Identification of potential groundwater zones in rice-fallow areas within the Mahanadi river basin, India, using GIS and the analytical hierarchy process
Abstract To feed the ever-growing population of India, it is essential to bring rice-fallow areas under cultivation, which is mostly restricted owing to surface water scarcity. Groundwater can be a viable alternative to meet the demand which needs to be explored using a suitable mechanism. The prese...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Das, Dwarika Mohan [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2022 |
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| Schlagwörter: |
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| Anmerkung: |
© The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2022 |
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| Übergeordnetes Werk: |
Enthalten in: Environmental earth sciences - Berlin : Springer, 2009, 81(2022), 15 vom: 28. Juli |
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| Übergeordnetes Werk: |
volume:81 ; year:2022 ; number:15 ; day:28 ; month:07 |
| Links: |
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| DOI / URN: |
10.1007/s12665-022-10517-3 |
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| Katalog-ID: |
SPR047708085 |
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| 245 | 1 | 0 | |a Identification of potential groundwater zones in rice-fallow areas within the Mahanadi river basin, India, using GIS and the analytical hierarchy process |
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| 520 | |a Abstract To feed the ever-growing population of India, it is essential to bring rice-fallow areas under cultivation, which is mostly restricted owing to surface water scarcity. Groundwater can be a viable alternative to meet the demand which needs to be explored using a suitable mechanism. The present study was undertaken to delineate groundwater potential zones in the rice-fallow areas of Kantamal catchment located in the middle reach of Mahanadi basin (India). These areas can be viable for growing a second crop during the rabi season provided assured irrigation water is available. Groundwater potential zoning is considered as a pre-requisite for groundwater exploration and sustainable well yield. Remote sensing and geographical information system using the analytical hierarchy process (AHP) were used for demarcating groundwater potential zones in the entire catchment as well as in the rice-fallow areas. Thematic layers of lithology, seasonal groundwater storage, lineament density, geomorphology, soil texture, slope, land use/land cover and drainage density were prepared and applied for groundwater potential zoning. The catchment was categorized into very good, good, moderate and poor groundwater potential zones that occupy 23, 24, 42 and 11% area of the catchment, respectively. Rice-fallow area masking over the groundwater potential map reveals that very good, good, moderate and poor groundwater zones are prevalent in 35, 31, 31 and 3% of the total rice-fallow area, respectively. This implies that around 66% of the rice-fallow area in the catchment has a very good to good groundwater potential, which can be judiciously irrigated with groundwater for growing low water requiring rabi crops. | ||
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10.1007/s12665-022-10517-3 doi (DE-627)SPR047708085 (SPR)s12665-022-10517-3-e DE-627 ger DE-627 rakwb eng Das, Dwarika Mohan verfasserin aut Identification of potential groundwater zones in rice-fallow areas within the Mahanadi river basin, India, using GIS and the analytical hierarchy process 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2022 Abstract To feed the ever-growing population of India, it is essential to bring rice-fallow areas under cultivation, which is mostly restricted owing to surface water scarcity. Groundwater can be a viable alternative to meet the demand which needs to be explored using a suitable mechanism. The present study was undertaken to delineate groundwater potential zones in the rice-fallow areas of Kantamal catchment located in the middle reach of Mahanadi basin (India). These areas can be viable for growing a second crop during the rabi season provided assured irrigation water is available. Groundwater potential zoning is considered as a pre-requisite for groundwater exploration and sustainable well yield. Remote sensing and geographical information system using the analytical hierarchy process (AHP) were used for demarcating groundwater potential zones in the entire catchment as well as in the rice-fallow areas. Thematic layers of lithology, seasonal groundwater storage, lineament density, geomorphology, soil texture, slope, land use/land cover and drainage density were prepared and applied for groundwater potential zoning. The catchment was categorized into very good, good, moderate and poor groundwater potential zones that occupy 23, 24, 42 and 11% area of the catchment, respectively. Rice-fallow area masking over the groundwater potential map reveals that very good, good, moderate and poor groundwater zones are prevalent in 35, 31, 31 and 3% of the total rice-fallow area, respectively. This implies that around 66% of the rice-fallow area in the catchment has a very good to good groundwater potential, which can be judiciously irrigated with groundwater for growing low water requiring rabi crops. Groundwater potential (dpeaa)DE-He213 Remote sensing (dpeaa)DE-He213 GIS (dpeaa)DE-He213 MCDM (dpeaa)DE-He213 AHP (dpeaa)DE-He213 Rice-fallow (dpeaa)DE-He213 Nayak, Dikshya aut Sahoo, Bharat Chandra aut Raul, Sanjay Kumar (orcid)0000-0002-2389-5893 aut Panigrahi, Balram aut Choudhary, Karun Kumar aut Enthalten in Environmental earth sciences Berlin : Springer, 2009 81(2022), 15 vom: 28. Juli (DE-627)599673451 (DE-600)2493699-6 1866-6299 nnns volume:81 year:2022 number:15 day:28 month:07 https://dx.doi.org/10.1007/s12665-022-10517-3 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_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_2119 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_2360 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 81 2022 15 28 07 |
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10.1007/s12665-022-10517-3 doi (DE-627)SPR047708085 (SPR)s12665-022-10517-3-e DE-627 ger DE-627 rakwb eng Das, Dwarika Mohan verfasserin aut Identification of potential groundwater zones in rice-fallow areas within the Mahanadi river basin, India, using GIS and the analytical hierarchy process 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2022 Abstract To feed the ever-growing population of India, it is essential to bring rice-fallow areas under cultivation, which is mostly restricted owing to surface water scarcity. Groundwater can be a viable alternative to meet the demand which needs to be explored using a suitable mechanism. The present study was undertaken to delineate groundwater potential zones in the rice-fallow areas of Kantamal catchment located in the middle reach of Mahanadi basin (India). These areas can be viable for growing a second crop during the rabi season provided assured irrigation water is available. Groundwater potential zoning is considered as a pre-requisite for groundwater exploration and sustainable well yield. Remote sensing and geographical information system using the analytical hierarchy process (AHP) were used for demarcating groundwater potential zones in the entire catchment as well as in the rice-fallow areas. Thematic layers of lithology, seasonal groundwater storage, lineament density, geomorphology, soil texture, slope, land use/land cover and drainage density were prepared and applied for groundwater potential zoning. The catchment was categorized into very good, good, moderate and poor groundwater potential zones that occupy 23, 24, 42 and 11% area of the catchment, respectively. Rice-fallow area masking over the groundwater potential map reveals that very good, good, moderate and poor groundwater zones are prevalent in 35, 31, 31 and 3% of the total rice-fallow area, respectively. This implies that around 66% of the rice-fallow area in the catchment has a very good to good groundwater potential, which can be judiciously irrigated with groundwater for growing low water requiring rabi crops. Groundwater potential (dpeaa)DE-He213 Remote sensing (dpeaa)DE-He213 GIS (dpeaa)DE-He213 MCDM (dpeaa)DE-He213 AHP (dpeaa)DE-He213 Rice-fallow (dpeaa)DE-He213 Nayak, Dikshya aut Sahoo, Bharat Chandra aut Raul, Sanjay Kumar (orcid)0000-0002-2389-5893 aut Panigrahi, Balram aut Choudhary, Karun Kumar aut Enthalten in Environmental earth sciences Berlin : Springer, 2009 81(2022), 15 vom: 28. Juli (DE-627)599673451 (DE-600)2493699-6 1866-6299 nnns volume:81 year:2022 number:15 day:28 month:07 https://dx.doi.org/10.1007/s12665-022-10517-3 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_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_2119 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_2360 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 81 2022 15 28 07 |
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10.1007/s12665-022-10517-3 doi (DE-627)SPR047708085 (SPR)s12665-022-10517-3-e DE-627 ger DE-627 rakwb eng Das, Dwarika Mohan verfasserin aut Identification of potential groundwater zones in rice-fallow areas within the Mahanadi river basin, India, using GIS and the analytical hierarchy process 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2022 Abstract To feed the ever-growing population of India, it is essential to bring rice-fallow areas under cultivation, which is mostly restricted owing to surface water scarcity. Groundwater can be a viable alternative to meet the demand which needs to be explored using a suitable mechanism. The present study was undertaken to delineate groundwater potential zones in the rice-fallow areas of Kantamal catchment located in the middle reach of Mahanadi basin (India). These areas can be viable for growing a second crop during the rabi season provided assured irrigation water is available. Groundwater potential zoning is considered as a pre-requisite for groundwater exploration and sustainable well yield. Remote sensing and geographical information system using the analytical hierarchy process (AHP) were used for demarcating groundwater potential zones in the entire catchment as well as in the rice-fallow areas. Thematic layers of lithology, seasonal groundwater storage, lineament density, geomorphology, soil texture, slope, land use/land cover and drainage density were prepared and applied for groundwater potential zoning. The catchment was categorized into very good, good, moderate and poor groundwater potential zones that occupy 23, 24, 42 and 11% area of the catchment, respectively. Rice-fallow area masking over the groundwater potential map reveals that very good, good, moderate and poor groundwater zones are prevalent in 35, 31, 31 and 3% of the total rice-fallow area, respectively. This implies that around 66% of the rice-fallow area in the catchment has a very good to good groundwater potential, which can be judiciously irrigated with groundwater for growing low water requiring rabi crops. Groundwater potential (dpeaa)DE-He213 Remote sensing (dpeaa)DE-He213 GIS (dpeaa)DE-He213 MCDM (dpeaa)DE-He213 AHP (dpeaa)DE-He213 Rice-fallow (dpeaa)DE-He213 Nayak, Dikshya aut Sahoo, Bharat Chandra aut Raul, Sanjay Kumar (orcid)0000-0002-2389-5893 aut Panigrahi, Balram aut Choudhary, Karun Kumar aut Enthalten in Environmental earth sciences Berlin : Springer, 2009 81(2022), 15 vom: 28. Juli (DE-627)599673451 (DE-600)2493699-6 1866-6299 nnns volume:81 year:2022 number:15 day:28 month:07 https://dx.doi.org/10.1007/s12665-022-10517-3 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_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_2119 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_2360 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 81 2022 15 28 07 |
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10.1007/s12665-022-10517-3 doi (DE-627)SPR047708085 (SPR)s12665-022-10517-3-e DE-627 ger DE-627 rakwb eng Das, Dwarika Mohan verfasserin aut Identification of potential groundwater zones in rice-fallow areas within the Mahanadi river basin, India, using GIS and the analytical hierarchy process 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2022 Abstract To feed the ever-growing population of India, it is essential to bring rice-fallow areas under cultivation, which is mostly restricted owing to surface water scarcity. Groundwater can be a viable alternative to meet the demand which needs to be explored using a suitable mechanism. The present study was undertaken to delineate groundwater potential zones in the rice-fallow areas of Kantamal catchment located in the middle reach of Mahanadi basin (India). These areas can be viable for growing a second crop during the rabi season provided assured irrigation water is available. Groundwater potential zoning is considered as a pre-requisite for groundwater exploration and sustainable well yield. Remote sensing and geographical information system using the analytical hierarchy process (AHP) were used for demarcating groundwater potential zones in the entire catchment as well as in the rice-fallow areas. Thematic layers of lithology, seasonal groundwater storage, lineament density, geomorphology, soil texture, slope, land use/land cover and drainage density were prepared and applied for groundwater potential zoning. The catchment was categorized into very good, good, moderate and poor groundwater potential zones that occupy 23, 24, 42 and 11% area of the catchment, respectively. Rice-fallow area masking over the groundwater potential map reveals that very good, good, moderate and poor groundwater zones are prevalent in 35, 31, 31 and 3% of the total rice-fallow area, respectively. This implies that around 66% of the rice-fallow area in the catchment has a very good to good groundwater potential, which can be judiciously irrigated with groundwater for growing low water requiring rabi crops. Groundwater potential (dpeaa)DE-He213 Remote sensing (dpeaa)DE-He213 GIS (dpeaa)DE-He213 MCDM (dpeaa)DE-He213 AHP (dpeaa)DE-He213 Rice-fallow (dpeaa)DE-He213 Nayak, Dikshya aut Sahoo, Bharat Chandra aut Raul, Sanjay Kumar (orcid)0000-0002-2389-5893 aut Panigrahi, Balram aut Choudhary, Karun Kumar aut Enthalten in Environmental earth sciences Berlin : Springer, 2009 81(2022), 15 vom: 28. Juli (DE-627)599673451 (DE-600)2493699-6 1866-6299 nnns volume:81 year:2022 number:15 day:28 month:07 https://dx.doi.org/10.1007/s12665-022-10517-3 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_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_2119 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_2360 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 81 2022 15 28 07 |
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10.1007/s12665-022-10517-3 doi (DE-627)SPR047708085 (SPR)s12665-022-10517-3-e DE-627 ger DE-627 rakwb eng Das, Dwarika Mohan verfasserin aut Identification of potential groundwater zones in rice-fallow areas within the Mahanadi river basin, India, using GIS and the analytical hierarchy process 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2022 Abstract To feed the ever-growing population of India, it is essential to bring rice-fallow areas under cultivation, which is mostly restricted owing to surface water scarcity. Groundwater can be a viable alternative to meet the demand which needs to be explored using a suitable mechanism. The present study was undertaken to delineate groundwater potential zones in the rice-fallow areas of Kantamal catchment located in the middle reach of Mahanadi basin (India). These areas can be viable for growing a second crop during the rabi season provided assured irrigation water is available. Groundwater potential zoning is considered as a pre-requisite for groundwater exploration and sustainable well yield. Remote sensing and geographical information system using the analytical hierarchy process (AHP) were used for demarcating groundwater potential zones in the entire catchment as well as in the rice-fallow areas. Thematic layers of lithology, seasonal groundwater storage, lineament density, geomorphology, soil texture, slope, land use/land cover and drainage density were prepared and applied for groundwater potential zoning. The catchment was categorized into very good, good, moderate and poor groundwater potential zones that occupy 23, 24, 42 and 11% area of the catchment, respectively. Rice-fallow area masking over the groundwater potential map reveals that very good, good, moderate and poor groundwater zones are prevalent in 35, 31, 31 and 3% of the total rice-fallow area, respectively. This implies that around 66% of the rice-fallow area in the catchment has a very good to good groundwater potential, which can be judiciously irrigated with groundwater for growing low water requiring rabi crops. Groundwater potential (dpeaa)DE-He213 Remote sensing (dpeaa)DE-He213 GIS (dpeaa)DE-He213 MCDM (dpeaa)DE-He213 AHP (dpeaa)DE-He213 Rice-fallow (dpeaa)DE-He213 Nayak, Dikshya aut Sahoo, Bharat Chandra aut Raul, Sanjay Kumar (orcid)0000-0002-2389-5893 aut Panigrahi, Balram aut Choudhary, Karun Kumar aut Enthalten in Environmental earth sciences Berlin : Springer, 2009 81(2022), 15 vom: 28. Juli (DE-627)599673451 (DE-600)2493699-6 1866-6299 nnns volume:81 year:2022 number:15 day:28 month:07 https://dx.doi.org/10.1007/s12665-022-10517-3 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_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_2119 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_2360 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 81 2022 15 28 07 |
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Groundwater can be a viable alternative to meet the demand which needs to be explored using a suitable mechanism. The present study was undertaken to delineate groundwater potential zones in the rice-fallow areas of Kantamal catchment located in the middle reach of Mahanadi basin (India). These areas can be viable for growing a second crop during the rabi season provided assured irrigation water is available. Groundwater potential zoning is considered as a pre-requisite for groundwater exploration and sustainable well yield. Remote sensing and geographical information system using the analytical hierarchy process (AHP) were used for demarcating groundwater potential zones in the entire catchment as well as in the rice-fallow areas. Thematic layers of lithology, seasonal groundwater storage, lineament density, geomorphology, soil texture, slope, land use/land cover and drainage density were prepared and applied for groundwater potential zoning. The catchment was categorized into very good, good, moderate and poor groundwater potential zones that occupy 23, 24, 42 and 11% area of the catchment, respectively. Rice-fallow area masking over the groundwater potential map reveals that very good, good, moderate and poor groundwater zones are prevalent in 35, 31, 31 and 3% of the total rice-fallow area, respectively. 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|
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Das, Dwarika Mohan |
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Das, Dwarika Mohan misc Groundwater potential misc Remote sensing misc GIS misc MCDM misc AHP misc Rice-fallow Identification of potential groundwater zones in rice-fallow areas within the Mahanadi river basin, India, using GIS and the analytical hierarchy process |
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Identification of potential groundwater zones in rice-fallow areas within the Mahanadi river basin, India, using GIS and the analytical hierarchy process Groundwater potential (dpeaa)DE-He213 Remote sensing (dpeaa)DE-He213 GIS (dpeaa)DE-He213 MCDM (dpeaa)DE-He213 AHP (dpeaa)DE-He213 Rice-fallow (dpeaa)DE-He213 |
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misc Groundwater potential misc Remote sensing misc GIS misc MCDM misc AHP misc Rice-fallow |
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misc Groundwater potential misc Remote sensing misc GIS misc MCDM misc AHP misc Rice-fallow |
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Identification of potential groundwater zones in rice-fallow areas within the Mahanadi river basin, India, using GIS and the analytical hierarchy process |
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Identification of potential groundwater zones in rice-fallow areas within the Mahanadi river basin, India, using GIS and the analytical hierarchy process |
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Das, Dwarika Mohan Nayak, Dikshya Sahoo, Bharat Chandra Raul, Sanjay Kumar Panigrahi, Balram Choudhary, Karun Kumar |
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identification of potential groundwater zones in rice-fallow areas within the mahanadi river basin, india, using gis and the analytical hierarchy process |
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Identification of potential groundwater zones in rice-fallow areas within the Mahanadi river basin, India, using GIS and the analytical hierarchy process |
| abstract |
Abstract To feed the ever-growing population of India, it is essential to bring rice-fallow areas under cultivation, which is mostly restricted owing to surface water scarcity. Groundwater can be a viable alternative to meet the demand which needs to be explored using a suitable mechanism. The present study was undertaken to delineate groundwater potential zones in the rice-fallow areas of Kantamal catchment located in the middle reach of Mahanadi basin (India). These areas can be viable for growing a second crop during the rabi season provided assured irrigation water is available. Groundwater potential zoning is considered as a pre-requisite for groundwater exploration and sustainable well yield. Remote sensing and geographical information system using the analytical hierarchy process (AHP) were used for demarcating groundwater potential zones in the entire catchment as well as in the rice-fallow areas. Thematic layers of lithology, seasonal groundwater storage, lineament density, geomorphology, soil texture, slope, land use/land cover and drainage density were prepared and applied for groundwater potential zoning. The catchment was categorized into very good, good, moderate and poor groundwater potential zones that occupy 23, 24, 42 and 11% area of the catchment, respectively. Rice-fallow area masking over the groundwater potential map reveals that very good, good, moderate and poor groundwater zones are prevalent in 35, 31, 31 and 3% of the total rice-fallow area, respectively. This implies that around 66% of the rice-fallow area in the catchment has a very good to good groundwater potential, which can be judiciously irrigated with groundwater for growing low water requiring rabi crops. © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2022 |
| abstractGer |
Abstract To feed the ever-growing population of India, it is essential to bring rice-fallow areas under cultivation, which is mostly restricted owing to surface water scarcity. Groundwater can be a viable alternative to meet the demand which needs to be explored using a suitable mechanism. The present study was undertaken to delineate groundwater potential zones in the rice-fallow areas of Kantamal catchment located in the middle reach of Mahanadi basin (India). These areas can be viable for growing a second crop during the rabi season provided assured irrigation water is available. Groundwater potential zoning is considered as a pre-requisite for groundwater exploration and sustainable well yield. Remote sensing and geographical information system using the analytical hierarchy process (AHP) were used for demarcating groundwater potential zones in the entire catchment as well as in the rice-fallow areas. Thematic layers of lithology, seasonal groundwater storage, lineament density, geomorphology, soil texture, slope, land use/land cover and drainage density were prepared and applied for groundwater potential zoning. The catchment was categorized into very good, good, moderate and poor groundwater potential zones that occupy 23, 24, 42 and 11% area of the catchment, respectively. Rice-fallow area masking over the groundwater potential map reveals that very good, good, moderate and poor groundwater zones are prevalent in 35, 31, 31 and 3% of the total rice-fallow area, respectively. This implies that around 66% of the rice-fallow area in the catchment has a very good to good groundwater potential, which can be judiciously irrigated with groundwater for growing low water requiring rabi crops. © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2022 |
| abstract_unstemmed |
Abstract To feed the ever-growing population of India, it is essential to bring rice-fallow areas under cultivation, which is mostly restricted owing to surface water scarcity. Groundwater can be a viable alternative to meet the demand which needs to be explored using a suitable mechanism. The present study was undertaken to delineate groundwater potential zones in the rice-fallow areas of Kantamal catchment located in the middle reach of Mahanadi basin (India). These areas can be viable for growing a second crop during the rabi season provided assured irrigation water is available. Groundwater potential zoning is considered as a pre-requisite for groundwater exploration and sustainable well yield. Remote sensing and geographical information system using the analytical hierarchy process (AHP) were used for demarcating groundwater potential zones in the entire catchment as well as in the rice-fallow areas. Thematic layers of lithology, seasonal groundwater storage, lineament density, geomorphology, soil texture, slope, land use/land cover and drainage density were prepared and applied for groundwater potential zoning. The catchment was categorized into very good, good, moderate and poor groundwater potential zones that occupy 23, 24, 42 and 11% area of the catchment, respectively. Rice-fallow area masking over the groundwater potential map reveals that very good, good, moderate and poor groundwater zones are prevalent in 35, 31, 31 and 3% of the total rice-fallow area, respectively. This implies that around 66% of the rice-fallow area in the catchment has a very good to good groundwater potential, which can be judiciously irrigated with groundwater for growing low water requiring rabi crops. © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2022 |
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Identification of potential groundwater zones in rice-fallow areas within the Mahanadi river basin, India, using GIS and the analytical hierarchy process |
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Nayak, Dikshya Sahoo, Bharat Chandra Raul, Sanjay Kumar Panigrahi, Balram Choudhary, Karun Kumar |
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|
| score |
7.4001007 |