确定由于70年代港口建设而导致的Saldanha湾水深变化

IF 0.3 Q4 REMOTE SENSING
Ivan Henrico, J. Bezuidenhout
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引用次数: 8

摘要

测深学是研究和测量海底深度的科学。利用地理信息系统(GIS)研究了水深、水下坡度和海底结构的差异。本文研究了20世纪70年代初港口建设对萨尔达尼亚湾水动力沉积过程的影响。港口的建设包括大规模的疏浚作业和由此产生的3000万立方米土壤的迁移。在ArcGIS中分析和比较了70年代初港口建设之前(1957年)和之后(1977年)Saldanha湾的水深数据。研究发现,Saldanha湾内部的总深度增加了约1.4米,底部和斜坡也变得平滑。为港口建造的物理结构对水动力沉积过程产生了严重影响。研究发现,这些干预措施改变了Saldanha湾的深度剖面,文章最终根据Saldanha海湾水动力沉积过程的变化,得出了关于海岸和海滩形成的结论。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Determining the change in the bathymetry of Saldanha Bay due to the harbour construction in the seventies
Bathymetry is the science to study and measure the depths of the ocean floor. The differences in water depth, underwater slope and ocean floor structure were investigated using a geographic information system (GIS). This article investigates changes to the hydrodynamic sedimentation processes in Saldanha Bay as a result of the harbour constructions that took place in the early 1970s. The construction of the harbour included the massive dredging operations and resultant relocation of 30 million m3 of soil. Bathymetric data from Saldanha Bay before (1957) and after (1977) the construction of the harbour in the early seventies were analysed and compared in ArcGIS. It was found that the overall depth of the inner part of Saldanha Bay increased with about 1.4 m and that the bottom and slopes were smoothed. The physical structure that was constructed for the harbour had a serious impact on the hydrodynamic sedimentation processes. It was found that these interventions altered the depth profile of the Bay and the article finally draws conclusions on coastal and beach formation, based on the change in the hydrodynamic sedimentation processes of Saldanha Bay.
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