长江口南汇嘴潮滩短期冲淤演变及其动力机制研究
Researches on characteristics and dynamic mechanism of short-term scouring and silting changes of the tidal flat on Nanhui Spit in the Changjiang Estuary in China
-
摘要: 潮滩地形的冲淤演变规律可以在一定程度上反映动力作用与地貌特征之间的相互耦合机制.根据近几年在长江口南汇嘴潮间带多断面连续观测资料,探讨区域内潮间带滩地的近期冲淤演变特征及其主要影响因子.研究结果表明:(1)南汇嘴潮滩近期主要呈现淤涨态势,而且年内过程季节性差异明显;受区位差异影响,不同观测断面的潮滩冲淤演变呈现特征不尽相同,断面1冲淤变化最为显著,年最大冲淤厚度均在10cm以上;(2)在波浪、潮流的作用下,区域内沉积物很容易被掀动悬扬,而且输沙环流系统的存在有利于悬沙向浅水区输运且在该区域内沉降淤积,从而为潮滩发育提供泥沙来源;(3)受"碧利斯"台风引起的风暴潮天气影响,研究区域内潮滩出现"大冲大淤"现象,即台风强侵蚀期过后滩面高程短期内恢复明显.由此可见,潮滩短期冲淤演变特征是各种动力因素作用下的综合体现.Abstract: To some extent,scouring and silting evolution of tidal flat may reflect the relationship and interaction between dynamic effect and geomorphologic characteristics.On the basis of Shanghai coastal zone investigation project,acontinuous observation was made at the intertidal zone of three sections on Nanhui Spit from June 2006 to June 2007,in order to research the properties of short-term scouring and silting changes as well as its influencing factors.The results show that(1) recently,the tidal flat of Nanhui Spit mostly has a scouring posture,and seasonal difference of flat variation in the year is relatively obvious;affected by it slocation,the respective section shows different developing properties,for example,scouring and silting changes of section one are the most obvious of all,the amount of which is both above 10cm; (2) acted by waves and tidal current,the surface sediment of this zone is easy to be stirred,and the existence of sediment circulation system is favorable for the suspended sediment to settle in shallow water area,which becomes the sediment source of tidal flat;(3) influenced by the storm surge caused by typhoon "Bilis",drastic scouring as well as silting happened in this zone.All of these have proved that the scouring and silting changes of tidal flat were affected by several kinds of dynamic conditions.
-
Key words:
- Changjiang Estuary /
- Nanhui Spit /
- tidal flat /
- scouring and silting evolution /
- dynamic effect
-
逢自安.浙江港湾淤泥质海岸剖面若干特性[J].海洋科学,1980,12(2):9-14. 任美锷,张忍顺,杨巨海,等.江苏王港地区淤泥质潮滩的沉积作用[J].海洋通报,1984,3(1):40-50. 陈才俊.江苏淤长型淤泥质潮滩的剖面发育[J].海洋与湖沼,1991,22(4):360-367. 徐元,王宝灿,章町奇.上海淤泥质潮滩潮锋作用及其形成机制初步探讨[J].地理研究,1994(13):60-68. 杨世伦,赵庆英,丁平兴,等.长江口拦门沙河槽季节性冲淤的主控因子探讨[J].长江流域资源与环境,2001,10(3):258-265. 胡刚,沈焕庭,庄克琳,等.长江河口岸滩侵蚀演变模式[J].海洋地质与第四纪地质,2007,27(1):13-21. 付桂,李九发,应铭,等.长江河口南汇嘴潮滩近期演变分析[J].海洋通报,2007,26(2):105-112. LI Jiu-fa.The rule of sediment transport on the Nanhui tidal flat in the Changjiang Estuary[J].Acta Oceano-ogica Sinica,1991,10(1):117-127. 陈吉余.上海市海岸带和海涂资源综合调查[M].上海:上海科学技术出版社,1988:15-40. 陈吉余,王宝灿.渤海湾泥质海岸剖面(海河口-黄河口)的塑造过程[G]//上海市科技论文选.上海:上海科学技术出版社,1981:1-6. 赵建春,戴志军,李九发,等.强潮海湾近岸表层沉积物时空分布特征及水动力响应——以杭州湾北岸为例[J].沉积学报,2008,26(6):1043~1051. 贺松林,劳治声,陈全.上海芦潮港岸滩冲淤动态及原因探究[J].东海海洋,1996,14(2):19-25. 李九发,戴志军,应铭,等.上海市沿海滩涂土地资源圈围与潮滩发育演变分析[J].自然资源学报,2007,22(3):361-371. 李九发,付桂,万新宁,等.闸下出海通道淤积原因及清淤措施研究[J].泥沙研究,2008(1):46-51. 窦国仁.论泥沙起动流速[J].水利学报,1960(4):44-60. 中华人民共和国交通部.JTJ213-98海港水文规范[S].北京:人民交通出版社,1998. 严恺,梁其荀.海岸工程[M].北京;海洋出版社,2002. 中国气象局中央气象台.0604号台风路径图[EB/OL].(2008-04-11),http://www.weathercn.com/maps/index.jsp?classlid=4&class2id=50.
计量
- 文章访问数: 1013
- HTML全文浏览量: 17
- PDF下载量: 1156
- 被引次数: 0