2022
DOI: 10.3390/ijerph19063229
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Susceptibility Analysis of Geohazards in the Longmen Mountain Region after the Wenchuan Earthquake

Abstract: Multitemporal geohazard susceptibility analysis can not only provide reliable results but can also help identify the differences in the mechanisms of different elements under different temporal and spatial backgrounds, so as to better accurately prevent and control geohazards. Here, we studied the 12 counties (cities) that were severely affected by the Wenchuan earthquake of 12 May 2008. Our study was divided into four time periods: 2008, 2009–2012, 2013, and 2014–2017. Common geohazards in the study area, suc… Show more

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Cited by 10 publications
(8 citation statements)
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“…In DA, the NDVI value changed greatly from 2007 to 2009 ( Figure 6 ). Due to the influence of the Wenchuan earthquake, the relatively strong vibration around the fault caused varying degrees of vegetation damage [ 67 ]. Secondary disasters such as landslides and collapses caused by the earthquake in this area gradually transformed the forest land into grassland or bare land [ 68 , 69 ].…”
Section: Resultsmentioning
confidence: 99%
“…In DA, the NDVI value changed greatly from 2007 to 2009 ( Figure 6 ). Due to the influence of the Wenchuan earthquake, the relatively strong vibration around the fault caused varying degrees of vegetation damage [ 67 ]. Secondary disasters such as landslides and collapses caused by the earthquake in this area gradually transformed the forest land into grassland or bare land [ 68 , 69 ].…”
Section: Resultsmentioning
confidence: 99%
“…Topography plays an important role in controlling geological hazards and determines the spatial distribution of geological hazard susceptibility to a large extent [ 36 ]. The study area is mainly mountainous, with a large difference in elevation between mountains and plains.…”
Section: Discussionmentioning
confidence: 99%
“…Elevation (E): Elevation is an inherent assessment indicator of landslide occurrence [ 36 ]. The study area is a hilly area with a maximum elevation difference of 1834 m. Since many indicators are changing with the dramatic ups and downs in the study area, the elevation becomes an indispensable indicator affecting the occurrence of landslides.…”
Section: Methodsmentioning
confidence: 99%
“…The developed cracks lead to rock and soil breakage, increase the water richness of rock layers, and accelerate rock erosion. In addition, a large number of secondary small faults are often developed near the large fault structural belt [52,53]. Regional tectonics leads to the complexity of geological conditions in the study area and aggravates the probability of landslide disasters.…”
Section: Geological and Hydrogeological Factorsmentioning
confidence: 99%