SURABAYA

Achmad Syafiuddin
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引用次数: 43

Abstract

Tides is a phenomenon rise and fall of the sea water periodically due to moon and sun gravity. Tides able to raise ocean current is called a tidal current. A tidal current influence the transport of sediment contained in the waters. The process of the deposition of sediment in the waters can affected the shape of topography at the base of waters, one of them is called silting up. The silting up of the sea waters can cause problems if there is in port waters, especially in the ways of shipping and port ponds. The depth of the sea no longer in accordance with the draft of the boats can cause a ship crash. Hence, it needs maintenance the depth of port waters territory by port authority.In this research, done modelling the flow of sediment material due to a tidal current to know the location where happened the largest depth changing in order maintenance the depth in port waters. Modelling the stream and the flow of sediment done in a numerical simulation on tides and grain size parameter. Based on the result of modelling, the largest sediment material flow happened in the estuary of Kali Semampir at coordinate (693905,38; 9204010,30) when the tides is high, with solid flux value 0,000584 m3/s. While the greatest of depth waters change in port ponds Zamrud with the change equals 0,9 m, so that it needs waters depth monitoring in this area routinely.
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潮汐是由于月球和太阳的引力导致海水周期性上升和下降的现象。能够引起海流的潮汐叫做潮汐流。潮汐流影响水中沉积物的输送。泥沙在水中的沉积过程会影响水底地形的形状,其中一种称为泥沙淤积。如果在港口水域,特别是在航运和港口池塘中,海水淤积会造成问题。大海的深度不再符合吃水的小船就会造成船撞船。因此,需要港务局对港区水域深度进行维护。本研究通过对受潮流影响的泥沙流动进行建模,了解港口水域深度变化最大的位置,从而保持港口水域的深度。在潮汐和粒度参数的数值模拟中,对水流和泥沙流动进行了模拟。根据模拟结果,最大的泥沙物质流发生在Kali Semampir河口,坐标(693905,38;9204010,30),固体通量值为0 000584 m3/s。而港塘Zamrud水深变化最大,变化幅度为0.9 m,需要对该地区进行常规水深监测。
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List of Illustrations RITE OF PASSAGE SURABAYA TANJUNG PRIOK Acknowledgments
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