岩石材料位移的岩性指数作为边坡敏感性评估的一部分

Q4 Earth and Planetary Sciences
M. Wódka
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引用次数: 0

摘要

在滑坡研究中使用多时相激光雷达数据提供了许多可能性。随着时间的推移,alsdata的可用性越来越高,这鼓励了使用差分数字地形模型开发滑坡的研究。决定滑坡(特别是喀尔巴阡山脉)发展的一个重要被动因素是岩性。作者提出了一个新的岩性位移指数,用来描述给定岩性单位每平方米面积上的位移地面体积(m3)。罗奥诺斯基湖试验区的实例表明,岩性位移指数可以评价滑坡的易感性,但其易感性是可变的,且受降雨量的影响。在强降雨期间,厚层地层中记录了大量的位移岩体。在干旱期,这一趋势则相反。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Litologiczny wskaźnik przemieszczeń materiału skalnego jako element oceny podatności stoków na osuwanie
The use of multi-temporal LIDAR data in the study of landslides gives many possibilities. The increasing-over-timeavailabilityofALSdataencouragedresearchondevelopmentoflandslidesusingDifferentialDigital Terrain Models. An important passive factor that determines the development of landslides (especially in the Carpathians) is lithology. The author propose a new lithological displacement index, that dscribes the volume of displaced ground (m3) per area of 1 m2 of a given lithological unit. The example of the test area of Ro¿nowskie Lake has shown that lithological displacement index can assess the landslide susceptibility, which is variable and depends on the amount of rainfall. During periods of heavy rainfall, large volumes of displaced rock masses were recorded in the thick-bedded formations. In dry periods, the trend is reversed.
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来源期刊
Przeglad Geologiczny
Przeglad Geologiczny Earth and Planetary Sciences-Geology
CiteScore
0.70
自引率
0.00%
发文量
24
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