Spatial-Temporal Regularities in Changing Chemical Composition of Bog Waters in Taiga Zone of Western Siberia
| Parent link: | Procedia Chemistry Vol. 15 : Chemistry and Chemical Engineering in XXI century (CCE 2015).— 2015.— [P. 206-212] |
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| Other Authors: | , , , |
| Summary: | 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 |
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2015
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| Online Access: | http://dx.doi.org/10.1016/j.proche.2015.10.033 http://earchive.tpu.ru/handle/11683/15054 |
| Format: | Electronic Book Chapter |
| KOHA link: | https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=645352 |
| Summary: | 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 |
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| DOI: | 10.1016/j.proche.2015.10.033 |