上海无居民海岛潮间带沉积物粒径特性研究

利用激光粒度仪对上海无居民岛30个表层沉积物样品进行粒度特征分析,研究区域的6个无居民岛的沉积物类型共有5类,其分布为粉砂在九段沙、东风西沙、黄瓜沙和青草沙;砂在青草沙和顾园沙;粉砂质砂在扁担沙和青草沙;砂质粉砂在青草沙;粘土质粉砂在黄瓜沙。其中粉砂类沉积物分布最广。沉积物呈现分选系数差,偏态均为正偏,窄峰型的特征。由于研究区域处于长江口,丰富的流域来沙,特别是大量的细颗粒泥沙为潮滩的建造提供了充裕的物质来源;而复杂的径流、潮流和风浪的作用,则成为了塑造潮滩的重要动力条件。通过绘制Pejurp三角图式显示,无居民岛样品均处于在Ⅲ、Ⅳ动力区,水动力条件总体上较强,粒径较粗。除顾园沙外由海向岸(由低潮滩到高潮滩),水动力逐渐减弱,沉积物颗粒逐渐变细,砂的含量逐渐减少,粘土和粉砂的含量逐渐增多。研究亮点:对上海无居民岛潮间带沉积物进行了粒径特性的分析,结果显示沉积物分布以粉砂为主,分选性差,正偏,呈窄峰型,通过绘制Pejurp三角图式,表明研究区域总体水动力较强,并根据各无居民岛的环境特征分析其不同的沉积动力环境。

Grain size characteristics of the inter tidal flat sediments of Shanghai non resident islands

30 surface sediment samples were collected from the islands of Shanghai.All of the samples were analyzed by using LS13320 laser particle size analyzer.There are five sediment types in the study area of six non-resident islands,among all types of sediments,the silt sediment is the most abundant.The sediment parameters of all samples are generally bad sorting,positively skewed,leptokurtic.The study area is located in the Yangtze River Estuary.The open mouth provides a broad space for the development of the tidal flat and the influence of the strong river runoff,tidal flow and waves provide dynamical factors to form the tidal flat.By drawing Pejurp triangle pattern,it displays that all the samples are in Ⅲand Ⅳdynamic sections which means the hydrodynamic condition is strong generally.Besides Guyuan Sha,accompanied by the declining hydrodynamic conditions,from ocean to shore,the grain size decreases and the sand content decreases,clay and silt increases.