2018
DOI: 10.1680/jwama.16.00015
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A one-dimensional flood routing model for rockfill dams considering exit height

Abstract: 2 3To predict the phreatic surface and conduct flood routing of rockfill dams, the flow hydraulics and rating curve need to be simulated. In this research, one-dimensional flow hydraulics through a trapezoidal rockfill dam was modelled via the standard step method. Regarding the non-Darcy flow, the relationship between the hydraulic gradient and the bulk velocity in power form was adopted. Using the exit height as the boundary condition significantly improves the prediction of the phreatic surface. For this pu… Show more

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Cited by 4 publications
(2 citation statements)
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“…Using these structures, the flood is temporarily stored in the reservoir of rockfill dams which then discharges to the downstream at a safe discharge automatically by seepage flows without needs for operational management. Since the body of these types of dams are constructed through the use of the coarse rock particles, the flow through these coarse pores will deviate from Darcy's law and generally be turbulent and the variation of flow velocity (V) with hydraulic gradient (i) will be a non-linear relation (Legrand, 2002;Sarkhosh, Samani, & Mazaheri, 2017). Where the flow in coarse porous media of rockfills is non-Darcian and turbulent, determination of seepage discharge, seepage force, flow net, and outlet discharge requires the use of non-linear relations of gradient hydraulic with flow velocity (Qian, Zhan, Zhao, & Sun, 2005).…”
Section: Introductionmentioning
confidence: 99%
“…Using these structures, the flood is temporarily stored in the reservoir of rockfill dams which then discharges to the downstream at a safe discharge automatically by seepage flows without needs for operational management. Since the body of these types of dams are constructed through the use of the coarse rock particles, the flow through these coarse pores will deviate from Darcy's law and generally be turbulent and the variation of flow velocity (V) with hydraulic gradient (i) will be a non-linear relation (Legrand, 2002;Sarkhosh, Samani, & Mazaheri, 2017). Where the flow in coarse porous media of rockfills is non-Darcian and turbulent, determination of seepage discharge, seepage force, flow net, and outlet discharge requires the use of non-linear relations of gradient hydraulic with flow velocity (Qian, Zhan, Zhao, & Sun, 2005).…”
Section: Introductionmentioning
confidence: 99%
“…Finally, Sarkhosh et al (2018) present an attempt of onedimensional hydraulic modelling of the flow through a rockfill dam, considering non-standard boundary conditions and building upon earlier work by Hansen et al (2005).…”
mentioning
confidence: 99%