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TRANSFORMATION OF THE IRKUTSK RESERVOIR SHORES BUILT UP BY LOESS-LIKE ROCKS

https://doi.org/10.15356/0435-4281-2014-2-

Abstract

The paper deals with the mechanisms of abrasion destruction on a near-dam shore strip of the Irkutsk Reservoir within the urban territory. The survey of five profiles showed that the retreat of the shore at the case site constituted 1–3 m for the 2004-2006 period. The investigation revealed the main stages of the process development to be closely related to the water level fluctuations in the reservoir. At the low water level the slope of the shore is flattening and its profile become stable and equilibrium. At the high level the shore is washing out and its profile become unstable. Loams and sandy loams present in the section, marked by low firmness and small strength, cause the development of plastic deformations at significant moistening. The water level fluctuations in the reservoir lead to cyclical nature of shore degradation; physical, physical-chemical, and stress-strain properties of soils affect its rate.

About the Authors

A. A. Rybchenko
Institute of the Earth’s Crust SB RAS, Irkutsk
Russian Federation


A. V. Kadetova
Institute of the Earth’s Crust SB RAS, Irkutsk
Russian Federation


V. A. Huck
Institute of the Earth’s Crust SB RAS, Irkutsk
Russian Federation


References

1. Ovchinnikov G.I. Dinamika beregovoy zony angarskikh vodohranilishch (Dynamics of the Angara reservoirs coastal zone). Doct. thesis. Irkusts: IG SB RAS, 2003, 50 p.

2. Kadetova A.V., Kozyreva E.A., Rybchenko A.A. Degradation of shores in the urban area of Irkutsk city under the infl uence of man-made reservoir. Bul. of the Geol. Soc. of Greece. 2007. V. XXXVII. P. 1433–1439.

3. Ryaschenko T.G. Regionalnoe gruntovedenie (Vostochnaya Sibir) (Regional gruntovedenie (Western Siberia)). Irkutsk: IEC SB RAS, 2010, 287 p.

4. Shirokov V.M. Formirovanie beregov I lozha krupnykh vodohranilisch Sibiri (Coasts and bed forming of the large Siberian reservoirs). Novosibirsk: Nauka, Sib. Branch (Publ.), 1974, 172 p.

5. Owchinnikow G.I. Wplyw processow abrazyjnych na rozwoj strefy przybrzeznej zbiornikow wodnych angarskiej kaskady elektrowni wodnych. Ksztaltowanie srodowiska geografi cznego i ochrona przyrody na obszarach uprzemyslowionych i zurbanizowanych. Katowice: Sosnowiec, 1996. ? 23. S. 38–42.

6. Ovchinnikov G.I., Pavlov S.H., Trzhinskiy Yu.B. Izmenenie geologicheskoy sredy v zonakh vliyaniya Angaro-Eniseyskhih vodohranilishch (Changes of geological environment in zones of the Angara- Yenisei reservoirs impact). Novosibirsk: Nauka, Sib. Branch (Publ.), 1999, 252 p.

7. Lomtadze V.D. Fiziko-mekhanicheskie svoystva gornykh porod. Metody laboratornykh issledovaniy (Physical-mechanical characters of rocks. Methods of laboratory research). Leningrad: Nedra (Publ.), 1990, 327 p.

8. Leshchikov F.N., Shats M.M. Merzlye porody yuga Sredney Sibiri (Frozen grounds of southern part of Middle Siberia). Novosibirsk: Nauka, Sib. Branch (Publ.), 1983, 168 p.

9. Ovchinnikov G.I., Trzhinskiy Yu.B, Zhentala M., Zhentala M.A. Abrazionno-akkumulyativnye protsessy v beregovoy zone vodohranilishch na primere Yuzhnogo Priangar’ya I Silezskoy vozvyshennosti (Abrasion-accumulative processes in coastal zone of reservoirs in terms of the South Anraga Region and Silezskaya upland). Sosnovets-Irkutsk: IEC SB RAS, 2002, 102 p.

10. Klimat Irkutska (Climate of Irkutsk). Leningrad: Gidrometeoizdat (Publ.), 1981, 245 p.


Review

For citations:


Rybchenko A.A., Kadetova A.V., Huck V.A. TRANSFORMATION OF THE IRKUTSK RESERVOIR SHORES BUILT UP BY LOESS-LIKE ROCKS. Geomorfologiya. 2014;(2):61-67. (In Russ.) https://doi.org/10.15356/0435-4281-2014-2-

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