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唐山湾潟湖沙坝海域表层沉积物粒级及分布特征

The Surface Sediments Size Fraction and the Distribution on Lagoon and Sand Barriers in Tangshan Bay

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【作者】 王勇智谷东起王文海乔璐璐

【Author】 WANG Yong-Zhi1,GU Dong-Qi1,WANG Wen-Hai1,QIAO Lu-Lu2(1.The First Institute of Oceanography,SOA.Qingdao 266061,China;2.College of Marine Geosciences,Ocean University of China,Qingdao 266100,China)

【机构】 国家海洋局第一研究所中国海洋大学海洋地球科学学院

【摘要】 利用2010年秋季在唐山湾潟湖沙坝(石臼坨、月坨和打网岗)周边海域实施的表层沉积物粒级的大面站调查资料,阐述了唐山湾潟湖沙坝附近海域的沉积物粒级及其分布特征,并结合同步实施的水文观测结果,初步分析了调查区的沉积动力条件。研究结果表明,唐山湾潟湖沙坝周边海域的平均粒度为4.18Φ,沙坝体近岸5m等深线以浅海域以单峰分布为主,5m等深线以深海域则为双峰分布,潟湖潮道处以单峰分布为主,潟湖内自潮道由东向西逐渐演变为三峰、双峰和单峰模式。调查海域的破波带以浅海域泥沙运动主要以跳跃搬运和推移搬运为主,以深海域中悬浮搬运逐渐占优。研究还表明打网岗岸线侵蚀程度不均匀,中北部岸段侵蚀较为严重。

【Abstract】 The surface sediment size fraction and its distribution characteristic were illustrated by the investigation in barrier-coast in Tangshan bay in October,2010.Based on the synchronous hydrological observation,sediment dynamic condition was preliminarily analyzed.The results show that the average grain size was 4.18Φ.There were three grain size distribution modes,unimodal distribution within isobath of 5 m,bimodal distribution outside of isobath of 5 m,in tidal channel gradually evolved into trimodal distribution,two peaks and the single peak pattern.In shallow waters,the sediment transport mode was mainly jump and bed load,but suspended load was dominated outside of isobath of 5 m.The research also shows that cocestal erosion of Da Wanggang sand barrier was uneven,the more serious erosion occered on north-central coast.

【基金】 海洋公益项目“海岛保护与利用规划顶层设计与沙泥类海岛应用示范”项目(200905004)资助
  • 【文献出处】 中国海洋大学学报(自然科学版) ,Periodical of Ocean University of China , 编辑部邮箱 ,2012年S1期
  • 【分类号】P737.1
  • 【被引频次】4
  • 【下载频次】194
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