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  • Auel, C. (26)
  • Boes, R.M. (23)
  • Albayrak, I. (13)
  • Sumi, T. (6)
  • Hagemann, M. (4)
  • Albaryak, I. (3)
  • Boes, R. (3)
  • Müller-Hagemann, M. (2)
  • Thene, J.R. (2)
  • Berchthold, T. (1)
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Bedload transport and hydro-abrasive erosion at steep bedrock rivers and hydraulic structures (2018)
Müller-Hagemann, M. ; Auel, C. ; Albaryak, I. ; Boes, R.M.
Rehabilitation of the Mud Mountain bypass tunnel invert (2018)
Auel, C. ; Thene, J.R. ; Carroll, J. ; Holmes, C. ; Boes, R.M.
This paper describes the design of the new tunnel invert lining of the 9-foot tunnel at Mud Mountain Dam, Washington, USA. The tunnel diverts all bed load sediments into the tailwater. Major invert abrasion has been observed in the existing steel lining. The new invert design consists of 0.59 m2 and 0.79 m2 granite blocks that are 0.25 m thick and placed tightly together along the tunnel. Stability analysis showed factors of safety ranging from 1.2 to 2.6 against uplift. This will be achieved with strip drains placed in the bedding material along the tunnel. A service-design-life analysis was performed using abrasion prediction modelling. This model was based on abrasion measurement data acquired from granite field tests at Pfaffensprung sediment bypass tunnel, Switzerland. The estimated annual abrasion depths for the granite were approximately 0.50 mm/year for average sediment transport conditions.
Laborversuche über die Partikelbewegung in schiessendem Abfluss (Laboratory experiments on particle motion in supercritical flows) (2014)
Auel, C. ; Albayrak, I. ; Boes, R.M.
Supercritical flow in sediment bypass tunnels (2013)
Albayrak, I. ; Auel, C. ; Boes, R.M.
This paper deals with an experimental investigation of the mean and turbulence characteristics of supercritical quasi-uniform and gradually varied open-channel flows over a transitional rough bed. These conditions are typical for sediment bypass tunnels. The results show that the log-law holds well in the inner region across the channel. The roughness shifts the velocity profiles downward by an amount of ΔU+. The velocity-dip phenomenon and strong secondary currents exist in the channel for narrow open-channel flow. These currents cause the Reynolds shear stress distributions to deviate from the linear distribution and an undulation on the transversal distribution of the bed shear stress, which matches with the bed abrasion pattern. The streamwise turbulence intensity profiles deviate from the semi-empirical universal function whereas the vertical turbulence intensity profiles fit well with it only at the centerline of the channel. A strong wall effect exists on the turbulence intensities in the outer region.
Sediment transport in high-speed flows over a fixed bed. 1: Particle dynamics (2017)
Auel, C. ; Albayrak, I. ; Sumi, T. ; Boes, R.M.
Particle dynamics are investigated experimentally in supercritical high-speed open channel flow over a fixed planar bed of low relative roughness height simulating flows in high-gradient non-alluvial mountain streams and hydraulic structures. Non-dimensional equations were developed for transport mode, particle velocity, hop length and hop height accounting for a wide range of literature data encompassing sub- and supercritical flow conditions as well as planar and alluvial bed configurations. Particles were dominantly transported in saltation and particle trajectories on planar beds were rather flat and long compared with alluvial bed data due to (1) increased lift forces by spinning motion, (2) strongly downward directed secondary currents, and (3) a planar flume bed where variation in particle reflection and damping effects were minor. The analysis of particle saltation trajectories revealed that the rising and falling limbs were almost symmetrical contradicting alluvial bed data. Furthermore, no or negligible effect of particle size and shape on particle dynamics were found. Implications of experimental findings for mechanistic saltation-abrasion models are briefly discussed.
Sedimentumleitstollen – eine nachhaltige Maßnahme gegen Stauraumverlandung (2017)
Auel, C. ; Boes, R.
Design and construction of the sediment bypass tunnel at Solis (2011)
Auel, C. ; Boes, R. ; Ziegler, T. ; Oertli, C.
Entlandung des Stausees Solis mittels Geschiebeumleitstollen (2010)
Auel, C. ; Berchthold, T. ; Boes, R.
Reviewing research and experience on sediment bypass tunnels (2016)
Hagemann, M. ; Albayrak, I. ; Boes, R.M. ; Auel, C. ; Sumi, T.
Hydroabrasion in Sedimentumleitstollen (2012)
Hagemann, M. ; Auel, C. ; Albayrak, I. ; Boes, R.M.
Sedimentumleitstollen leiten die sedimentreichen Hochwasserspitzen um die Tal-sperre herum in den Unterlauf des Flusses und verhindern so eine fortschreitende Verlandung des Stauraums. Aufgrund der hohen Fließgeschwindigkeiten und gro-ßen Sedimentfrachten in Umleitstollen weisen diese starke Verschleißerscheinun-gen auf, die zu hohen Unterhaltskosten führen. Es gibt verschiedene Konzepte um diesem Problem entgegen zu wirken. Einerseits kann der Umleitstollen hydrau-lisch optimiert werden, um die Belastung auf die Sohle zu minimieren. Auf der anderen Seite kann der Widerstand der Stollensohle verbessert werden. An der Versuchsanstalt für Wasserbau, Hydrologie und Glaziologie (VAW) der ETH Zü-rich werden zur Zeit zwei Forschungsarbeiten durchgeführt, die sich diesen zwei Aspekten widmen. In großskaligen Laborversuchen erfolgt eine systematische Untersuchung und Optimierung der maßgebenden Parameter wie Fortbewegungs-art des Sediments und Abrasionstiefe der Stollensohle. Anhand von Prototypver-suchen im neu errichteten Sedimentumleitstollen Solis in Graubünden (Schweiz) werden die Zusammenhänge zwischen Beanspruchung, Materialeigenschaften und Abrasion im Prototyp ermittelt. Darauf basierend können Empfehlungen be-züglich Materialwahl, konstruktiver Durchbildung und Dimensionierung abgege-ben und so zu einer nachhaltigen und wirtschaftlichen Wasserbewirtschaftung in Stauseen beigetragen werden.
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