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黄河三角洲桩西101站潮沟地貌形态及其水动力学研究
引用本文:尹延鸿,成国栋,范顺庭,王玉荣,朱兰部.黄河三角洲桩西101站潮沟地貌形态及其水动力学研究[J].海洋科学,1997,21(5):46-49.
作者姓名:尹延鸿  成国栋  范顺庭  王玉荣  朱兰部
作者单位:地质矿产部海洋地质研究所
基金项目:国家自然科学基金资助项目!49476 2 82号
摘    要:在潮沟下游,横跨且生趣与潮沟的横断面设了5个观测站,进行了24h的水动力测量。结果表明,涨落潮流速流向不对称,在潮沟内,涨落潮流流速差别很大,涨潮流流速最大为9cm/2,而落潮流流速最大可达38cm/s。据推测,潮沟内之所以落潮流流速明显大于涨潮流流速,可能是由于潮沟与岸线斜交有关。

关 键 词:黄河三角洲  三角洲  潮沟  地貌形态  水动力学
收稿时间:9/3/1996 12:00:00 AM

MORPHOLOGY AND HYDRODYNAMICS OF THE TIDAL CHANNEL NEAR WELL 101, ZHUANGXI,YELLOW RIVER DELTA
Yin Yanhong ,Cheng Guodong ,Fan Shunting ,Wang Yurong and Zhu Lanbu.MORPHOLOGY AND HYDRODYNAMICS OF THE TIDAL CHANNEL NEAR WELL 101, ZHUANGXI,YELLOW RIVER DELTA[J].Marine Sciences,1997,21(5):46-49.
Authors:Yin Yanhong  Cheng Guodong  Fan Shunting  Wang Yurong and Zhu Lanbu
Institution:Yin Yanhong 1,Cheng Guodong 1,Fan Shunting 2,Wang Yurong 2 and Zhu Lanbu 2
Abstract:Research into the hydrodynamics of the tidal channel near Well 101, Zhuangxi, Yellow River delta was carried out. Crossing the tidal channel, we have set up 5 stations and measured its hydrodynamic. It was found that the current velocities and current directions of flooding and ebbing tide are asymmetry in the tidal channel. A small flooding tide current velocity (smaller than 9 cm/s) and a larger ebbing tide current velocity (up to 38 cm/s) are found. The sea water converges toward the oblique tidal channel and makes a larger ebbing tide current velocity durring ebbing tide.
Keywords:Tidal channels  Flooding and ebbing tide  Hydrodynamics  Geomorphology  asymmetry  
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