地球资源卫星图像在震后滑坡制图中的应用,以2012年伊朗西北部Ahar-Varzegan地震为例

IF 1 Q4 GEOSCIENCES, MULTIDISCIPLINARY Iranian Journal of Earth Sciences Pub Date : 2020-10-01 DOI:10.30495/IJES.2020.677468
Leila Khodaei Geshlag, S. Roostaei, D. Mokhtari, K. Valizadeh
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引用次数: 0

摘要

2012年Ahar-Varzegan地震及其余震不仅造成了巨大的破坏和严重的生命财产损失,而且诱发了许多地质灾害,主要类型为崩塌、蠕变、滑动、泥石流和坠落,在本研究中通常被认为是滑坡,对受灾地区造成持续的威胁。本文提出了一种半自动化的地质灾害检测方法,利用地震前后的双时相Landsat图像来确定2012年阿哈尔-瓦尔扎汗地区的阿哈尔-瓦尔扎汗地震引发的滑坡。利用野外观测、谷歌地球图像和误差矩阵检验了结果的准确性。与谷歌地球影像的视觉验证结果表明,所采用的方法能够以较高的精度检测滑坡。由于landsat5和landsat8的多光谱优势,可以作为研究不稳定性的合适数据源。最后,利用误差矩阵得到的验证结果表明,总准确率为92.1%,kappa系数为0.99。因此,根据上述方法得到的结果,滑坡主要分布在15 ~ 40度的斜坡上,失稳高度分布在1420 ~ 2000米。同样基于植被指数,地震后滑坡密度有所增加。不稳定边坡一般位于深谷陡坡山区的河谷和道路沿线。根据本研究的性质,所得结果可为环境规划者及项目发展商提供参考。
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Application of landsat imageries for mapping post-earthquake landslide, case study: 2012 Ahar-Varzegan earthquake, NW Iran
The 2012 Ahar-Varzegan earthquake and its aftershocks have not only caused huge damage with a severe loss of life and property but also induced many geo-hazards with the major type of collapse, creep, slip, debris flow, and fallings that are generally considered as landslide in this study which can cause continuous threats to the affected region. in this study, a semi-automated geo-hazard detection method has been presented to determine the Landslides due to 2012 Ahar-Varzaghan earthquake in area from Ahar to Varzaghan by the use of bi- temporal Landsat images from before and after the earthquake. The accuracy of the results was checked out using field observations, Google Earth images and the error matrix. The results of the visual validation with the Google Earth images showed that the used method can detect landslids with relatively high accuracy.The images of landsat5 and 8 Because of their multispectral advantages can be used as a suitable data source for research on Instabilities. Finally, the validating results obtained by using the error matrix showed the total accuracy of 92.1% and kappa coefficient was 0.99. So based on the results obtained from the above method, the landslides were distributed mainly in slopes between 15 and 40 degrees and the height distribution of instabilities of 1420 to 2000 meters. Also based on vegetation indices, density of landslides have been increased after the earthquake. Generally unstabel slopes are located along river valleys and roads in mountain regions with deep valleys and steep slopes. According to the nature of present study, the obtained result can be useful for environmental planners and project developers.
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来源期刊
Iranian Journal of Earth Sciences
Iranian Journal of Earth Sciences GEOSCIENCES, MULTIDISCIPLINARY-
CiteScore
1.40
自引率
12.50%
发文量
0
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