Research Article

Rigorous Solution of Slopes’ Stability considering Hydrostatic Pressure

Table 1

Variation of the ultimate loads and the distribution of the sliding belt with the depth .

Ground water depth (m)Ultimate load (kPa) (m) (m)
Rigid regionPlastic region (average)

077.80107.692.320.87
0.577.54107.252.320.87
1.076.69106.742.310.87
1.573.34105.392.310.86
2.070.78104.382.300.86
2.564.09101.672.290.86
3.059.8399.932.280.85
4.043.8993.512.270.85
No ground water33.8586.982.250.85