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The short-term changes of gully erosion forms in the context of the water level fluctuations in the Bratsk reservoir (Russia)

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Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
The results of investigations ascertain the influence of the water level regime on the erosion dynamics that was estimated according gullies volume change within the space-time between two measurements. The development of gullies in the shore zone is to a large extent influenced by the abrasion of shore slopes, which is intense at high water level in the reservoir. The minimum rate of gully development (4.5-54.7m3 yr-1) was due to the action of shore abrasion and eolian processes within the period of 2004-2007. A large positive dynamics can be attributed to the increasing number of erosion cuts. The maximum material loss from gullies (in total 627.66 m3 ) and the average volumetric retreat rate for all gullies (16.5 m3 yr-1) were recorded at the permanent lowering of the reservoir water level during the 2007-2008 period. Water level fluctuations cause cyclic changes in the dynamics of processes and initiate the new mechanism of erosion that is not typical of regular conditions.
Czasopismo
Rocznik
Tom
Strony
117--123
Opis fizyczny
Bibliogr. 9 poz., rys.
Twórcy
autor
autor
autor
  • Institute of the Earth's Crust Russian Academy of Sciences Siberian Branch, Laboratory of engineering geology and geoecology, Russia, moks@crust.irk.ru
Bibliografia
  • Burkard M.B. & Kostaschuk R.A., 1997. Patterns and controls of gully growth along the shoreline of lake Huron. Earth Surface Processes and Landforms: 901–911.
  • Foster I.D.L., Poesen J., Boardman J. & Keay-Bright J., 2007. Sediment tracing and environmental history for two small catchments, Karoo Uplands, South Africa. 90, 1–2: 126–143.
  • Grobelska H., Mazaeva O.A. & Hak V., 2007. Conditions of development of erosion forms in the shore zone of Bratsk reservoir (Angara-river, Russia). In: Funkcjonowanie geoekosystemow zlewni rzecznych, 4. Procesy ekstremalne w srodowisku geograficznym: 275–285 (in Polish).
  • Hu Gang, Wu Yongqiu, Liu Baoyuan, Yu Zhangtao, You Zhimin & Zhang Yongguang, 2007: Shortterm gully retreat rates over rolling hill areas in black soil of Northeast China. Catena71: 321–329.
  • Ovchinnikov G.I., Pavlov S.Kh. & Trzhtsinsky Yu.B., 1999. Change of the geological environment in the Angaro-Yenisei reservoir-affected areas. Nauka, Novosibursk: 254 pp. (in Russian).
  • Pecherkin I.A., 1969.Geodynamics of the shore areas of the Kama reservoirs. Part 2. Geological processes. Perm: 308 pp. (in Russian).
  • Poesen J., Nachtergaele J., Verstraeten G. & Valentin C., 2003. Gully erosion and environmental change:importance and research needs.Catena50: 91–133.
  • Popov I.V., 1951. Engineering Geology. Geolizdat, Moscow: 444 pp. (in Russian).
  • Vandekerckhove, L., Poesen, J., Oostwoud Wijdenes, D. & Gyssels, G., 2001: . Catena 44, 2: 133–161.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BUJ5-0051-0064
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