Variations of Amur water chemistry during the historical 2013 flood


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Abstract

Water chemistry in the Amur R. at Khabarovsk was studied during the historical 2013 flood. The concentrations of dissolved substances were shown to vary significantly over both time and space, because of the difference between the discharge and chemistry in the main flood-forming tributaries. The ion runoff, nutrient runoff, and microelement runoff were estimated for the flood peak and all over flood period.

About the authors

V. P. Shesterkin

Institute of Water and Environmental Problems, Far East Branch

Author for correspondence.
Email: shesterkin@ivep.as.khb.ru
Russian Federation, ul. Dikopol’tseva 56, Khabarovsk, 680000

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