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首页> 外文期刊>Journal of Coastal Research: An International Forum for the Littoral Sciences >Long-Term Morphological Evolution of a Tidal Island as Affected by Natural Factors and Human Activities, the Yangtze Estuary
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Long-Term Morphological Evolution of a Tidal Island as Affected by Natural Factors and Human Activities, the Yangtze Estuary

机译:长江口受自然因素和人类活动影响的潮汐岛长期形态演变

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摘要

Bathymetric data based on sounding surveys and intertidal elevations measured using Real-Time Kinematic Global Positioning System methodology were analyzed using Geographical Information System techniques to examine the morphological evolution of the tidal island Jiu Duan Sha (JDS) in the Yangtze estuary. It was found that, from 1958 to 2005, the area and sediment volume of JDS increased by 96% and 156% above the 5 m isobath and by 331% and 504% above the Lowest Astronomic Tide (LAT). Specifically, the maximum elevation of the island increased from 0.3 to 4.9 m above the LAT, and the salt marsh increased from 0% to 40% of the intertidal area. The dominant factor controlling the growth of this wetland was found to have varied with time. The growth was mainly due to the deposition of riverine sediment before the 1970s but was primarily the result of the merging of a shoal into JDS between 1971 and 1994 and, later, the local engineering projects between 1994 and 2005. It was concluded that human activities are playing an increasingly important role in the morphological evolution of tidal wetlands in the Yangtze estuary.
机译:基于测深调查的潮汐数据和使用实时运动学全球定位系统方法测得的潮间高程,使用地理信息系统技术进行了分析,以检查长江口九段沙(JDS)的形态演变。研究发现,从1958年到2005年,JDS的面积和沉积物量比5 m等值线高出96%和156%,比最低天文潮(LAT)高出331%和504%。具体来说,该岛的最大海拔从LAT上方增加0.3到4.9 m,盐沼从潮间带面积的0%增加到40%。发现控制该湿地生长的主要因素随时间变化。增长主要是由于1970年代之前河道沉积物的沉积,但主要是由于浅滩在1971年至1994年之间合并到JDS中,以及后来在1994年至2005年之间在当地进行的工程项目的结果。得出的结论是,人类活动在长江口的潮汐湿地形态演变中起着越来越重要的作用。

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