首页> 外文期刊>Earth Surface Processes and Landforms: The journal of the British Geomorphological Research Group >Block removal and step backwearing as erosion processes on rock shore platforms: A preliminary case study of the chalk shore platforms of south-east England
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Block removal and step backwearing as erosion processes on rock shore platforms: A preliminary case study of the chalk shore platforms of south-east England

机译:岩石海岸平台上的块体去除和台阶磨耗作为侵蚀过程:英格兰东南部粉笔海岸平台的初步案例研究

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摘要

Shore platforms frequently exhibit steps or risers facing seaward, landwards or obliquely across-shore. A combination of soft copy photogrammetry, ortho-rectification, geo referencing and field measurement of step height are linked in a GIS environment to measure step retreat on chalk shore platforms at sample sites in the south of England over two periods, 1973-2001, 2001-2007. The methods used allow for the identification, delineation and measurement of historic change at high spatial resolution. The results suggest that while erosion of chalk shore platforms by step backwearing is highly variable, it appears to be of similar magnitude to surface downwearing of the same platforms measured by micro-erosion meters (MEMs) and laser scanning, in a range equivalent to 0·0006 - 0·0050my~(-1) of surface downwearing. This equates to annual chalk volume loss from the platforms, by the two erosion processes combined, of between 0·0012m~3m~(-2) and 0·0100m~3m~(-2). Results from the more recent years' data suggests that step retreat has variability in both space and time which does not relate solely to climatic variability. The results must be viewed with caution until much larger numbers of measurements have been made of both downwearing and step erosion at higher spatial and temporal resolution.
机译:岸上平台经常表现出面向海,陆或斜跨岸的台阶或立管。在GIS环境中将软拷贝摄影测量法,正射矫正,地理参考和台阶高度的现场测量结合起来,以测量1973-2001年和2001年在英格兰南部两个地点的粉笔海岸平台上的台阶后退-2007。所使用的方法可以在高空间分辨率下识别,描绘和测量历史变化。结果表明,虽然通过逐步回磨对粉笔海岸平台的侵蚀变化很大,但看起来与通过微腐蚀仪(MEM)和激光扫描测量的同一平台的表面磨损程度相近,其范围为0 ·0006--0·0050my〜(-1)的表面磨损。这等于通过两个侵蚀过程相结合,平台每年的白垩体积损失在0·0012m〜3m〜(-2)和0·0100m〜3m〜(-2)之间。近年来数据的结果表明,步退在空间和时间上均具有可变性,而不仅仅是与气候可变性有关。必须仔细查看结果,直到在较高的空间和时间分辨率下对磨损和阶梯腐蚀进行了大量测量为止。

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