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首页> 外文期刊>Engineering Geology >First delimitation of areas affected by ground deformations in the Guadalfeo River Valley and Granada metropolitan area (Spain) using the DInSAR technique
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First delimitation of areas affected by ground deformations in the Guadalfeo River Valley and Granada metropolitan area (Spain) using the DInSAR technique

机译:使用DInSAR技术首次划定瓜达菲奥河谷和格拉纳达都会区(西班牙)的地面变形影响区域

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摘要

A Differential Interferometric SAR (DInSAR) analysis of terrain displacements in the province of Granada (southern Spain) is presented here for two different study zones. The first zone concerns the Guadalfeo River Basin, where abundant landslides and unstable slopes were previously identified and inventoried on a GIS application. However, no instrumental quantification of landslide activity was available. Considering morphological criteria and field observations, these deep-seated landslides were considered to be "dormant" or moving extremely slowly. The second study zone corresponds to the Granada metropolitan area, where no previous information was available on any vertical movement. The analysis was based on ERS1 and ERS2 images, covering the period from 1993 to 2000. By using DInSAR, we made an initial qualitative assessment of movements on landsliding slopes in the Guadalfeo River Basin and also vertical land movements in the alluvial Quaternary sediments to the west and south of the Granada metropolitan area. The terrain instability assessment resulting from this research shows maximum annual velocities along the SAR line of sight (LOS) of 6 mm/yr for the Tablones landslide, and up to 13 mm/yr for the Albunuelas village; where progressive differential settlement processes were established as the origin of the movement. In the case of the Granada metropolitan area, two sites were detected with subsidence affecting two villages: Santa Fe, located in the western part of the area, with an estimated average velocity of 8 mm/yr and Otura in the south of the area, with maximum velocities of 12 mm/yr. A description of geological features of the different sites, showing LOS ground displacement, is presented with a discussion of the application of the rates to landslide-activity assessment found, local ground conditions, or exploitation of subterranean water in urban areas.
机译:本文针对两个不同的研究区,对格拉纳达省(西班牙南部)的地形位移进行了差分干涉SAR(DInSAR)分析。第一个区域涉及瓜达尔福河流域,该流域先前已通过GIS应用程序识别并清查了大量滑坡和不稳定的斜坡。但是,没有对滑坡活动进行仪器量化的工具。考虑到形态学标准和野外观察,这些深层滑坡被认为是“休眠”或移动非常缓慢。第二个研究区域对应于格拉纳达大都会地区,该地区以前没有关于任何垂直运动的信息。该分析是基于ERS1和ERS2图像(涵盖1993年至2000年)。通过使用DInSAR,我们对Guadalfeo流域滑坡的运动以及冲积第四纪沉积物到陆地的垂直陆地运动进行了初步定性评估。格拉纳达都会区的西部和南部。这项研究得出的地形不稳定性评估结果表明,塔布洛尼斯滑坡沿SAR视线(LOS)的最大年速度为6 mm / yr,Albunuelas村高达13 mm / yr。建立了逐步的差异解决过程作为运动的起源。以格拉纳达市区为例,发现有两个地点的沉降影响了两个村庄:位于该地区西部的圣达菲(Santa Fe),估计平均速度为8毫米/年;位于该地区南部的奥图拉(Otura);最大速度为12毫米/年。介绍了不同地点的地质特征,显示了LOS地面位移,并讨论了将速率应用于发现的滑坡活动评估,当地地面条件或城市地区地下水开采的讨论。

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