Groundwater quality evaluation by electrical resistivity method for optimized tubewell site selection in an ago-stressed Thal Doab Aquifer in Pakistan

Abstract Rapid and unchecked growths of private tubewells in poor water quality zones of Punjab province, Pakistan are the major sources of environmental degradation through the deployment of agricultural stresses on the underlying aquifer. There are broadly two environmental menaces associated with...
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Autor*in:	Hussain, Yawar [verfasserIn] Ullah, Sadia Fida Akhter, Gulraiz Aslam, Abdul Qayyum

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2017

Schlagwörter:	Groundwater quality Argo-stressed aquifer TWS Tehsil Kot Adhu

Anmerkung:	© Springer International Publishing Switzerland 2017

Übergeordnetes Werk:	Enthalten in: Modeling earth systems and environment - Berlin : Springer, 2015, 3(2017), 1 vom: 17. Feb.
Übergeordnetes Werk:	volume:3 ; year:2017 ; number:1 ; day:17 ; month:02

Links:	Volltext

DOI / URN:	10.1007/s40808-017-0282-3

Katalog-ID:	SPR037839365

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100	1		\|a Hussain, Yawar \|e verfasserin \|0 (orcid)0000-0002-4155-6764 \|4 aut
245	1	0	\|a Groundwater quality evaluation by electrical resistivity method for optimized tubewell site selection in an ago-stressed Thal Doab Aquifer in Pakistan
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520			\|a Abstract Rapid and unchecked growths of private tubewells in poor water quality zones of Punjab province, Pakistan are the major sources of environmental degradation through the deployment of agricultural stresses on the underlying aquifer. There are broadly two environmental menaces associated with these agricultural stresses, increase of non-point source pollution loads at the surface and instigation of problem of secondary salinity (SS). The present study is applied vertical electrical soundings with Schlumberger electrode configuration having maximum current electrodes separation 300 m to assess the potential of freshwater layer lying over the saline groundwater. Primarily, the collected earth’s resistivities were converted to groundwater quality using groundwater electrical conductivity (EC) from exploratory wells drilled at regular interval in the entire Thal Doab. Secondly, based on these EC values, the study area is divided into three different tubewell suitability classes as high, moderate and low with interpreted EC values as less than 1.5 dS/m, between 1.5 and 2.5 dS/m and greater than 2.5 dS/m, respectively. The spatial distribution maps of these suitability classes are done at six depth zones (0–50, 50–100, 100–150, 150–200, 200–250, 250–300 m). Results indicate that there is an inverse relationship between the surface water recharge and SS which should be used for both tubewell depth as well as site optimization and a check on their future growth rates. In this way the eco-friendly agricultural growth rates can be established in Tehsil Kot Adhu, Thal Doab, Pakistan and the other areas having similar hydrogeological conditions.
650		4	\|a Groundwater quality \|7 (dpeaa)DE-He213
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650		4	\|a Tehsil Kot Adhu \|7 (dpeaa)DE-He213
700	1		\|a Ullah, Sadia Fida \|4 aut
700	1		\|a Akhter, Gulraiz \|4 aut
700	1		\|a Aslam, Abdul Qayyum \|4 aut
773	0	8	\|i Enthalten in \|t Modeling earth systems and environment \|d Berlin : Springer, 2015 \|g 3(2017), 1 vom: 17. Feb. \|w (DE-627)825736587 \|w (DE-600)2821317-8 \|x 2363-6211 \|7 nnns
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912			\|a GBV_ILN_24
912			\|a GBV_ILN_31
912			\|a GBV_ILN_32
912			\|a GBV_ILN_39
912			\|a GBV_ILN_40
912			\|a GBV_ILN_60
912			\|a GBV_ILN_62
912			\|a GBV_ILN_63
912			\|a GBV_ILN_65
912			\|a GBV_ILN_69
912			\|a GBV_ILN_70
912			\|a GBV_ILN_73
912			\|a GBV_ILN_74
912			\|a GBV_ILN_90
912			\|a GBV_ILN_95
912			\|a GBV_ILN_100
912			\|a GBV_ILN_105
912			\|a GBV_ILN_110
912			\|a GBV_ILN_120
912			\|a GBV_ILN_138
912			\|a GBV_ILN_150
912			\|a GBV_ILN_151
912			\|a GBV_ILN_161
912			\|a GBV_ILN_170
912			\|a GBV_ILN_171
912			\|a GBV_ILN_187
912			\|a GBV_ILN_213
912			\|a GBV_ILN_224
912			\|a GBV_ILN_230
912			\|a GBV_ILN_250
912			\|a GBV_ILN_281
912			\|a GBV_ILN_285
912			\|a GBV_ILN_293
912			\|a GBV_ILN_370
912			\|a GBV_ILN_602
912			\|a GBV_ILN_636
912			\|a GBV_ILN_702
912			\|a GBV_ILN_2001
912			\|a GBV_ILN_2003
912			\|a GBV_ILN_2004
912			\|a GBV_ILN_2005
912			\|a GBV_ILN_2006
912			\|a GBV_ILN_2007
912			\|a GBV_ILN_2008
912			\|a GBV_ILN_2009
912			\|a GBV_ILN_2010
912			\|a GBV_ILN_2011
912			\|a GBV_ILN_2014
912			\|a GBV_ILN_2015
912			\|a GBV_ILN_2020
912			\|a GBV_ILN_2021
912			\|a GBV_ILN_2025
912			\|a GBV_ILN_2026
912			\|a GBV_ILN_2027
912			\|a GBV_ILN_2031
912			\|a GBV_ILN_2034
912			\|a GBV_ILN_2037
912			\|a GBV_ILN_2038
912			\|a GBV_ILN_2039
912			\|a GBV_ILN_2044
912			\|a GBV_ILN_2048
912			\|a GBV_ILN_2049
912			\|a GBV_ILN_2050
912			\|a GBV_ILN_2055
912			\|a GBV_ILN_2057
912			\|a GBV_ILN_2059
912			\|a GBV_ILN_2061
912			\|a GBV_ILN_2064
912			\|a GBV_ILN_2065
912			\|a GBV_ILN_2068
912			\|a GBV_ILN_2070
912			\|a GBV_ILN_2086
912			\|a GBV_ILN_2088
912			\|a GBV_ILN_2093
912			\|a GBV_ILN_2106
912			\|a GBV_ILN_2107
912			\|a GBV_ILN_2108
912			\|a GBV_ILN_2110
912			\|a GBV_ILN_2111
912			\|a GBV_ILN_2112
912			\|a GBV_ILN_2113
912			\|a GBV_ILN_2116
912			\|a GBV_ILN_2118
912			\|a GBV_ILN_2119
912			\|a GBV_ILN_2122
912			\|a GBV_ILN_2129
912			\|a GBV_ILN_2143
912			\|a GBV_ILN_2144
912			\|a GBV_ILN_2147
912			\|a GBV_ILN_2148
912			\|a GBV_ILN_2152
912			\|a GBV_ILN_2153
912			\|a GBV_ILN_2188
912			\|a GBV_ILN_2190
912			\|a GBV_ILN_2232
912			\|a GBV_ILN_2336
912			\|a GBV_ILN_2446
912			\|a GBV_ILN_2470
912			\|a GBV_ILN_2472
912			\|a GBV_ILN_2507
912			\|a GBV_ILN_2522
912			\|a GBV_ILN_2548
912			\|a GBV_ILN_4035
912			\|a GBV_ILN_4037
912			\|a GBV_ILN_4046
912			\|a GBV_ILN_4112
912			\|a GBV_ILN_4125
912			\|a GBV_ILN_4242
912			\|a GBV_ILN_4246
912			\|a GBV_ILN_4249
912			\|a GBV_ILN_4251
912			\|a GBV_ILN_4305
912			\|a GBV_ILN_4306
912			\|a GBV_ILN_4307
912			\|a GBV_ILN_4313
912			\|a GBV_ILN_4322
912			\|a GBV_ILN_4323
912			\|a GBV_ILN_4324
912			\|a GBV_ILN_4325
912			\|a GBV_ILN_4326
912			\|a GBV_ILN_4333
912			\|a GBV_ILN_4334
912			\|a GBV_ILN_4335
912			\|a GBV_ILN_4336
912			\|a GBV_ILN_4338
912			\|a GBV_ILN_4393
912			\|a GBV_ILN_4700
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author_variant	y h yh s f u sf sfu g a ga a q a aq aqa
matchkey_str	article:23636211:2017----::rudaeqaiyvlainylcrcleitvtmtofrpiietbwlstslcinnng
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publishDate	2017
allfields	10.1007/s40808-017-0282-3 doi (DE-627)SPR037839365 (SPR)s40808-017-0282-3-e DE-627 ger DE-627 rakwb eng Hussain, Yawar verfasserin (orcid)0000-0002-4155-6764 aut Groundwater quality evaluation by electrical resistivity method for optimized tubewell site selection in an ago-stressed Thal Doab Aquifer in Pakistan 2017 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer International Publishing Switzerland 2017 Abstract Rapid and unchecked growths of private tubewells in poor water quality zones of Punjab province, Pakistan are the major sources of environmental degradation through the deployment of agricultural stresses on the underlying aquifer. There are broadly two environmental menaces associated with these agricultural stresses, increase of non-point source pollution loads at the surface and instigation of problem of secondary salinity (SS). The present study is applied vertical electrical soundings with Schlumberger electrode configuration having maximum current electrodes separation 300 m to assess the potential of freshwater layer lying over the saline groundwater. Primarily, the collected earth’s resistivities were converted to groundwater quality using groundwater electrical conductivity (EC) from exploratory wells drilled at regular interval in the entire Thal Doab. Secondly, based on these EC values, the study area is divided into three different tubewell suitability classes as high, moderate and low with interpreted EC values as less than 1.5 dS/m, between 1.5 and 2.5 dS/m and greater than 2.5 dS/m, respectively. The spatial distribution maps of these suitability classes are done at six depth zones (0–50, 50–100, 100–150, 150–200, 200–250, 250–300 m). Results indicate that there is an inverse relationship between the surface water recharge and SS which should be used for both tubewell depth as well as site optimization and a check on their future growth rates. In this way the eco-friendly agricultural growth rates can be established in Tehsil Kot Adhu, Thal Doab, Pakistan and the other areas having similar hydrogeological conditions. Groundwater quality (dpeaa)DE-He213 Argo-stressed aquifer (dpeaa)DE-He213 TWS (dpeaa)DE-He213 Tehsil Kot Adhu (dpeaa)DE-He213 Ullah, Sadia Fida aut Akhter, Gulraiz aut Aslam, Abdul Qayyum aut Enthalten in Modeling earth systems and environment Berlin : Springer, 2015 3(2017), 1 vom: 17. Feb. (DE-627)825736587 (DE-600)2821317-8 2363-6211 nnns volume:3 year:2017 number:1 day:17 month:02 https://dx.doi.org/10.1007/s40808-017-0282-3 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_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_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 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_2116 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_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_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_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 3 2017 1 17 02
spelling	10.1007/s40808-017-0282-3 doi (DE-627)SPR037839365 (SPR)s40808-017-0282-3-e DE-627 ger DE-627 rakwb eng Hussain, Yawar verfasserin (orcid)0000-0002-4155-6764 aut Groundwater quality evaluation by electrical resistivity method for optimized tubewell site selection in an ago-stressed Thal Doab Aquifer in Pakistan 2017 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer International Publishing Switzerland 2017 Abstract Rapid and unchecked growths of private tubewells in poor water quality zones of Punjab province, Pakistan are the major sources of environmental degradation through the deployment of agricultural stresses on the underlying aquifer. There are broadly two environmental menaces associated with these agricultural stresses, increase of non-point source pollution loads at the surface and instigation of problem of secondary salinity (SS). The present study is applied vertical electrical soundings with Schlumberger electrode configuration having maximum current electrodes separation 300 m to assess the potential of freshwater layer lying over the saline groundwater. Primarily, the collected earth’s resistivities were converted to groundwater quality using groundwater electrical conductivity (EC) from exploratory wells drilled at regular interval in the entire Thal Doab. Secondly, based on these EC values, the study area is divided into three different tubewell suitability classes as high, moderate and low with interpreted EC values as less than 1.5 dS/m, between 1.5 and 2.5 dS/m and greater than 2.5 dS/m, respectively. The spatial distribution maps of these suitability classes are done at six depth zones (0–50, 50–100, 100–150, 150–200, 200–250, 250–300 m). Results indicate that there is an inverse relationship between the surface water recharge and SS which should be used for both tubewell depth as well as site optimization and a check on their future growth rates. In this way the eco-friendly agricultural growth rates can be established in Tehsil Kot Adhu, Thal Doab, Pakistan and the other areas having similar hydrogeological conditions. Groundwater quality (dpeaa)DE-He213 Argo-stressed aquifer (dpeaa)DE-He213 TWS (dpeaa)DE-He213 Tehsil Kot Adhu (dpeaa)DE-He213 Ullah, Sadia Fida aut Akhter, Gulraiz aut Aslam, Abdul Qayyum aut Enthalten in Modeling earth systems and environment Berlin : Springer, 2015 3(2017), 1 vom: 17. Feb. (DE-627)825736587 (DE-600)2821317-8 2363-6211 nnns volume:3 year:2017 number:1 day:17 month:02 https://dx.doi.org/10.1007/s40808-017-0282-3 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_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_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 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_2116 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_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_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_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 3 2017 1 17 02
allfields_unstemmed	10.1007/s40808-017-0282-3 doi (DE-627)SPR037839365 (SPR)s40808-017-0282-3-e DE-627 ger DE-627 rakwb eng Hussain, Yawar verfasserin (orcid)0000-0002-4155-6764 aut Groundwater quality evaluation by electrical resistivity method for optimized tubewell site selection in an ago-stressed Thal Doab Aquifer in Pakistan 2017 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer International Publishing Switzerland 2017 Abstract Rapid and unchecked growths of private tubewells in poor water quality zones of Punjab province, Pakistan are the major sources of environmental degradation through the deployment of agricultural stresses on the underlying aquifer. There are broadly two environmental menaces associated with these agricultural stresses, increase of non-point source pollution loads at the surface and instigation of problem of secondary salinity (SS). The present study is applied vertical electrical soundings with Schlumberger electrode configuration having maximum current electrodes separation 300 m to assess the potential of freshwater layer lying over the saline groundwater. Primarily, the collected earth’s resistivities were converted to groundwater quality using groundwater electrical conductivity (EC) from exploratory wells drilled at regular interval in the entire Thal Doab. Secondly, based on these EC values, the study area is divided into three different tubewell suitability classes as high, moderate and low with interpreted EC values as less than 1.5 dS/m, between 1.5 and 2.5 dS/m and greater than 2.5 dS/m, respectively. The spatial distribution maps of these suitability classes are done at six depth zones (0–50, 50–100, 100–150, 150–200, 200–250, 250–300 m). Results indicate that there is an inverse relationship between the surface water recharge and SS which should be used for both tubewell depth as well as site optimization and a check on their future growth rates. In this way the eco-friendly agricultural growth rates can be established in Tehsil Kot Adhu, Thal Doab, Pakistan and the other areas having similar hydrogeological conditions. Groundwater quality (dpeaa)DE-He213 Argo-stressed aquifer (dpeaa)DE-He213 TWS (dpeaa)DE-He213 Tehsil Kot Adhu (dpeaa)DE-He213 Ullah, Sadia Fida aut Akhter, Gulraiz aut Aslam, Abdul Qayyum aut Enthalten in Modeling earth systems and environment Berlin : Springer, 2015 3(2017), 1 vom: 17. Feb. (DE-627)825736587 (DE-600)2821317-8 2363-6211 nnns volume:3 year:2017 number:1 day:17 month:02 https://dx.doi.org/10.1007/s40808-017-0282-3 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_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_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 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_2116 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_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_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_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 3 2017 1 17 02
allfieldsGer	10.1007/s40808-017-0282-3 doi (DE-627)SPR037839365 (SPR)s40808-017-0282-3-e DE-627 ger DE-627 rakwb eng Hussain, Yawar verfasserin (orcid)0000-0002-4155-6764 aut Groundwater quality evaluation by electrical resistivity method for optimized tubewell site selection in an ago-stressed Thal Doab Aquifer in Pakistan 2017 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer International Publishing Switzerland 2017 Abstract Rapid and unchecked growths of private tubewells in poor water quality zones of Punjab province, Pakistan are the major sources of environmental degradation through the deployment of agricultural stresses on the underlying aquifer. There are broadly two environmental menaces associated with these agricultural stresses, increase of non-point source pollution loads at the surface and instigation of problem of secondary salinity (SS). The present study is applied vertical electrical soundings with Schlumberger electrode configuration having maximum current electrodes separation 300 m to assess the potential of freshwater layer lying over the saline groundwater. Primarily, the collected earth’s resistivities were converted to groundwater quality using groundwater electrical conductivity (EC) from exploratory wells drilled at regular interval in the entire Thal Doab. Secondly, based on these EC values, the study area is divided into three different tubewell suitability classes as high, moderate and low with interpreted EC values as less than 1.5 dS/m, between 1.5 and 2.5 dS/m and greater than 2.5 dS/m, respectively. The spatial distribution maps of these suitability classes are done at six depth zones (0–50, 50–100, 100–150, 150–200, 200–250, 250–300 m). Results indicate that there is an inverse relationship between the surface water recharge and SS which should be used for both tubewell depth as well as site optimization and a check on their future growth rates. In this way the eco-friendly agricultural growth rates can be established in Tehsil Kot Adhu, Thal Doab, Pakistan and the other areas having similar hydrogeological conditions. Groundwater quality (dpeaa)DE-He213 Argo-stressed aquifer (dpeaa)DE-He213 TWS (dpeaa)DE-He213 Tehsil Kot Adhu (dpeaa)DE-He213 Ullah, Sadia Fida aut Akhter, Gulraiz aut Aslam, Abdul Qayyum aut Enthalten in Modeling earth systems and environment Berlin : Springer, 2015 3(2017), 1 vom: 17. Feb. (DE-627)825736587 (DE-600)2821317-8 2363-6211 nnns volume:3 year:2017 number:1 day:17 month:02 https://dx.doi.org/10.1007/s40808-017-0282-3 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_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_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 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_2116 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_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_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_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 3 2017 1 17 02
allfieldsSound	10.1007/s40808-017-0282-3 doi (DE-627)SPR037839365 (SPR)s40808-017-0282-3-e DE-627 ger DE-627 rakwb eng Hussain, Yawar verfasserin (orcid)0000-0002-4155-6764 aut Groundwater quality evaluation by electrical resistivity method for optimized tubewell site selection in an ago-stressed Thal Doab Aquifer in Pakistan 2017 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer International Publishing Switzerland 2017 Abstract Rapid and unchecked growths of private tubewells in poor water quality zones of Punjab province, Pakistan are the major sources of environmental degradation through the deployment of agricultural stresses on the underlying aquifer. There are broadly two environmental menaces associated with these agricultural stresses, increase of non-point source pollution loads at the surface and instigation of problem of secondary salinity (SS). The present study is applied vertical electrical soundings with Schlumberger electrode configuration having maximum current electrodes separation 300 m to assess the potential of freshwater layer lying over the saline groundwater. Primarily, the collected earth’s resistivities were converted to groundwater quality using groundwater electrical conductivity (EC) from exploratory wells drilled at regular interval in the entire Thal Doab. Secondly, based on these EC values, the study area is divided into three different tubewell suitability classes as high, moderate and low with interpreted EC values as less than 1.5 dS/m, between 1.5 and 2.5 dS/m and greater than 2.5 dS/m, respectively. The spatial distribution maps of these suitability classes are done at six depth zones (0–50, 50–100, 100–150, 150–200, 200–250, 250–300 m). Results indicate that there is an inverse relationship between the surface water recharge and SS which should be used for both tubewell depth as well as site optimization and a check on their future growth rates. In this way the eco-friendly agricultural growth rates can be established in Tehsil Kot Adhu, Thal Doab, Pakistan and the other areas having similar hydrogeological conditions. Groundwater quality (dpeaa)DE-He213 Argo-stressed aquifer (dpeaa)DE-He213 TWS (dpeaa)DE-He213 Tehsil Kot Adhu (dpeaa)DE-He213 Ullah, Sadia Fida aut Akhter, Gulraiz aut Aslam, Abdul Qayyum aut Enthalten in Modeling earth systems and environment Berlin : Springer, 2015 3(2017), 1 vom: 17. Feb. (DE-627)825736587 (DE-600)2821317-8 2363-6211 nnns volume:3 year:2017 number:1 day:17 month:02 https://dx.doi.org/10.1007/s40808-017-0282-3 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_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_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 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_2116 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_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_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_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 3 2017 1 17 02
language	English
source	Enthalten in Modeling earth systems and environment 3(2017), 1 vom: 17. Feb. volume:3 year:2017 number:1 day:17 month:02
sourceStr	Enthalten in Modeling earth systems and environment 3(2017), 1 vom: 17. Feb. volume:3 year:2017 number:1 day:17 month:02
format_phy_str_mv	Article
institution	findex.gbv.de
topic_facet	Groundwater quality Argo-stressed aquifer TWS Tehsil Kot Adhu
isfreeaccess_bool	false
container_title	Modeling earth systems and environment
authorswithroles_txt_mv	Hussain, Yawar @@aut@@ Ullah, Sadia Fida @@aut@@ Akhter, Gulraiz @@aut@@ Aslam, Abdul Qayyum @@aut@@
publishDateDaySort_date	2017-02-17T00:00:00Z
hierarchy_top_id	825736587
id	SPR037839365
language_de	englisch
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author	Hussain, Yawar
spellingShingle	Hussain, Yawar misc Groundwater quality misc Argo-stressed aquifer misc TWS misc Tehsil Kot Adhu Groundwater quality evaluation by electrical resistivity method for optimized tubewell site selection in an ago-stressed Thal Doab Aquifer in Pakistan
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topic_title	Groundwater quality evaluation by electrical resistivity method for optimized tubewell site selection in an ago-stressed Thal Doab Aquifer in Pakistan Groundwater quality (dpeaa)DE-He213 Argo-stressed aquifer (dpeaa)DE-He213 TWS (dpeaa)DE-He213 Tehsil Kot Adhu (dpeaa)DE-He213
topic	misc Groundwater quality misc Argo-stressed aquifer misc TWS misc Tehsil Kot Adhu
topic_unstemmed	misc Groundwater quality misc Argo-stressed aquifer misc TWS misc Tehsil Kot Adhu
topic_browse	misc Groundwater quality misc Argo-stressed aquifer misc TWS misc Tehsil Kot Adhu
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title	Groundwater quality evaluation by electrical resistivity method for optimized tubewell site selection in an ago-stressed Thal Doab Aquifer in Pakistan
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title_full	Groundwater quality evaluation by electrical resistivity method for optimized tubewell site selection in an ago-stressed Thal Doab Aquifer in Pakistan
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author_browse	Hussain, Yawar Ullah, Sadia Fida Akhter, Gulraiz Aslam, Abdul Qayyum
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title_sort	groundwater quality evaluation by electrical resistivity method for optimized tubewell site selection in an ago-stressed thal doab aquifer in pakistan
title_auth	Groundwater quality evaluation by electrical resistivity method for optimized tubewell site selection in an ago-stressed Thal Doab Aquifer in Pakistan
abstract	Abstract Rapid and unchecked growths of private tubewells in poor water quality zones of Punjab province, Pakistan are the major sources of environmental degradation through the deployment of agricultural stresses on the underlying aquifer. There are broadly two environmental menaces associated with these agricultural stresses, increase of non-point source pollution loads at the surface and instigation of problem of secondary salinity (SS). The present study is applied vertical electrical soundings with Schlumberger electrode configuration having maximum current electrodes separation 300 m to assess the potential of freshwater layer lying over the saline groundwater. Primarily, the collected earth’s resistivities were converted to groundwater quality using groundwater electrical conductivity (EC) from exploratory wells drilled at regular interval in the entire Thal Doab. Secondly, based on these EC values, the study area is divided into three different tubewell suitability classes as high, moderate and low with interpreted EC values as less than 1.5 dS/m, between 1.5 and 2.5 dS/m and greater than 2.5 dS/m, respectively. The spatial distribution maps of these suitability classes are done at six depth zones (0–50, 50–100, 100–150, 150–200, 200–250, 250–300 m). Results indicate that there is an inverse relationship between the surface water recharge and SS which should be used for both tubewell depth as well as site optimization and a check on their future growth rates. In this way the eco-friendly agricultural growth rates can be established in Tehsil Kot Adhu, Thal Doab, Pakistan and the other areas having similar hydrogeological conditions. © Springer International Publishing Switzerland 2017
abstractGer	Abstract Rapid and unchecked growths of private tubewells in poor water quality zones of Punjab province, Pakistan are the major sources of environmental degradation through the deployment of agricultural stresses on the underlying aquifer. There are broadly two environmental menaces associated with these agricultural stresses, increase of non-point source pollution loads at the surface and instigation of problem of secondary salinity (SS). The present study is applied vertical electrical soundings with Schlumberger electrode configuration having maximum current electrodes separation 300 m to assess the potential of freshwater layer lying over the saline groundwater. Primarily, the collected earth’s resistivities were converted to groundwater quality using groundwater electrical conductivity (EC) from exploratory wells drilled at regular interval in the entire Thal Doab. Secondly, based on these EC values, the study area is divided into three different tubewell suitability classes as high, moderate and low with interpreted EC values as less than 1.5 dS/m, between 1.5 and 2.5 dS/m and greater than 2.5 dS/m, respectively. The spatial distribution maps of these suitability classes are done at six depth zones (0–50, 50–100, 100–150, 150–200, 200–250, 250–300 m). Results indicate that there is an inverse relationship between the surface water recharge and SS which should be used for both tubewell depth as well as site optimization and a check on their future growth rates. In this way the eco-friendly agricultural growth rates can be established in Tehsil Kot Adhu, Thal Doab, Pakistan and the other areas having similar hydrogeological conditions. © Springer International Publishing Switzerland 2017
abstract_unstemmed	Abstract Rapid and unchecked growths of private tubewells in poor water quality zones of Punjab province, Pakistan are the major sources of environmental degradation through the deployment of agricultural stresses on the underlying aquifer. There are broadly two environmental menaces associated with these agricultural stresses, increase of non-point source pollution loads at the surface and instigation of problem of secondary salinity (SS). The present study is applied vertical electrical soundings with Schlumberger electrode configuration having maximum current electrodes separation 300 m to assess the potential of freshwater layer lying over the saline groundwater. Primarily, the collected earth’s resistivities were converted to groundwater quality using groundwater electrical conductivity (EC) from exploratory wells drilled at regular interval in the entire Thal Doab. Secondly, based on these EC values, the study area is divided into three different tubewell suitability classes as high, moderate and low with interpreted EC values as less than 1.5 dS/m, between 1.5 and 2.5 dS/m and greater than 2.5 dS/m, respectively. The spatial distribution maps of these suitability classes are done at six depth zones (0–50, 50–100, 100–150, 150–200, 200–250, 250–300 m). Results indicate that there is an inverse relationship between the surface water recharge and SS which should be used for both tubewell depth as well as site optimization and a check on their future growth rates. In this way the eco-friendly agricultural growth rates can be established in Tehsil Kot Adhu, Thal Doab, Pakistan and the other areas having similar hydrogeological conditions. © Springer International Publishing Switzerland 2017
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title_short	Groundwater quality evaluation by electrical resistivity method for optimized tubewell site selection in an ago-stressed Thal Doab Aquifer in Pakistan
url	https://dx.doi.org/10.1007/s40808-017-0282-3
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author2	Ullah, Sadia Fida Akhter, Gulraiz Aslam, Abdul Qayyum
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up_date	2024-07-03T14:38:17.179Z
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fullrecord_marcxml	<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">SPR037839365</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230328210653.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">201007s2017 xx \|\|\|\|\|o 00\| \|\|eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/s40808-017-0282-3</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)SPR037839365</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(SPR)s40808-017-0282-3-e</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Hussain, Yawar</subfield><subfield code="e">verfasserin</subfield><subfield code="0">(orcid)0000-0002-4155-6764</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Groundwater quality evaluation by electrical resistivity method for optimized tubewell site selection in an ago-stressed Thal Doab Aquifer in Pakistan</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2017</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">© Springer International Publishing Switzerland 2017</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract Rapid and unchecked growths of private tubewells in poor water quality zones of Punjab province, Pakistan are the major sources of environmental degradation through the deployment of agricultural stresses on the underlying aquifer. There are broadly two environmental menaces associated with these agricultural stresses, increase of non-point source pollution loads at the surface and instigation of problem of secondary salinity (SS). The present study is applied vertical electrical soundings with Schlumberger electrode configuration having maximum current electrodes separation 300 m to assess the potential of freshwater layer lying over the saline groundwater. Primarily, the collected earth’s resistivities were converted to groundwater quality using groundwater electrical conductivity (EC) from exploratory wells drilled at regular interval in the entire Thal Doab. Secondly, based on these EC values, the study area is divided into three different tubewell suitability classes as high, moderate and low with interpreted EC values as less than 1.5 dS/m, between 1.5 and 2.5 dS/m and greater than 2.5 dS/m, respectively. The spatial distribution maps of these suitability classes are done at six depth zones (0–50, 50–100, 100–150, 150–200, 200–250, 250–300 m). Results indicate that there is an inverse relationship between the surface water recharge and SS which should be used for both tubewell depth as well as site optimization and a check on their future growth rates. 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Groundwater quality evaluation by electrical resistivity method for optimized tubewell site selection in an ago-stressed Thal Doab Aquifer in Pakistan

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