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| # | Search | Downloads | ||||
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| 1 | Happen to the results a calculation sewer of the spring high water with systems hign-moor mires, located on spur Vasyugan mires by method declivity flow. Digital analogue landcape-typecal of the card was created for determination of the areas microlandcape. The Single filtration consuption with different types marsh landcape was defined on level of mires water partly, on tabular data partly. Keywords: high-moor mire, sewer, filtering, deyatelinyy layer, landscape, phytocenosis, single consuption, declivity sidebar, level of mires water | 1627 | ||||
| 2 | The work makes analysis of the regularities of sharing of the separate groups of microorganisms in oligotrophic mires of West Siberia with using cluster-analytical method. The relationships between characteristic, regimes of oligotrophic mires and activity of the biochemical processes are revealed. Keywords: peat mire, peat formation, biochemical processes, microflora, cluster analysis | 1725 | ||||
| 3 | The aim of this study is to investigate composition and dynamics of hydrohimichal flow with river-water from oligotrophic deposits in North-eastern part of Vasyugan Mire. Module of the ion sewer has formed 1.38 g/(s-km2). Keywords: concentration, macrocomponents, organic substances, a mineralization, the module of an ionic sewer, the background content, time dynamic, Vasyugan mire | 1466 | ||||
| 4 | The presented results of the calculation water balance element for three represent water basin of big Vasyugan mires with a different degree of paludification on month interval for the period 1990–2009 years. There was analysed the perennial track records of the precipitation, evaporations and expenses of water, influence of the change the climate on hydrological marshes regimen. The correlations are estimated between elements of the water balances at different years. Keywords: paludification water basin, hydra-climatic facility, evaporation, run off water and heat exchange, wood-marsh zone, West Siberia, hydrological regimes, time dynamic | 1409 | ||||




