Chemical Composition of Bottom Sediments in Small Mountain Rivers (Altai, the Russian Federation)

Bibliographic Details
Parent link:MATEC Web of Conferences
Vol. 85 : Chemistry and Chemical Technology in XXI Century (CCT 2016).— 2016.— [01031, 7 p.]
Main Author: Savichev O. G. Oleg Gennadievich
Corporate Authors: Национальный исследовательский Томский политехнический университет (ТПУ) Институт природных ресурсов (ИПР) Кафедра иностранных языков (ИЯПР), Национальный исследовательский Томский политехнический университет (ТПУ) Институт природных ресурсов (ИПР) Кафедра гидрогеологии, инженерной геологии и гидрогеоэкологии (ГИГЭ)
Other Authors: Matveenko I. A. Irina Alekseevna, Paromov V. Vladimir
Summary:Title screen
The article deals with the chemical composition of bottom sediments in the small mountain rivers Aktru, Tyute, and Uznezya (Altai, Russia). It is established that as compared to small and middle plain rivers in Taiga zone, Siberia bottom sediments of the Aktru River contain less amount of K, Na, V, Cr, Mn, Ni, Al, Si, Ti, Sr, approximately the same - Fe, Co, Cu, Zn, Pb and more - As, Ca, Mg. It is suggested that there is a sharp increase of relative Al, Na, K and Si shares from the upland to lowland due to both weathering products accumulation of primary alumosilicates in bottom sediments and export of Ca and Mg from them when dissolving carbonate minerals. Composition transformations of bottom sediments is non-linear and considerably depends on composition of underlying and water-bearing rocks and water exchange intensity that manages time, conditions, and stages of interactions in "water - organic matter - rock" system.
Language:English
Published: 2016
Subjects:
Online Access:http://dx.doi.org/10.1051/matecconf/20168501031
http://earchive.tpu.ru/handle/11683/36584
Format: Electronic Book Chapter
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=652862