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Spatio-temporal variation of trace elements distributed over surface water of Upper Ganga River Basin in Western Himalayan Region

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Abstract

The rivers draining from the Himalayan range distribute enormous amount of fresh water to the people living in downstream regions. Trace metals flowed with river water can lead to serious impact on ecological system and human health. Nevertheless, the documentation on trace elements of Himalayan rivers is inadequately documented. The current study deals with the spatial and temporal variability of the major and trace elements of Ganga river water in epirhithron, metarhithron and hyporhithron zone belonging to Himalayan segment. Water samples from nineteen monitoring locations were collected in pre-monsoon (May–June), monsoon (August–September) and post-monsoon (December) seasons and subjected to be assessed for 20 elements (Ag, Al, Ba, Cd, Ca, Cr, Cu, Fe, Ga, K, Mn, Mg, Na, Ni, Pb, Sr, Th, U, Zn, and Zr) using ICP-OES (Inductively Coupled Plasma-Optical Emission Spectrometer). Different water pollution indexes such as HPI (Heavy Metal Pollution Index), MI (Metal Index) and PI (Pollution Index) were used to describe current water quality status at each monitoring station under particular classified ecological zone. The studied stations in hyporhithron zone had the value of Metal Index (MI>1), indicating threshold of warning. Further, the highest values of HPI in hyporhithron zone correspond to poor water quality status. Sites with poor water quality were also found to be contaminated as per the Pollution Index (PI), exhibiting high concentrations for element (Fe). However, the epirhithron and metarhithron zone in Himalayan segment showed excellent water quality mainly contributed from natural sources. Cluster Analysis (CA) and Principal Component Analysis (PCA) were applied to identify the main influential sources for Ganga river water pollution. The Kriging interpolation method was also applied to prepare spatial distribution map of computed indexes (HPI, MI, and PI). With the help of index of local Moran’s I (LMI), identified spatial clusters and spatial outliers revealed the elevated concentration of most elements in hyporhithron zone. The dataset presented in this study would be convenient for government officials in developing more effective management policies and necessary steps to check and monitor the Ganga river water quality. It was also suggested that further investigations in terms of trace elemental sources and their role in self-purification properties of Ganga water can be addressed in future.

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Acknowledgments

The authors are grateful to the Doon University, Dehradun, India, for the financial support to carry out the research work. The authors are thankful to the Ex-Chancellor, Dr. K.K. Paul, of Uttarakhand and Ex-Vice Chancellor, Prof. V.K. Jain, Doon University for their encouragement, support, and suggestions. We also thank IIT, Roorkee for performing trace element analysis

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Correspondence to Archana Sharma.

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Dimri, D., Kumar, A., Mishra, D.K. et al. Spatio-temporal variation of trace elements distributed over surface water of Upper Ganga River Basin in Western Himalayan Region. J. Mt. Sci. 20, 145–162 (2023). https://doi.org/10.1007/s11629-021-6703-9

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  • DOI: https://doi.org/10.1007/s11629-021-6703-9

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