Dynamics of riverbed evolution in the middle Ural River and natural management risks
https://doi.org/10.1134/S2587556618050126
Abstract
Data on the shifts of riverbeds in the Ural River basin were obtained based on the analysis of remote sensing data (Landsat, 1985–2015) and archival data. The stages of development of free bends and riverbed, the degree of their completeness for rivers with different hydrological regime and conditions of formation of runoff in catchments (Ural and Sakmara) are marked. It was revealed that the peculiarities of riverbed transformation in wide floodplain conditions are mainly due to runoff values during the spring flood. It is noted that the dynamics of riverbed evolution processes in general is reduced due to a decrease in the share of spring flow as a result of macroregional climatically determined trends and regulation of runoff by reservoirs. The most actively developing elements of the riverbed are the peaks of free bends, the rates of spatial displacement of which range from 3–5 m to 11 m per year. The main reasons for the current risks of destruction of economic facilities located in the immediate vicinity of the coastal ledges are due to insufficient account of riverbed activity during the development of the region. The location of part of the state Russian-Kazakhstan border along the Ural and Ilek rivers in conditions of constant riverbed transformations causes the emergence of disputed territories.
About the Authors
V. M. PavleichikRussian Federation
Orenburg
Zh. T. Sivokhip
Russian Federation
Orenburg
Yu. A. Padalko
Russian Federation
Orenburg
References
1. Alekseevskiy N.I. Formirovanie i dvizhenie rechnykh nanosov [Formation and Movement of River Sediments]. Moscow: Moscow St. Univ., 1988. 202 p.
2. Barovsky N.A. Hydrological-morphodynamic analysis of freely meandering channels at different stages of their development. Geomorphology RAS, 2005, no. 4, pp. 54–63. (In Russ.).
3. Butakov G.P., Nazarov N.N., Chalov R.S., Chernov A.V. Conditions for the formation of channels and channel deformations on the rivers of the basin of the Kama river. In Erozionnye i ruslovye protsessy [Erosion and Сhannel Processes]. Moscow: Moscow St. Univ., 2000, vol. 3, pp. 138–148. (In Russ.).
4. Vtoroi otsenochnyi doklad Rosgidrometa ob izmeneniyakh klimata i ikh posledstviyakh na territorii Rossiiskoi Federatsii. Obshchee rezyume [The Second Assessment Report of Roshydromet on Climate Change and Its-Consequences in the Territory of the Russian Federation. General Summary]. Moscow: Rosgidromet Publ., 2014. 58 p.
5. Zavadsky A.S., Kargapolova I.N., Chalov P.S. Stages of development of free bends and their hydrologicalmorphological analysis. Vestn. Mosk. Univ. Ser. 5: Geogr., 2002, no. 2, pp. 17–22. (In Russ.).
6. Kurganovich K.A., Noskova E.V. The use of water indices to assess the change in the area of the water mirror of steppe soda lakes in the Southeast of Transbaikal, according to remote sensing data. Vestn. Zabaikal. Gos.Univ., 2015, no. 6 (121), pp. 16–23. (In Russ.).
7. Levashova I.A., Levashov A.A. Estimation and forecast of channel deformations in connection with the change in the hydrological regime. Modelirovanie i Prognozy Gidrologicheskikh Protsessov, St. Peterburg, 1992, pp. 50–56. (In Russ.).
8. Natsional’nyi doklad o sostoyanii okruzhayushchei sredy i ob ispol’zovanii prirodnykh resursov Respubliki Kazakhstan za 2015 god [National Report on the State of the Environment and the Use of Natural Resources of the Republic of Kazakhstan, 2015]. Available at: http://ecogosfond.kz/wp-content/uploads/2018/03/140320171.pdf (accessed 08.07.2018).
9. Sergaliev N.H., Akhmedenov K.M. Stream Processes on the Ural River. Novosti Nauki Kazakhstana, 2013, no. 3 (117), pp. 201–205. (In Russ.).
10. Sivohip J.T., Padalko Yu.A. Geographical and hydrological factors of dangerous hydrological phenomena in the Ural river basin. Izv. Ross. Akad. Nauk. Ser. Geogr., 2014, no. 6, pp. 53–61. (In Russ.).
11. Spetsial’naya Karta Evropeiskoi Rossii [Special Map of European Russia]. Map scale 1:420000. I.A. Strel’bitskiy, Ed. Voen. Topogr. Otdel Publ., 1874. Sheets no.130, 141.
12. The Federal Law of the Russian Federation No. 148-FZ of December 2, 2005 On the Ratification of the Treaty between the Russian Federation and the Republic of Kazakhstan on the Russian-Kazakh State Border. Ross. Gazeta, Dec. 6, 2005, no. 3943.
13. Chibilyov A.A., Pavleychik V.M., Damrin A.G. Iriklinskoe vodokhranilishche: geoekologiya i prirodno-resursnyi potentsial [Iriklinsky Reservoir: Geoecology and Natural Resource Potential]. Ekaterinburg: UrO RAN Publ., 2006. 183 p.
14. Shiklomanov I.A. Antropogennye izmeneniya vodnosti rek [Anthropogenic Changes in the Water Content of Rivers]. Leningrad: Gidrometeoizdat Publ., 1979. 301 p.
15. Feyisa G.L., Meilby H., Fensholt R., Proud S.R. Automated Water Extraction Index: A new technique for surface water mapping using Landsat imagery. Rem. Sens. Environ., 2014, no. 140, pp. 23–35.
- Quantitative assessment of the intensity of channel transformations for rivers with different water regimes.
- The determining factor of channel transformations is the value of spring runoff, especially for the rivers with high spring flood waves.
- Reduction in spring floods due to climate change and runoff control.
- Risks for river settlements and transport infrastructure and risks of territorial claims in border area.
Review
For citations:
Pavleichik V.M., Sivokhip Zh.T., Padalko Yu.A. Dynamics of riverbed evolution in the middle Ural River and natural management risks. Izvestiya Rossiiskoi Akademii Nauk. Seriya Geograficheskaya. 2018;(5):37-45. (In Russ.) https://doi.org/10.1134/S2587556618050126