Bearing Capacity of Soil — Terzaghi vs Meyerhof

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What Is Bearing Capacity of Soil?

Bearing capacity is the soil’s fundamental promise to a structure — it defines how much load the ground can carry before something breaks, shifts, or collapses.

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In geotechnical engineering, bearing capacity refers to the maximum contact pressure between a foundation and the supporting soil at which the soil mass can resist shear failure without undergoing excessive settlement. It is expressed in units of pressure — typically kN/m² (or kPa) in SI units, and t/m² in older Indian practice.

Every time a column load transfers through a footing into the earth, the soil beneath is being asked to carry that stress. If the stress exceeds what the soil can handle, one of two things happens: either the soil shears along a failure surface and the structure collapses suddenly, or it settles slowly and unevenly under a load it was never designed to carry. Both outcomes are disastrous, and both can be prevented through proper bearing capacity analysis.

In India, the governing code for determination of bearing capacity of shallow foundations is IS 6403:1981, published by the Bureau of Indian Standards. This code incorporates both Terzaghi’s classical theory and the more comprehensive Meyerhof-Vesic approach, and it remains the primary reference for all geotechnical design work in the country — from residential buildings to highway bridges to industrial structures.

Two Criteria Always Apply

Bearing capacity design must satisfy two independent criteria: (1) Shear failure — checked using Terzaghi, Meyerhof, or IS 6403:1981 equations; and (2) Settlement — checked as per IS 1904:1978. The more critical of the two governs the final footing size. Shear capacity alone is never sufficient.

Types of Bearing Capacity

Understanding the terminology is essential before working with any bearing capacity equation. These four terms are regularly confused, particularly in exam questions and design reports.

The total contact pressure at the foundation base at which shear failure occurs. Calculated directly from Terzaghi, Meyerhof, or IS 6403:1981 equations. Includes the overburden stress.

The additional stress beyond the existing overburden at foundation level: qₙᵤ = qᵤ − γ·Df. This is the net increase in stress the soil is being asked to carry above what it already carries.

The net ultimate bearing capacity divided by a factor of safety: qₛ = qₙᵤ / FoS. As per IS 6403:1981, FoS = 2.5 to 3.0 for most foundations.

The smaller of the safe bearing capacity (shear criterion) and the maximum pressure that limits settlement to permissible values as per IS 1904. This is the final value used in design.

Three Modes of Bearing Capacity Failure

The type of failure mode that occurs under a footing depends primarily on the density or consistency of the supporting soil. This distinction matters because the Terzaghi equations are adjusted differently for each mode.

1. General Shear Failure

This is the classical, well-defined failure mode. It occurs in dense sands and stiff clays. A continuous failure surface develops from the edge of the footing all the way to the ground surface on one or both sides, accompanied by visible heaving of the ground. Failure is sudden and catastrophic. This is the mode assumed in Terzaghi’s original equations, and the one used for most standard bearing capacity calculations.

Relative density: Dense sand (Dᵣ > 67%) or stiff/hard clay.

2. Local Shear Failure

In medium-dense sands and medium clays, the failure surface does not extend to the ground surface. Significant settlement occurs before failure, and the transition is gradual rather than sudden. The soil bulges slightly but does not heave dramatically. IS 6403:1981 treats φ < 28° as a local shear zone and requires the use of reduced shear parameters: c* = 0.67c and tan φ* = 0.67 tan φ.

Relative density: Medium sand (Dᵣ = 35–67%) or medium clay.

3. Punching Shear Failure

In very loose sands and soft clays, the footing simply punches into the soil without any recognisable lateral failure pattern. There is no heave, no defined failure surface — the footing just sinks progressively under load. This mode is also common for deep foundations where the failure mechanism is largely confined to the zone immediately beneath the footing tip.

Relative density: Loose sand (Dᵣ < 35%) or soft clay.

Terzaghi’s Bearing Capacity Method (1943)

Karl Terzaghi — widely regarded as the father of modern soil mechanics — published his bearing capacity theory in Theoretical Soil Mechanics (1943). He was the first to provide a rigorous analytical framework for shallow foundation failure, and his equations remain foundational to geotechnical engineering education worldwide.

Key Assumptions

Terzaghi’s theory rests on several important assumptions that define when it is valid:

  • The foundation is shallow — depth of embedment Df ≤ width B.
  • The soil above the base of the footing acts only as a surcharge (q = γ·Df); its shear strength is ignored.
  • The footing base is rough (full mobilisation of friction between soil and footing).
  • The load is vertical, central, and uniformly distributed — no eccentricity, no inclination.
  • Failure is by general shear (unless modified for local shear).
  • Soil is homogeneous, isotropic, and semi-infinite.

Terzaghi’s Equations

Terzaghi gave separate equations for each footing shape based on experimental shape multipliers:

qᵤ = c·Nc + q·Nq + 0.5·γ·B·Nγ

c = cohesion of soil (kN/m²)
q = surcharge pressure at foundation level = γ·Df (kN/m²)
γ = unit weight of soil (kN/m³)
B = width of footing (m)
Nc, Nq, Nγ = dimensionless bearing capacity factors (function of φ only)

qᵤ = 1.3·c·Nc + q·Nq + 0.4·γ·B·Nγ

qᵤ = 1.3·c·Nc + q·Nq + 0.3·γ·B·Nγ

qᵤ = (1 + 0.3·B/L)·c·Nc + q·Nq + (1 − 0.2·B/L)·0.5·γ·B·Nγ

Terzaghi’s Bearing Capacity Factors

The factors Nc, Nq, and Nγ are functions of the soil friction angle φ only. They are derived from the geometry of the failure wedge and the logarithmic spiral shear zones. Key values are given below:

φ (degrees)NcNqFailure Mode
5.701.000.00Pure cohesive
7.341.570.45Local shear zone
10°9.612.691.22Local shear zone
15°12.864.452.50Local shear zone
20°17.697.445.00Local shear zone
25°25.1312.729.70Transition zone
30°37.1622.4619.13Transition zone
35°57.7541.4442.92General shear
40°95.6681.27100.40General shear

Terzaghi’s Local Shear Failure Modification

For φ < 28° (local shear failure zone), Terzaghi introduced modified shear parameters to correct for the fact that the full shear strength is not mobilised:

c* = (2/3)·c = 0.67c
tan φ* = (2/3)·tan φ → φ* = arctan(0.67 tan φ)

Use c* and φ* in place of c and φ when computing bearing capacity factors for local shear failure conditions.

Meyerhof’s Bearing Capacity Method (1951, 1963)

G.G. Meyerhof extended Terzaghi’s work significantly. His 1951 paper introduced the concept of shape factors, depth factors, and inclination factors — recognising that real-world footings are never just strip footings with perfectly vertical, perfectly centred loads. His 1963 paper refined these factors based on field test data from Canada, making the method applicable to a much wider range of practical conditions.

It is the Meyerhof framework — later refined by Vesic (1973) for the bearing capacity factors — that forms the theoretical backbone of IS 6403:1981.

The General Equation

qₙᵤ = c·Nc·Sc·dc·ic + γ·Df·(Nq − 1)·Sq·dq·iq + 0.5·γ·B·Nγ·Sγ·dγ·iγ·W’

c = cohesion (kN/m²)  |  γ = unit weight (kN/m³)  |  Df = depth of foundation (m)  |  B = width (m)
Nc, Nq, Nγ = bearing capacity factors (Vesic, 1973)
Sc, Sq, Sγ = shape factors  |  dc, dq, dγ = depth factors
ic, iq, iγ = inclination factors  |  W’ = water table correction factor

Note that IS 6403:1981 uses the net ultimate bearing capacity (qₙᵤ) form, which subtracts the overburden stress γ·Df from the gross capacity. This is why the Nq term appears as (Nq − 1) in the IS formula.

Meyerhof’s Bearing Capacity Factors (as per Vesic, 1973 — used in IS 6403)

Nq = e^(π·tan φ) · tan²(45 + φ/2)
Nc = (Nq − 1) · cot φ   [For φ = 0: Nc = 5.14]
Nγ = 2·(Nq + 1)·tan φ   [Vesic, 1973]

φ (°)Nc (Vesic)Nq (Vesic)Nγ (Vesic)
5.141.000.00
6.491.570.45
10°8.352.471.22
15°10.983.942.65
20°14.836.405.39
25°20.7210.6610.88
28°25.8014.7216.72
30°30.1418.4022.40
35°46.1233.3048.03
40°75.3164.20109.41

Shape Factors (IS 6403:1981, Clause 5.1.2.1)

Footing ShapeScSq
Strip (B/L → 0)1.01.01.0
Square (B = L)1 + 0.2·tan²(45+φ/2)1 + 0.2·tan²(45+φ/2)1 − 0.4·(B/L)
Circular1 + 0.2·tan²(45+φ/2)1 + 0.2·tan²(45+φ/2)0.6
Rectangular1 + 0.2·(B/L)·tan²(45+φ/2)1 + 0.2·(B/L)·tan²(45+φ/2)1 − 0.4·(B/L)

Depth Factors (IS 6403:1981, Clause 5.1.2.2)

dc = 1 + 0.2·(Df/B)·tan(45 + φ/2)
dq = dγ = 1 + 0.1·(Df/B)·tan(45 + φ/2)   [for φ > 10°]
dq = dγ = 1.0   [for φ = 0°]

Inclination Factors (IS 6403:1981, Clause 5.1.2.3)

ic = iq = (1 − α/90°)²
iγ = (1 − α/φ)²   [valid only for φ > 0°]

α = angle of load inclination from vertical (degrees). For vertical load, α = 0 and all inclination factors = 1.0.

IS 6403:1981 — Key Provisions for Geotechnical Engineers

IS 6403:1981 — Code of Practice for Determination of Bearing Capacity of Shallow Foundations

Published by: Bureau of Indian Standards (BIS), Civil Engineering Division, Soil and Foundation Engineering Section (CED 43).

First revision: 1981. Reaffirmed in 1997 and 2002. Still the primary governing code for shallow foundation bearing capacity in India.

Scope: Covers determination of safe bearing capacity for shallow foundations using theoretical methods (Terzaghi/Meyerhof/Vesic), plate load tests, and SPT/CPT correlations.

Complementary codes: IS 1904:1978 (permissible settlements), IS 2131:1981 (Standard Penetration Test), IS 1888:1982 (Plate Load Test), IS 8009 Part I & II (settlement calculation).

Factor of Safety as per IS 6403:1981

IS 6403:1981 requires the safe bearing capacity (qₛ) to be determined by dividing the net ultimate bearing capacity by a factor of safety. The code recommends:

qₛ = qₙᵤ / FoS

Allowable Bearing Pressure: qₐ = qₛ + γ·Df

FoS = 2.5 — thorough investigation, low soil variability, well-defined loads
FoS = 3.0 — routine building foundations, standard site investigation (most common)
FoS = 3.0 — critical structures, major infrastructure, uncertain soil conditions

Cohesive Soils (φ = 0 Condition — Undrained Analysis)

For saturated clays under rapid undrained loading (short-term stability), IS 6403:1981 specifies the use of undrained shear parameters: φ = 0 and c = cᵤ (undrained cohesion). In this case, the bearing capacity equation simplifies significantly because Nq = 1 and Nγ = 0:

qₙᵤ = cᵤ · Nc · Sc · dc · ic

For a strip footing on level ground with vertical load: Nc = 5.14 (Vesic), all shape/depth/inclination factors = 1.0 → qₙᵤ = 5.14·cᵤ

SPT-Based Bearing Capacity (IS 6403:1981, Clause 5.3)

IS 6403:1981 also provides correlations between the Standard Penetration Test N-value and the safe bearing capacity for cohesionless soils (sands and gravels). This approach is widely used in India for preliminary design when direct shear strength tests are not available:

SPT N-value (corrected)Soil DescriptionSafe Bearing Capacity (kN/m²)
< 4Very loose sand< 50 (not suitable for direct foundation)
4–10Loose sand50–100
10–30Medium dense sand100–200
30–50Dense sand200–400
> 50Very dense sand / gravel> 400

Note: N-values must be corrected for overburden pressure (CN correction) and, where applicable, for fine content and water table as per IS 2131:1981 before using these correlations.

Effect of Water Table on Bearing Capacity

The position of the water table has a direct and significant effect on bearing capacity, primarily by reducing the effective unit weight of soil and hence the effective overburden and self-weight terms in the equation. IS 6403:1981 handles this using water table correction factors Rw1 and Rw2.

Three Water Table Positions — IS 6403:1981 Treatment

Modified equation: qₙᵤ = c·Nc·Sc·dc·ic + Rw1·γ·Df·(Nq−1)·Sq·dq·iq + 0.5·Rw2·γ·B·Nγ·Sγ·dγ·iγ

Water Table PositionRw1 (Surcharge term)Rw2 (Self-weight term)
Water table at or above ground surface0.50.5
Water table at foundation level (Zw1 = Df)1.00.5
Water table at depth B below foundation level1.01.0
Water table at depth > B below foundation1.01.0 (no correction needed)

Terzaghi vs Meyerhof — Full Comparison

ParameterTerzaghi (1943)Meyerhof / IS 6403:1981
Year developed19431951 (Meyerhof), 1963 (revised), 1973 (Vesic factors)
Foundation depth assumptionDf ≤ B (shallow only)Any depth — handled by depth factors
Load inclination✗ Not considered✔ Inclination factors (ic, iq, iγ)
Shape factorsEmpirical multipliers (1.3 for square/circular)Analytical shape factors (Sc, Sq, Sγ)
Depth factors✗ Not included✔ dc, dq, dγ
Eccentric loading✗ Not considered✔ Effective width method (B’ = B − 2e)
Sloped ground / sloped footing base✗ Not considered◑ (Hansen method; IS 6403 references for such cases)
Local shear failure✔ Reduced c* and φ*✔ IS 6403 φ classification
Nγ formulaTerzaghi’s original (slightly different values)Vesic (1973): Nγ = 2(Nq + 1)·tan φ
Bearing capacity resultHigher (conservative for some shapes)More realistic — typically 5–21% lower than Terzaghi for same conditions
IS code adoption◑ Referenced for educational/comparison✔ Primary method in IS 6403:1981
Best suited forQuick preliminary estimates; simple vertical loadsAll foundation design — preferred for final design

Worked Numerical Examples

Problem: A 2.0 m × 2.0 m square footing is placed at a depth of 1.5 m in dense sand. The soil has: c = 0 (cohesionless), φ = 36°, γ = 18 kN/m³. Water table is well below the influence zone. Using Terzaghi’s method, find the (a) ultimate bearing capacity, (b) safe bearing capacity with FoS = 3.0.

Step 1 — Identify failure modeφ = 36° → φ > 36° → General shear failure. Use full c and φ values.

Step 2 — Bearing capacity factors from Terzaghi’s table (φ = 35°–36°, interpolate)At φ = 36°: Nc ≈ 63.5, Nq ≈ 47.2, Nγ ≈ 51.2 (by interpolation from standard Terzaghi table). Note: For exam purposes, many references give φ = 35°: Nc = 57.8, Nq = 41.4, Nγ = 42.9 — use the values given in the question.

Step 3 — Surcharge pressure q = γ · Df = 18 × 1.5 = 27 kN/m²

Step 4 — Apply Terzaghi’s square footing equationqᵤ = 1.3·c·Nc + q·Nq + 0.4·γ·B·Nγ
qᵤ = 1.3 × 0 × 63.5 + 27 × 47.2 + 0.4 × 18 × 2.0 × 51.2
qᵤ = 0 + 1274.4 + 737.3 =2011.7 kN/m²

Step 5 — Net ultimate bearing capacityqₙᵤ = qᵤ − γ·Df = 2011.7 − 27 = 1984.7 kN/m²

Step 6 — Safe bearing capacity (FoS = 3.0)qₛ = qₙᵤ / FoS = 1984.7 / 3.0 = 661.6 kN/m²
Allowable bearing pressure: qₐ = qₛ + γ·Df = 661.6 + 27 =688.6 kN/m²

Example 3IS 6403:1981 — Rectangular Footing on c-φ Soil

Problem: A rectangular footing 3.0 m × 2.0 m is founded at a depth of 1.5 m in soil with: c = 20 kN/m², φ = 25°, γ = 17 kN/m³. Load is vertical and central. Water table is at a depth of 5 m (no correction needed). Compute the safe bearing capacity as per IS 6403:1981 with FoS = 3.0.

Step 1 — Failure mode classification (IS 6403:1981)φ = 25° → 28° > φ > 0° → Transition zone approaching local shear. Use IS 6403:1981 bearing capacity factors directly from Table 1 at φ = 25°. From IS 6403:1981 Table 1: Nc = 20.72, Nq = 10.66, Nγ = 10.88

Step 2 — Shape factors (IS 6403:1981, Clause 5.1.2.1) — rectangular, B = 2.0 m, L = 3.0 mkp = tan²(45 + φ/2) = tan²(57.5°) = 2.46
Sc = 1 + 0.2·(B/L)·kp = 1 + 0.2 × (2/3) × 2.46 = 1.328
Sq = 1 + 0.2·(B/L)·kp = 1.328
Sγ = 1 − 0.4·(B/L) = 1 − 0.4 × (2/3) = 0.733

Step 3 — Depth factors (IS 6403:1981, Clause 5.1.2.2)Df/B = 1.5/2.0 = 0.75; kp^0.5 = √2.46 = 1.568
dc = 1 + 0.2 × (Df/B) × kp^0.5 = 1 + 0.2 × 0.75 × 1.568 = 1.235
dq = dγ = 1 + 0.1 × 0.75 × 1.568 = 1.118

Step 4 — Inclination factors (vertical load, α = 0)ic = iq = iγ = 1.0

Step 5 — Surcharge and apply IS 6403:1981 net equationq = γ·Df = 17 × 1.5 = 25.5 kN/m²
qₙᵤ = 20 × 20.72 × 1.328 × 1.235 × 1 + 25.5 × (10.66−1) × 1.328 × 1.118 × 1 + 0.5 × 17 × 2.0 × 10.88 × 0.733 × 1.118 × 1
qₙᵤ = 679.3 + 365.4 + 135.4 =1180.1 kN/m²

Step 6 — Safe bearing capacityqₛ = 1180.1 / 3.0 = 393.4 kN/m²
qₐ = qₛ + q = 393.4 + 25.5 =418.9 kN/m²

Example 3Effect of Water Table — Strip Footing on Sand

Problem: A 1.5 m wide strip footing is founded at 1.2 m depth in medium dense sand: c = 0, φ = 30°, γ_bulk = 19 kN/m³. Compute the net ultimate bearing capacity as per IS 6403:1981 for two cases: (a) water table is 5 m below ground (no effect), and (b) water table is at foundation level.

Common data — IS 6403:1981 factors at φ = 30°Nc = 30.14, Nq = 18.40, Nγ = 22.40
Strip footing: Sc = Sq = Sγ = 1.0; dc = dq = dγ = 1.0 (shallow); ic = iq = iγ = 1.0

Case (a) — Water table well below influence zone (Rw1 = Rw2 = 1.0)qₙᵤ = 0 + 19 × 1.2 × (18.40−1) × 1.0 + 0.5 × 19 × 1.5 × 22.40 × 1.0
qₙᵤ = 396.7 + 319.2 =715.9 kN/m²

Case (b) — Water table at foundation level (Rw1 = 1.0, Rw2 = 0.5)Use γ’ = γ_sat − γ_w = 19 − 9.81 = 9.19 kN/m³ for self-weight term (Rw2 = 0.5 equivalent)
qₙᵤ = Rw1·q·(Nq−1) + 0.5·Rw2·γ·B·Nγ
qₙᵤ = 1.0 × 22.8 × 17.4 + 0.5 × 0.5 × 19 × 1.5 × 22.40
qₙᵤ = 396.7 + 159.6 =556.3 kN/m²

Presumptive Bearing Capacity Values — Indian Soils (IS 6403:1981)

IS 6403:1981 includes a table of presumptive safe bearing capacity values for preliminary design. These values are based on the soil type and condition, and are intended only as starting points. They must always be confirmed by site-specific investigation before final design.

Soil / Rock TypeConditionSafe Bearing Capacity (kN/m²)
Soft / Medium ClayPlastic consistency50 – 100
Stiff ClaySemi-firm100 – 200
Hard ClayFirm, stiff200 – 400
Loose SandBelow water table — N < 10~100
Medium Dense SandN = 10–30100 – 200
Dense SandN = 30–50200 – 400
GravelDense, well-graded400 – 600
Black Cotton SoilMedium; varies seasonally50 – 150 (use with caution)
Laterite SoilHard crust150 – 300
Soft Rock / Weathered RockFractured or weathered600 – 2000
Hard Rock (Basalt, Granite)Fresh, sound, unweathered3000 – 10000+

Frequently Asked Questions

What is bearing capacity of soil in simple terms?

Bearing capacity is the maximum pressure the soil under a foundation can safely carry without failing by shear or settling excessively. Think of it as the ground’s weight limit. Every foundation design starts with checking whether the soil can hold the building’s load within safe limits.

What is the key difference between Terzaghi and Meyerhof methods?

Terzaghi’s 1943 method is the original classical approach — simple, conservative, and limited to vertical, central loads on shallow footings. Meyerhof’s method (1951–1963) extended it by adding three sets of correction factors: shape factors for non-strip footings, depth factors for deeper embedment, and inclination factors for loads that aren’t perfectly vertical. IS 6403:1981 uses the Meyerhof-Vesic framework as the primary design method.

What factor of safety should be used as per IS 6403:1981?

IS 6403:1981 recommends a factor of safety between 2.5 and 3.0 applied to the net ultimate bearing capacity. For most routine building foundations in India, FoS = 3.0 is used. A lower value of 2.5 is only appropriate when the site investigation is very thorough — multiple boreholes, full lab testing, and confirmed uniform soil conditions.

How does the water table affect bearing capacity?

Rising water table reduces bearing capacity because it decreases the effective unit weight of the soil. When the water table reaches the foundation level, the self-weight term in the bearing capacity equation is roughly halved (Rw2 = 0.5). This can reduce the overall bearing capacity by 15–25% depending on soil type. IS 6403:1981 uses water table correction factors Rw1 and Rw2 to account for this. Foundation design must always use the worst-case (highest anticipated) water table position.

When should you use Terzaghi’s method and when should you use Meyerhof?

Use Terzaghi’s method for quick preliminary estimates on simple cases: shallow strip, square, or circular footings with vertical, central loads on level ground. Use Meyerhof’s method (as per IS 6403:1981) for all final design — especially when loads are inclined (wind, seismic), foundations are deeply embedded (Df/B > 1), loads are eccentric, or the footing is rectangular. In India, IS 6403:1981 (Meyerhof-Vesic framework) is mandatory for formal geotechnical reports.

What are the three failure modes in bearing capacity?

General shear failure (dense soils — sudden, well-defined failure surface to ground surface), Local shear failure (medium soils — gradual failure without reaching ground surface, large settlement before failure), and Punching shear failure (loose/soft soils — footing punches straight down, no visible heave). IS 6403:1981 classifies failure mode based on φ: below 28° is local shear, above 36° is general shear, and 28°–36° is a transition zone.

How does foundation depth (Df) affect bearing capacity?

Increasing the depth of foundation improves bearing capacity through two mechanisms. First, it increases the overburden surcharge pressure (q = γ·Df), which multiplies with Nq in the bearing capacity equation. Second, the depth factors dc, dq, dγ in Meyerhof’s method also increase with Df/B, contributing additional capacity. For sandy soils where Nq is large, even a modest increase in foundation depth produces a significant gain in bearing capacity.

What IS codes are referred to alongside IS 6403 in foundation design?

IS 6403:1981 (bearing capacity) is used together with: IS 1904:1978 (permissible settlement criteria), IS 2131:1981 (Standard Penetration Test procedure), IS 1888:1982 (Plate Load Test), IS 8009 Part I (settlement of shallow foundations in granular soils), IS 8009 Part II (settlement of shallow foundations in cohesive soils), and IS 1893:2016 (seismic effects on foundations in earthquake zones).

Summary — What Every Engineer Should Remember

On method selection: For any formal geotechnical report or final foundation design in India, IS 6403:1981 (Meyerhof-Vesic approach) is the governing method. Terzaghi’s equations are valuable for building intuition and quick preliminary estimates, but they overestimate bearing capacity in many real-world conditions.

On failure modes: Always identify the failure mode first. For φ < 28°, use reduced parameters c* and φ*. For φ > 36°, use full parameters. Transition zone requires interpolation per IS 6403.

On factor of safety: Default to FoS = 3.0 for routine work. The IS code permits 2.5 only when investigation quality justifies it — this requires explicit documentation in the geotechnical report.

On water table: Never design for current water table position. Always design for the highest anticipated water table over the life of the structure. In monsoon-prone regions, this distinction has caused real failures.

On settlement: Shear capacity check alone is never enough. Always check settlement as per IS 1904:1978 independently. In soft clays and loose sands, settlement governs long before shear failure becomes relevant.

TheCivilStudies.com — Soil Mechanics Series

Published: April 2, 2026  ·  Last reviewed: April 2, 2026

References: IS 6403:1981, IS 1904:1978, Terzaghi K. (1943) Theoretical Soil Mechanics, Meyerhof G.G. (1963) Some Recent Research on the Bearing Capacity of Foundations, Vesic A.S. (1973) Analysis of Ultimate Loads of Shallow Foundations, Das B.M. Principles of Geotechnical Engineering, Gopal Ranjan & A.S.R. Rao Basic and Applied Soil Mechanics

Related reading:   Pressure Bulb in Foundation Design  ·  Soil Mechanics Hub  ·  Building Construction

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