Hydrochemistry of reservoirs of Damodar River basin, India: weathering processes and water quality assessment
Abstract Water samples collected from the six reservoirs of Damodar River basin in pre- and post-monsoon, have been analysed, to study the major ion chemistry and the weathering and geochemical processes controlling the water composition. Ca, Na and $ HCO_{3} $ dominate the chemical composition of t...
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| Autor*in: |
Singh, Abhay Kumar [verfasserIn] |
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| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2005 |
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| Anmerkung: |
© Springer-Verlag 2005 |
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| Übergeordnetes Werk: |
Enthalten in: Environmental geology - Springer-Verlag, 1975, 48(2005), 8 vom: 20. Sept., Seite 1014-1028 |
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| Übergeordnetes Werk: |
volume:48 ; year:2005 ; number:8 ; day:20 ; month:09 ; pages:1014-1028 |
| Links: |
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| DOI / URN: |
10.1007/s00254-005-1302-6 |
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| Katalog-ID: |
OLC2074406088 |
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| 520 | |a Abstract Water samples collected from the six reservoirs of Damodar River basin in pre- and post-monsoon, have been analysed, to study the major ion chemistry and the weathering and geochemical processes controlling the water composition. Ca, Na and $ HCO_{3} $ dominate the chemical composition of the reservoir water. The seasonal data shows a minimum concentration of most of the ions in post-monsoon and a maximum concentration in pre-monsoon seasons, reflecting the concentrating effects due to elevated temperature and increased evaporation during the low water level period of the pre-monsoon season. Water chemistry of the reservoirs strongly reflects the dominance of continental weathering aided by atmospheric and anthropogenic activities in the catchment area. Higher concentration of $ SO_{4} $ and TDS in Panchet, Durgapur and Tenughat reservoirs indicate mining and anthropogenic impact on water quality. The high contribution of (Ca+Mg) to the total cations, high concentration of dissolved silica, relatively high (Na+K)/$ TZ^{+} $ ratio (0.3) and low equivalent ratio of (Ca+Mg)/(Na+K) suggests combined influence of carbonate and silicate weathering. Kaolinite is the possible mineral that is in equilibrium with the water, implying that the chemistry of reservoir water favours kaolinite formation. The calculated values of SAR, RSC and sodium percentage indicate the ‘excellent to good quality’ of water for irrigation uses. | ||
| 650 | 4 | |a Hydrochemistry | |
| 650 | 4 | |a Reservoirs | |
| 650 | 4 | |a Damodar River | |
| 650 | 4 | |a Weathering | |
| 650 | 4 | |a Anthropogenic | |
| 650 | 4 | |a Water Quality | |
| 650 | 4 | |a Solute Flux | |
| 650 | 4 | |a India | |
| 700 | 1 | |a Mondal, G. C. |4 aut | |
| 700 | 1 | |a Singh, P. K. |4 aut | |
| 700 | 1 | |a Singh, S. |4 aut | |
| 700 | 1 | |a Singh, T. B. |4 aut | |
| 700 | 1 | |a Tewary, B. K. |4 aut | |
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10.1007/s00254-005-1302-6 doi (DE-627)OLC2074406088 (DE-He213)s00254-005-1302-6-p DE-627 ger DE-627 rakwb eng 330 550 VZ 550 VZ 13 ssgn TE 3140 VZ rvk Singh, Abhay Kumar verfasserin aut Hydrochemistry of reservoirs of Damodar River basin, India: weathering processes and water quality assessment 2005 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 2005 Abstract Water samples collected from the six reservoirs of Damodar River basin in pre- and post-monsoon, have been analysed, to study the major ion chemistry and the weathering and geochemical processes controlling the water composition. Ca, Na and $ HCO_{3} $ dominate the chemical composition of the reservoir water. The seasonal data shows a minimum concentration of most of the ions in post-monsoon and a maximum concentration in pre-monsoon seasons, reflecting the concentrating effects due to elevated temperature and increased evaporation during the low water level period of the pre-monsoon season. Water chemistry of the reservoirs strongly reflects the dominance of continental weathering aided by atmospheric and anthropogenic activities in the catchment area. Higher concentration of $ SO_{4} $ and TDS in Panchet, Durgapur and Tenughat reservoirs indicate mining and anthropogenic impact on water quality. The high contribution of (Ca+Mg) to the total cations, high concentration of dissolved silica, relatively high (Na+K)/$ TZ^{+} $ ratio (0.3) and low equivalent ratio of (Ca+Mg)/(Na+K) suggests combined influence of carbonate and silicate weathering. Kaolinite is the possible mineral that is in equilibrium with the water, implying that the chemistry of reservoir water favours kaolinite formation. The calculated values of SAR, RSC and sodium percentage indicate the ‘excellent to good quality’ of water for irrigation uses. Hydrochemistry Reservoirs Damodar River Weathering Anthropogenic Water Quality Solute Flux India Mondal, G. C. aut Singh, P. K. aut Singh, S. aut Singh, T. B. aut Tewary, B. K. aut Enthalten in Environmental geology Springer-Verlag, 1975 48(2005), 8 vom: 20. Sept., Seite 1014-1028 (DE-627)129421634 (DE-600)190352-4 (DE-576)014797453 0943-0105 nnns volume:48 year:2005 number:8 day:20 month:09 pages:1014-1028 https://doi.org/10.1007/s00254-005-1302-6 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_22 GBV_ILN_30 GBV_ILN_40 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_267 GBV_ILN_2006 GBV_ILN_2010 GBV_ILN_2014 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_4012 GBV_ILN_4046 GBV_ILN_4277 GBV_ILN_4309 GBV_ILN_4314 TE 3140 AR 48 2005 8 20 09 1014-1028 |
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10.1007/s00254-005-1302-6 doi (DE-627)OLC2074406088 (DE-He213)s00254-005-1302-6-p DE-627 ger DE-627 rakwb eng 330 550 VZ 550 VZ 13 ssgn TE 3140 VZ rvk Singh, Abhay Kumar verfasserin aut Hydrochemistry of reservoirs of Damodar River basin, India: weathering processes and water quality assessment 2005 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 2005 Abstract Water samples collected from the six reservoirs of Damodar River basin in pre- and post-monsoon, have been analysed, to study the major ion chemistry and the weathering and geochemical processes controlling the water composition. Ca, Na and $ HCO_{3} $ dominate the chemical composition of the reservoir water. The seasonal data shows a minimum concentration of most of the ions in post-monsoon and a maximum concentration in pre-monsoon seasons, reflecting the concentrating effects due to elevated temperature and increased evaporation during the low water level period of the pre-monsoon season. Water chemistry of the reservoirs strongly reflects the dominance of continental weathering aided by atmospheric and anthropogenic activities in the catchment area. Higher concentration of $ SO_{4} $ and TDS in Panchet, Durgapur and Tenughat reservoirs indicate mining and anthropogenic impact on water quality. The high contribution of (Ca+Mg) to the total cations, high concentration of dissolved silica, relatively high (Na+K)/$ TZ^{+} $ ratio (0.3) and low equivalent ratio of (Ca+Mg)/(Na+K) suggests combined influence of carbonate and silicate weathering. Kaolinite is the possible mineral that is in equilibrium with the water, implying that the chemistry of reservoir water favours kaolinite formation. The calculated values of SAR, RSC and sodium percentage indicate the ‘excellent to good quality’ of water for irrigation uses. Hydrochemistry Reservoirs Damodar River Weathering Anthropogenic Water Quality Solute Flux India Mondal, G. C. aut Singh, P. K. aut Singh, S. aut Singh, T. B. aut Tewary, B. K. aut Enthalten in Environmental geology Springer-Verlag, 1975 48(2005), 8 vom: 20. Sept., Seite 1014-1028 (DE-627)129421634 (DE-600)190352-4 (DE-576)014797453 0943-0105 nnns volume:48 year:2005 number:8 day:20 month:09 pages:1014-1028 https://doi.org/10.1007/s00254-005-1302-6 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_22 GBV_ILN_30 GBV_ILN_40 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_267 GBV_ILN_2006 GBV_ILN_2010 GBV_ILN_2014 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_4012 GBV_ILN_4046 GBV_ILN_4277 GBV_ILN_4309 GBV_ILN_4314 TE 3140 AR 48 2005 8 20 09 1014-1028 |
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10.1007/s00254-005-1302-6 doi (DE-627)OLC2074406088 (DE-He213)s00254-005-1302-6-p DE-627 ger DE-627 rakwb eng 330 550 VZ 550 VZ 13 ssgn TE 3140 VZ rvk Singh, Abhay Kumar verfasserin aut Hydrochemistry of reservoirs of Damodar River basin, India: weathering processes and water quality assessment 2005 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 2005 Abstract Water samples collected from the six reservoirs of Damodar River basin in pre- and post-monsoon, have been analysed, to study the major ion chemistry and the weathering and geochemical processes controlling the water composition. Ca, Na and $ HCO_{3} $ dominate the chemical composition of the reservoir water. The seasonal data shows a minimum concentration of most of the ions in post-monsoon and a maximum concentration in pre-monsoon seasons, reflecting the concentrating effects due to elevated temperature and increased evaporation during the low water level period of the pre-monsoon season. Water chemistry of the reservoirs strongly reflects the dominance of continental weathering aided by atmospheric and anthropogenic activities in the catchment area. Higher concentration of $ SO_{4} $ and TDS in Panchet, Durgapur and Tenughat reservoirs indicate mining and anthropogenic impact on water quality. The high contribution of (Ca+Mg) to the total cations, high concentration of dissolved silica, relatively high (Na+K)/$ TZ^{+} $ ratio (0.3) and low equivalent ratio of (Ca+Mg)/(Na+K) suggests combined influence of carbonate and silicate weathering. Kaolinite is the possible mineral that is in equilibrium with the water, implying that the chemistry of reservoir water favours kaolinite formation. The calculated values of SAR, RSC and sodium percentage indicate the ‘excellent to good quality’ of water for irrigation uses. Hydrochemistry Reservoirs Damodar River Weathering Anthropogenic Water Quality Solute Flux India Mondal, G. C. aut Singh, P. K. aut Singh, S. aut Singh, T. B. aut Tewary, B. K. aut Enthalten in Environmental geology Springer-Verlag, 1975 48(2005), 8 vom: 20. Sept., Seite 1014-1028 (DE-627)129421634 (DE-600)190352-4 (DE-576)014797453 0943-0105 nnns volume:48 year:2005 number:8 day:20 month:09 pages:1014-1028 https://doi.org/10.1007/s00254-005-1302-6 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_22 GBV_ILN_30 GBV_ILN_40 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_267 GBV_ILN_2006 GBV_ILN_2010 GBV_ILN_2014 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_4012 GBV_ILN_4046 GBV_ILN_4277 GBV_ILN_4309 GBV_ILN_4314 TE 3140 AR 48 2005 8 20 09 1014-1028 |
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10.1007/s00254-005-1302-6 doi (DE-627)OLC2074406088 (DE-He213)s00254-005-1302-6-p DE-627 ger DE-627 rakwb eng 330 550 VZ 550 VZ 13 ssgn TE 3140 VZ rvk Singh, Abhay Kumar verfasserin aut Hydrochemistry of reservoirs of Damodar River basin, India: weathering processes and water quality assessment 2005 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 2005 Abstract Water samples collected from the six reservoirs of Damodar River basin in pre- and post-monsoon, have been analysed, to study the major ion chemistry and the weathering and geochemical processes controlling the water composition. Ca, Na and $ HCO_{3} $ dominate the chemical composition of the reservoir water. The seasonal data shows a minimum concentration of most of the ions in post-monsoon and a maximum concentration in pre-monsoon seasons, reflecting the concentrating effects due to elevated temperature and increased evaporation during the low water level period of the pre-monsoon season. Water chemistry of the reservoirs strongly reflects the dominance of continental weathering aided by atmospheric and anthropogenic activities in the catchment area. Higher concentration of $ SO_{4} $ and TDS in Panchet, Durgapur and Tenughat reservoirs indicate mining and anthropogenic impact on water quality. The high contribution of (Ca+Mg) to the total cations, high concentration of dissolved silica, relatively high (Na+K)/$ TZ^{+} $ ratio (0.3) and low equivalent ratio of (Ca+Mg)/(Na+K) suggests combined influence of carbonate and silicate weathering. Kaolinite is the possible mineral that is in equilibrium with the water, implying that the chemistry of reservoir water favours kaolinite formation. The calculated values of SAR, RSC and sodium percentage indicate the ‘excellent to good quality’ of water for irrigation uses. Hydrochemistry Reservoirs Damodar River Weathering Anthropogenic Water Quality Solute Flux India Mondal, G. C. aut Singh, P. K. aut Singh, S. aut Singh, T. B. aut Tewary, B. K. aut Enthalten in Environmental geology Springer-Verlag, 1975 48(2005), 8 vom: 20. Sept., Seite 1014-1028 (DE-627)129421634 (DE-600)190352-4 (DE-576)014797453 0943-0105 nnns volume:48 year:2005 number:8 day:20 month:09 pages:1014-1028 https://doi.org/10.1007/s00254-005-1302-6 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_22 GBV_ILN_30 GBV_ILN_40 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_267 GBV_ILN_2006 GBV_ILN_2010 GBV_ILN_2014 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_4012 GBV_ILN_4046 GBV_ILN_4277 GBV_ILN_4309 GBV_ILN_4314 TE 3140 AR 48 2005 8 20 09 1014-1028 |
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10.1007/s00254-005-1302-6 doi (DE-627)OLC2074406088 (DE-He213)s00254-005-1302-6-p DE-627 ger DE-627 rakwb eng 330 550 VZ 550 VZ 13 ssgn TE 3140 VZ rvk Singh, Abhay Kumar verfasserin aut Hydrochemistry of reservoirs of Damodar River basin, India: weathering processes and water quality assessment 2005 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 2005 Abstract Water samples collected from the six reservoirs of Damodar River basin in pre- and post-monsoon, have been analysed, to study the major ion chemistry and the weathering and geochemical processes controlling the water composition. Ca, Na and $ HCO_{3} $ dominate the chemical composition of the reservoir water. The seasonal data shows a minimum concentration of most of the ions in post-monsoon and a maximum concentration in pre-monsoon seasons, reflecting the concentrating effects due to elevated temperature and increased evaporation during the low water level period of the pre-monsoon season. Water chemistry of the reservoirs strongly reflects the dominance of continental weathering aided by atmospheric and anthropogenic activities in the catchment area. Higher concentration of $ SO_{4} $ and TDS in Panchet, Durgapur and Tenughat reservoirs indicate mining and anthropogenic impact on water quality. The high contribution of (Ca+Mg) to the total cations, high concentration of dissolved silica, relatively high (Na+K)/$ TZ^{+} $ ratio (0.3) and low equivalent ratio of (Ca+Mg)/(Na+K) suggests combined influence of carbonate and silicate weathering. Kaolinite is the possible mineral that is in equilibrium with the water, implying that the chemistry of reservoir water favours kaolinite formation. The calculated values of SAR, RSC and sodium percentage indicate the ‘excellent to good quality’ of water for irrigation uses. Hydrochemistry Reservoirs Damodar River Weathering Anthropogenic Water Quality Solute Flux India Mondal, G. C. aut Singh, P. K. aut Singh, S. aut Singh, T. B. aut Tewary, B. K. aut Enthalten in Environmental geology Springer-Verlag, 1975 48(2005), 8 vom: 20. Sept., Seite 1014-1028 (DE-627)129421634 (DE-600)190352-4 (DE-576)014797453 0943-0105 nnns volume:48 year:2005 number:8 day:20 month:09 pages:1014-1028 https://doi.org/10.1007/s00254-005-1302-6 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_22 GBV_ILN_30 GBV_ILN_40 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_267 GBV_ILN_2006 GBV_ILN_2010 GBV_ILN_2014 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_4012 GBV_ILN_4046 GBV_ILN_4277 GBV_ILN_4309 GBV_ILN_4314 TE 3140 AR 48 2005 8 20 09 1014-1028 |
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Hydrochemistry of reservoirs of Damodar River basin, India: weathering processes and water quality assessment |
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Abstract Water samples collected from the six reservoirs of Damodar River basin in pre- and post-monsoon, have been analysed, to study the major ion chemistry and the weathering and geochemical processes controlling the water composition. Ca, Na and $ HCO_{3} $ dominate the chemical composition of the reservoir water. The seasonal data shows a minimum concentration of most of the ions in post-monsoon and a maximum concentration in pre-monsoon seasons, reflecting the concentrating effects due to elevated temperature and increased evaporation during the low water level period of the pre-monsoon season. Water chemistry of the reservoirs strongly reflects the dominance of continental weathering aided by atmospheric and anthropogenic activities in the catchment area. Higher concentration of $ SO_{4} $ and TDS in Panchet, Durgapur and Tenughat reservoirs indicate mining and anthropogenic impact on water quality. The high contribution of (Ca+Mg) to the total cations, high concentration of dissolved silica, relatively high (Na+K)/$ TZ^{+} $ ratio (0.3) and low equivalent ratio of (Ca+Mg)/(Na+K) suggests combined influence of carbonate and silicate weathering. Kaolinite is the possible mineral that is in equilibrium with the water, implying that the chemistry of reservoir water favours kaolinite formation. The calculated values of SAR, RSC and sodium percentage indicate the ‘excellent to good quality’ of water for irrigation uses. © Springer-Verlag 2005 |
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Abstract Water samples collected from the six reservoirs of Damodar River basin in pre- and post-monsoon, have been analysed, to study the major ion chemistry and the weathering and geochemical processes controlling the water composition. Ca, Na and $ HCO_{3} $ dominate the chemical composition of the reservoir water. The seasonal data shows a minimum concentration of most of the ions in post-monsoon and a maximum concentration in pre-monsoon seasons, reflecting the concentrating effects due to elevated temperature and increased evaporation during the low water level period of the pre-monsoon season. Water chemistry of the reservoirs strongly reflects the dominance of continental weathering aided by atmospheric and anthropogenic activities in the catchment area. Higher concentration of $ SO_{4} $ and TDS in Panchet, Durgapur and Tenughat reservoirs indicate mining and anthropogenic impact on water quality. The high contribution of (Ca+Mg) to the total cations, high concentration of dissolved silica, relatively high (Na+K)/$ TZ^{+} $ ratio (0.3) and low equivalent ratio of (Ca+Mg)/(Na+K) suggests combined influence of carbonate and silicate weathering. Kaolinite is the possible mineral that is in equilibrium with the water, implying that the chemistry of reservoir water favours kaolinite formation. The calculated values of SAR, RSC and sodium percentage indicate the ‘excellent to good quality’ of water for irrigation uses. © Springer-Verlag 2005 |
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Abstract Water samples collected from the six reservoirs of Damodar River basin in pre- and post-monsoon, have been analysed, to study the major ion chemistry and the weathering and geochemical processes controlling the water composition. Ca, Na and $ HCO_{3} $ dominate the chemical composition of the reservoir water. The seasonal data shows a minimum concentration of most of the ions in post-monsoon and a maximum concentration in pre-monsoon seasons, reflecting the concentrating effects due to elevated temperature and increased evaporation during the low water level period of the pre-monsoon season. Water chemistry of the reservoirs strongly reflects the dominance of continental weathering aided by atmospheric and anthropogenic activities in the catchment area. Higher concentration of $ SO_{4} $ and TDS in Panchet, Durgapur and Tenughat reservoirs indicate mining and anthropogenic impact on water quality. The high contribution of (Ca+Mg) to the total cations, high concentration of dissolved silica, relatively high (Na+K)/$ TZ^{+} $ ratio (0.3) and low equivalent ratio of (Ca+Mg)/(Na+K) suggests combined influence of carbonate and silicate weathering. Kaolinite is the possible mineral that is in equilibrium with the water, implying that the chemistry of reservoir water favours kaolinite formation. The calculated values of SAR, RSC and sodium percentage indicate the ‘excellent to good quality’ of water for irrigation uses. © Springer-Verlag 2005 |
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