An early identification method of loess landslide based on land subsidence information
A land subsidence and early identification technology, which is applied in the direction of surveying instruments, instruments, surveying and navigation, etc., can solve the problems of limited coverage, low degree of automation, and high cost, so as to reduce field workload, improve accuracy, and operate simple effect
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[0030] The specific implementation method is as follows: Interferometric processing is performed on the SAR image of the research area, and the annual rate of ground deformation in the area is obtained by the time-series InSAR method, and then the land subsidence information is obtained. When the land subsidence in the area is caused by the change of groundwater, it is considered that The area has the necessary conditions for landslides within a certain range.
[0031] The next step is to confirm the specific location of the landslide.
[0032] The change of groundwater level is the first condition. When the groundwater level of a certain place has the same change trend as the groundwater level of the ground subsidence center, a landslide may form there, and this area is A.
[0033] Slope and aspect constitute the second condition. The slope requirement of a single landslide is 30°-50°, and the area that meets these conditions is B.
[0034] The third condition is the seepage...
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