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    請使用永久網址來引用或連結此文件: https://ir.lib.ncu.edu.tw/handle/987654321/102436


    題名: Study on Flow Fields of Boundary-Layer Separation and Hydraulic Jump during Rundown Motion of Shoaling Solitary Wave
    作者: 吳祚任;Lin, Chang;Kao, Ming-Jer;Tzeng, Guang-Wei;Wong, Wei-Ying;Yang, James;Raikar, Rajkumar V.;Wu, Tso-Ren;Liu, Philip Li-Fang
    貢獻者: 地球科學學院水文與海洋科學研究所
    關鍵詞: Aerodynamics;Air bubbles;Air entrainment;Bifurcations;Boundary layers;Dependence;Diffusers;Digital cameras;Digital imaging;Earthquake;Entrainment;Evolution;Fields;Flow separation;Flow visualization;Fluid flow;Free surfaces;Froude number;High speed;Hydraulic jump;Hydraulics;Mountains;Movement;Offshore;Particle image velocimetry;Particle trajectories;Pressure gradients;Rapid flow;Rivers;Separation;Shear;Shoaling;Shoaling Solitary Wave;Shoaling waves;Solitary waves;Stagnation point;Subcritical flow;Supercritical flow;Tranquil flow;Tsunami;Velocity distribution;Velocity measurement;Vortices;Water depth;Wave propagation
    日期: 2015-12-01
    上傳時間: 2026-04-23 11:08:40 (UTC+8)
    出版者: World Scientific Publishing Co. Pte Ltd;Hackensack: World Scientific Pub Co Pte Lt
    摘要: 摘要: 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 rundown 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 runup 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 rundown 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.
    出版者: Hackensack: World Scientific Pub Co Pte Lt
    出版日期: 2015-12
    出處: Journal of Earthquake and Tsunami, 2015-12, Vol.9 (5), p.1
    資源來源: Alma/SFX Local Collection
    版權: 2015, World Scientific Publishing Company
    版權: 2015. World Scientific Publishing Company
    識別號: ISSN: 1793-4311
    識別號: ISSN: 1793-7116
    識別號: EISSN: 1793-7116
    識別號: DOI: 10.1142/s1793431115400023
    顯示於類別:[水文與海洋科學研究所] 期刊論文

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