🎓 Lesson 8 D5

Real-World Project Walkthrough

Soil bearing capacity is how much weight the ground can safely hold without sinking or collapsing.

🎯 Learning Objectives

  • Calculate ultimate bearing capacity using Terzaghi’s equation for shallow foundations
  • Analyze the effect of water table depth on net allowable bearing pressure
  • Design a square footing size given applied load and site-specific soil parameters
  • Explain the difference between gross, net, and allowable bearing capacity
  • Apply correction factors (shape, depth, inclination) to modify theoretical capacity for real-world conditions

📖 Why This Matters

In mining infrastructure—like haul road subgrades, crusher pad foundations, or blast monitoring station bases—underestimating soil bearing capacity leads to catastrophic settlement, equipment misalignment, or even slope instability. A 2019 incident at a Western Australian iron ore mine resulted in $4.2M in downtime after a portable lab building settled 12 cm due to unverified clay subgrade capacity—highlighting why this isn’t just theory—it’s operational safety.

📘 Core Principles

Bearing capacity rests on three interrelated mechanisms: soil shear strength (cohesion c and friction angle φ), foundation geometry (width B, depth D_f), and load application (vertical vs. eccentric). Terzaghi’s classical theory assumes a rigid, continuous strip footing on homogeneous, cohesion-friction soil with no water table influence. Meyerhof extended this to account for foundation shape, depth, and load inclination—critical for irregular blast-related pads. Later, Vesic introduced generalized bearing capacity factors (N_c, N_q, N_γ) tied to φ, while Hansen and others added correction coefficients for real-world complexities like layered soils and dynamic loading from nearby blasts.

📐 Terzaghi’s Ultimate Bearing Capacity (Strip Footing)

Terzaghi’s equation provides the foundational model for shallow foundations on cohesive-frictional soils. It separates contributions from cohesion, surcharge (overburden), and soil weight—and serves as the baseline before applying Meyerhof/Vesic corrections.

💡 Worked Example

Problem: A 1.8-m-wide strip footing is placed at 1.2 m depth in sandy clay (c = 25 kPa, φ = 22°, γ = 18.5 kN/m³). Groundwater is at 3.0 m depth (i.e., below footing). Calculate q_u.
1. Step 1: Determine bearing capacity factors for φ = 22°: N_c ≈ 16.9, N_q ≈ 7.8, N_γ ≈ 4.9 (from standard tables, e.g., Das, 2016).
2. Step 2: Compute effective surcharge q = γ × D_f = 18.5 × 1.2 = 22.2 kPa.
3. Step 3: Plug into formula: q_u = (25)(16.9) + (22.2)(7.8) + 0.5(18.5)(1.8)(4.9) = 422.5 + 173.2 + 81.9 = 677.6 kPa.
4. Step 4: Apply FS = 3.0 → q_all = q_u / 3 = 225.9 kPa. Verify against typical range for sandy clay (150–300 kPa); result is acceptable but warrants verification with SPT correlation.
Answer: The ultimate bearing capacity is 677.6 kPa; allowable capacity is 225.9 kPa—within safe design limits for this soil profile.

🏗️ Real-World Application

At the Diavik Diamond Mine (Northwest Territories, Canada), engineers designed a 4.2 m × 4.2 m reinforced concrete pad for a high-frequency blast vibration sensor array. Site investigation revealed glacial till (c = 45 kPa, φ = 31°, γ = 20.1 kN/m³) over bedrock at 2.5 m. Using Vesic’s modified equation with shape (s_c=1.3, s_q=s_γ=1.2), depth (d_c=1.1, d_q=d_γ=1.05), and inclination factors, they calculated q_u = 1,420 kPa → q_all = 473 kPa (FS=3). Field plate load tests confirmed 465 kPa at 25 mm settlement—validating the model and preventing post-installation drift in sensor calibration.

📋 Case Connection

📋 Cost Optimization in Soil Bearing Capacity Analysis

Maintaining quality while reducing costs

📚 References