工业区洪水控制工程

Shofwatul Fadila, Sentot Purboseno
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引用次数: 0

摘要

3月17日,日惹省Wukirsari村的Celeng河发生洪水,成为有史以来发生在Bog河上的最大洪水。洪水是由来自伊莫吉里和德林戈地区山区的大量水流造成的。塞楞河泛滥,淹没了伊莫吉里地区乌基尔萨里村的四个村庄。本研究旨在确定色冷小流域的防洪措施。研究地点位于日惹省Imogiri Wukirsari Kali Celeng子流域,控制点位于Celeng河下游,位于Celeng河和Oyo河的交汇处。水文分析采用Gamma 1单位水文线法计算,周期为10年。各子流域的最大洪流量分别为75.73 m3/s、38.22 m3/s、37.20 m3/s、18.54 m3/s、21.57 m3/s和26.29 m3/s,而Oyo流域的10年复发洪流量为959.60 m3/s。利用HEC-RAS 4.1软件对13.35 km长的色冷河河道进行了水力分析。流场模拟稳定进行。模拟结果表明,在现状模拟过程中,色冷河断面存在几个溢流点。然后用调整到洪水点位置的特定槽尺寸将溢流部分归一化。归一化后的流量模拟结果表明,色冷河大部分河道能够容纳发生的洪流量。对归一化后仍有溢流的路段进行堤防,堤防平均高度为0.75 m。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Upaya Pengendalian Banjir Kawasan Sub-Das Celeng Pra Pembangunan Embung Imogiri
Flood on March 17 in the Celeng River, Wukirsari Village, D.I. Yogyakarta became the biggest flood that ever happened on the Bog River. Floods are caused by heavy flow of water from the hills in the Imogiri and Dlingo areas. The Celeng River overflowed and submerged four hamlets in Wukirsari Village, Imogiri District. This study aims to determine flood control efforts in the Celeng sub-watershed area. The research location is in the Kali Celeng sub-watershed, Wukirsari, Imogiri, D.I. Yogyakarta with the control point located in the lower reaches of the Celeng River right at the confluence of the Celeng River and the Oyo River. The hydrological analysis was calculated using the Gamma 1 unit hydrograph method with a return period of 10 years. The maximum flood discharges for each of the Celeng sub-watersheds are 75.73 m3/s, 38.22 m3/s, 37.20 m3/s, 18.54 m3/s, and 21.57 m3/s, and 26.29 m3/s, while the 10-year return flood discharges for the Oyo watershed is 959.60 m3/s. The hydraulic analysis was carried out by modeling the 13.35 km long Celeng River channel with HEC-RAS 4.1 software. The flow simulation is carried out steadily. The simulation results show that during the simulation of the existing state there are several points of the section of the Celeng River that overflow. The overflowing sections are then normalized with certain groove dimensions that are adjusted to the location of the flood point. The results of the flow simulation after normalization show that most of the Celeng River channel can accommodate the flood discharge that occurred. The sections that still overflow after normalization are then given embankments with an average height of 0.75 m.
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