Email this article Variations of Amur water chemistry during the historical 2013 flood
- Authors: Shesterkin V.P.1
-
Affiliations:
- Institute of Water and Environmental Problems, Far East Branch
- Issue: Vol 43, No 3 (2016)
- Pages: 495-503
- Section: Water Quality and Protection: Environmental Aspects
- URL: https://ogarev-online.ru/0097-8078/article/view/173978
- DOI: https://doi.org/10.1134/S0097807816030155
- ID: 173978
Cite item
Open Access
Access granted
Subscription Access
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
Supplementary files
