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Physics · Ch 9 — Mechanical Properties of Solids

Elastic Moduli

9.5

Elastic Moduli

Three Types of Elastic Moduli

The textbook introduces three distinct moduli, each corresponding to a specific type of strain:

  1. Young's modulus — for linear (tensile or compressive) strain
  2. Shear modulus (or modulus of rigidity) — for shearing strain
  3. Bulk modulus — for volumetric strain (uniform compression)

Let's take them one by one.


Properties and Relations Among Moduli

The textbook lists several important properties. Let's go through each one with its derivation.

›Proof

Property 1: For a given material, Young's modulus and shear modulus are related by:

Y=2G(1+μ)Y = 2G(1 + \mu)

where μ\mu is Poisson's ratio.

Derivation: Consider a cube of side LL subjected to a tensile force FF along one axis. The longitudinal strain is ϵ=ΔL/L\epsilon = \Delta L / L. Due to Poisson effect, the lateral strain is −μϵ-\mu \epsilon (the sides contract). Now consider a shear deformation of the same cube. The shear strain θ\theta is related to the tensile and compressive strains along the diagonals. For a pure shear, the principal axes are at 45∘45^\circ to the faces. The tensile strain along one diagonal equals θ/2\theta/2, and the compressive strain along the other diagonal equals −θ/2-\theta/2. Using Hooke's law for the diagonal direction (which experiences both axial stress and lateral contraction from the perpendicular direction), one obtains the relation. The full derivation involves tensor analysis, which is beyond Class 11 scope — the result is stated here for completeness.

›Proof

Property 2: For a given material, Young's modulus and bulk modulus are related by:

Y=3B(1−2μ)Y = 3B(1 - 2\mu)

Derivation: Consider a cube under uniform hydrostatic pressure Δp\Delta p. The stress on each face is Δp\Delta p. The volumetric strain is ΔV/V=3ϵ\Delta V/V = 3\epsilon (for small strains, where ϵ\epsilon is the linear strain along each axis). But each face also experiences lateral contraction from the perpendicular stresses. Using the generalized Hooke's law for three dimensions:

ϵx=1Y[σx−μ(σy+σz)]\epsilon_x = \frac{1}{Y}[\sigma_x - \mu(\sigma_y + \sigma_z)]

For hydrostatic pressure, σx=σy=σz=−Δp\sigma_x = \sigma_y = \sigma_z = -\Delta p. So:

ϵx=1Y[−Δp−μ(−2Δp)]=−ΔpY(1−2μ)\epsilon_x = \frac{1}{Y}[-\Delta p - \mu(-2\Delta p)] = -\frac{\Delta p}{Y}(1 - 2\mu)

The volumetric strain is ΔV/V=3ϵx=−3ΔpY(1−2μ)\Delta V/V = 3\epsilon_x = -\frac{3\Delta p}{Y}(1 - 2\mu).

But by definition, B=−Δp/(ΔV/V)=Y3(1−2μ)B = -\Delta p / (\Delta V/V) = \frac{Y}{3(1 - 2\mu)}.

Rearranging: Y=3B(1−2μ)Y = 3B(1 - 2\mu).

›Proof

Property 3: The three moduli are related by:

9Y=3G+1B\frac{9}{Y} = \frac{3}{G} + \frac{1}{B}

Derivation: From Property 1: Y=2G(1+μ)Y = 2G(1 + \mu), so μ=Y2G−1\mu = \frac{Y}{2G} - 1.

From Property 2: Y=3B(1−2μ)Y = 3B(1 - 2\mu), so μ=12(1−Y3B)\mu = \frac{1}{2}\left(1 - \frac{Y}{3B}\right).

Equating the two expressions for μ\mu:

Y2G−1=12−Y6B\frac{Y}{2G} - 1 = \frac{1}{2} - \frac{Y}{6B} …