Hydrogeochemical delineation of groundwater fitness for drinking and agricultural utilities in Thiruvallur district, South India
Abstract Appraisal of groundwater fitness to drinking, agricultural, and domestic purposes was attempted within the Thiruvallur district of South India since groundwater is the significant sources for the above utilities. Groundwater samples collected from a sum of 110 locations have to be analyzed...
Ausführliche Beschreibung
Autor*in: |
Senthilkumar, Subramani [verfasserIn] Gowtham, Balu [verfasserIn] Srinivasamoorthy, Krishnaraj [verfasserIn] Gopinath, Selvaraj [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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Übergeordnetes Werk: |
Enthalten in: Arabian journal of geosciences - Berlin : Springer, 2008, 14(2021), 6 vom: März |
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Übergeordnetes Werk: |
volume:14 ; year:2021 ; number:6 ; month:03 |
Links: |
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DOI / URN: |
10.1007/s12517-021-06547-z |
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Katalog-ID: |
SPR043508413 |
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245 | 1 | 0 | |a Hydrogeochemical delineation of groundwater fitness for drinking and agricultural utilities in Thiruvallur district, South India |
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520 | |a Abstract Appraisal of groundwater fitness to drinking, agricultural, and domestic purposes was attempted within the Thiruvallur district of South India since groundwater is the significant sources for the above utilities. Groundwater samples collected from a sum of 110 locations have to be analyzed for major concentrations of which higher values of total dissolved solids (TDS), chloride ($ Cl^{−} $), and sodium ($ Na^{+} $) ions were noted during pre-monsoon (PRM) specifically besides the east along with the southeastern part of the study region and higher calcium ($ Ca^{2+} $) and nitrate ($ NO_{3} $−) values disseminated besides the central and eastern parts of the study region during the post-monsoon (POM) season. Suitability of water quality depends upon total dissolved solids; Water Quality Index (WQI) suggests 70% and 62% of the study area representing hard and sedimentary formations are appropriate for consumption utilities. Irrigation aptness of water for utility suggests the majority of study area is suitable in view of electrical conductance, sodium adsorption ratio, USSL plot, Na%, Wilcox’s plot, Kelly’s ratio, and Doneen’s plot. Dominant hydrochemical facies were observed to be Na-Cl, mixed Ca-Mg-Cl, and Ca-$ HCO_{3} $, and parameters like $ Na^{+} $, $ Ca^{2+} $, $ HCO_{3} $−, $ Cl^{−} $, and $ NO_{3} $− ions have been observed to be higher in the central region next to the east and may be appropriate to influence geogenic, anthropogenic, and seawater encroachment. | ||
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650 | 4 | |a Encroachment |7 (dpeaa)DE-He213 | |
700 | 1 | |a Gowtham, Balu |e verfasserin |4 aut | |
700 | 1 | |a Srinivasamoorthy, Krishnaraj |e verfasserin |4 aut | |
700 | 1 | |a Gopinath, Selvaraj |e verfasserin |4 aut | |
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10.1007/s12517-021-06547-z doi (DE-627)SPR043508413 (DE-599)SPRs12517-021-06547-z-e (SPR)s12517-021-06547-z-e DE-627 ger DE-627 rakwb eng 550 ASE Senthilkumar, Subramani verfasserin aut Hydrogeochemical delineation of groundwater fitness for drinking and agricultural utilities in Thiruvallur district, South India 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Appraisal of groundwater fitness to drinking, agricultural, and domestic purposes was attempted within the Thiruvallur district of South India since groundwater is the significant sources for the above utilities. Groundwater samples collected from a sum of 110 locations have to be analyzed for major concentrations of which higher values of total dissolved solids (TDS), chloride ($ Cl^{−} $), and sodium ($ Na^{+} $) ions were noted during pre-monsoon (PRM) specifically besides the east along with the southeastern part of the study region and higher calcium ($ Ca^{2+} $) and nitrate ($ NO_{3} $−) values disseminated besides the central and eastern parts of the study region during the post-monsoon (POM) season. Suitability of water quality depends upon total dissolved solids; Water Quality Index (WQI) suggests 70% and 62% of the study area representing hard and sedimentary formations are appropriate for consumption utilities. Irrigation aptness of water for utility suggests the majority of study area is suitable in view of electrical conductance, sodium adsorption ratio, USSL plot, Na%, Wilcox’s plot, Kelly’s ratio, and Doneen’s plot. Dominant hydrochemical facies were observed to be Na-Cl, mixed Ca-Mg-Cl, and Ca-$ HCO_{3} $, and parameters like $ Na^{+} $, $ Ca^{2+} $, $ HCO_{3} $−, $ Cl^{−} $, and $ NO_{3} $− ions have been observed to be higher in the central region next to the east and may be appropriate to influence geogenic, anthropogenic, and seawater encroachment. Coastal groundwater (dpeaa)DE-He213 Hydrochemical facies (dpeaa)DE-He213 Wilcox diagram (dpeaa)DE-He213 Encroachment (dpeaa)DE-He213 Gowtham, Balu verfasserin aut Srinivasamoorthy, Krishnaraj verfasserin aut Gopinath, Selvaraj verfasserin aut Enthalten in Arabian journal of geosciences Berlin : Springer, 2008 14(2021), 6 vom: März (DE-627)572421877 (DE-600)2438771-X 1866-7538 nnns volume:14 year:2021 number:6 month:03 https://dx.doi.org/10.1007/s12517-021-06547-z kostenfrei 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 6 03 |
spelling |
10.1007/s12517-021-06547-z doi (DE-627)SPR043508413 (DE-599)SPRs12517-021-06547-z-e (SPR)s12517-021-06547-z-e DE-627 ger DE-627 rakwb eng 550 ASE Senthilkumar, Subramani verfasserin aut Hydrogeochemical delineation of groundwater fitness for drinking and agricultural utilities in Thiruvallur district, South India 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Appraisal of groundwater fitness to drinking, agricultural, and domestic purposes was attempted within the Thiruvallur district of South India since groundwater is the significant sources for the above utilities. Groundwater samples collected from a sum of 110 locations have to be analyzed for major concentrations of which higher values of total dissolved solids (TDS), chloride ($ Cl^{−} $), and sodium ($ Na^{+} $) ions were noted during pre-monsoon (PRM) specifically besides the east along with the southeastern part of the study region and higher calcium ($ Ca^{2+} $) and nitrate ($ NO_{3} $−) values disseminated besides the central and eastern parts of the study region during the post-monsoon (POM) season. Suitability of water quality depends upon total dissolved solids; Water Quality Index (WQI) suggests 70% and 62% of the study area representing hard and sedimentary formations are appropriate for consumption utilities. Irrigation aptness of water for utility suggests the majority of study area is suitable in view of electrical conductance, sodium adsorption ratio, USSL plot, Na%, Wilcox’s plot, Kelly’s ratio, and Doneen’s plot. Dominant hydrochemical facies were observed to be Na-Cl, mixed Ca-Mg-Cl, and Ca-$ HCO_{3} $, and parameters like $ Na^{+} $, $ Ca^{2+} $, $ HCO_{3} $−, $ Cl^{−} $, and $ NO_{3} $− ions have been observed to be higher in the central region next to the east and may be appropriate to influence geogenic, anthropogenic, and seawater encroachment. Coastal groundwater (dpeaa)DE-He213 Hydrochemical facies (dpeaa)DE-He213 Wilcox diagram (dpeaa)DE-He213 Encroachment (dpeaa)DE-He213 Gowtham, Balu verfasserin aut Srinivasamoorthy, Krishnaraj verfasserin aut Gopinath, Selvaraj verfasserin aut Enthalten in Arabian journal of geosciences Berlin : Springer, 2008 14(2021), 6 vom: März (DE-627)572421877 (DE-600)2438771-X 1866-7538 nnns volume:14 year:2021 number:6 month:03 https://dx.doi.org/10.1007/s12517-021-06547-z kostenfrei 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 6 03 |
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10.1007/s12517-021-06547-z doi (DE-627)SPR043508413 (DE-599)SPRs12517-021-06547-z-e (SPR)s12517-021-06547-z-e DE-627 ger DE-627 rakwb eng 550 ASE Senthilkumar, Subramani verfasserin aut Hydrogeochemical delineation of groundwater fitness for drinking and agricultural utilities in Thiruvallur district, South India 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Appraisal of groundwater fitness to drinking, agricultural, and domestic purposes was attempted within the Thiruvallur district of South India since groundwater is the significant sources for the above utilities. Groundwater samples collected from a sum of 110 locations have to be analyzed for major concentrations of which higher values of total dissolved solids (TDS), chloride ($ Cl^{−} $), and sodium ($ Na^{+} $) ions were noted during pre-monsoon (PRM) specifically besides the east along with the southeastern part of the study region and higher calcium ($ Ca^{2+} $) and nitrate ($ NO_{3} $−) values disseminated besides the central and eastern parts of the study region during the post-monsoon (POM) season. Suitability of water quality depends upon total dissolved solids; Water Quality Index (WQI) suggests 70% and 62% of the study area representing hard and sedimentary formations are appropriate for consumption utilities. Irrigation aptness of water for utility suggests the majority of study area is suitable in view of electrical conductance, sodium adsorption ratio, USSL plot, Na%, Wilcox’s plot, Kelly’s ratio, and Doneen’s plot. Dominant hydrochemical facies were observed to be Na-Cl, mixed Ca-Mg-Cl, and Ca-$ HCO_{3} $, and parameters like $ Na^{+} $, $ Ca^{2+} $, $ HCO_{3} $−, $ Cl^{−} $, and $ NO_{3} $− ions have been observed to be higher in the central region next to the east and may be appropriate to influence geogenic, anthropogenic, and seawater encroachment. Coastal groundwater (dpeaa)DE-He213 Hydrochemical facies (dpeaa)DE-He213 Wilcox diagram (dpeaa)DE-He213 Encroachment (dpeaa)DE-He213 Gowtham, Balu verfasserin aut Srinivasamoorthy, Krishnaraj verfasserin aut Gopinath, Selvaraj verfasserin aut Enthalten in Arabian journal of geosciences Berlin : Springer, 2008 14(2021), 6 vom: März (DE-627)572421877 (DE-600)2438771-X 1866-7538 nnns volume:14 year:2021 number:6 month:03 https://dx.doi.org/10.1007/s12517-021-06547-z kostenfrei 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 6 03 |
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10.1007/s12517-021-06547-z doi (DE-627)SPR043508413 (DE-599)SPRs12517-021-06547-z-e (SPR)s12517-021-06547-z-e DE-627 ger DE-627 rakwb eng 550 ASE Senthilkumar, Subramani verfasserin aut Hydrogeochemical delineation of groundwater fitness for drinking and agricultural utilities in Thiruvallur district, South India 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Appraisal of groundwater fitness to drinking, agricultural, and domestic purposes was attempted within the Thiruvallur district of South India since groundwater is the significant sources for the above utilities. Groundwater samples collected from a sum of 110 locations have to be analyzed for major concentrations of which higher values of total dissolved solids (TDS), chloride ($ Cl^{−} $), and sodium ($ Na^{+} $) ions were noted during pre-monsoon (PRM) specifically besides the east along with the southeastern part of the study region and higher calcium ($ Ca^{2+} $) and nitrate ($ NO_{3} $−) values disseminated besides the central and eastern parts of the study region during the post-monsoon (POM) season. Suitability of water quality depends upon total dissolved solids; Water Quality Index (WQI) suggests 70% and 62% of the study area representing hard and sedimentary formations are appropriate for consumption utilities. Irrigation aptness of water for utility suggests the majority of study area is suitable in view of electrical conductance, sodium adsorption ratio, USSL plot, Na%, Wilcox’s plot, Kelly’s ratio, and Doneen’s plot. Dominant hydrochemical facies were observed to be Na-Cl, mixed Ca-Mg-Cl, and Ca-$ HCO_{3} $, and parameters like $ Na^{+} $, $ Ca^{2+} $, $ HCO_{3} $−, $ Cl^{−} $, and $ NO_{3} $− ions have been observed to be higher in the central region next to the east and may be appropriate to influence geogenic, anthropogenic, and seawater encroachment. Coastal groundwater (dpeaa)DE-He213 Hydrochemical facies (dpeaa)DE-He213 Wilcox diagram (dpeaa)DE-He213 Encroachment (dpeaa)DE-He213 Gowtham, Balu verfasserin aut Srinivasamoorthy, Krishnaraj verfasserin aut Gopinath, Selvaraj verfasserin aut Enthalten in Arabian journal of geosciences Berlin : Springer, 2008 14(2021), 6 vom: März (DE-627)572421877 (DE-600)2438771-X 1866-7538 nnns volume:14 year:2021 number:6 month:03 https://dx.doi.org/10.1007/s12517-021-06547-z kostenfrei 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 6 03 |
allfieldsSound |
10.1007/s12517-021-06547-z doi (DE-627)SPR043508413 (DE-599)SPRs12517-021-06547-z-e (SPR)s12517-021-06547-z-e DE-627 ger DE-627 rakwb eng 550 ASE Senthilkumar, Subramani verfasserin aut Hydrogeochemical delineation of groundwater fitness for drinking and agricultural utilities in Thiruvallur district, South India 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Appraisal of groundwater fitness to drinking, agricultural, and domestic purposes was attempted within the Thiruvallur district of South India since groundwater is the significant sources for the above utilities. Groundwater samples collected from a sum of 110 locations have to be analyzed for major concentrations of which higher values of total dissolved solids (TDS), chloride ($ Cl^{−} $), and sodium ($ Na^{+} $) ions were noted during pre-monsoon (PRM) specifically besides the east along with the southeastern part of the study region and higher calcium ($ Ca^{2+} $) and nitrate ($ NO_{3} $−) values disseminated besides the central and eastern parts of the study region during the post-monsoon (POM) season. Suitability of water quality depends upon total dissolved solids; Water Quality Index (WQI) suggests 70% and 62% of the study area representing hard and sedimentary formations are appropriate for consumption utilities. Irrigation aptness of water for utility suggests the majority of study area is suitable in view of electrical conductance, sodium adsorption ratio, USSL plot, Na%, Wilcox’s plot, Kelly’s ratio, and Doneen’s plot. Dominant hydrochemical facies were observed to be Na-Cl, mixed Ca-Mg-Cl, and Ca-$ HCO_{3} $, and parameters like $ Na^{+} $, $ Ca^{2+} $, $ HCO_{3} $−, $ Cl^{−} $, and $ NO_{3} $− ions have been observed to be higher in the central region next to the east and may be appropriate to influence geogenic, anthropogenic, and seawater encroachment. Coastal groundwater (dpeaa)DE-He213 Hydrochemical facies (dpeaa)DE-He213 Wilcox diagram (dpeaa)DE-He213 Encroachment (dpeaa)DE-He213 Gowtham, Balu verfasserin aut Srinivasamoorthy, Krishnaraj verfasserin aut Gopinath, Selvaraj verfasserin aut Enthalten in Arabian journal of geosciences Berlin : Springer, 2008 14(2021), 6 vom: März (DE-627)572421877 (DE-600)2438771-X 1866-7538 nnns volume:14 year:2021 number:6 month:03 https://dx.doi.org/10.1007/s12517-021-06547-z kostenfrei 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 6 03 |
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Enthalten in Arabian journal of geosciences 14(2021), 6 vom: März volume:14 year:2021 number:6 month:03 |
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Senthilkumar, Subramani @@aut@@ Gowtham, Balu @@aut@@ Srinivasamoorthy, Krishnaraj @@aut@@ Gopinath, Selvaraj @@aut@@ |
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Groundwater samples collected from a sum of 110 locations have to be analyzed for major concentrations of which higher values of total dissolved solids (TDS), chloride ($ Cl^{−} $), and sodium ($ Na^{+} $) ions were noted during pre-monsoon (PRM) specifically besides the east along with the southeastern part of the study region and higher calcium ($ Ca^{2+} $) and nitrate ($ NO_{3} $−) values disseminated besides the central and eastern parts of the study region during the post-monsoon (POM) season. Suitability of water quality depends upon total dissolved solids; Water Quality Index (WQI) suggests 70% and 62% of the study area representing hard and sedimentary formations are appropriate for consumption utilities. Irrigation aptness of water for utility suggests the majority of study area is suitable in view of electrical conductance, sodium adsorption ratio, USSL plot, Na%, Wilcox’s plot, Kelly’s ratio, and Doneen’s plot. 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Senthilkumar, Subramani |
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Senthilkumar, Subramani ddc 550 misc Coastal groundwater misc Hydrochemical facies misc Wilcox diagram misc Encroachment Hydrogeochemical delineation of groundwater fitness for drinking and agricultural utilities in Thiruvallur district, South India |
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550 ASE Hydrogeochemical delineation of groundwater fitness for drinking and agricultural utilities in Thiruvallur district, South India Coastal groundwater (dpeaa)DE-He213 Hydrochemical facies (dpeaa)DE-He213 Wilcox diagram (dpeaa)DE-He213 Encroachment (dpeaa)DE-He213 |
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ddc 550 misc Coastal groundwater misc Hydrochemical facies misc Wilcox diagram misc Encroachment |
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Hydrogeochemical delineation of groundwater fitness for drinking and agricultural utilities in Thiruvallur district, South India |
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Hydrogeochemical delineation of groundwater fitness for drinking and agricultural utilities in Thiruvallur district, South India |
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Senthilkumar, Subramani |
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Arabian journal of geosciences |
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Senthilkumar, Subramani Gowtham, Balu Srinivasamoorthy, Krishnaraj Gopinath, Selvaraj |
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Senthilkumar, Subramani |
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hydrogeochemical delineation of groundwater fitness for drinking and agricultural utilities in thiruvallur district, south india |
title_auth |
Hydrogeochemical delineation of groundwater fitness for drinking and agricultural utilities in Thiruvallur district, South India |
abstract |
Abstract Appraisal of groundwater fitness to drinking, agricultural, and domestic purposes was attempted within the Thiruvallur district of South India since groundwater is the significant sources for the above utilities. Groundwater samples collected from a sum of 110 locations have to be analyzed for major concentrations of which higher values of total dissolved solids (TDS), chloride ($ Cl^{−} $), and sodium ($ Na^{+} $) ions were noted during pre-monsoon (PRM) specifically besides the east along with the southeastern part of the study region and higher calcium ($ Ca^{2+} $) and nitrate ($ NO_{3} $−) values disseminated besides the central and eastern parts of the study region during the post-monsoon (POM) season. Suitability of water quality depends upon total dissolved solids; Water Quality Index (WQI) suggests 70% and 62% of the study area representing hard and sedimentary formations are appropriate for consumption utilities. Irrigation aptness of water for utility suggests the majority of study area is suitable in view of electrical conductance, sodium adsorption ratio, USSL plot, Na%, Wilcox’s plot, Kelly’s ratio, and Doneen’s plot. Dominant hydrochemical facies were observed to be Na-Cl, mixed Ca-Mg-Cl, and Ca-$ HCO_{3} $, and parameters like $ Na^{+} $, $ Ca^{2+} $, $ HCO_{3} $−, $ Cl^{−} $, and $ NO_{3} $− ions have been observed to be higher in the central region next to the east and may be appropriate to influence geogenic, anthropogenic, and seawater encroachment. |
abstractGer |
Abstract Appraisal of groundwater fitness to drinking, agricultural, and domestic purposes was attempted within the Thiruvallur district of South India since groundwater is the significant sources for the above utilities. Groundwater samples collected from a sum of 110 locations have to be analyzed for major concentrations of which higher values of total dissolved solids (TDS), chloride ($ Cl^{−} $), and sodium ($ Na^{+} $) ions were noted during pre-monsoon (PRM) specifically besides the east along with the southeastern part of the study region and higher calcium ($ Ca^{2+} $) and nitrate ($ NO_{3} $−) values disseminated besides the central and eastern parts of the study region during the post-monsoon (POM) season. Suitability of water quality depends upon total dissolved solids; Water Quality Index (WQI) suggests 70% and 62% of the study area representing hard and sedimentary formations are appropriate for consumption utilities. Irrigation aptness of water for utility suggests the majority of study area is suitable in view of electrical conductance, sodium adsorption ratio, USSL plot, Na%, Wilcox’s plot, Kelly’s ratio, and Doneen’s plot. Dominant hydrochemical facies were observed to be Na-Cl, mixed Ca-Mg-Cl, and Ca-$ HCO_{3} $, and parameters like $ Na^{+} $, $ Ca^{2+} $, $ HCO_{3} $−, $ Cl^{−} $, and $ NO_{3} $− ions have been observed to be higher in the central region next to the east and may be appropriate to influence geogenic, anthropogenic, and seawater encroachment. |
abstract_unstemmed |
Abstract Appraisal of groundwater fitness to drinking, agricultural, and domestic purposes was attempted within the Thiruvallur district of South India since groundwater is the significant sources for the above utilities. Groundwater samples collected from a sum of 110 locations have to be analyzed for major concentrations of which higher values of total dissolved solids (TDS), chloride ($ Cl^{−} $), and sodium ($ Na^{+} $) ions were noted during pre-monsoon (PRM) specifically besides the east along with the southeastern part of the study region and higher calcium ($ Ca^{2+} $) and nitrate ($ NO_{3} $−) values disseminated besides the central and eastern parts of the study region during the post-monsoon (POM) season. Suitability of water quality depends upon total dissolved solids; Water Quality Index (WQI) suggests 70% and 62% of the study area representing hard and sedimentary formations are appropriate for consumption utilities. Irrigation aptness of water for utility suggests the majority of study area is suitable in view of electrical conductance, sodium adsorption ratio, USSL plot, Na%, Wilcox’s plot, Kelly’s ratio, and Doneen’s plot. Dominant hydrochemical facies were observed to be Na-Cl, mixed Ca-Mg-Cl, and Ca-$ HCO_{3} $, and parameters like $ Na^{+} $, $ Ca^{2+} $, $ HCO_{3} $−, $ Cl^{−} $, and $ NO_{3} $− ions have been observed to be higher in the central region next to the east and may be appropriate to influence geogenic, anthropogenic, and seawater encroachment. |
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container_issue |
6 |
title_short |
Hydrogeochemical delineation of groundwater fitness for drinking and agricultural utilities in Thiruvallur district, South India |
url |
https://dx.doi.org/10.1007/s12517-021-06547-z |
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author2 |
Gowtham, Balu Srinivasamoorthy, Krishnaraj Gopinath, Selvaraj |
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doi_str |
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up_date |
2024-07-03T19:07:31.834Z |
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score |
7.400666 |