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For TUNEL assay SK-N-SH cells were seeded in BD Falcon™ 8-well culture slides (surface area 0.7 cm2/well) at 104 cells/well.
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Note that the source area, the depth of the sliding surface, and the volume of the landslide mass could be estimated according to the topographical maps before and after the earthquake.
It is suggested that in the source area, the landslide gained velocity when the "sliding surface liquefaction" phenomenon occurred as a result of undrained shearing in a saturated sliding zone.
In the source area, there was much slide debris that remained, covering the sliding surface of the landslide, making it difficult to determine the material in the slide zone.
It could be inferred from the geological setting of the source area that during the initiation stage of the landslide, the mass moved approximately northward on the sliding surface, as shown in Fig. 1.
A sliding surface functional is firstly constructed.
Landslide S10 has imminent sliding cliff, collapsed valley, hilly landslide mass and arc-shaped sliding surface, featuring multiphase sliding.
Firstly, a new integral sliding mode surface named stochastic sliding surface (SSS) is introduced.
A thin, weak layer developed along the sliding surface.
Sassa et al. ([2004]) called this phenomenon "sliding surface liquefaction".
FL is used to automatically adjust the variable gain based on sliding surface and derivative of the sliding surface.
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