NATURAL AND ANTHROPOGENIC IRREVERSIBLE VERTICAL RIVERBED DEFORMATIONS
https://doi.org/10.15356/0435-4281-2017-4-3-15
Abstract
Irreversible vertical deformation implies the systematic incision or sediment deposition within a considerable length of the river, in the course of which rise or lowering of river long profile and change of its general shape occur. Contemporary deformations occur in time intervals documented by historical materials and direct observations, that span several centuries, develop under the human influence or have a purely anthropogenic origin, although natural deformations due to tectonics and climate change play some role as well.
To analyze the dynamics of the riverbed vertical deformations process, published sources for several rivers over the World were used as well as authors’ own studies in a number of rivers: Ob river upstream and downstream of Novosibirsk reservoir, Kama river downstream of the Votkinsk dam, Selected reaches in rivers Tom’, Oka, Belaya Rivers with a large scale in-stream mines. Dam construction and creation of reservoirs as well as in-stream extraction of building materials most notably contribute to the development of vertical deformations.
Results show that both the process of incision downstream of dam and in sections with in-stream mines and the process of regressive accumulation upstream of the reservoirs are described by an exponential relationship reflecting the asymptotic nature of the lowering or rise of the riverbed. The relationship coefficients depend on the mobility of the channel. In the course of incision, riverbed becomes less movable, and its recovery may occur in other hydrological and geomorphological setting.
About the Authors
K. M. BerkovichRussian Federation
Faculty of Geography, Moscow
L. V. Zlotina
Russian Federation
Faculty of Geography, Moscow
L. A. Turykin
Russian Federation
Faculty of Geography, Moscow
References
1. Lohtin V.M. O mehanizme rechnogo rusla (On river channel mechanisms). Sankt-Peterburg, 1897. 80 p.
2. Makkaveyev N.I. Ruslo reki i erozia v ee bassejne (Riverbed and erosion within its watershed). M.: Izdvo AN SSSR (Publ.), 1955. 347 p.
3. Chalov R.S. Main types of riverbed deformations, their phenomenon and correlation in various natural condition, in Doklady sektsii ruslovykh protsessov Nauchnogo soveta “Kompleksnoe ispolzovanie i ohrana vodnykh resursov” (Reports of riverbed processes Section “Water resources complex use and conservation”). Iss. 2. Leningrad: Gidrometeoizdat (Publ.), 1986. P. 100–113.
4. Dröge B., Engel H., and Gölz E. Channel erosion and erosion monitoring along the Rhine River. Erosion and Sediment Transport Monitoring Programs in River Basins. Oslo, IAHS Publ., 1992. No. 210. P. 493–503.
5. Whipple K.X. and Tucker G.E. Dynamics of the stream-power river incision model: Implications for height limits of mountain ranges, landscape response timescales, and research needs. J. Geophys. Res. 1999. Vol. 104. P. 661–674.
6. Makkaveyev N.I., Mandych A.F., and Chalov R.S. Relief rising development impact on erosion and sediment yield of West Georgia’s Rivers. Vestn. Mos. Univ. Ser. 5. Geogr. 1968. No. 4. P. 52–58. (in Russ.)
7. Nikonov A.A. River incision rate determination. Geomorfologiya (Geomorphology RAS). 1973. No. 1. P. 24–35. (in Russ.)
8. Shcheglova O.P. Formirovanie stoka vzveshennyh nanosov i smyv s gornoj chasti Srednej Azii (Suspended sediment yield formation and erosion in Middle Asia mountain Area). Leningrad: Gidrometeoizdat (Publ.), 1972. 228 p.
9. Schumm S.A. Alluvial river response to active tectonics. National Research Council. Active Tectonics: Impact on society. Washington, DC: The National Academies Press, 1986. P. 80–94.
10. Harkins N., Kirby E., Heimsath A., Robinson R., and Reiser U. Transient fluvial incision in the headwaters of the Yellow River, northeastern Tibet, China. Journal of geophysical research. Vol. 112. 2007. P. 1–21.
11. Sidorchuk A.Yu. and Chalov R.S. The incision of the rivers of mountain: rates and causes. Priroda. 1996. No. 12. P. 36–45. (in Russ.)
12. Wyżga B. A review on channel incision in the Polish Carpathian Rivers during the 20th century. Gravel-Bed Rivers VI: From Process Understanding to River Restoration. Elsevier, Amsterdam, 2008. P. 525–555.
13. Simon A. Energy, time, and channel evolution in catastrophically disturbed fluvial systems. Geomorphology. 1992. No. 5. P. 345–372.
14. Nazarov N.N., Chalov R.S., Chalov S.R., and Chernov A.V. Rivers longitudinal profiles, riverbed morphology and dynamics in mountain and plain areas. Geogr. Vestn. Iss. 2. 2006. P. 40–52. (in Russ.)
15. Babiński Z. Wspólczesne procesy korytowe dolnej Wisly. Prace Geogr. 1992. Vol. 157. 185 s. (Contemporary riverbed processes of lower Vistula River. Geographical Works. 1992. Iss. 157. 185 p).
16. Makkaveyev N.I. and Chalov R.S. Some features of large river valley bottom related to the periodical changes of the rate of flow, in Voprosy Geografii (Geographical Issues). Vol. 79. Moscow: Mysl’ (Publ.), 1970. P. 156–167.
17. Gray J.R., Osterkamp W.R., and Xu Jianhua. Effects of Water Use Diversion Regulation and Conservation on Sediment Transport in China’s Yellow River with Comparisons from the United States. 12th ISCO Conference Beijing. 2002. P. 565–569.
18. Slater L.J. and Singer M.B. Imprint of climate and climate change in alluvial riverbeds: Continental United States, 1950–2011. Geological Society of America, 2013. DOI: 10.1130/G34070.1
19. Alekseevski N.I., Obodovski A.G., and Samohin M.A. Water level changes mechanisms in Rivers, in Eroziya i ruslovye protsessy (Erosion and riverbed processes). Iss. 4. Moscow, MSU (Publ.), 2005. P. 216–237.
20. Koltunova M.A. Water discharge curves by vertical riverbed deformation analysis, in Ecologo-geograficheskie issledovaniya v rechnykh basseynakh (4th All-Russia scientific practical conference Materials). Voronezh. 2014. P. 42–45
21. Ruslovye protsessy i vodnye puti na rekah bassejna Severnoj Dviny (Riverbed processes and waterways on the rivers of North Dvina catchment). Moscow: Zhurnal RT, 2012. 492 p.
22. Borsuk O.A. and Chalov R.S. On the Lena River channel incision. Izv. VGO. Vol. 105. iss. 5. 1973. P. 452–456. (in Russ.)
23. Alekseevski N.I., Berkovich K.M., Chalov R.S., and Chalov S.R. Spatial and temporal riverbed deformation changeability in Russia’s Rivers. Geogr. Prir. Resur. 2012. No. 3. P. 13–21. (in Russ.)
24. Singh S.K. Erosion and weathering in the Brahmaputra River System, in Large Rivers Geomorphology and Management. Ed. by A. Gupta. John Wiley & Sons Ltd, 2007. P. 373–391.
25. Billi P. and Rinaldi M. Human impact on sediment yield and channel dynamics in the Arno River basin (central Italy) Human Impact on Erosion and Sedimentation (Proceedings of Rabat Symposium S6, April 1997). IAHS Publ. 1997. no. 245. P. 301–311.
26. Torres W.F. and Jain S. Aggradation and degradation of alluvial-channel beds. IIHR report No. 274. Iova, 1984. 135 p.
27. Church M. Bed material transport and the morphology of alluvial river channels. Annual review of Earth and Planetary Sciences. 2006. Vol. 34. P. 325–354.
28. Makkaveyev N.I., Belinovich I.V., and Khmeleva N.V. Riverbed processes within backwater zones, in Ruslovye protsessy (Riverbed processes). Moscow: Izd-vo AN SSSR (Publ.), 1958. P. 318–337.
29. Wang Zhaoyin and Hu Chunhong. Interaction between fluvial systems and large scale hydro-projects. Proceedings of the Ninth International Symposium on River Sedimentation, Yichang, China, 2004. P. 46–64.
30. Rinaldi M., Wyzga B., and Surian N. Sediment mining in alluvial channels: physical effects and management perspectives. River research and applications. 2005. Vol. 21. P. 805–828.
Review
For citations:
Berkovich K.M., Zlotina L.V., Turykin L.A. NATURAL AND ANTHROPOGENIC IRREVERSIBLE VERTICAL RIVERBED DEFORMATIONS. Geomorfologiya. 2017;(4):3-15. (In Russ.) https://doi.org/10.15356/0435-4281-2017-4-3-15