CALCULATION OF THE SPRING RUNOFF WITH SYSTEM OF OLIGOTROPHIC BOGS BY METHOD OF OVERLAND RUNOFF
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
References:
1. Ivanov K.E. Hydrology for Mires. L.: Gidrometeoizdat, 1953. 297 s.
2. Inisheva L.I., Petkevich M.V. Landcape-typecal feature of the pool r. Kluch //Questions to geographies Siberia. 1999. 23. S.237-243.
3. Vasyugan Mire: Natural conditions, structure and operation /Under red. L.I. Inisheva, Tomsk: CNTI, 2003. 212 s.
4. Petkevich M.V., Inishev N.G., Knyazikov A.S. Factors for Formation Landcapes the river sewer in pool r. Kluch // Mires and biosphere. Full-grown. 2- Scientific School. Tomsk: CNTI, 2003. S.145–148.
5. The Instructions on calculation of the sewer with undranned and dranned riding mires. L.: Gidrometeoizdat, 1971.84с.
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Issue: 3, 2009
Rubric: Hydrology and Melioration of Peat Lands
Pages: 132 — 136
Downloads: 1020