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首页> 外文期刊>Natural hazards and earth system sciences >Factors selection in landslide susceptibility modelling on large scale following the gis matrix method: Application to the river Beiro basin (Spain)
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Factors selection in landslide susceptibility modelling on large scale following the gis matrix method: Application to the river Beiro basin (Spain)

机译:遵循GIS矩阵方法的大规模滑坡敏感性模型中的因素选择:在贝罗河盆地(西班牙)中的应用

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摘要

A procedure to select the controlling factors connected to the slope instability has been defined. It allowed us to assess the landslide susceptibility in the Rio Beiro basin (about 10 km2) over the northeastern area of the city of Granada (Spain). Field and remote (Google EarthTM) recognition techniques allowed us to generate a landslide inventory consisting in 127 phenomena. To discriminate between stable and unstable conditions, a diagnostic area had been chosen as the one limited to the crown and the toe of the scarp of the landslide. 15 controlling or determining factors have been defined considering topographic, geologic, geomorphologic and pedologic available data. Univariate tests, using both association coefficients and validation results of single-variable susceptibility models, allowed us to select the best predictors, which were combined for the unique conditions analysis. For each of the five recognised landslide typologies, susceptibility maps for the best models were prepared. In order to verify both the goodness of fit and the prediction skill of the susceptibility models, two different validation procedures were applied and compared. Both procedures are based on a random partition of the landslide archive for producing a test and a training subset. The first method is based on the analysis of the shape of the success and prediction rate curves, which are quantitatively analysed exploiting two morphometric indexes. The second method is based on the analysis of the degree of fit, by considering the relative error between the intersected target landslides by each of the different susceptibility classes in which the study area was partitioned. Both the validation procedures confirmed a very good predictive performance of the susceptibility models and of the actual procedure followed to select the controlling factors.
机译:已经定义了选择与斜坡不稳定性相关的控制因素的程序。它使我们能够评估格拉纳达市(西班牙)东北地区里约贝罗盆地(约10 km2)的滑坡敏感性。现场和远程(Google EarthTM)识别技术使我们能够生成包含127种现象的滑坡清单。为了区分稳定状态和不稳定状态,已选择诊断区域作为仅限于滑坡顶和趾尖的区域。考虑地形,地质,地貌和儿科的可用数据,已经定义了15个控制或决定因素。使用关联系数和单变量磁化率模型的验证结果进行的单变量检验使我们能够选择最佳预测变量,将其组合起来进行独特的条件分析。对于五种公认的滑坡类型中的每一种,都准备了最佳模型的敏感性图。为了验证拟合优度和磁化率模型的预测技巧,应用了两种不同的验证程序并进行了比较。两种程序都基于滑坡档案库的随机分区,以产生测试和训练子集。第一种方法是基于对成功曲线的形状和预测率曲线的分析,并利用两个形态计量指标对其进行定量分析。第二种方法是基于适合度的分析,通过考虑划分研究区域的每个不同的磁化率类别,考虑相交的目标滑坡之间的相对误差。两种验证程序都证实了敏感性模型和选择控制因素所遵循的实际程序具有很好的预测性能。

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