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Hydrological and Sediment Characteristics of Sand Ridge Field in Jiangsu coastal area of China

机译:江苏沿海地区沙脊田的水文与沉积物特征

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The sand ridges field in Jiangsu coastal area has been the key region of tidal flat reclamation, waterway regulation and port construction. Adopting the hydrological and sediment data in winter, the tidal patterns were revealed. In addition, the depth-averaged velocity, sediment grain size and sediment concentration in each station were analyzed and compared in detail. The result shows that the tidal in study area is regular semidiurnal and diurnal inequality. The velocity has a decreasing tendency with the Tiaozini water area being centered towards the surrounding areas. The grain size gradually decreases and then increases from north to south, while the sediment concentration gradually increases and then decreases from north to south.
机译:江苏沿海地区的沙坡场一直是潮汐平填海,水路调节和港口建设的关键区域。在冬季采用水文和沉积物数据,揭示了潮汐模式。另外,分析并详细比较了每个站的深度平均速度,沉积物粒度和沉积物浓度。结果表明,研究区的潮汐是常规的半衰老和昼夜不平等。速度具有降低与朝向周围地区的水位的趋势。晶粒尺寸逐渐降低,然后从北向南增加,而沉积物浓度逐渐增加,然后从北到南部减少。

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