Research Article
Study on the Loess Immersion Test of Metro Line 2 in Xi’an, Shaanxi Province, China
Table 3
Calculation table of deep subsidence of deep markers.
| | 
 |  | Soil layer | Depth of the marker (m) | Deformation of the marker (mm) | Depth of the soil layer (m) | Deformation of the soil layer (mm) |  | 
 |  | New loess | 6.50 | −9.95 | 6.5–9.4 | −10.05 |  | 9.40 | 0.1 | 9.4–12.4 | 0.1 |  | 
 |  | Paleosol | 12.40 | 0 | 12.4–14 | 0.95 |  | 
 |  | Old loess | 14.00 | −0.95 | 14–16 | 0.25 |  | 16.00 | −1.2 | 16–18 | −1.35 |  | 18.00 | 0.15 | 18–20 | 0.15 |  | 20.00 | 0 | 20–22.5 | 8.6 |  | 
 |  | Paleosol | 22.50 | −8.6 | 22.5–23.5 | 0 |  | 
 |  | Old loess | 23.50 | −8.6 | 23.5–24.5 | −9.1 |  | 
 |  | Paleosol | 24.50 | 0.5 | 24.5–28 | 1.5 |  | 
 |  | Old loess | 28.00 | −1 | 28–30.5 | −1.05 |  | 30.50 | 0.05 | 30.5–33 | 0.55 |  | 
 |  | Paleosol | 33.00 | −0.5 | ≥33 | −0.5 |  | 
 | 
 | 
| Negative for subsidence; positive for elevation.
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