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Quaestiones Geographicae

The Journal of Adam Mickiewicz University

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CONCEPTUAL MODEL FOR ASSESSING THE CHANNEL CHANGES UPSTREAM FROM DAM RESERVOIR

Maciej Liro
  • Department of Geomorphology, Jagiellonian University, Cracow, Poland
Published Online: 2014-03-27 | DOI: https://doi.org/10.2478/quageo-2014-0007

Abstract

Most of geomorphological studies related to the impact of dam reservoirs are focused on its effect on the river channels downstream of dams. However, little is known about the evolution of river channels upstream of dams (in backwater areas). In this paper I propose a conceptual model of alluvial channel changes in the backwater. It assumes that three conditions of a channel that may occur in the pre-dam period. These are sediment supply deficit, balance and surplus compared to the river transport capacity. These conditions can be strengthened, stable or weakened. In the post-dam period these conditions is modified by the influence of the dam reservoir, which may affect the trajectory of channel changes, as well as its response and adjustment time in the backwater. The adjustment of channel parameters, in spite of the reservoir operation mode, also depends on the local river, reach characteristics and the magnitude and frequency of floods. Therefore, the use of an appropriate reference reach is inherent in this model. The model suggests that some adverse changes to backwater channels degraded by the regulation can be hampered. The model is based on Lane’s balance concept. It may be useful for explaining and predicting channel changes upstream of reservoirs and forming hypotheses in other studies.

Keywords: dam; reservoir; backwater; alluvial; channel adjustment

References

  • Alibert M., Assani A.A., Gratton D., Leroux D., Laurencelle M., 2011. Statistical analysis of the evolution of a semialluvial stream channel upstream from an inversion-type reservoir: The case of the Matawin River (Quebec, Canada). Geomorphology 131: 28-34. DOI: 10.1016/j.geomorph. 2011.04.018. ISSN: 0169-555X. [Crossref] [Web of Science]

  • Bhowmik N.G., Adams J.R., Demisse M., 1988. Sedimentation of four reaches of the Mississippi and Illinois Rivers, Sediment Budgets (Proceedings of the Porto Alegre Symposium, December 1988). IAHS Publication 174: 11-19.

  • Brandt S.A., 2000. Classification of geomorphological effects downstream of dams. Catena 40: 375-401. [Crossref]

  • Chien N., 1985. Changes in river regime after the construction of upstream reservoirs. Earth Surface Processes and Landforms 10: 143-159. DOI: 10.1002/esp.3290100207. [Crossref]

  • Chorley R.J., Schumm S.A., Sugden D.E., 1984. Geomorphology. London: Methuen.

  • Dust D., Wohl E., 2012. Conceptual model for complex river responses using an expanded Lane's relation. Geomorphology 139-140: 109-121. DOI: 10.1016/j.geomorph. 2011.10.008. [Crossref] [Web of Science]

  • Evans J.E., Huxley J.M., Vincent R.K., 2007. Upstream Channel Changes Following Dam Construction and Removal Using a GIS/Remote Sensing Approach. Journal of the American Water Resources Association 43: 683-697. DOI: 10.1111/ j.1752-1688.2007.00055.x. [Web of Science] [Crossref]

  • Fischenich C., 2001. Stability Threshold for Stream Restoration Materials. EMRRP Technical Notes Collection (ERDC TN- EMRRR-SR-29), U.S Army Engineer Research and Development Center, Vicksburg, MS. Online: el.erdc.usace.army.mil/elpubs/pdf/sr29.pdf, April 15, 2013.

  • Florek E., Florek W., Łęczyński L., 2008. Funkcjonowanie zbiorników zaporowych na Słupi jako czynnik rzeźbotwórczy (Reservoirs of the Słupia River as morphogenetic agents). Landform Analysis 7: 12-22.

  • Grant G.E., 2012. The Geomorphic Response of Gravel-bed Rivers to Dams: Perspectives and Prospects. In: M. Church, P.M. Biron, A.G. Roy (eds), Gravel Bed Rivers VII: Processes, Tools, Environments. John Wiley & Sons: 165-181.

  • Gurnell A., 2013. Plants as river system engineers. Earth Surface Processes and Landforms 39: 4-25. DOI: 10.1002/ esp.3397. [Crossref] [Web of Science]

  • Hey R.D., 1986. River response to inter-basin water transfers: Craig Goch feasibility study. Journal of Hydrology 85: 407-421. [Crossref]

  • Hoey T.B., Sutherland A.J., 1991. Channel morphology and bedload pulses in braided rivers: a laboratory study. Earth Surface Processes and Landforms 16: 447-462. DOI: 10.1002/esp.3290160506. [Crossref]

  • ICOLD, 1988. World Register of Dams, Update. International Commision on Large Dams, Paris.

  • ICOLD, 2007. World Register of Dams, Update. International Commision on Large Dams, Paris.

  • Kamykowska M., Kaszowski L., Krzemień K., 1999. River channel mapping instruction. Key to the river bed description. Prace Geograficzne UJ 104: 9-25.

  • Kellerhals R., 1982. Effect of river regulation on channel stability. In: Hey R.D., Bathurst J.C., Thorne C.R. (eds), Gravel-bed Rivers. Wiley, Chichester: 685-715.

  • Klimek K., Łajczak A., Zawilińska L., 1990. Sedimentary environment of the modern Dunajec delta in artifical Lake Rożnów, Carpathian Mts., Poland. Quaestiones Geographicae 11/12: 81-92.

  • Książek L., 2006. Morfologia koryta rzeki Skawy w zasięgu cofki zbiornika Świnna Poręba (The morphology of the Skawa River bed within back-water reach of Świnna Poręba Reservoir). Infrastruktura i Ekologia Terenów Wiejskich 4/1: 249-267.

  • Kummu M., Lu X.X., Wang J.J., Varis O., 2010. Basin-wide sediment trapping efficiency of emerging reservoirs along the Mekong. Geomoporphology 119: 181-19. DOI: 10.1016/j.geomorph.2010.03.018. [Crossref]

  • Lane E.W., 1955. The Importance of Fluvial Morphology in Hydraulic Engineering. American Society of Civil Engineer, Proceedings, 81. Paper 745: 1-17.

  • Leopold L.B., Bull W.B., 1979. Base level, aggradation and grade. American Philosophical Society, 123: 168-202.

  • Leopold L.B., Wolman M.G., Miller J.P., 1964. Fluvial Processes in Geomorphology. W.H. Freeman, San Francisco.

  • Lu Y., Zuo L., Ji R., Liu H., 2010. Deposition and erosion in the fluctuating backwater reach of the Three Gorges Project after upstream reservoir adjustment. International Journal of Sediment Research 25: 64-80. DOI:10.1016/S1001-6279(10)60028-5. [Web of Science] [Crossref]

  • Lusby G.C., Hadley R.F., 1967. Deposition behind low dams and barriers in the South-western United States. Journal of Hydrology (NZ) 6: 89-105.

  • Maddock T. Jr., 1966. Behavior of channel upstream from reservoirs. IAHS Publication 77: 812-823.

  • Petts G.E., 1979. Complex response of river channel morphology subsequent to reservoir construction. Progress in Physical Geography 3: 329-362. DOI: 10.1177/030913337900300302. [Crossref]

  • Petts G.E., 1980. Long-term consequences of upstream impoundment. Environmental Conservation 7: 325-332. DOI: 10.1017/S0376892900008183. [Crossref]

  • Petts G.E., Gurnell A.M., 2005. Dams and geomorphology: Research progress and future directions. Geomorphology 71: 27-47. DOI: 10.1016/j.geomorph.2004.02.015. [Crossref]

  • Phillips J.D., 2013. Geomorphic responses to changes in stream flows: the flow-channel fitness model. River Research and Applications 29: 1175-1194. DOI: 10.1002/ rra.2602. [Web of Science] [Crossref]

  • Pollock M.M., Beechie T.J., Jordan C.J., 2007. Geomorphic changes upstream of beaver dams in Bridge Creek, an incised stream channel in the interior Columbia River basin, eastern Oregon. Earth Surface Processes and Landforms 32: 1174-1185. DOI: 10.1002/esp.1553. [Crossref] [Web of Science]

  • Schumm S.A., 2005. River Variability and Complexity. Cambridge, New York.

  • Van Haveren, B.P., Jackson, W.L., Lusby, G.C., 1987. Sediment deposition behind Sheep Creek Barrier Dam, Southern Utah. Journal of Hydrology (NZ) 26: 185-196.

  • Werrity A., 1997. Short-term changes in channel stability. In: C.R. Thorne, R.D. Hey, M.D. Newson (eds), Applied Fluvial Geomorphology for River Engineering and Management, John Wiley, Chichester: 47-65.

  • Williams G.P., Wolman M.G., 1984. Downstream effects of dams on alluvial rivers. Geological Survey Professional Paper 1286: 1-83.

  • Xu J., 1990. Complex response in adjustment of Weihe channel to the construction of the Sanmenxia Reservoir. Zeitschrift für Geomorphologie 34: 233-245.

  • Xu J., 2001a. Adjustment of mainstream-tributary relation upstream from a reservoir: An example from the Laohahe River, China. Zeitschrift für Geomorphologie 45: 359-372.

  • Xu J., 2001b. Modified conceptual model for predicting the tendency of alluvial channel adjustment induced by human activities. Chinese Science Bulletin 46: 51-56. DOI:10.1007/BF03187236. [Crossref]

  • Xu J., Shi C., 1997. The river channel pattern changes as influenced by the floodplain geoecosystem: an example from the Hongshan Reservoir. Zeitschrift für Geomorphologie 41: 97-113.

About the article

Published Online: 2014-03-27

Published in Print: 2014-03-01



Citation Information: Quaestiones Geographicae, ISSN (Print) 0137-477X, DOI: https://doi.org/10.2478/quageo-2014-0007. Export Citation

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