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扬子浅滩沙波底形活动性评估

ACTIVITY MAGNITUDE OF THE SMALL-MEDIUM SUBAQUEOUS DUNES IN THE YANGTZE SHOAL

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【作者】 龙海燕庄振业刘升发吕海青叶银灿杜文博

【Author】 LONG Hai-yan1,ZHUANG Zhen-ye1,LIU Sheng-fa2,L Hai-qing1 YE Yin-can3,DU Wen-bo3(1 Ocean University of China,Qingdao 266100,China;2 Institute of Oceanology,Chinses Academy of Sciences,Qingdao 266071,China;3 Second Institute of Oceanography,State Oceanic Administration,Hangzhou 310012,China)

【机构】 中国海洋大学海洋地球科学学院中国科学院海洋研究所国家海洋局第二海洋研究所国家海洋局第二海洋研究所 青岛266100青岛266100青岛266007杭州310012

【摘要】 扬子浅滩位于长江口以东,水深40 m左右,普遍发育中小水下沙丘并处于运动状态。按32片沙波参数统计,迁移方向在90°~180°之间,其中150°~180°者占30%,120°~150°者占69%;使用Rubin和改进的Hardisty公式计算,以潮流作用为主的常态海况下,沙波迁移率为19.70 m/a,以浪流为主的暴风浪期间,约为12.72 m/a,一年总迁移率约为32.4 m/a,与世界上若干海底沙波定位观测数据相对比,这一迁移率应属于缓慢—中等的量级。

【Abstract】 The Yangtze shoal,located in the east of the Yangtze River Estuary and about 40 m deep below sea level,has widely spread small-medium subaqueous dunes,whose wave height is 0.6 m and which are generally in activity.Statistical result of 32 subaqueous dune areas shows that the movement direction is within 90°~180°.150°~180° direction accounts for 30% and 120°~150° for 69%.The movement velocity of the small-medium subaqueous dunes,calculated using the formulas from Rubin and Hardisty,is usually 19.70 m/a and controlled by tidal currents,and is 12.7 m/a in storm season.And the total migration rate is 32.4 m/a.Compared with observation data from other small-medium subaqueous dunes in the world,the activity of small-medium subaqueous dunes in the Yangtze shoal belongs to a slow-medium magnitude.

【基金】 国家自然科学基金项目(40476032)
  • 【文献出处】 海洋地质与第四纪地质 ,Marine Geology & Quaternary Geology , 编辑部邮箱 ,2007年06期
  • 【分类号】P737
  • 【被引频次】22
  • 【下载频次】227
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