Laboratory analysis of incipient motion velocity for non-uniform non-cohesive sediments movement in rectangular flumes
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  • 作者:Najafi-mood Mohammad Hossein ; Khozeymehnezhad Hossein…
  • 关键词:Incipient motion velocity ; Non ; uniform non ; cohesive sediment ; Slope ; Rectangular flume
  • 刊名:Arabian Journal of Geosciences
  • 出版年:2016
  • 出版时间:January 2016
  • 年:2016
  • 卷:9
  • 期:1
  • 全文大小:984 KB
  • 参考文献:Agudo JR, Dasilva S, Wierschem A (2014) How do neighbors affect incipient particle motion in laminar shear flow. Phys Fluids 26:053303CrossRef
    Bravo R, Ortiz P, Perez-Aparicio JL (2014) Incipient sediment transport for non-cohesive landforms by the discrete element method (dem). Appl Math Model 38(4):1326鈥?337CrossRef
    Egiazaroff IV (1965) Calculation of nonuniform sediment concentrations. J Hydraulic Div 91(4):225鈥?47
    Govers G (1987) Initiation of motion in overland flow, Sedimentology, No. 34., pp 1157鈥?164
    Gessler, J. 1965. The beginning of bed load movement of mixture investigated as natural armoring in channels, W.M. Kech laboratory of hydraulic and water resource, California instate of technology, Pasadena.
    Hrissanthou V, Hartmann S (1998) Measurement of critical shear stress in sewer. J Water Res 32(7):2035鈥?040CrossRef
    Hjulstorm F (1935) The morphological activity of rivers as illustrated by River Fyris, Bulletin of the geological institute, Uppsala, vol. 25, chap. 3
    Jahanshahi M, Sabeti E, Ghomeshi M (2011) Investigation of incipient motion based on fall velocity of particles. Second National Conference on Integrated Water Resources Management, Kerman. Shahid Bahonar University of Kerman. Irrigation and Water Engineering. (In Persian)
    Khozeymehnezhad H, Shafai Bejestan M (2010) Sediment particles incipient motion criteria at closed box conduits. J Irrig Eng (JISE) 33(2):51鈥?1 (In Persian)
    Khozeymehnezhad H, Shafai Bejestan M (2011) Study of the conditions of incipient motion of non cohesive sediment in open channel flow with rectangular section and milled slop. Irrigation and water engineering, scientific research journal. Vol 1. No 2. pp: 13鈥?3. (In Persian)
    Mantz P (1975) Low transport stages by water streams of fine, cohesion less granular and flaky sediments. University of London, London, Ph.D. dissertation
    Michalik, A. 1990, Bed-load transport investigations in some Polish Carpathians rivers, (in Polish). Zesz. Nauk. AR Krakow seria Rozpr. Hab., 138, 115.
    Nazari A, Heydari MM (2010) Incipient motion of uniform sediment. Eighth Conference of Hydraulic of Iran. Iranian Hydraulic Association, Faculty of Engineering, Tehran University, Tehran (In Persian)
    Rasooliyanfar P, Afzalimehr H (2007) The effect of components of turbulent flow on incipient motion of sediment, the Seventh International Seminar on River Engineering. Khuzestan Water and Power Authority, Shahid Chamran University of Ahvaz, Ahvaz (In Persian)
    Safari, M. J. S. Mohamadi, M. A. Manafpour, M. 2012. Incipient motion of sediment in channels with constant wall and V cross section. Tenth Conference of Hydraulic of Iran, Rasht, Iran hydraulic Association, University of Guilan. (In Persian)
    Shafai Bejestan, M. 2009. Basic theory and practice of Hydraulic of sediment transport. Shahid Chamran University. Second edition. (In Persian)
    Shields A (1936) Application of similarity principles, and turbulence research to bed load movement. California institute of technology, Pasadena (translated from German)
    Wan Mohtar WHM (2015) Threshold criteria for incipient grain motion with turbulent fluctuations on a horizontal bed. Sains Malaysiana 44(1):147鈥?53CrossRef
    Wang T, Liu X, Nie R, Huang E (2010) Comparative study on the incipient motion conditions of non-uniform non-cohesive sediment. J Hydroelectric Eng 29(6):126鈥?31
    Yalin MS, Karahan E (1979) Inception of sediment transport. J Hydraulic Div 105:1433鈥?443
  • 作者单位:Najafi-mood Mohammad Hossein (1)
    Khozeymehnezhad Hossein (1)
    Mazloom-shahraki Rasoul (2)

    1. University of Birjand, Birjand, Iran
    2. Irrigation and Drainage of University of Birjand, Birjand, Iran
  • 刊物类别:Earth and Environmental Science
  • 出版者:Springer Berlin Heidelberg
  • ISSN:1866-7538
文摘
The moment when sediment particles start to move is known as incipient motion of sediments. Many studies have been conducted to determine the incipient motion velocity of uniform non-cohesive sediments across open channels with a positive slope, and some equations and diagrams have been proposed in this regard; however, studies carried out on the non-uniform non-cohesive sediments, especially with the reverse slope, are very few. In this study, a lab flume and the dimensional analysis were used to analyze the inception motion condition of non-uniform non-cohesive sediments. In this study, a number of nine samples of non-uniform non-cohesive sediments with different sizes and uniformity coefficients were analyzed through three positive slopes 0.0005, 0.001, and 0.002 and also through three reverse slopes 0.0005, 0.001, and 0.002. The results indicated that particle stability is decreased with increasing the positive slope, whereas it is increased with increasing the reverse slope. The results also showed that particle鈥檚 stability is decreased with increasing the particle size, whereas it is increased with increasing the uniformity coefficient of sediments. Keywords Incipient motion velocity Non-uniform non-cohesive sediment Slope Rectangular flume

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