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

• Published in: Procedia Chemistry
• Main Authors: Matveenko, Irina Alekseevna, Savichev, Oleg Gennadievich, Bazanov, V. A., Ivanova, Ye. V.
• Format: Conference Object
• Language: English
• Published: Elsevier 2015
• Subjects: пространственно-временные закономерности; химический состав; воды; Западная Сибирь; болота; taiga; Siberia
• Online Access: http://earchive.tpu.ru/handle/11683/15054; https://doi.org/10.1016/j.proche.2015.10.033

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.