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珠江口河流输沙、河口沉积与粒度信息之间的联系
引用本文:贾建军,高抒,高建华,潘少明,王爱军.珠江口河流输沙、河口沉积与粒度信息之间的联系[J].海洋科学进展,2005,23(3):297-304.
作者姓名:贾建军  高抒  高建华  潘少明  王爱军
作者单位:1. 海底科学国家海洋局重点实验室,浙江,杭州,310012;国家海洋局,第二海洋研究所,浙江,杭州,310012;南京大学,海岸与海岛开发教育部重点实验室,江苏,南京210093
2. 南京大学,海岸与海岛开发教育部重点实验室,江苏,南京210093
3. 中国科学院,南京湖泊与地理研究所,江苏,南京210008
4. 国家海洋局,第三海洋研究所,福建,厦门,361005
基金项目:国家重点基础研究发展规划项目--中国典型河口-近海陆海相互作用及其环境效应第一子课题--河流入海物质通量变导及其对流域自然变化和人类活动的响应(2002CB412401);国家自然科学青年基金项目--海洋环境中沉积物粒度趋势形成的动力机制(40206006);国家自然科学重点基金项目--强潮海湾与粉砂物质系统行为(40231010)
摘    要:河口三角洲地区泥沙供应充分,是现代沉积速率较高的区域。快速沉积的泥沙包含高分辨率的环境信息。采用放射性同位素测年方法研究了珠江口伶仃洋大铲湾海域6个柱样的现代沉积速率,以2mm的间隔分析了其中2个柱样上部的粒度,并对其平均粒径和珠江流域的年输沙量进行了快速傅里叶变换,以期获取河流泥沙供应、河口沉积速率和沉积物垂向粒度变化的对应关系。结果表明,大铲湾海域的沉积速率为1~3cm/a,受动力条件和泥沙供应条件的影响显著。2个柱样的平均粒径的最显著重现周期与珠江年输沙量的周期性有较好的对应关系,并可能反映了季节的、年的和多年的沉积速率信息。对于每年沉积厚度在厘米级的环境,以毫米级的高分辨率进行粒度分析,有可能揭示出沉积物供应的季节变化和年际变化。本研究亦可为其他河口的相关工作提供借鉴。

关 键 词:沉积速率  放射性同位素测年  粒度  快速傅利叶变换(FFT)  珠江口
文章编号:1671-6647(2005)03-0297-08
收稿时间:2004-10-08
修稿时间:2004年10月8日

Linkage of Grain Size Information With River Sediment Discharge and Estuarine Deposition at the Pearl River Estuary
JIA Jian-jun,GAO Shu,GAO Jian-hua,PAN Shao-ming,WANG Ai-jun.Linkage of Grain Size Information With River Sediment Discharge and Estuarine Deposition at the Pearl River Estuary[J].Advances in Marine Science,2005,23(3):297-304.
Authors:JIA Jian-jun  GAO Shu  GAO Jian-hua  PAN Shao-ming  WANG Ai-jun
Abstract:The estuarine delta area is abundant in sediment supply,and is a high modern sedimentation rate area. The quickly deposited sediments contain high resolution environmental information. In this paper, the radioactive isotope dating method is used to study the modern sedimentation rates of 6 cores from the Dachan Bay, Pearl River estuary, and the grain size analysis at intervals of 2 mm is also made for the upper parts of two cores. The fast Fourier transformation (FFT) is made for the mean grain size and the annual sediment discharge in the Pearl River basin to derive the relationship between river sediment supply, estuarine sedimentation rate and vertical sediment grain size variation. It is shown from the analysis results that the sedimentation rate in the Dachan Bay sea area is in the range 1 to 3 cm/a, and is significantly affected by the dynamic and sediment supply conditions. There is a good correlation between the most signi-ficant recurrence periods of mean grain size of two cores and the periodicity of the annual Pearl River sediment discharge, which might reveal the seasonal and interannual variations of sediment supply. This study can also be used as a reference for other estuarine studies.
Keywords:sedimentation rate  radioactive isotope dating  grain size  fast Fourier transform(FFT)  Pearl River estuary
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