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

Author:

Beg Zafar,Joshi Suneel KumarORCID,Singh Digvijay,Kumar Sudhir,Gaurav Kumar

Publisher

Springer Science and Business Media LLC

Subject

Management, Monitoring, Policy and Law,Pollution,General Environmental Science,General Medicine

Reference55 articles.

1. Bhattacharya, S., Gupta, S., & Krishnamurthy, R. (1985). Oxygen and hydrogen isotopic ratios in groundwaters and river waters from India. Proceedings of the Indian Academy of Sciences - Earth and Planetary Sciences, 94(3), 283–295.

2. Boral, S., & Sen, I. S. (2020). Tracing ‘Third Pole’ice meltwater contribution to the Himalayan rivers using oxygen and hydrogen isotopes. Geochemical Perspectives Letters, 13, 48–53.

3. Brenninkmeijer, C. A. M., & Morrison, P. D. (1987). An automated system for isotopic equilibration of CO2 and H2O for 18O analysis of water. Chemical Geology: Isotope Geoscience Section, 66(1–2), 21–26.

4. CGWB. (2009). Methodology for assessment of development potential of deeper aquifers, Central Ground Water Board, Ministry of Water Resources, River Development & Ganga Rejuvenation, Government of India, Faridabad.

5. Chakraborty, T., Kar, R., Ghosh, P., & Basu, S. (2010). Kosi megafan: Historical records, geomorphology and the recent avulsion of the Kosi river. Quaternary International, 227(2), 143–160.

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