排水设计集中时间估算公式的一种简便方法

A. Yulianur, S. Sugianto, Frystia Mala Puspita
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引用次数: 3

摘要

降雨集中时间是确定排水设计的一个重要方面。在城市排水规划中,特别是雨水渠设计中,设计洪峰流量的确定采用一般合理公式。使用这个平衡公式需要降雨强度,其降雨持续时间等于或大于集中时间。这个浓度时间是用一个估算公式确定的,该公式的形成需要浓度时间的测量数据。本文介绍了如何利用有理线的概念来测量浓度时间,其中峰值流量出现在浓度时间。为了实现本研究的目的,在集水区种植结缕草并进行了降雨模拟器降雨试验。采用陆地流道长度L,分别为50 cm、100 cm、150 cm、200 cm、250 cm 5个变量。土地的坡度S有3种变化,分别是2.8%、5.5%、6%和8.8%。对于L和S的每个变化,实验集水区以固定的降雨强度倾倒,降雨强度为60 mm/h。每隔5分钟测量一次流量。然后,根据流量与时间的关系,得到了合理的水程曲线,并由此推导出了浓度时间Tc。将该Tc值作为实测Tc,利用回归公式形成Tc估计公式。公式为Tc = 3.543 + 1.211 L - 17.119 S,决定系数r2 = 0.98。这些结果表明,用有理线的概念来测定Tc是可以接受的。此公式适用于L和S值大于零的情况,适用于结缕草覆盖的土地。其他类型的土地覆被需要进一步的研究来验证本研究得出的公式。
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A Simple Method to Develop a Formula for Estimating Concentration Time of Drainage Design
Concentration time of rainfall is an important aspect to determine drainage design. A general rational formula is used to determine design flood or peak flow in urban drainage planning, especially for storm sewer design. The use of this balanced formula requires rainfall intensity, whose duration of rain is equal or more than the time of concentration. This time of concentration is determined using an estimation formula whose formation requires measurement data of the time of concentration. This study introduces how to measure the time of concentration using the concept of-rational-hydrograph, in which peak flow occurs at the time of concentration. To fulfill the aim of this research, an experimental of catchment area planted with Zoysia Japonica grass and showered with a rainfall simulator was conducted. The length of the flow path on the land, L, given in 5 variations, namely 50 cm, 100 cm, 150 cm, 200 cm, and 250 cm, was used. The slope of the land, S, is given in 3 variations, namely 2.8 %, 5,6%, and 8.8%. For each variation of L and S, the experimental catchment area was poured with a fixed rainfall intensity, which is 60 mm/hour. The flow was measured every 5 minutes intervals. Then, from the relationship of flow and time, a rational hydrograph was formed, from which the time of concentration, Tc, was deduced. This Tc value was treated as the measured Tc to form the Tc estimation formula using the regression formula. The formula is Tc = 3.543 + 1.211 L – 17.119 S, with the coefficient of determination R 2 = 0.98. These results show that the determination of Tc using the concept of the rational- hydrograph is acceptable. This formula applies to L and S values greater than zero and applies to land covered by Zoysia Japonica grass. Further research is needed for other types of land cover to validate the formula obtained in this research.
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审稿时长
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