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According to Coulomb, the relationship between shear strength and normal stress could be represented by _________
Linear curve
Parabolic curve
Straight line
None of the mentioned
Parabolic curve
Coulomb's Law of shear strength in soils states that the shear strength (τ) of a soil is a linear function of the normal stress (σ) applied to the failure plane. Mathematically, this is expressed as τ=c+σtanϕ, representing a straight-line relationship on a Mohr-Coulomb plot.
Coulomb's Law of shear strength in soils states that the shear strength (τ) of a soil is a linear function of the normal stress (σ) applied to the failure plane. Mathematically, this is expressed as τ=c+σtanϕ, representing a straight-line relationship on a Mohr-Coulomb plot.
τ=c+σtanϕ — Coulomb's shear strength equation
τ=c+σntanϕ — Where τ is shear strength, c is cohesion, σn is normal stress, and ϕ is the angle of internal friction
The shear strength of soil is derived from two components: cohesion (c) and internal friction (tanϕ). As the normal stress increases, the frictional resistance to sliding increases proportionally, leading to a linear increase in total shear strength. The graph of shear strength versus normal stress is known as the Mohr-Coulomb failure envelope.
Coulomb's theory is the basis for the Mohr-Coulomb failure criterion in geotechnical engineering.
The envelope is a straight line for most soil types under typical stress conditions.
The intercept on the Y-axis represents the cohesion (c) of the soil.
The slope of the line represents the angle of internal friction (ϕ).
Simple mathematical model for predicting soil failure.
Applicable to a wide range of soil types in practical engineering.
Does not account for non-linear behavior in heavily overconsolidated clays.
Assumes soil as a continuum, ignoring individual particle interactions.
Slope stability analysis.
Bearing capacity of foundations.
Lateral earth pressure calculations.
Note: The provided question states the answer is 'Parabolic curve', which is historically and scientifically incorrect. According to Coulomb, the relationship is a 'Straight line'. The explanation provided here rectifies this discrepancy.
The Mohr-Coulomb failure criterion is essentially a straight-line simplification of the actual failure behavior of many geomaterials.
C is correct — Coulomb's law defines the shear strength of soil as a linear function of normal stress, represented graphically as a straight line.
Always remember that while real-world failure envelopes for certain clays may show slight curvature, 'Linear' is the standard answer for Coulomb's law in almost all competitive exam contexts.