TY - GEN
T1 - Discussion of the impact of pressure fluctuations on local scouring
AU - Schanderl, W.
AU - Manhart, M.
AU - Link, O.
N1 - Publisher Copyright:
© 2017 Taylor & Francis Group, London.
PY - 2017
Y1 - 2017
N2 - We aim at discussing the potential impact of pressure fluctuations on the local scour process around a bridge pier by estimating the force FB acting on the sediment layer due to these fluctuations. To do so, we apply highly resolved large-eddy simulations of the flow around a wall-mounted cylinder at three moderate Reynolds numbers. To provide the required grid resolution in the region of interest around the cylinder, the grid is refined by locally embedded grids. Instantaneous fluctuations of the pressure coefficient Cp are up to two orders of magnitudes larger than the friction coefficient Cf in significant regions around the cylinder. Furthermore, regions of low pressure are located in close vicinity to regions of high pressure, which implies strong pressure gradients and fluctuations in time. Pressure gradients in the fluid phase induce velocity fields in the sediment layer. We estimate the time scales by which such a velocity field reaches quasi-steady conditions and the resulting volume forces on the sediment. Furthermore, we discuss a practical experimental setup of the flow around a bridge pier. For the assumptions made in this study, the estimated forces due to pressure gradients cannot overcome the gravity force acting on a sediment grain. Nevertheless, the estimated forces are of the same order of magnitude than forces stabilizing the sediment layer and should be taken into account in future models of scour evolution.
AB - We aim at discussing the potential impact of pressure fluctuations on the local scour process around a bridge pier by estimating the force FB acting on the sediment layer due to these fluctuations. To do so, we apply highly resolved large-eddy simulations of the flow around a wall-mounted cylinder at three moderate Reynolds numbers. To provide the required grid resolution in the region of interest around the cylinder, the grid is refined by locally embedded grids. Instantaneous fluctuations of the pressure coefficient Cp are up to two orders of magnitudes larger than the friction coefficient Cf in significant regions around the cylinder. Furthermore, regions of low pressure are located in close vicinity to regions of high pressure, which implies strong pressure gradients and fluctuations in time. Pressure gradients in the fluid phase induce velocity fields in the sediment layer. We estimate the time scales by which such a velocity field reaches quasi-steady conditions and the resulting volume forces on the sediment. Furthermore, we discuss a practical experimental setup of the flow around a bridge pier. For the assumptions made in this study, the estimated forces due to pressure gradients cannot overcome the gravity force acting on a sediment grain. Nevertheless, the estimated forces are of the same order of magnitude than forces stabilizing the sediment layer and should be taken into account in future models of scour evolution.
UR - http://www.scopus.com/inward/record.url?scp=85016546841&partnerID=8YFLogxK
M3 - Conference contribution
AN - SCOPUS:85016546841
SN - 9781138029453
T3 - River Sedimentation - Proceedings of the 13th International Symposium on River Sedimentation, ISRS 2016
SP - 394
EP - 401
BT - River Sedimentation - Proceedings of the 13th International Symposium on River Sedimentation, ISRS 2016
A2 - Wieprecht, Silke
A2 - Haun, Stefan
A2 - Weber, Karolin
A2 - Noack, Markus
A2 - Terheiden, Kristina
PB - CRC Press/Balkema
T2 - 13th International Symposium on River Sedimentation, ISRS 2016
Y2 - 19 September 2016 through 22 September 2016
ER -