The Study of Total Sediment Transport Characteristics at Kanching Forest Waterfall

Siti Nur Khalila Zulkarnain, S. Abdullah, \Shahrul Jainudin
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Abstract

Families and environment enthusiasts frequently visit Kanching Rainforest Waterfall, also known as Kanching Recreational Forest. It is located nearby in the Rawang neighbourhood to the north of Kuala Lumpur and has an area of around 47,000 square metres. Due to its proximity to the city, the region has become a popular place for people to enjoy picnics, camping, swimming, and jungle walks during the holidays. The movement or discharge of water flow is closely related with sediment. Since a specific discharge is necessary to propel and carry particles of a particular weight or size along the pathways. In essence, sediment estimates are so crucial because rivers in Malaysia continue to fill reservoirs with river water for daily use. Sedimentation in reservoirs can reduce the amount of accessible water, hence restricting its application. In this study, the Hjulström graph were used to predict the sediments and particles flow distributions, and the correlation between particle size and particle mobility in the flows of rivers was determined at three (3) checkpoints to examine the sediments and particles flow distributions. According to the data obtained, Checkpoint 1 has a particle velocity of around 0.4703 N/s, or 40 grammes per second, whereas Checkpoint 2 has a velocity of roughly 1.534 N/s, or 156 grammes per second. Lastly, Checkpoint 3 lacks a full load transfer. In addition to preserving one of the region's leisure areas, the significance of complete load transit estimation will ensure its maintenance. By using this method, the estimation of the total load that may be eroded along the river by calculating the total transport load can be forecasted hence, provide a maintenance program toward the rehabilitation of the Kanching Recreational Forest.
康庆森林瀑布总输沙特征研究
家庭和环境爱好者经常参观康清雨林瀑布,也被称为康清休闲森林。它位于吉隆坡北部的拉旺社区附近,面积约为47,000平方米。由于靠近城市,该地区已成为人们在假期享受野餐,露营,游泳和丛林散步的热门场所。水流的运动或排出与泥沙密切相关。因为特定的放电是必要的,以推动和携带特定重量或大小的颗粒沿着路径。从本质上讲,沉积物的估计是如此重要,因为马来西亚的河流继续向水库注入日常使用的河水。水库的沉积会减少可利用水量,从而限制其应用。本研究采用Hjulström图预测沉积物和颗粒流分布,并在3个检查点确定河流中粒径与颗粒迁移率的相关性,以检验沉积物和颗粒流分布。根据获得的数据,检查点1的粒子速度约为0.4703 N/s,即每秒40克,而检查点2的速度约为1.534 N/s,即每秒156克。最后,检查点3缺少满载传输。除了保留该地区的休闲区之一外,完全负荷运输估计的意义将确保其维护。利用该方法,可以通过计算总输沙量来预测沿江可能被侵蚀的总负荷,从而为康清游憩林的恢复提供维护方案。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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