Hydrologic conditions for chemical composition of the Siberian river waters

Bibliographic Details
Parent link:IOP Conference Series: Earth and Environmental Science
Vol. 232 : Natural and Human Environment of Arctic and Alpine Areas: Relief, Soils, Permafrost, Glaciers, Biota Life Style of Native Ethnic Groups in a Rapidly Changing Climate.— 2019.— [012012, 7 p.]
Main Author: Savichev O. G. Oleg Gennadievich
Corporate Author: Национальный исследовательский Томский политехнический университет Инженерная школа природных ресурсов Отделение геологии
Other Authors: Zemtsov V. A. Valeriy Alekseevich, Pasechnik E. Yu. Elena Yurievna
Summary:Title screen
The influence of hydrologic conditions on the Siberian river waters chemical composition, their spatial and temporal changes are analysed. The dependencies between the hydrochemical and hydrological parameters are determined. It is shown that: 1) many hydrochemical parameter changes are defined by lognormal probability distribution; 2) variability of the chemical composition and elevated concentrations of some substances will be more likely to occur in the inter-annual and intra-annual runoff variability; 3) the main features of the water chemical composition are formed at the stages of the slope, subsurface and underground runoff formation.
Language:English
Published: 2019
Subjects:
Online Access:https://doi.org/10.1088/1755-1315/232/1/012012
Format: Electronic Book Chapter
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=664513
Description
Summary:Title screen
The influence of hydrologic conditions on the Siberian river waters chemical composition, their spatial and temporal changes are analysed. The dependencies between the hydrochemical and hydrological parameters are determined. It is shown that: 1) many hydrochemical parameter changes are defined by lognormal probability distribution; 2) variability of the chemical composition and elevated concentrations of some substances will be more likely to occur in the inter-annual and intra-annual runoff variability; 3) the main features of the water chemical composition are formed at the stages of the slope, subsurface and underground runoff formation.
DOI:10.1088/1755-1315/232/1/012012