分析了河流对城市地区侵蚀和减少减少的正规性影响:雅加达遣散格拉干河

Siti Murniningsih, Alfisalam Ghifari Mustafa
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引用次数: 1

摘要

洪水是DKI雅加达地区经常发生的问题之一,其原因之一是原本属于开发区的流域土地利用的变化。然而,由于河岸的丧失和河流断面的变窄,河流的横截面往往会被破坏。为了克服这一问题,雅加达省政府于2013年对穿越DKI省的几条河流进行了标准化,其中一条是Pesanggrahan河,将进一步调查。本研究的目的是分析河流归一化对侵蚀和沉积的影响,这将导致河流的纵向和横截面的变化。为了获得准确的流域地图,使用Arc-GIS软件,并根据公共工程部河流区域中心办公室Ciliwung-Cisadane的数据进行了归一化前后的河流流量识别。在河流的上游、中游和下游3个点采集了沉积物样本,对这些样本进行了审查,以确定沉积物颗粒的级配。应用HEC-RAS模拟归一化前后河段输沙情况。模拟结果用于确定侵蚀和沉积引起的断面变化以及确定河流水位。从水位出发,计算水力半径,利用Ackers-White方程进行输沙计算,因为该方程采用的是0.02 - 4.94 mm范围内的颗粒分布。结果表明:上游输沙量增加155.11 t /年,中游输沙量增加89.64 t /年,下游输沙量减少0.28 t /年。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
ANALISIS DAMPAK NORMALISASI SUNGAI TERHADAP EROSI DAN SEDIMENTASI DI DAERAH PERKOTAAN STUDI KASUS: SUNGAI PESANGGRAHAN, JAKARTA
Flooding is one of the problems that often occurs in the DKI Jakarta area, which one of the causes is the change of land use in watersheds that were originally into development areas. Whereas, its often the cross section of the river will be disrupted due to the loss of the riverbanks and the narrower cross section of the river. In order to overcome this, the Jakarta Provincial Government in 2013 normalized several rivers that crossed the DKI Province and one of them was the Pesanggrahan River which will be further investigated. The purpose of this study is to analyze the effect of river normalization on erosion and sedimentation which will result in changes in the longitudinal and cross section of the river. To get an accurate map of the
Watershed Area, Arc-GIS software is used while identification of river flow before and after normalization was carried out based on data from Central Office of River Region Ciliwung-Cisadane, Ministry of Public Works. Sediment samples were taken at 3 points on the river, upstream, middle and downstream, that were reviewed to determine the gradation of the sediment grains. The HEC-RAS application is used to simulate sediment transport on the river section before and after normalization. The simulation results are used to determine the cross section changes due to erosion and sedimentation and to determine the water level in the river. From the water level, the hydraulic radius can be calculated and then carried out sediment transport calculation using Ackers-White equation since the equation using grain distribution from range 0.02 – 4.94 mm. The results it was found that the sediment transport in the upstream point increased 155.11 tons / year,
at the midpoint increased 89.64 tons / year and the downstream point decreased 0.28 tons / year.


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