fig17

Figure 17. The relationships between Lf /H and crtanφr/γH for clay slopes with (A) β = 45°; (B) β = 40°; (C) β = 35°; and (D) β = 30°, respectively.
Figure 17. The relationships between Lf /H and crtanφr/γH for clay slopes with (A) β = 45°; (B) β = 40°; (C) β = 35°; and (D) β = 30°, respectively.
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