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B. S. Sukhija
Researcher at Council of Scientific and Industrial Research
Publications - 10
Citations - 332
B. S. Sukhija is an academic researcher from Council of Scientific and Industrial Research. The author has contributed to research in topics: Aquifer & Groundwater. The author has an hindex of 7, co-authored 10 publications receiving 291 citations.
Papers
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Fluoride dynamics in the granitic aquifer of the Wailapally watershed, Nalgonda District, India
TL;DR: The Wailapally granitic aquifer of Nalgonda district, Andhra Pradesh, India has high concentrations of fluoride (up to 7.6 mg/L) as discussed by the authors.
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Understanding hydrological processes in a highly stressed granitic aquifer in southern India
TL;DR: The results of a study evaluating the recharge/discharge conditions of an unconfined stressed granitic aquifer situated in a semi-arid region of Andhra Pradesh, Southern India are presented in this paper.
Patent
A process utilizing natural carbon-13 isotope for identification of early breakthrough of injection water in oil wells
TL;DR: In this article, a process utilizing natural carbon-13 isotope for identification of early breakthrough of injection water in oil wells is described, where all natural water sources are labeled by unique ratios of carbon isotopes (13C/12C) and the carbon isotope ratio for oil bearing formation water and for local aquifer water which is to be injected in to the oil reservoir rock is determined.
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Earthquake (M 5.1) induced hydrogeochemical and δ18O changes: validation of aquifer breaching—mixing model in Koyna, India
TL;DR: In this paper, a model of aquifer breaching and mixing of deep aquifer waters with shallow aquifer water due to an earthquake was proposed. But the model was only applied to the Koyna-Warna reservoir.
Journal Article
Palaeoliquefaction evidence of prehistoric large/great earthquakes in North Bihar, India
B. S. Sukhija,M. N. Rao,Dontireddy Venkat Reddy,P. Nagabhushanam,Devender Kumar,B. V. Lakshmi,Pankaj Sharma +6 more
TL;DR: In this article, the authors used palaeoliquefaction studies in the meizoseismal area of the 1934 earthquake to provide evidence for two prehistoric seismic events dated to have occurred: (i) during 1700 to 5300 years BP and (ii) earlier than 25,000 years BP, besides the well documented 1934 and 1833 seismic events.