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Distribution Pattern of Suspended Sediments in Wulan Delta, Demak, Indonesia

机译:悬浮的沉积物的分布模式在Demak,Demak,Indonesia

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Suspended sediments are important factor in a sedimentation process. Oceanographic, hydrodynamic, andmeteorological conditions along; benthic habitat, mangroves, and ponds in coastal area, affect sedimentationdistribution in Wulan Delta. The purpose of this study wasto estimate the concentration of suspended sediments from2016 to 2018 and analyze its distribution patterns in Wulan Delta, Wedung District, Demak Regency, Central Java,Indonesia. We used quantitative methods and descriptive analyses to process and analyse data. The oceanographic,hydrodynamic, and meteorological paramaters such as wind, waves, currents, and tides, were used to examine thedistribution of suspended sediments, while remote sensing images data were used to estimate the concentration ofsuspended sediments. The hydrodynamic of Wulan Delta in the west season was more significant than in the eastseason, with wind velocities ranging from 8.8 to 11.1 m/s and wave height of <1 m. Waves are destructive in theformer while constructive in the latter. Current velocities ranging from 0 to 0,25 m/s and mixed tides with prevailingdiurnal type. From 2016 to 2018, the concentration of the suspended sediments varied between 60 and 180 mg/l, andtheir distribution followed the development of Wulan Delta, that is, leftward (southwest-south).
机译:悬浮沉积物是沉积过程中的重要因素。海洋,流体动力学,和气象条件围际栖息地,红树林和池塘在沿海地区,影响沉降武兰三角洲的分布。本研究的目的Wasto估计了悬浮沉积物的浓度2016年至2018年,分析了武兰三角洲,德国省德马克地震,中爪哇省的武兰三角洲的分布模式,印度尼西亚。我们使用定量方法和描述性分析来处理和分析数据。海洋学,流体动力学,以及风,波,电流和潮汐等气象参数,用于检查悬浮沉积物的分布,而遥感图像数据用于估计浓度悬浮沉积物。西部乌兰三角洲的流体动力学比东方更重要季节,风速度为8.8至11.1米/秒和波高的波高<1米。波浪是破坏性的前者,而在后者的建设性。当前速度范围为0至0.25米/秒,并具有普遍存在的混合潮汐昼夜类型。从2016到2018年,悬浮沉积物的浓度在60和180毫克/升之间变化,而且他们的分销遵循武兰三角洲的发展,即左(西南南)。

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