Estimation of Conversion Coefficient for the Surface Velocity of Irrigation Channel

Jin Young Kang, Da Ye Kim, Bae Jung Yong, Jin Maeng Seung, A. Muhammad
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Abstract

The continuous flow velocity monitoring has become a difficult and expensive task in hydrological survey due to unpredictable rainfall patterns. Therefore, the velocity measurements using a non-contact type flowmeter is more effective and easy to use. The generally used average velocity conversion factor 0.85 does not take into account the regional characteristics such as curves of a river, bed materials which consequentially affects the vertical flow characteristics. Therefore, considering the those characteristics of irrigation channels of two small reservoirs (Ssangam and Hangye reservoir), results showed that the gentle bed slope of irrigation channel of the Ssangam reservoir, has a velocity conversion factor of 1.06 and the depth-averaged velocity of V0.6, was measured to be higher compared to the surface velocity. On the other hand, velocity conversion factor of 0.83 was computed in case of Hangye reservoir with a relatively sharp bed slope, which is similar to the generally used velocity conversion factor of 0.85. This shows that the bed slope is the dominant factor in affecting the depth-wise velocity characteristics of a waterway.
灌溉渠道表面流速转换系数的估算
由于降雨模式难以预测,连续流速监测已成为水文勘测中一项既困难又昂贵的任务。因此,使用非接触式流量计进行流速测量更为有效和方便。一般使用的平均流速换算系数 0.85 没有考虑到河流的曲线、河床材料等区域特征,而这些特征会对垂直流特征产生影响。因此,考虑到两座小型水库(双岩水库和坑叶水库)灌溉渠道的特点,结果表明双岩水库灌溉渠道的河床坡度较缓,流速换算系数为 1.06,测得的深度平均流速 V0.6 比地表流速高。另一方面,杭冶水库的河床坡度较大,计算出的速度换算系数为 0.83,与一般使用的速度换算系数 0.85 相似。这表明,河床坡度是影响水道深度速度特征的主要因素。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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