Research Article

An Improved Approach of Classical Upper Bound Theory for Stability Analysis of Layered Slopes

Table 2

Comparison of Ns between researchers and the presented for layered slopes with of 20° (Example 1).

mSource
45°50°55°60°65°70°75°80°

0.2Kumar and Samui [20]15.6913.6011.8610.308.957.897.066.32
Sun et al. [21]13.5111.7210.309.228.297.466.77
Present15.6113.5111.7310.339.238.307.496.78

0.4Kumar and Samui [20]13.8612.1010.789.478.57.556.065.56
Sun et al. [21]12.8411.219.948.917.296.615.81
Present15.0612.8511.229.968.928.367.306.62
Geo-Slope (Morgenstern–Price)15.318.307.516.80

0.6Kumar and Samui [20]13.2611.7810.489.228.257.316.65.95
Sun et al. [21]11.7010.639.248.357.596.916.31
Present13.5311.7210.349.268.367.596.926.31