基于10年监测结果的港口对周边海岸的影响:港口Sillamäe案例研究(波罗的海芬兰湾)

H. Tõnisson, R. Aps, K. Orviku, U. Suursaar, S. Sasi, A. Kont
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引用次数: 1

摘要

目前的研究重点是海岸过程和Sillamäe镇的沿海海。在最近的过去,Sillamäe附近的海岸从Voka定居点向西开始,结束于Kannuka角的顶部,被描述为一个具有良好自然平衡的岩性动力系统。本文的主要目的是分析港口建设对Sillamäe镇附近海岸演变和沉积物预算变化的影响,基于定期监测结果(9个不同的海岸剖面-使用RTK-GPS或徕卡水平,在几个地点重复拍摄照片,海岸线测绘-使用RTK-GPS或手持GPS,陡崖测量-使用正射影像仪和RTK-GPS)。结果表明,在研究的大部分海岸沿线,要么是稳定的地貌状态,要么是缓慢的堆积状态。在更强的风暴之后,研究地点的几个部分记录了偶尔的侵蚀事件。然而,这些变化大多是暂时的,通常在侵蚀事件发生后不久就会恢复稳定状态。最后,我们可以得出结论,2004-2013年的海岸过程监测没有记录到受新港直接影响的海岸的任何变化。海岸上的重大变化是由自然极端事件引起的。这些事件造成的海岸过程变化与爱沙尼亚其他自然发展地点所记录的变化相当。
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The impact of a port to the surrounding shores based on the 10 years monitoring results: Port of Sillamäe case study (Gulf of Finland, Baltic Sea)
The current study was focusing on the shore processes and the coastal sea fronting Sillamäe town. The shores near the Sillamäe starting west from the Voka settlement and ending at the top of Cape Kannuka were described as one litho dynamic system with a good natural balance in the recent past. The main aim of the paper was to analyse the impact of a port establishment to the changes in the coastal evolution and sediment budget in the vicinity of Sillamäe town based on the regular monitoring results (9 different shore profiles - by using RTK-GPS or Leica level, repeated photographs in several locations, shoreline mapping - by using RTK-GPS or handheld GPS, scarp measurements - by using orthophotos and RTK-GPS). The results suggest that either a stable geomorphic state or a slow accumulation prevailed along major part of the studied coast. After stronger storms, occasional erosion events were registered in several sections of the study site. However, these changes were mostly temporary and a stable state was usually restored soon after the erosion event. Finally, we can conclude that the monitoring of shore processes from 2004-2013 has not registered any changes on the shores directly influenced from the new harbour. Major changes on the shores are caused by natural extreme events. The changes in shore processes resulted from these events are comparable to the ones registered in the other naturally developing sites in Estonia.
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