Effects of long-term drainage on vegetation, surface topography, hydrology and water chemistry of north-eastern part of Great Vasyugan Mire (Western Siberia)

In this study, we determine the influence of a long-term drainage on the vegetation, surface topography, hydrology, and water chemistry of the north-eastern drained part of the Great Vasyugan Mire. Many studies have shown an increase in the projective coverage of V. Uliginosum, A. polifolia, P. schr...

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Bibliographic Details
Published in:IOP Conference Series: Earth and Environmental Science
Main Authors: Sinyutkina, A. A., Gashkova, L. P., Kharanzhevskaya, Yulia A., Magur, M. G., Voistinova, E. S., Ivanova, E. S., Chudinovskaya, L. A., Khaustova, A. A., Maloletko, A. A.
Format: Article in Journal/Newspaper
Language:English
Published: 2018
Subjects:
Большое Васюганское болото
дренаж
растительность
топография
гидрология
химия воды
Cladonia rangiferina
Siberia
Online Access:https://doi.org/10.1088/1755-1315/211/1/012033
https://openrepository.ru/article?id=331237
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Summary:In this study, we determine the influence of a long-term drainage on the vegetation, surface topography, hydrology, and water chemistry of the north-eastern drained part of the Great Vasyugan Mire. Many studies have shown an increase in the projective coverage of V. Uliginosum, A. polifolia, P. schreberi, P. Strictum and D. polysetum, Cladonia stellaris and Cladonia rangiferina and a decrease in the projective coverage of C. calyculata, and L. palustre, S. angustifolium S. magellanicum. In the peat core, in comparison with archival data (1985), an increase in the degree of peat decomposition by 5-10% in the top 10-100 cm layer is noted, which may be due to the partial degradation of the peat deposit as a result of dehumidification. The microrelief is characterized by a decrease in the proportion of heights at the middle surface from 44 to 37% and the presence of steep slopes between the positive and negative forms of the microrelief. A decrease in the water table levels of bog waters and an increase in the amplitude of the oscillation are noted. In the chemical composition of the drained bog, we note an increase in the concentrations of the main ions by 6-38%, as well as DOC by 13%, Pb by 9%, Cu by 46%, and Zn by 215%. In the river waters there is an increase in NO3 − by 11%, NH4 + by 26%, SO4 2-by 36%, Fetotal by 89%, and DOC by 17%; no increase in the concentrations of Pb, Cu, Zn is observed.

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