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首页> 外文期刊>Natural hazards and earth system sciences >Analysing the spatial patterns of erosion scars using point process theory at the coastal chalk cliff of Mesnil-Val, Normandy, northern France
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Analysing the spatial patterns of erosion scars using point process theory at the coastal chalk cliff of Mesnil-Val, Normandy, northern France

机译:使用点过程理论分析法国北部诺曼底梅斯尼尔瓦尔的沿海粉笔崖上侵蚀痕迹的空间格局

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摘要

Over the last decade, many cliff erosion studies have focused on frequency-size statistics using inventories of sea cliff retreat sizes. By comparison, only a few paid attention to quantifying the spatial and temporal organisation of erosion scars over a cliff face. Yet, this spatial organisation carries essential information about the external processes and the environmental conditions that promote or initiate sea-cliff instabilities. In this article, we use summary statistics of spatial point process theory as a tool to examine the spatial and temporal pattern of a rockfall inventory recorded with repeated terrestrial laser scanning surveys at the chalk coastal cliff site of Mesnil-Val (Normandy, France). Results show that: (1) the spatial density of erosion scars is specifically conditioned alongshore by the distance to an engineered concrete groyne, with an exponential-like decreasing trend, and vertically focused both at wave breaker height and on strong lithological contrasts; (2) small erosion scars (10(-3) to 10(-2) m(3)) aggregate in clusters within a radius of 5 to 10 m, which suggests some sort of attraction or focused causative process, and disperse above this critical distance; (3) on the contrary, larger erosion scars (10(-2) to 10(1) m(3)) tend to disperse above a radius of 1 to 5 m, possibly due to the spreading of successive failures across the cliff face; (4) large scars significantly occur albeit moderately, where previous large rockfalls have occurred during preceding winter; (5) this temporal trend is not apparent for small events. In conclusion, this study shows, with a worked example, how spatial point process summary statistics are a tool to test and quantify the significance of geomorphological observation organisation.
机译:在过去的十年中,许多悬崖侵蚀研究都集中在使用海崖撤退规模清单进行频率大小统计上。相比之下,只有极少数人关注量化悬崖表面侵蚀痕迹的时空组织。然而,这种空间组织携带着有关促进或引发海崖不稳定的外部过程和环境条件的重要信息。在本文中,我们使用空间点过程理论的摘要统计数据作为工具,通过在Mesnil-Val(法国诺曼底)的白垩沿海峭壁站点进行的反复地面激光扫描勘测来检查落石清单的时空格局。结果表明:(1)侵蚀疤痕的空间密度特别受到沿岸至工程混凝土防波堤的距离的影响,呈指数状下降趋势,并且既垂直于波浪破碎器高度,又受到强烈的岩性对比。 (2)小侵蚀痕迹(10(-3)至10(-2)m(3))聚集在半径5至10 m内的簇中,这表明存在某种吸引或集中的致病过程,并在其上方分散临界距离(3)相反,较大的侵蚀疤痕(10(-2)至10(1)m(3))倾向于在半径1至5 m上方散布,这可能是由于连续破坏遍及整个悬崖面所致; (4)大疤痕虽然适度,但在先前的冬季曾发生过大的崩落,但仍明显发生。 (5)对于小事件,这种时间趋势并不明显。总而言之,本研究以一个工作实例展示了空间点过程摘要统计如何成为测试和量化地貌观测组织重要性的工具。

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