Spatial-Temporal Regularities in Changing Chemical Composition of Bog Waters in Taiga Zone of Western Siberia

Bibliografske podrobnosti
Parent link:Procedia Chemistry
Vol. 15 : Chemistry and Chemical Engineering in XXI century (CCE 2015).— 2015.— [P. 206-212]
Korporativna značnica: Национальный исследовательский Томский политехнический университет (ТПУ) Институт природных ресурсов (ИПР) Кафедра гидрогеологии, инженерной геологии и гидрогеоэкологии (ГИГЭ)
Drugi avtorji: Matveenko I. A. Irina Alekseevna, Savichev O. G. Oleg Gennadievich, Bazanov V. A., Ivanova Ye. V.
Izvleček:Title screen
The generalization of data on bog water chemistry has been performed in taiga zone of Western Siberia within 1998-2011. It is shown that the decrease in dissolved salt concentrations over the territories included in the row «eutrophic swamp - mesotrophic swamp - oligotrophic bog» is observed in the course of deterioration of water-mineral supply for bog plants, in the cross-section of peat formation - from inert layer to the upper part of active layer. It is stated that during a year there are maximums in trace element contents, biogenic matter, organic acids in spring and most of principle ions - in summer.
Режим доступа: по договору с организацией-держателем ресурса
Jezik:angleščina
Izdano: 2015
Teme:
Online dostop:http://dx.doi.org/10.1016/j.proche.2015.10.033
http://earchive.tpu.ru/handle/11683/15054
Format: Elektronski Book Chapter
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=645352

MARC

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330 |a The generalization of data on bog water chemistry has been performed in taiga zone of Western Siberia within 1998-2011. It is shown that the decrease in dissolved salt concentrations over the territories included in the row «eutrophic swamp - mesotrophic swamp - oligotrophic bog» is observed in the course of deterioration of water-mineral supply for bog plants, in the cross-section of peat formation - from inert layer to the upper part of active layer. It is stated that during a year there are maximums in trace element contents, biogenic matter, organic acids in spring and most of principle ions - in summer. 
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