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Distribution Characteristics of Suspended Sediment Concentration in Yangshan Deep-water Port Sea Area, China

机译:中国阳山深水港区悬浮沉积物集中的分布特征

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The Yangshan deep-water port locates in the Qiqu Archipelago with many islands and tidal channels. Taking Yangshan deep-water port sea area as an example, it was researched that distribution characteristics of suspended sediment concentration in archipelago waters, China. Based on the measured data of Oct. 1996, Jan. 1999, May 2006 and May 2007 and the measured surface suspended sediment concentration data from 1998 to 2007, the change characteristic of suspended sediment concentration is analyzed. The suspended sediment concentration in the Yangshan sea area shows four pronounced time-scale variations, i.e. yearly variation, seasonal variation, neap-spring cycle and intra-tidal variation and two spatial scale variations (horizontal distribution and vertical distribution). Moreover, it is discussed to the causes of the variation of suspended sediment concentration. The sediments from the Yangtze Estuary have no direct effect on suspended sediment concentration of the study area, and it is also shown that the suspended sediment concentration is mainly due to local bottom sediment resuspension. There is the high suspended sediment concentration in the part area of Yangshan sea area, especially, along the Xiaoyangshan Island and Dayangshan Island chain direction. The phenomenon is mainly due to the “strait-channel effects”
机译:阳山深水港位于Quie群岛与许多岛屿和潮汐渠道找到。以阳山深水港口海域为例,研究了中国群岛水域悬浮沉积物集中的分布特征。基于1996年10月1999年10月,2006年5月和2007年5月的测量数据,分析了1998年至2007年的测量表面悬浮沉积物浓度数据,分析了悬浮沉积物浓度的变化特征。阳山海域的悬浮沉积物浓度显示了四个明显的时间尺度变化,即年度变化,季节变化,NeAp-Spring周期和潮汐变化和两个空间尺度变化(水平分布和垂直分布)。此外,讨论了悬浮沉积物浓度变异的原因。长江河口的沉积物对研究区域的悬浮沉积物浓度没有直接影响,并且还表明悬浮的沉积物浓度主要是由于局部底部沉积物重悬浮。阳山海域的部分地区有高悬浮沉积物浓度,特别是沿小阳山岛和大浪山岛链方向。现象主要是由于“海峡渠道效应”

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