Usage of an empirical equation for determination of mean sediment diameter in beds of small mountain rivers

• Autorzy: Lenar-Matyas A. , Wolak A.

Identyfikatory

DOI

10.14597/infraeco.2017.4.2.115

• Języki publikacji: EN

Abstrakty

EN

Knowledge of properties of materials deposited in beds of small reservoirs is important, as it can be used for a range of analytic works, concerning river rehabilitation and river management and other similar undertakings. Usually the one property - the d₅₀ value can be obtained using in-situ measurements using sieves but in most cases of preliminary, large scale research may not be feasible. In this paper the Osuch empirical formula for determination of standard sediment grain sizes of d₅₀ is presented. Besides the original formula an improved method of assessing of the slope value for that formula is proposed, which may greatly improve the usefulness of the original, unmodified method. The calculation results are then compared with the in-situ measurements done on many samples taken from the Trzebuńka dam reservoir. The dam was recently partially removed and partially rebuilt, so there was an unique and easy access to wide strata of different layers of sediments, accumulated across many years of dam operation in the exposed bed of partially emptied reservoir. Additionally, the Ratomski formula for riverbed slope determination near dams was used as a reference. The mentioned methods taken together can be used for preliminary analysis before significant works are to be done. The results are quite encouraging and can be a starting point for further method refinement.

Słowa kluczowe

EN

mean sediment diameter; empirical formula; check dam

• Wydawca: Stowarzyszenie Infrastruktura i Ekologia Terenów Wiejskich
• Czasopismo: Infrastruktura i Ekologia Terenów Wiejskich
• Rocznik: 2017
• Tom: nr IV/2
• Strony: 1513--1527
• Opis fizyczny: Bibliogr. 11 poz., rys., tab., zdj.

Twórcy

autor

Lenar-Matyas A.

• Krakow University of Technology Institute of Engineering and Water Management ul. Warszawska 24, 31-155 Kraków, Poland

autor

Wolak A.

• Krakow University of Technology Institute of Engineering and Water Management ul. Warszawska 24, 31-155 Kraków, Poland

Bibliografia

• Ashley J. T. F., Bushaw-Newton K., Wilhelm M., Boettner A., Drames G.& Velinsky D. J., (2006). The effects of small dam removal on the distribution of sedimentary contaminants. Environmental Monitoring and Assessment 114: 287-312.
• Brandt S. A. (2000). Classification of geomorphological effects downstream of dams. Catena, 40(4), 375-401.
• Ferrer-Boix C., Martín-Vide J.P., Parker G., (2014) Channel evolution after dam removal in a poorly sorted sediment mixture: experiments and numerical model. Water Resour. Res., 50 (2014).
• Evans J.E., Huxley J.M. and 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.
• Magilligan, F. J., Nislow, K. H. (2005). Changes in hydrologic regime by dams. Geomorphology, 71(1), 61-78.
• Marren, P. M., Grove, J. R., Webb, J. A., & Stewardson, M. J. (2014). The potential for dams to impact lowland meandering river floodplain geomorphology. The Scientific World Journal, 2014.
• Osuch B. (1964). Skład granulometryczny niespoistego materiału skalnego cieków karpackich w świetle potrzeb budownictwa [Grain size distrubution of coarse rocky soils of Carpathian river, used for building purposes], praca doktorska - Kraków, Politechnika Krakowska (In Polish)
• Ratomski J. (1991). Sedymentacja rumowiska w zbiornikach przeciwrumowiskowych na obszarze Karpat fliszowych [Accumulation of sediments in reservoirs of check dams in Caparhian flysh area]; Politechnika Krakowska, Monografia, 123: 1-131. (In Polish)
• Wildman L. A., and MacBroom J. G. (2005), The evolution of gravel bed channels after dam removal: Case study of the Anaconda and Union City dam removals, Geomorphology, 71(1172), 245-262.
• Ab Ovo (2011). Tarliska Górnej Raby. Opis techniczny [A technical description] TGRO-R-002-02 (Available on http://www.tarliskagornejraby.pl/ download.php?view.11) (In Polish)
• PKN-CEN ISO/TS 17892-4, Oznaczenie składu granulometrycznego [Determination of grain size composition] (In Polish)

Uwagi

Opracowanie rekordu w ramach umowy 509/P-DUN/2018 ze środków MNiSW przeznaczonych na działalność upowszechniającą naukę (2018).