印度尼西亚丹中品港市沿海水域和小岛屿的养分分布模型和流动模式

F. Lestari
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摘要

对丹中槟榔市沿海水域的营养物分布模式和水流格局进行了研究。研究的目的是发展一个沿海水域和小岛屿的营养分布和目前格局的模型,作为管理群岛沿岸水域和小岛屿的富营养化的努力。在几个预定的研究站进行有目的的涨潮和退潮取样,以确定观测地点。结果表明,丹戎槟榔湾海域的营养物分布模式与东pak海峡海域不同,低潮和涨潮时的营养物分布模式基本一致,在部分沿海地区呈近海减少、近海高的趋势。围绕着塞河的水域与丹戎槟榔湾水域相连的加朗河口。在丹戎槟榔市沿海水域和小岛屿地区,最高潮时的水流模式为波浪和满月,这表明入口从水域的西部流出,然后向北流出进入开阔水域。然而,它周围存在的小岛屿的一部分水体变得支离破碎,导致丹中槟榔市沿海水域的南部转向,最大流速为1.1米/秒。
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Nutrient distribution models and flow patterns in Coastal Waters and Small Islands, Tanjungpinang City, Indonesia
Research has been done on the model of nutrient distribution and current pattern in coastal water of Tanjungpinang City. The research objective was to develop a model of nutrient distribution and current patterns in coastal waters and small islands as an effort to manage the eutofication of coastal waters and small islands in the archipelago. Determining the location of the observations was done by purposive sampling at high tide and low tide at several predetermined research stations. The results showed the nutrient distribution model in the waters of Tanjungpinang Bay, a different distribution pattern compared to the waters of the Dompak Strait, with the distribution of nutrients from the yield model at low tide and at high tide shows the same pattern, which tends to decrease offshore and high in some coastal locations. around the waters of the Sei. Carang estuary which is connected to the waters of Tanjungpinang Bay. The pattern of currents during the highest tide is bandage and full moon in coastal waters and small islands in the area of Tanjungpinang City, which shows that the inlet flows from the west of the waters, then exits towards the north into open water. However, part of the water mass in the presence of small islands around it becomes fragmented causing a turn to the south of the coastal waters of the city of Tanjungpinang, with a maximum current speed of 1.1 m/s.
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