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Study on generation mechanism of vertical force peak values on T-girder attacked by tsunami bore

机译:海啸冲击作用下T形梁竖向力峰值的产生机理研究

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The generation mechanism and characteristics of peak values of tsunami bore vertical force are investigated comprehensively and thoroughly. A scaled down two-dimensional T-girder model, whose surface is divided into a series of panels, is tested in the cases with fixed initial downstream water depth, different incoming wave height and different initial clearance. Time history of vertical force is divided into four stages, in which the impinging stage is further divided into four sub-stages. Then the contribution rates of panels to the vertical force are discussed. Results show each peak value of vertical force in the impinging stage is composed of at least one peak value of vertical force on bottom panels of the girder, the continue increase of vertical force peak value is the result of more and more panels suffering static pressure of entrapped air when the chambers are successively dosed by tsunami bore. The vertical force peak values on top panels of the chambers are mainly generated by the static pressure peak values of entrapped air. The entrapped air decreases the vertical velocity of tsunami bore under already closed chambers, resulting the simultaneous occurrences of pressure peaks of entrapped air in previous closed chambers.
机译:全面深入地研究了海啸孔垂直力峰值的产生机理和特征。在固定的初始下游水深,不同的入射波高和不同的初始净空的情况下,对按比例缩小的二维T型梁模型进行了测试,该模型的表面分为一系列面板。垂直力的时程分为四个阶段,其中撞击阶段又分为四个子阶段。然后讨论了面板对垂直力的贡献率。结果表明,在冲击阶段,垂直力的每个峰值都是由大梁底板上至少一个垂直力的峰值组成的,垂直力峰值的持续增加是越来越多的面板承受静压力的结果。当腔室被海啸钻孔连续注入时,空气被夹带。腔室顶部板上的垂直力峰值主要由残留空气的静压峰值产生。夹带的空气降低了已经关闭的密闭腔室中海啸孔的垂直速度,导致在先前的密闭腔室中同时出现夹带的空气压力峰值。

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