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The influence of aquatic buffer characteristic of Ciliwung River from the Katulampa Weir to Manggarai Water Gate on hydrograph characteristics of design flood

机译:卡图兰帕堰至芒加莱水闸的慈里翁河水体缓冲特征对设计洪水水文特征的影响。

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Increasing population in Jakarta leads to increased needs of settlements and their supporting facilities. To compensate, various methods are being undertaken, from utilization of open area to the riparian, especially in the Ciliwung River. This utilization results in the loss of riparian natural ability, which changes the river’s hydraulic condition. These riparian changes will significantly affect the roughness coefficient. The roughness coefficient is a value that is affected by channel irregularity, variation of cross-section, effects of obstructions, vegetation, and degree of meandering. Changes of the roughness coefficient will influence the velocity of the stream. The purpose of this research is to determine the effect of riparian characteristics to the roughness coefficient that affects the stream velocity, which has impact on the peak time of the hydrograph. The peak time shift can be seen in the flood hydrograph characteristics of the Ciliwung River from the Katulampa Weir to the Manggarai sluice gate. Identification of Ciliwung riparian conditions at that segment is conducted by river routing. HEC-RAS 4.1.0 [1] application is used to obtain a design flood hydrograph at Manggarai Water Gate. To know the influence of riparian characteristics to roughness coefficient, HEC-RAS 4.1.0 simulation is done using existing and natural condition to compare the hydrographs between those two conditions. It obtains a lower peak discharge and extended duration of the hydrograph.
机译:雅加达人口的增加导致定居点及其配套设施的需求增加。为了补偿,从开放区域到河岸,尤其是在七里翁河中,采取了各种方法。这种利用会导致河岸自然能力的丧失,从而改变河流的水力状况。这些河岸变化将显着影响粗糙度系数。粗糙度系数是受通道不规则性,横截面变化,障碍物,植被和曲折度影响的值。粗糙度系数的变化将影响流的速度。这项研究的目的是确定河岸特征对影响河流流速的粗糙度系数的影响,粗糙度系数影响水文图的峰值时间。从卡图兰帕堰到曼加赖水闸的七里翁河洪水水文特征可以看出高峰时移。在该路段的Ciliwung河岸条件的确定是通过河道进行的。 HEC-RAS 4.1.0 [1]应用程序用于在Manggarai水闸获得设计洪水水位图。为了了解河岸特征对粗糙度系数的影响,使用现有条件和自然条件进行了HEC-RAS 4.1.0仿真,以比较这两种条件之间的水位图。它获得了较低的峰值流量和更长的水文持续时间。

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