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Study on Flow Fields of Boundary-Layer Separation and Hydraulic Jump during Rundown Motion of Shoaling Solitary Wave
Vise andre og tillknytning
2015 (engelsk)Inngår i: Journal of Earthquake and Tsunami, ISSN 1793-7116, Vol. 9, nr 5Artikkel i tidsskrift (Fagfellevurdert) Published
Abstract [en]

The characteristics of flow fields for a complete evolution of the non-breaking solitary wave, having a wave-height to water-depth ratio of 0.363 and propagating over a 1:5 sloping bottom, are investigated experimentally. This study mainly focuses on the occurrences of both flow separation on the boundary layer under an adverse pressure gradient and subsequent hydraulic jump with the abrupt rising of free surface during run-down motion of the shoaling wave, together with emphasis on the evolution of vortex structures underlying the separated shear layer and hydraulic jump. A flow visualization technique with particle trajectory method and a high-speed particle image velocimetry (HSPIV) system with a high-speed digital camera were used. Based on the instantaneous flow images visualized and/or the ensemble-averaged velocity fields measured, the following interesting features, which are unknown up to date, are presented and discussed in this study: (1) Flow bifurcation occurring on both offshore and onshore sides of the explicit demarcation curve and the stagnation point during run-up motion; (2) The dependence of the diffuser-like flow field, being changed from the supercritical flow in the shallower region to the subcritical flow in the deeper counterpart, on the Froude number during the early and middle stages of run-down motion; (3) The positions and times for the occurrences of the incipient flow separation and the sudden rising of free surface of the hydraulic jump; (4) The associated movement and evolution of vortex structures under the separated shear layer, the hydraulic jump and/or the high-speed external main stream of the retreated flow; and (5) The entrainment of air bubbles from the free surface into the external main stream of the retreated flow.

sted, utgiver, år, opplag, sider
World Scientific, 2015. Vol. 9, nr 5
Emneord [en]
Earthquake, Tsunami, Shoaling Solitary Wave
HSV kategori
Identifikatorer
URN: urn:nbn:se:kth:diva-179744DOI: 10.1142/S1793431115400023ISI: 000369868000003Scopus ID: 2-s2.0-84952715787OAI: oai:DiVA.org:kth-179744DiVA, id: diva2:889210
Merknad

QC 20160104. QC 20160318

Tilgjengelig fra: 2015-12-22 Laget: 2015-12-22 Sist oppdatert: 2016-03-18bibliografisk kontrollert

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