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New insights into water cycle in permafrost region of northern Greater Khingan Mountains, China

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Abstract

This study investigated the influence of precipitation and temperature on the runoff and forest growth in the northern Greater Khingan Mountains of China through the hydrology, hydrochemistry and remote sensing methods. The rivers were found to be recharged not only by precipitation, but also by subpermafrost groundwater through water balance calculation and the relationships between precipitation, temperature and runoff. The stable isotope compositions of the river and groundwater more depleted than local precipitation indicating the great contribution of subpermafrost groundwater to runoff. Participation of subpermafrost groundwater makes the forest-permafrost water cycle in the northern Greater Khingan Mountains unique.

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Acknowledgements

This study is financially supported by the National Key Technologies R&D Program (20185056032), and the Fundamental Research Funds for the Central Universities (2018B48814). The authors are grateful for the help of the State Key Laboratory of Hydrology–Water Resources and Hydraulic Engineering at Hohai University, where all analyses were performed.

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Correspondence to Jiansheng Chen.

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Ma, F., Chen, J., Zhan, L. et al. New insights into water cycle in permafrost region of northern Greater Khingan Mountains, China. J Radioanal Nucl Chem 330, 631–642 (2021). https://doi.org/10.1007/s10967-021-08013-2

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  • DOI: https://doi.org/10.1007/s10967-021-08013-2

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