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青岛市浮山湾、汇泉湾、崂山湾海滩与海底沉积环境分析
引用本文:于洪军,徐兴永,李萍,李培英,韩贻兵.青岛市浮山湾、汇泉湾、崂山湾海滩与海底沉积环境分析[J].海岸工程,2003,22(3):12-18.
作者姓名:于洪军  徐兴永  李萍  李培英  韩贻兵
作者单位:1. 国家海洋局,第一海洋研究所,山东,青岛,266061
2. 中国科学院,海洋研究所,山东,青岛,266071
基金项目:国家自然科学基金(40076014),青岛市自然科学基金(03-2-JSH-10和02-2-KJ-YJ-27)
摘    要:距今12000a,世界洋面已上升至今日海面以下60m处。而后海面继续回升,在距今6000a时,海面已上升到比今日海面还要高3~4m的位置,这就是汇泉广场下面存在海相地层的原因。也是唠山太清官门前存在干枯小泻湖的原因。大约在距今6000a时,青岛市的浮山湾、汇泉湾、唠山湾已经形成,并在海湾中,形成最初的海湾沉积。自那时以来,崂山湾变化不大;而浮山湾、汇泉湾则发生明显的变化。浮山湾展示为宽阔的沙滩形态,自上世纪60年代在燕儿岛建立船厂以来,大面积的沙滩已经消失。目前所见海岸完全为人造海岸,现已不存在海滩。汇泉湾与汇泉广场的填平有关,早期的海岸线,有可能到达中山公园的院墙一带。现在所见的第一海滨浴场也是人为建设所致。

关 键 词:青岛市  浮山湾  汇泉湾  崂山湾  海滩  海底沉积环境
文章编号:1002-3682(2003)03-0012-07
修稿时间:2003年1月9日

Analysis of Beach and Submarine Sediment Environments in the Fushan Bay, Huiquan Bay and Laoshan Bay of Qingdao
YU Hong-jun,XU Xing-yong,LI Ping,LI Pei-ying,HAN Yi-bin.Analysis of Beach and Submarine Sediment Environments in the Fushan Bay, Huiquan Bay and Laoshan Bay of Qingdao[J].Coastal Engineering,2003,22(3):12-18.
Authors:YU Hong-jun  XU Xing-yong  LI Ping  LI Pei-ying  HAN Yi-bin
Abstract:The sea level about 12,000 years ago was about 60 m lower than that at pre-sent, the sea level then continued to rise and was 3 to 4 m higher than that at present about 6,000 years ago, which is the reason for the marine sediment to exist under the Huiquan Square. The Fushan Bay, Huiquan Bay and Laoshan Bay of Qingdao came in- to being about 6,000 years ago, and the original marine sediments were formed in these bays. Since then, no big changes in the Laoshan Bay have taken place, but the Fushan Bay and Huiquan Bay have changed greatly. The broad beach in the Fushan Bay has disappeared since the shipyard was built in Yanerdao area in 1960s, and the present coast is an artificial coast with no beach. The changes in the Huiquan Bay are related with the construction of the Huiquan Square, the former coastline was close to the Zhongshan Park, and the First Bathing Beach in the Huiquan Bay is a manmade beach.
Keywords:Qingdao  beach  submarine sediment environment  
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