Anak Agung Ratu Ritaka Wangsa
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引用次数: 0

摘要

摘要:巴东三边克罗德地区是人口密集地区之一。这导致了从稻田到住房的土地利用功能的变化,减少了水的渗透,造成了地表径流。因此,笔者需要对该地区的泄洪排水规划进行计算。从计算洪水流量到规划排水渠道的各个阶段包括寻找受影响的站,即Ngurah Rai站、Sanglah站、Ship站,并利用现有的排水渠道。之后,计算总降雨量和最大降雨量,这意味着数据将用于进一步的计算,如双质量分析法的一致性检验,计算区域平均降雨量,检验分布的选择,计算降雨量,设计Log Person Type III方法,计算降雨强度(Talbot, Sherman, Ishiguro),计算分布适宜性检验(Smirnov Kolmogorov),计算洪流量分析(理性),以量纲计算。在洪流量分析中,5年回复期的洪流量计划为0.049 (m3/s)>现有洪流量为0.030 (m3/s),因此有必要对巴东三边克罗德地区进行排水沟规划。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Analisis Debit Banjir Pada Perencanaan Saluran Drainase Daerah Padangsambian Kelod Ruas Jalan Gunung Salak
ABSTRACT: The Padangsambian Kelod area is one of the densely populated areas. This causes changes in the land use function from rice fields to housing, which reduces water infiltration, causing surface runoff. So that the author needs to calculate the flood discharge and drainage planning in the area. The stages in calculating flood discharge to planning drainage channels include looking for stations that affect, namely Ngurah Rai Station, Sanglah Station, Ship Station, conducting existing drainage channels. After that, calculate the total rainfall and maximum rainfall, which means that the data will be used for further calculations such as the consistency test of the Double Mass Analysis method, calculating the regional average rainfall, testing the selection of distribution, calculating rainfall, design the Log Person Type III method, calculating Rain intensity (Talbot, Sherman, Ishiguro), Calculating distribution suitability test (Smirnov Kolmogorov), Calculating flood discharge analysis (Rational) to dimensional calculations. In the analysis of the flood discharge, the flood discharge plan for the 5 year return period is 0.049 (m3/s)> the existing flood discharge is 0.030 (m3/s) so it is necessary to plan drainage channels in the Padangsambian Kelod area.
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