摘要
为研究黄河三角洲海底冲刷演变规律,2004年6月和9月,在黄河三角洲北部、飞雁滩以东岸段进行了2次共21条水深剖面测线的调查工作。通过1985年、1999年两期历史水深资料与本次实测水深资料的对比研究发现:自1985年以来,研究区一直处于冲蚀状态,1999年以后局部区域出现微弱淤积,侵蚀中心逐渐向东南、向岸迁移。测区总体演变趋势以侵蚀为主,强度逐渐减弱,并向冲淤平衡缓慢过渡。
Changes in the morphology of the coastal zone were monitored in June and September 2004 in the northern area of the Yellow River delta. Through collecting and comparing water-depth data of 1985 and 1999, we got the result that this area was in the condition of erosion from 1985, after 1999, part of the area seemed to be in slight accretion, and the center of the erosion moved southeastwards and towards the shore. The total evolution trend is that this area will keep eroded, but the intensity will decline gradually into balance of accretion and erosion.
出处
《海洋地质动态》
2006年第8期7-11,共5页
Marine Geology Letters
基金
国家重点基础研究发展规划(973)项目(2002CB412408)
关键词
水深测量
岸滩演变
海底侵蚀
黄河三角洲
water-depth
coastal evolution
seabed erosion
Yellow River delta
作者简介
孙永福（1964-），男，研究员，主要从事海洋工程地质研究工作．
