DISTRIBUTION PATTERN OF TOTAL SUSPENDED SOLIDS (TSS) IN KAMPAR RIVER ESTUARY, PELALAWAN REGENCY, RIAU PROVINCE

Febi Betania Melas, M. Mubarak, R. Rifardi
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Abstract

The Kampar River Estuary is the main river in Riau province, which empties into the Malacca Strait and has a unique potential for research. The characteristics of the Kampar River Estuary are concurrent and have high tidal elevations, resulting in the occurrence of a Tidal Bore, which is referred to as Bono. The impact of sedimentation is generally quite detrimental, namely the siltation in several places, such as the waters of the Kampar River Estuary, which are dense areas of human activity. This study aimed to determine the relationship between hydrodynamic patterns, suspended solids' distribution pattern, and the concentration value of suspended solids distribution in the Kampar River estuary. This research method is surveyed and discussed descriptively. Current patterns affect the distribution of sediments in the Kampar River estuary. The TSS distribution pattern tends to follow the same direction as the movement of tidal currents where, during high tide, it tends to lead to the southwest of the Kampar River estuary, while during low tide tends to lead to the northeast and northwest, it this is because, in the Kampar River estuary, there is an island that makes the mouth of the Kampar River estuary V-shaped. Between hydrodynamic patterns and TSS distribution patterns, there is a moderate negative relationship (r = 0.50), which means that there is a significant influence between hydro patterns and TSS distribution patterns in the waters of the Kampar River estuary, between hydrodynamic patterns and TSS distribution patterns in the waters of the Kampar River estuary. The lowest value of TSS concentration in the waters of the Kampar River Estuary at high tide to low tide is Station 7, with a range of 102 mg/L, and the highest value at Stations 3, 4, and 9. At station 3, there are values ranging from 1756 mg/L; at station 4, there are values ranging from 2823 mg/L; and at station 9, there are values ranging from 1269 mg/L; the high concentration of TSS results in low brightness in the study area.
里约省佩拉拉万县甘帕河口总悬浮固体(TSS)的分布模式
甘榜河口是廖内省的主要河流,注入马六甲海峡,具有独特的研究潜力。甘榜河口的特点是潮汐并发,潮位较高,因此会出现潮滩,即博诺河。沉积物的影响通常是相当有害的,即在一些地方出现淤积,如人类活动密集的甘榜河口水域。本研究旨在确定水动力模式、悬浮固体分布模式和甘榜河口悬浮固体分布浓度值之间的关系。本研究采用描述性的调查和讨论方法。水流模式会影响甘榜河口的沉积物分布。总悬浮固体的分布模式往往与潮汐流的运动方向一致,在涨潮时,总悬浮固体倾向于流向甘榜河口的西南方,而在退潮时,则倾向于流向东北方和西北方,这是因为甘榜河口有一个岛屿,使得甘榜河口呈 V 形。水动力形态与 TSS 分布形态之间存在中等程度的负相关关系(r = 0.50),这意味着水动力形态与 TSS 分布形态之间、水动力形态与 Kampar 河河口水域 TSS 分布形态之间存在显著影响。贡榜河口水域从涨潮到落潮的 TSS 浓度值最低的是第 7 站,范围为 102 mg/L,最高的是第 3、4 和 9 站。在第 3 站,数值范围为 1756 毫克/升;在第 4 站,数值范围为 2823 毫克/升;在第 9 站,数值范围为 1269 毫克/升;总悬浮固体的高浓度导致研究区域的低亮度。
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