墙内及墙周围帮派流动分析

W. A. B. N. Sidiq, F. Hanafi, Dwi Priakusuma, Willar Haruman, Muhammad Yunan Sumarso, Nanik Setyowati
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引用次数: 1

摘要

三宝垄市有几个地区地势低平,因此雨季洪水泛滥的风险很高,空间分布在市中心地区。2022年,洪水淹没了877.66公顷的土地,其中一个位于特姆巴朗地区及其周边地区,高度约为275 MDPL,发生在20个地点,面积约为33.62公顷,该地区是巴邦流域的下游部分。Babon流域20年来的降雨分析结果表明,该流域相对稳定,变化不大,其中计算2022年2年一遇合理洪水流量的结果约为25.80 m³/s。此外,对流域的形态计量分析表明,Babon流域的形状相对细长,圆形比<0.50,河流密度指数为0.25–10 km/km²,属于中等密度类别,相对较长的时间浓度(TC)约为3.2小时,因此对下游洪水的影响较小。Babon流域径流系数受土地覆盖条件的影响,其中解释结果表明,从2002年到2022年,建成区的土地覆盖面积发生了变化,增加了708.44公顷,植被面积减少了486.77公顷。渠道容量分析表明,7个子流域的现有渠道可能发生溢流,从而导致淹没。本研究的结论表明,过去20年的降雨量相对稳定,流域的地形测量对下游洪水没有太大影响,Babon DAS的主要河流容量仍然足以容纳25年一遇的计划洪水流量。因此,发生的洪水更多是由下游土地覆盖和排水能力的变化引起的。
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Analisis Banjir Genangan di Kawasan Tembalang dan Sekitarnya
Semarang City has a low and flat topography in several areas so that it has a high risk of inundation during the rainy season with a spatial distribution in the city center area. In 2022 inundation floods have inundated 877.66 hectares, one of which is in the Tembalang area and its surroundings with a height of around 275 MDPL which occurred in 20 locations with an area of around 33.62 hectares, where the area is the downstream part of the Babon Watershed. The results of the analysis of rain in the Babon watershed area for 20 years show that it is relatively stable, not too much variation, where the results of calculating the rational flood discharge for 2022 with a return period of 2 years are around 25.80 m³/s. Furthermore, the morphometric analysis of the watershed shows that the shape of the Babon watershed is relatively elongated with a circularity ratio <0.50, the density index of the river is 0.25 – 10 km/km² which is in the medium density category with a relatively long Time Concentration (TC) of around 3.2 hours so that it is less thus impacting flooding downstream. The Babon watershed runoff coefficient is affected by land cover conditions, where the interpretation results show that there was a change in land cover from 2002 – 2022 for the area of built-up land which increased by 708.44 hectares and the vegetation area decreased by 486.77 hectares. Analysis of channel capacity shows that there is potential for overflow from existing channels in 7 sub-watersheds which will result in inundation. The conclusion of this study shows that rainfall over the past 20 years has been relatively stable and the morphometry of the watershed has not had much impact on downstream flooding, the main river capacity of the Babon DAS is still sufficient to accommodate the planned flood discharge with a return period of 25 years. So that inundation that occurs is more caused by changes in land cover and drainage capacity in the downstream. 
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