DHARM
BEARING CAPACITY 587
If Df = 1.5 m,
qult = γDf
1
1
2
+
−
F
HG
I
KJ
sin
sin
φ
φ
= 18 × 1.5
118
118
2
+°
−°
F
HG
I
KJ
sin
sin
= 96.8 kN/m^2.
Example 14.3: Calculate the ultimate bearing capacity of a strip footing, 1 m wide, in a soil for
γ = 18 kN/m^3 , c = 20 kN/m^2 , and φ = 20°, at a depth of 1 m. Use Rankine’s and Bell’s approaches.
φ = 20°
In Rankine’s approach, cohesion is not considered.
qult =
1
2
γ b Nγ + γ Df Nq
where Nγ =
1
2
NNφφ()^2 −^1 and Nq = Nφ^2
Nφ = tan^2 (45° + φ/2) = tan^2 55° = 2.04
Nγ =
1
2
× tan 55° (tan^4 55° – 1) = 2.256
Nq = tan^4 55° = 4.16
∴ qult =
1
2
× 18 × 1 × 2.256 + 18 × 1 × 4.16 = 95.2 kN/m^2
In Bell’s approach, cohesion is also considered.
qult = cNc +
1
2
γb Nγ + γDf Nq
where Nc = 2 NNφ()φ+^1 , Nγ =
1
2
NNφφ()^2 −^1 , and Nq = Nφ^2
∴ Nc = 2 tan 55° (tan^2 55° + 1) = 8.682
Nγ =
1
2
tan 55° (tan^4 55° – 1) = 2.256
Nq = tan^4 55° = 4.16
∴ qult = 20 × 8.682 +
1
2
× 18 × 1 × 2.256 + 18 × 1 × 4.16 = 268.8 kN/m^2.
Example 14.4: A strip footing, 1.5 m wide, rests on the surface of a dry cohesionless soil
having φ = 20° and γ = 19 kN/m^3. If the water table rises temporarily to the surface due to
flooding, calculate the percentage reduction in the ultimate bearing capacity of the soil. Assume
Nγ = 5.0. (S.V.U.—B.E., (Part-Time)—Apr., 1982)
φ = 20° Nγ = 5.0 b = 1.5 m Df = 0
Dry cohesionles soil, ∴ c = 0
qult = cNc +
1
2
γb Nγ + γDf Nq =
1
2
γ b Nγ in this case.
=
1
2
× 19 × 1.5 × 5.0 = 71.3 kN/m^2
If the water table rises temporarily to the surface due to flooding, reduction factors Rγ
and Rq shall be applied as the maximum values for the Nγ and Nq terms respectively.
In this case, Rγ = 0.5 is applied for Nγ-term.