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渤海湾海岸带环境演变及控制因素研究
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摘要
本文主要利用海岸带卫星遥感影像处理技术和沉积动力数值模拟的手段,依托国家“908专项”在渤海湾海洋底质调查资料和近岸海洋工程建设中的调查资料,收集了潮位、潮流、水深地形等资料,结合前人研究成果,对渤海湾近四十年来海岸带环境演变进行了较为全面的研究,并对其演变的控制因素进行了分析和探讨。
     通过对渤海湾不同时期卫星遥感影像的研究发现,渤海湾近四十年来海岸形态发生了巨大变化。海岸线不断向海洋推进,最远达20多公里,海岸线长度呈现先轻微减小后大幅度增加的趋势,至2010年除部分河口类岸线外,其它海域沿岸几乎全部变为人工海岸线。海湾面积一直呈现逐渐缩小的趋势,并且面积减小速率逐渐增大,海湾的纳潮量也呈现逐年递减的趋势,2010年的纳潮量比1975年共减小了约13.15%。
     渤海湾表层沉积物调查资料表明,表层沉积物类型主要由砂、粉砂质砂、砂质粉砂、粉砂和粘土质粉沙组成,沉积物粒度整体呈现中部和南部细、北部较粗的特点。通过对比不同时期的表层沉积物资料,发现不同海域表层沉积物在时间序列上发生了一定的变化。
     数值模拟结果表明,1984至2010年间渤海湾大量的海岸工程建设改变了海湾水动力条件,渤海湾南部和西部近岸海域潮流流速和流向变化比较大,北部和中部潮流变化相对较小,流速略有增加,流向变化非常小。随着渤海湾水动力条件的改变,导致部分岸段发生潮滩淤涨,部分岸段发生侵蚀,海底冲淤环境发生了一定的变化。
     渤海湾海岸带环境的演变是自然环境因素和人类活动影响共同作用的结果,而人类开发利用海洋的活动在环境演变中的作用则越来越明显和越来越重要。
The coastal remote sensing image processing technique and sedimentary dynamic numericalsimulation method are mainly applied in this paper. The marine sediment data mainly derived fromthe national "908" survey project and the survey of marine engineering construction in Bohai Bay,and the tide, tidal current, bathymetric data are also collected. Based on the above techniques anddata, combined with the results of previous studies, the author research the coastal environmentevolution of the Bohai bay in the recent40years, and the controlling factors of the evolution areanalyzed and discussed.
     Great changes have taken place in coastal line and morphology in the recent40years based onthe study of different periods of remote sensing satellite image in Bohai Bay. The coastline extendedtowards the marine all the time, and the most distance was more than20kilometers. The length ofthe coastline appears to decrease slightly first and then increased substantially. Almost all the typesof the coastline in the bay have turned into artificial coastline except for some estuary classcoastline since2010.The area of the bay has been decreasing, and the reduction rate graduallyincreased. The tidal prism of the bay has also been decreasing, and the tidal prism of the baydecreased about13.15%between the nearly40years.
     The survey data of surface sediment in Bohai Bay shows that, the surface sediment types areprimarily composed of sand, silty sand, sandy silt sand, silt and clay silt. The feature of the sedimentis that the grain size is coarse in northern and thin in central and southern of the bay. By comparingthe different periods of surficial sediment data, the author found that surface sediment in differentsea area changed in temporal sequence.
     The results of numerical simulation show that, between1984and2010, the hydrodynamicconditions in Bohai Bay changed greatly because of the coastal engineering constructions. Thecoastal current velocity and direction in southern and western of the bay changed bigger than that innorthern and central of the bay. With the change of hydrodynamic condition in Bohai Bay, some portion of coast caused deposition, and some caused erosion, and the seabed erosion and depositionenvironment obviously changed.
     The coastal environment evolution of Bohai bay was affected by the natural environmentfactors and the human activities factor. In recent years, with the increase of the human activities onthe sea development, its impact on the environment evolution was becoming more and moreobvious and important, which affected coastal environment evolvement all the time.
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