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Surface water and groundwater interaction in the Kosi River alluvial fan of the Himalayan Foreland

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Abstract

We report the isotopic composition of the surface water and groundwater of the Kosi River fan on the Himalayan Foreland, India. We have collected 65 water samples from surface water (Kosi River (n = 2), streams (n = 9), waterlogging (n = 29), and canal (n = 4)), and groundwater (n = 21) for δ18O and δ2H analysis during December 2019. We obtained groundwater level data measured at the observation wells from the Central Groundwater Board, India, for 1996 and 2017. The groundwater level varies from 1.0 to 8.1 m below ground level (bgl) and from 0.5 to 9.0 m bgl during 1996 and 2017, respectively. We have used water table fluctuation approach to estimate the recharge rate. The recharge rate in the Kosi Fan varies from 0.7 to 21.4 mm/year from 1996 to 2017. Further, we have used δ18O and δ2H values of water samples to identify the source and the interaction between surface water and groundwater. The δ18O value of groundwater shows a wide variation (from −9.3‰ to −5.6‰) compared to the surface water, i.e., streams (−7.8‰ to −6.4‰) and canals (−6.9‰ to −6.0‰), suggesting mixing in groundwater during recharge processes. Furthermore, we have used a two-component mixing model to assess the fraction contribution from streams and precipitation to groundwater. The estimated fraction contribution from stream water to groundwater ranges from 45 to 83%. We also suggest higher recharge is limited up to the depth of 6 m bgl. We suggest precipitation and surface water actively recharge groundwater. We conclude that marked spatial variation in the isotopic composition of groundwater is mainly due to the local recharge sources and interaction between surface water and groundwater.

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Data availability

The groundwater level data used in the present study is freely available in various reports published by the Central Groundwater Board, State Government Departments, and Ministry of Jal Sakti, India (http://cgwb.gov.in/).

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Funding

Kumar Gaurav would like to acknowledge the research grant from the Science and Engineering Research Board (SERB), Government of India, through grant no. SERB/EES/2018075. Zafar Beg Ph.D. is funded through the institutional fellowship of IISER Bhopal. Suneel Kumar Joshi and Sudhir Kumar are also thankful to the Director, National Institute of Hydrology, Roorkee, for institutional support. Suneel Kumar Joshi is also grateful to Mr. Prasad Babu, Geo Climate Risk Solution Pvt. Ltd. We acknowledge the Central Groundwater Board, India, for providing the groundwater level data.

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Authors and Affiliations

  1. Department of Earth and Environmental Sciences, Indian Institutes of Science Education and Research, Bhopal, India

    Zafar Beg, Digvijay Singh & Kumar Gaurav

  2. Geo Climate Risk Solutions Pvt Ltd, Visakhapatnam, India

    Suneel Kumar Joshi

  3. Hydrological Investigations Division, National Institute of Hydrology, Roorkee, India

    Suneel Kumar Joshi & Sudhir Kumar

  4. Indian Institute of Technology, Kanpur, India

    Digvijay Singh

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  1. Zafar Beg
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Beg, Z., Joshi, S.K., Singh, D. et al. Surface water and groundwater interaction in the Kosi River alluvial fan of the Himalayan Foreland. Environ Monit Assess 194, 556 (2022). https://doi.org/10.1007/s10661-022-10192-8

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