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长江口海域悬浮物的粒度特征与成因分析
摘要点击 3002  全文点击 2462  投稿时间:2009-04-07  修订日期:2009-08-12
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中文关键词  LISST-100X C型  絮凝体  粒径分布  中值粒径  有效密度  长江口
英文关键词  LISST-100X Type C  flocs  grain size distribution  median grain size  effective density  Changjiang Estuary
作者单位
庞重光 中国科学院海洋研究所青岛266071 
于炜 中国科学院海洋研究所青岛266071 
杨扬 中国科学院海洋研究所青岛266071 
中文摘要
      利用现场激光粒度仪(LISST-100X C型),在不扰动天然细颗粒泥沙絮凝体的情况下,于2008年7月在长江口海域测量了24个站位不同层次悬浮絮凝体的粒径分布和体积浓度.结合同步测得的海水温度、盐度和浊度数据,得出了长江口海域悬浮物的粒度特征并进行了成因分析.长江口观测海域悬浮物的平均中值粒径为4.69φ,粒级分布具有分选较差、峰态宽、近对称的特征.悬浮絮凝体的垂向平均体积含量随离岸距离的增加而显著降低,而中值粒径却具有增大的趋势;在31.0°N断面,平均中值粒径从11 μm 增加到了60 μm.随着离岸距离的增加,细颗粒悬浮泥沙的含量显著降低,而一些粒径较大的生物体或大粒径絮凝体的含量相对增多,造成了中值粒径的明显增大.本次观测所得的有效密度在246~1 334 kg/m3之间,平均为613 kg/m3.当悬浮物含量较高时,由于大絮凝体比小絮凝体的沉降速度快,大絮凝体有效密度小于小絮凝体,从而导致悬浮物的中值粒径随水深的增大而明显增大,絮凝体有效密度随水深的增加而减小;37和44站有效密度与中值粒径的相关系数均在0.9以上.
英文摘要
      In July of 2008,under the natural condition of sea water,the Laser in-situ scattering and transmissometry (LISST-100X Type C) was used to measure grain size distribution spectrum and volume concentration of total suspended matter in the sea water,including flocs at different layers of 24 sampling stations at Changjiang Estuary and its adjacent sea. The characteristics and its forming mechanism on grain size distribution of total suspended matter were analyzed based on the observation data of LISST-100X Type C,and combining with the temperature,salinity and turbidity of sea water,simultaneously observed by Alec AAQ1183. The observation data showed that the average median grain size of total suspended matter was about 4.69φ in the whole measured sea area,and the characteristics of grain size distribution was relatively poor sorted,wide kurtosis,and basically symmetrical. The conclusion could be drawn that vertically average volume concentration decreased with the distance from the coastline,while median grain size had an increase trend with the distance,for example,at 31.0°N section,the depth-average median grain size had been increased from 11 μm up to 60 μm. With the increasing of distance from the coast,the concentration of fine suspended sediment reduced distinctly,nevertheless some relatively big organic matter or big flocs appeared in quantity,so its grain size would rise. The observation data indicated that the effective density was ranged from 246 kg/m3 to 1 334 kg/m3,with average was 613 kg/m3. When the concentration of total suspended matter was relatively high,median grain size of total suspended matter increased with the water depth,while effective density decreased with the depth,because of the faster settling velocity and less effective density of large flocs that of small flocs. As for station 37 and 44,their correlation coefficients between effective density and median grain size were larger than 0.9.

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