开发用于估算元桐木水库入库流量的无测量集水区综合相似单元水文图

Kurniawan Putra, Istiarto Santoso, Rachmad Jayadi
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摘要

沃诺吉里水库(Wonogiri Reservoir)是位于上本加湾梭罗流域(Upper Bengawan Solo Watershedhed)的一个多功能水库,主要设计用作洪水控制系统。然而,由于水文站有限,无法准确估算流入水库的水量。观测结果显示,在 Wonogiri 水库流域的十个单位水文图中只有四个。因此,本研究采用基于相似性的综合方法来设计无测站流域的单位水文图。这一过程包括使用水文和物理特性参数评估已测量-未测量集水区之间的综合相似性。最终选择相似度得分最高的供体集水区或已测量集水区,为未测量集水区绘制单位水文图。开发出的单位水文图被进一步用于估算 2007 年 12 月 25 日洪水事件的水库入库流量。结果显示,计算出的洪峰流量比之前的研究低 10.9%。随后,使用 HEC-HMS 模拟模型将更新的设计洪水水文图预测到水库中。设计降雨量来自自动降雨记录仪 (ARR) 和 PERSIANN 卫星数据。自动雨量记录仪数据显示,极端降雨持续时间为 5 小时,而卫星数据显示为 6 小时。将自动降雨记录仪的 5 小时持续时间应用于更新的洪水水文图,得出 60 年一遇、500 年一遇和 PMF 洪水的峰值排水量分别为 5123 m3 s-1、7041 m3 s-1 和 10,370 m3 s-1,符合 Wonogiri 水库的洪水设计标准。据观测,这些估计值明显高于 1982 年的设计洪水,当时的洪水流量分别为 4000 立方米/秒、5100 立方米/秒和 9600 立方米/秒。这一更新的防洪设计对于更新元野尻水库在洪水期的运行规则非常重要。
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The Development of Ungauged-Catchment Integrated-Similarity Unit Hydrograph to Estimate Inflow of Wonogiri Reservoir
The Wonogiri Reservoir is a multipurpose reservoir at the Upper Bengawan Solo Watershed, primarily designed to serve as a flood control system. However, there is no accurate estimation of the inflow into the reservoir due to the limited availability of hydrological stations. Observations showed only four out of ten unit hydrographs of the Wonogiri Reservoir watershed. Therefore, this study was conducted to apply an integrated similarity-based approach for designing unit hydrographs in ungauged catchments. The process involved evaluating the integrated similarity between pairs of gauged-ungauged catchments using hydrologic and physical property parameters. This led to the selection of the donor or gauged catchment with the highest similarity score to develop the unit hydrograph for the ungauged catchments. The developed UHs were further applied to estimate the reservoir inflow for the December 25, 2007, flood event. The results showed that the computed peak discharge was 10.9% lower than a previous study. Subsequently, the HEC-HMS simulation model was used to project the updated design flood hydrographs to the reservoir. The design rainfall was derived from automatic rainfall recorder (ARR) and PERSIANN satellite-based data. The ARR data showed that the extreme rainfall duration was 5 hours while satellite data indicated 6 hours. The application of the ARR 5-hour duration to the updated flood hydrographs led to a peak discharge of 5123 m3 s-1, 7041 m3 s-1, and 10,370 m3 s-1 for the 60-year, 500-year, and PMF floods respectively in line with the flood design criteria of Wonogiri Reservoir. These estimates were observed to be significantly higher than the 1982 design floods which were 4000 m3 s-1, 5100 m3 s-1, and 9600 m3 s-1 respectively. This updated flood control design was important to renew the operation rule of the Wonogiri reservoir during flood periods.
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审稿时长
15 weeks
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