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Prediction of Maximum General Scour Depth during a Flood for Intermittent Rivers

机译:断断续续的河流洪水时最大冲刷深度的预测

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Most rivers in Taiwan are intermittent rivers. A short-term general scour usually occurs in the river during the risingrnlimb of a flood due to the transitory sediment imbalance and the steep slope gradient (Lu et al., 2008). However, duringrnthe recession limb the entrained sediment particles tend to deposit on the riverbed to nearly the initial mean bed levelrnbefore the flood if the river is in quasi-equilibrium condition over the long term. This type of short-term general scourrnhas caused many casualties in Taiwan such as bridge and embankment failures, e.g. the Houfeng Bridge failure inrnDajia River (Typhoon Sinlaku, peak flow Qp= 4,225 m3/s, 2008) and the Shuangyuan Bridge failure in Gaoping Riverrn(Typhoon Morakot, Qp= 27,360 m3/s, 2009). In this study, the maximum general scour depths of the floods werernmeasured using the “numbered brick column” technique for both gravel-bed and sand-bed rivers. A maximum generalrnscour depth of 4.5 m was measured near the river reach of Highway Bridge hydrological station (D50 = 96 mm, S0 =rn1/90) in Dajia River, which was caused by a flood induced by Typhoon Sinlaku with a corresponding peak scoured flowrndepth of 7.73 m. The experimental results indicate that the short-term general scour for the gravel-bed intermittentrnrivers is usually very significant and cannot be neglected as it is one of the most important factors causing the bridgernfailure (Lu et al., 2007). Based on the data collected in the Dajia River and Choshui River, a general scour formula wasrntentatively developed with consideration of both the flow and sediment characteristics to predict the peak scoured flowrndepth. It was found that the proposed equation gave better predictions as compared with the Blench’s (1969) formula.rnIn conjunction with the real-time ultrasonic water level gauge, the formula can be used as an efficient tool for thernbridge closure or emergency evacuation purposes.
机译:台湾的大部分河流都是断断续续的河流。由于短暂的沉积物失衡和陡峭的坡度,洪水泛滥期间河道通常会发生短期的冲刷(Lu等,2008)。但是,在衰退时期,如果河流长期处于准平衡状态,则夹带的沉积物颗粒倾向于沉积在河床附近,接近洪水之前的初始平均水位。这种短期的一般性袭击在台湾造成了许多人员伤亡,例如桥梁和路堤倒塌等。达家河后凤大桥的破坏(台风神乐,峰值流量Qp = 4,225 m3 / s,2008)和高坪河双源大桥的破坏(台风莫拉克特,Qp = 27,360 m3 / s,2009)。在这项研究中,对于砾石床和沙床河,使用“编号砖柱”技术测量了洪水的最大冲刷深度。在大加河公路大桥水文站附近河段(D50 = 96 mm,S0 = rn1 / 90)处测得的最大一般深度为4.5 m,这是由辛拉库台风引发的洪水和相应的峰值冲刷水深引起的。的7.73 m。实验结果表明,砾石层断续河道的短期总体冲刷通常非常显着,并且不能忽略,因为它是造成桥梁破坏的最重要因素之一(Lu等,2007)。根据在大家河和Cho水河收集的数据,在考虑流量和泥沙特性的基础上,拟定了通用冲刷公式,以预测冲刷峰值。结果发现,与Blench(1969)公式相比,该公式具有更好的预测效果。rn与实时超声波水位计结合使用,该公式可作为有效的工具用于桥梁封闭或紧急疏散。

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    Dept. of Civil Eng., Natl. Chung Hsing Univ.250 Kuo-Kuang Rd., Taichung, Taiwan 402, R.O.C. - E-mail: jylu@mail.nchu.edu.tw;

    Dept. of Civil Eng., Natl. Chung Hsing Univ.250 Kuo-Kuang Rd., Taichung, Taiwan 402, R.O.C. - E-mail: ccsu@nchu.edu.tw;

    School of Civil and Environmental Eng.Nangyang Technological Univ., Singapore - E-mail: jhhong@ntu.edu.sg;

    Natl. Chung Hsing Univ.250 Kuo-Kuang Rd., Taichung, Taiwan 402, R.O.C. - E-mail: yellow70053@hotmail.com;

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