Monica T.R Utung, Judi K. Nasjono, Elia Hunggurami
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引用次数: 0

摘要

穆克河容易发生洪水。洪水是由迁移的种植园系统导致的土地利用转变引起的。在木克河中,有必要对流量估算进行分析,以确定木克河的水势。在本研究中,作者采用实测计算模型进行峰值放电计算。采用流量曲线进行测量计算,采用合成单元即中须的水文法进行计算。分析计算的结果Muke河上的放电使用获得的放电曲线的洪峰流量发生在2012年Qmax = 99.41立方米/秒,最小的放电发生在2010年与Qmin = 13.19立方米/秒,分析计算结果Muke河上的放电使用Nakayasu方法获得的洪峰流量发生在2010年Qmax = 184.74立方米/秒,最小的放电发生在2014年与Qmin = 94.33立方米/秒。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Debit Puncak Harian Tahunan Metode HSS Nakayasu dan Debit Terukur di DAS Muke Kabupaten TTSS SERVICES-CURVE NUMBER DAN DEBIT TERUKUR DI DAERAH ALIRAN SUNGAI MUKE KABUPATEN TIMOR TENGAH SELATAN
The Muke River is prone to flooding. flooding is caused by conversion in land use due to the migrating plantation system. In the Muke river, it is necessary to analyze the discharge estimation to determine the potential of water in the Muke river. In this study, the authors performed peak discharge calculation using measured calculation model and calculate. Measured calculations using discharge’s curve and calculated by using hydrographic method of synthetic unit namely Nakayasu. The results of the analysis for the calculation of discharge on the Muke river using the discharge curve obtained that the peak discharge occurred in 2012 with Qmax = 99.41 m3/s and the smallest discharge occurred in 2010 with Qmin = 13.19 m3/s, the results of the analysis for the calculation of discharge on the Muke river using the Nakayasu method obtained peak discharge occurred in 2010 with Qmax= 184.74 m3/s and the smallest discharge occurred in 2014 with Qmin = 94.33 m3/s.
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