用数学模型方法分析宋普特里水库库区沉积速率

N. A. S. Purwono, A. Barkah, Elvina Kusumawati, Rena Ning Tyas
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引用次数: 0

摘要

宋普特里水库是一座以灌溉水田和防洪为目的的人工水库。该水库位于woogiri县Eromoko区,需要对Song Putri水库进行沉积建模,以分析Song Putri水库的沉积物沉积量。利用SMS (Surface-water Modeling System) 8.0软件对水库的水流形态和泥沙分布进行分析。本研究旨在确定水流模式和泥沙分布对水库变化的影响。使用的数据包括宋普特里水库技术数据、2009-2018年10年日降雨量数据、沉积物数据、水库入流数据、测深图。对宋普特里水库的进出水量进行分析,采用经验方法进行水文分析,沉降建模模拟采用SMS 8.0。软件模拟结果表明,50年回归期的最大流速为0.097 m / s,最小流速为0.00 m / s,根据水库基础720小时(1个月)变化的模拟结果,50年、100年和最高1000年的回归期的最大流速为5.795 m,最小流速为0.001 m。基于沉积物增长率的预测计算,获得的结果沉积物增长率与50年重现期的35.68%的比例在19% - 21%之间,100年29.103%的比例重现期的百分比在22% - 24%之间,而1000年的增长比例重现期沉积物是98,20%比例范围在55% - 57%之间。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The Analysis of Song Putri Reservoir Storage Area on Sedimentation Rate Using Mathematical Model Approach
Song Putri Reservoir is an artificial reservoir with the aim of irrigation channels for rice fields and flood control. This reservoir is located in Eromoko District, Wonogiri Regency Sedimentation modeling in the Song Putri reservoir is needed to analyze the amount of sediment deposition against the Song Putri Reservoir. To analyze the flow patterns and sediment distribution that occurs in reservoirs, SMS (Surface-water Modeling System) 8.0 Softwarse is used. This study aims to determine the flow patterns and effects of sediment distribution on reservoir changes. The data used include Song Putri Reservoir technical data, daily rainfall data for 10 years (2009-2018), sediment data, reservoir inflow data, and bathymetry maps. To analyze the magnitude of inflow and outflow of Song Putri Reservoir, hydrological analysis using empirical methods is used, while sedimentation modeling simulation uses SMS 8.0. Software based on the simulation, result the highest flow velocity in the 50 year return period is 0.097 m / s and the smallest is 0.00 m / s. Based on the simulation results of changes in the reservoirs base for 720 hours (1 month), the values ​​that in the return period of 50 years, 100 years and the highest 1000 years the highest was 5.795 m and the smallest of 0.001 m. Based on the calculation of prediction of sediment growth rates, it obtained the results of sediment growth rates with a percentage for a 50 year return period of 35.68% with a range of percentages between 19% - 21% and a percentage of 29.103% for a 100 year return period with a range of percentages between 22% - 24%, while the percentage growth rate of 1000 year return period sediments is 98 , 20% with a percentage range between 55% - 57%.
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