Sone megafan: a non-Himalayan megafan of craton origin, forming a potential groundwater reservoir in marginal parts of Ganga Basin, India

Sahu, S.; Saha, D.; Shukla, R. R.

Sone megafan: a non-Himalayan megafan of craton origin, forming a potential groundwater reservoir in marginal parts of Ganga Basin, India | Le méga-fan de la rivière Sone: un méga-fan non Himalayen d’origine cratonique, formant un réservoir potentiel d’eaux souterraines aux marges du bassin du Gange, Inde El gran abanico del Sone: un gran abanico no himalayo de origen cratónico, que forma un reservorio potencial de agua subterránea en las partes marginales de la cuenca del Ganges, India Sone 巨型沉积扇: 克拉通源的非喜马拉雅巨型扇, 在印度恒河流域边缘地区形成潜在的地下水水储 Megaleque alluvial de Sone: um megaleque não Himalaio de origem cratônica, formando um potencial reservatório de águas subterrâneas em partes marginais da Bacia do Ganges, Índia

2018

Sahu, S. | Saha, D. | Shukla, R. R.

The Sone River megafan in the Marginal Alluvial Plain (MAP) in the southern parts of the Ganga Basin (India) holds potential aquifer systems within a hydrogeologically poor region with limited groundwater potential. The work investigates the hydrostratigraphy and hydrogeological characteristics, including the yield potential and hydraulic parameters of the aquifer systems in the megafan, by analyzing borehole lithologs (n = 78), drill-cut sediment (n = 5), depth to water level (n = 112) and pumping test data (n = 19). The aquifer materials comprise oxidized and brownish-yellow fine to very coarse sand and gravels (mean size range 0.21–1.34 mm), constituting ~10–90% of the sedimentary column within the depth of 250 m below ground level (bgl). Two aquifer systems are delineated within the depth, marked by a middle clay layer lying at 87–139 m bgl. The phreatic aquifer within the top aquitard depicts shallow water levels, which varied between 0.6 and 12.0 m bgl. The discharge in the tube wells tapping the second aquifer system varies between ~46 and 250 m³/h. The transmissivity values were estimated up to 23,696 m²/d (generally 5,000–10,000 m²/d). The storativity values (range 2.6 × 10⁻⁹ to 5.0 × 10⁻³) indicate a confined state of groundwater in the aquifer system. The hydraulic conductivity values of 21–369 and 31–196 m/d, as estimated by a grain-size based empirical method, suggest high groundwater potential of both the first and second aquifer systems, respectively. The groundwater source availability in the megafan is supported by copious supply of source water where the palaeochannels act as conduits of recharge.

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