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Correlation between soil erosion by water and degradation, retrogradation phenomena

机译:水分降解土壤侵蚀之间的相关性,逆行现象

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Soil erosion varies greatly over space and neglecting information about estimation uncertainty may lead to inappropriate decision-making. Spatially distributed models coupled with Geographic Information System and a geo-statistical approach allow to identify areas sensitive of soil loss and carry out a good representation of the erosion process. Slope instability is correlated to landslide generation in soil retrogradation and degradation process. The objective of this paper is to carry out and validate correlation between soil erosion process and slope instability, degradation and retrogradation phenomena, and to propose a procedure that allows mapping the areas more prone to risk erosion and happening landslide generation in soil retrogradation and degradation process from the proposed correlation. Using a graphic calculation, based on LabView tool, from the proposed correlation is possible to previously localize and mapping the areas more prone to soil erosion phenomena. So using the proposed approach it's possible to previously identify the areas that could be interest from intense erosive phenomena. The first results show as the proposed procedure identifies the foot of the registered landslide and other areas interested by this phenomena, with an accuracy that allow urban planning as a decision making support. From the body to the crown of the landslide, the model prediction is less accurate. It is due to the fact that the landslide generation happened by retrogradation phenomena. By the first fall, the slope equilibrium become precarious, so it's realize slope instability conditions and it starts a trigger effect in case of aggressive rainfall or earthquakes, which begin the landslide phenomena by retrogradation. An important future development of these studies can be the mapping with accuracy and precision of the total area interested in these phenomena using the equilibrium slope models coupled with the proposed approach.
机译:土壤侵蚀在空间上变化很大,忽视有关估计不确定性的信息可能导致不恰当的决策。空间分布式模型与地理信息系统耦合,地理统计方法允许识别土壤损失敏感的区域,并进行侵蚀过程的良好代表。边坡不稳定性与土壤逆转和降解过程中的滑坡产生相关。本文的目的是在土壤侵蚀过程和坡度不稳定性,降解和逆转现象之间进行相关性和验证相关性,并提出一种允许在土壤逆转和降解过程中更容易发生风险侵蚀和发生滑坡生成的地位的程序。从提出的相关性。使用基于LabVIEW工具的图形计算,从所提出的相关性可以以前可以定位和映射更容易产生土壤侵蚀现象的区域。因此,使用所提出的方法可以以前识别可能来自激烈的侵蚀现象的区域。第一个结果表明,作为所提出的程序,确定了登记的滑坡和这种现象感兴趣的其他地区的脚,精确允许城市规划作为决策支持。从身体到滑坡的冠冕,模型预测不太准确。这是由于逆行现象发生的山体滑坡。在第一次下降,坡度平衡变得不稳定,因此它是实现坡度不稳定条件,并且在积极的降雨或地震的情况下开始触发效果,从而通过逆行开始滑坡现象。这些研究的重要未来发展可以是使用与所提出的方法相结合的均衡斜坡模型对这些现象感兴趣的总面积的准确性和精度的映射。

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