abstract_unstemmed |
Abstract This study was performed to characterize hydrochemical properties of springs based on their geological origins in Taiwan. Stepwise discriminant analysis (DA) was used to establish a linear classification model of springs using hydrochemical parameters. Two hydrochemical datasets—ion concentrations and relative proportions of equivalents per liter of major ions—were included to perform prediction of the geological origins of springs. Analyzed results reveal that DA using relative proportions of equivalents per liter of major ions yields a 95.6% right assignation, which is superior to DA using ion concentrations. This result indicates that relative proportions of equivalents of major hydrochemical parameters in spring water are more highly associated with the geological origins than ion concentrations do. Low percentages of $ Na^{ + } $ equivalents are common properties of springs emerging from acid-sulfate and neutral-sulfate igneous rock. Springs emerging from metamorphic rock show low percentages of $ Cl^{ − } $ equivalents and high percentages of HCO$_{3}^{-}$ equivalents, and springs emerging from sedimentary rock exhibit high $ Cl^{ − } $/SO$_{4}^{2-}$ ratios. © Springer Science+Business Media B.V. 2011 |
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| title_short |
Characterizing hydrochemical properties of springs in Taiwan based on their geological origins |
| url |
https://doi.org/10.1007/s10661-011-1947-4 |
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| author2 |
Chen, Jui-Sheng Lin, Yun-Bin Liu, Chen-Wuing |
| author2Str |
Chen, Jui-Sheng Lin, Yun-Bin Liu, Chen-Wuing |
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| doi_str |
10.1007/s10661-011-1947-4 |
| up_date |
2024-07-03T19:39:19.675Z |
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