Retention Pool As Alternative For Flood Control Case Study Of Bapertarum Housing, Sumenep Regency

Ach. Desmantri Rahmanto, Faisal Rosihan
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Abstract

Indonesia is a water country with thousands of rivers and hundreds of deep seas. This causes Indonesia to become a country that is very prone to flooding. But basically, there are several factors that cause this to happen, namely: natural events, drainage damage and environmental degradation caused by human activity itself. Geographically, Bapetarum Housing is an area located in a rainwater catchment area so that it is prone to flood events. High rainfall intensity can cause flood inundation as high as 30 cm. The purpose of this study is to calculate the adequacy of the retention pond to cope with flooding. The procedure for collecting research data begins with analyzing the flood, namely primary and secondary data. Meanwhile, the data analysis techniques used are planning rain analysis, rainfall intensity, flood discharge analysis, retention pond capacity. The retention pond capacity is sufficient because the dimensions of the retention pond are larger than the volume of the retention pond capacity when the flood is 6750m3>6447m3. The retention pond is planned in the downstream area of the residential river with a pool area of 50 x 40 meters and a depth of 4.5 m. The bottom condition of the pond is saturated because it is always inundated with water, the infiltration rate is constant (fc). The constant infiltration for clayey soil type is 0.5 m/day, the infiltration volume rate that occurs at the bottom of the pond is 179 m3/hour, the volume is below the threshold 8283.21 m3, infiltration time is 46 hours.
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蓄水池作为防洪的替代方案——苏梅内普市巴巴塔姆住宅案例研究
印度尼西亚是一个拥有数千条河流和数百个深海的水国。这使得印尼成为一个非常容易发生洪水的国家。但基本上,有几个因素导致这种情况的发生,即:自然事件,排水破坏和人类活动本身造成的环境退化。从地理上看,Bapetarum Housing位于雨水集水区,因此容易发生洪水事件。强降雨可造成高达30厘米的洪水淹没。本研究的目的是计算贮水池是否足以应付水浸。收集研究资料的程序从分析洪水开始,即第一手资料和第二手资料。同时,采用的数据分析技术有规划雨量分析、降雨强度分析、洪流量分析、蓄水池容量分析。当洪水为6750m3>6447m3时,蓄水池尺寸大于蓄水池容量体积,蓄水池容量充足。蓄水池规划在住宅河流下游区域,池面积为50 × 40米,深度为4.5米。由于池底总是被水淹没,所以池底处于饱和状态,入渗速率恒定(fc)。黏性土壤类型的恒定入渗量为0.5 m/d,池底发生入渗量速率为179 m3/h,体积低于阈值8283.21 m3,入渗时间为46 h。
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