Rahma Sarita, Mario Putra Suhana, Harish Wirayuhanto
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引用次数: 0
摘要
沉积和侵蚀过程可受水文海洋因素的影响。这些因素包括波浪、海流和潮汐,因为它们直接与海岸/沿海地区相互作用。与这些问题相关的是,沉积和侵蚀是一个需要研究的问题。提供这些信息的一种方法是使用水动力学模型,这种方法被广泛使用。由此可见,在Berakit村和Pengudang村进行泥沙输沙模型研究,确定泥沙类型、类型等泥沙性质的重要性。该研究于2021年6月使用MIKE21软件水动力学建模进行了为期一个月的研究,使用了流体动力学建模,Flow Model FM输沙模块。观测到的泥沙输运是底沙或床沙。研究结果显示在4种情况下,即向高潮、向高潮、向低潮和向低潮。涨潮时输沙量为-0.10,侵蚀量为0.25 m/d,最潮时输沙量为-0.24,沉积量为0.32 m/d。随侵蚀向低潮输沙
Pemodelan Pola Transport Sedimen di Perairan Desa Berakit dan Pengudang Kabupaten Bintan
Sedimentation and erosion processes can be influenced by hydro-oceanographic factors. These factors include waves, currents, and tides because they interact directly with the coastal/coastal area. Related to these problems, sedimentation and erosion is one thing that needs to be studied. One way that is used in providing information about these that is widely used is to use a hydrodynamic model. Based on this, it can be seen that it is important to conduct research to determine sediment properties such as the type and type of sediment with sediment transport modeling in Berakit and Pengudang villages. This research was carried out using the MIKE21 Software hydrodynamic modeling for one month in June 2021 using hydrodynamic modeling, the Flow Model FM Sand Transport module. Sediment transport observed is bottom sediment or bed load. The research results are shown in 4 conditions, namely towards high tide, highest tide, towards low tide and lowest tide. Sediment transport at high tide with erosion of -0.10 and sedimentation of 0.25 m/day and at the highest tide shows an erosion value of -0.24 and sedimentation of 0.32 m/day. Sediment transport towards low tide with erosion