Barely Significant

Excerpts

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HR showed a gradual increase in D-value in the shallow soil layer (0–40 cm); CF showed a gradual increase in the middle soil layer (40–140 cm); CF showed a slight decrease in the deeper soil layer (140–200 cm), while the other three vegetation showed an increasing trend in deeper soil layer.
Figure 10 depicts an increasing trend in the east–west cumulative deformation of observation points within the Maojiayu landslide, whereas the Taohuasi landslide area shows a more pronounced increasing trend in east–west cumulative deformation, though the overall magnitude of deformation remains small.