印度尼西亚南科纳威县weir aepodu潜在的沉积物输运

A. Sukri, S. M, Riswal Karama, N. Nasrul, R. Talanipa
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引用次数: 0

摘要

土地利用变化对埃波都流域产沙有显著影响,导致河流淤积。这项研究的目的是确定埃波都河的水流状况,这项研究对于了解进入埃波都河堰的沉积物的潜力和弯曲的年龄至关重要。本研究采用观察和调查相结合的定性方法。研究中使用的数据包括14年的降雨数据、流域条件、流量和埃波度堰的沉积物观测数据。从膨胀沉积物显著势为0.0124m2 / s、大颗粒沉降角为D75 = 3.5 mm的流量为1050 m3 / s来看,埃波度流域的现状对沉积势有显著影响。apudo堰潜在侧容(QT)= 308,371,965吨/年,上游堰(QV)容量= 39,375吨,因此堰无效,必须进行泥沙疏浚。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
POTENTIAL SEDIMENT TRANSPORT IN WEIR AEPODU SOUTH KONAWE REGENCY, INDONESIA
Land changes and use significantly affected sediment production in the Aepodu watershed, leading to river siltation. The study aims to determine the condition of the Aepodu river flow, and this study is essential to know the potential of sediments that enter the Aepodu weir and the age of the bend.  The study uses a qualitative approach with observation and survey methods. The data used in the study included fourteen years of rainfall data, watershed conditions, flow discharge, and sediment observations in the Aepodu weir. The current condition of the Aepodu watershed significantly affects the sedimentation potential judging by the significant potential of expansion sediments of 0.0124m2 / sec, the flow rate of 1,050 m3 / second with large grains that settle at the angle of D75 = 3.5 mm. Potential sidemen in weir Aepudo (QT)= 308,371,965 tons/year, with upstream weir (QV) capacity = 39,375 tons so that the weir is ineffective and must be held sediment dredging.
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