Class 11 · Notes

Mechanical Properties of Solids— Notes, Formulas & Revision

Complete revision notes and formulas for Mechanical Properties of Solids (Class 11). Curated for JEE, NEET, AP Physics, SAT, and CUET. Tap any topic to open the live simulation and full PYQ set.

Stress–Strain Curve

Full σ–ε curve with proportional, elastic, yield, plastic, UTS and fracture zones. Watch a rod neck and snap.

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A typical stress-strain curve for a ductile material (e.g., mild steel) has several distinct regions.

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1. Proportional region (linear) — stress ∝ strain; Hooke's law holds; modulus is the slope.

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2. Elastic limit (just beyond proportional limit) — still recoverable, but stress and strain not strictly proportional.

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3. Yield point — material begins permanent deformation; visible necking starts.

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4. Plastic region — large strain for small stress increase; ductile materials stretch significantly.

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5. Ultimate tensile strength — maximum stress before necking dominates.

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6. Fracture point — material breaks.

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Ductile materials (steel, copper) show large plastic region. Brittle materials (glass, ceramic) break almost immediately past elastic limit.

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Area under the curve = energy absorbed per unit volume (toughness).

Young's modulus from slope

Slope of linear part of stress-strain curve.

Yield strength σ_y

Above this, plastic deformation begins.

Ultimate strength σ_u

Defines material's tensile strength.

Toughness (area under curve)

Energy absorbed per unit volume until fracture.

Hooke's law applies ONLY in the proportional region (linear part).

Ductile vs brittle: ductile has long plastic region (steel, copper); brittle has tiny or no plastic region (glass, cast iron).

Yield strength is what's reported for structural design — beyond this, deformation is permanent.

Beyond ultimate strength, the cross-section necks down — stress (engineering) decreases but true stress keeps rising.

Annealed metals are more ductile than cold-worked ones — stress-strain curve shape changes with heat treatment.

Brittle materials fail in TENSION; in COMPRESSION they can be very strong (concrete is ~10× stronger in compression than tension).

Hooke's Law

σ = Yε — stretch a steel bar, watch ΔL grow linearly with F. Live σ–ε point on the Hooke line.

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For small deformations, the stress in a solid is DIRECTLY proportional to the strain: stress = E × strain. This is Hooke's law.

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The proportionality constant E is the MODULUS OF ELASTICITY — material-specific, geometry-independent.

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Stress = force per unit area (N/m² = Pa). Strain = fractional deformation (dimensionless).

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Three types of stress/strain: tensile/compressive (longitudinal), volumetric (bulk), shear (tangential).

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Each has its own modulus: Young's (Y) for longitudinal, Bulk (B) for volume, Shear (G) for shape.

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Linear region: Hooke's law holds. Beyond the proportional limit, the curve deviates.

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Spring force F = −kx is a special case of Hooke's law applied to a spring; k = stiffness.

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Elastic deformations are REVERSIBLE — strain disappears when stress is removed. Beyond the elastic limit, deformation is permanent (plastic).

Hooke's law (general)

σ = stress, ε = strain, E = modulus (Young's, bulk, or shear depending on the geometry).

Longitudinal (Young's)

Force per area causes a fractional length change.

Spring (1D Hookean)

k = elastic constant; restoring force opposes displacement.

Elastic potential energy

Per unit volume: ½·stress·strain.

Hooke's law is LINEAR — valid only for small strains (typically < 0.1%).

The modulus depends on the MATERIAL but not on the shape or size of the sample.

Stress is intensive (Pa, like pressure). Strain is dimensionless.

Beyond elastic limit: no longer linear, plastic deformation begins, eventually fracture.

Real materials may show small NON-LINEARITY even in the elastic regime — Hooke's law is a first-order approximation.

Hooke's law extends to fluids (bulk modulus) and to torsion (shear modulus) — same idea, different geometry.

Young's Modulus Compared

Four wires (steel, copper, Al, brass) under same load — stiff materials stretch less.

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Young's modulus Y measures a material's stiffness under TENSILE/COMPRESSIVE stress: Y = stress/strain = (F/A)/(ΔL/L).

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Units: Pa (N/m²). Reported in GPa for typical solids.

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Y values: steel ≈ 200 GPa, copper ≈ 110 GPa, aluminum ≈ 70 GPa, glass ≈ 70 GPa, rubber ≈ 0.01-0.1 GPa, wood (along grain) ≈ 12 GPa.

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Wire of length L, cross-section A: extension ΔL = FL/(YA). Stiffer (higher Y) ⇒ smaller ΔL for given F.

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Force constant of a wire viewed as a spring: k = YA/L. Long, thin wires are softer; short, thick ones are stiffer.

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Used in structural engineering, materials selection, vibration analysis, and acoustics.

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Y is approximately constant for moderate strains; varies slightly with temperature.

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For composite or anisotropic materials (wood, carbon fibre), Y depends on direction.

Young's modulus definition

Slope of stress vs strain in the elastic region.

Extension under load

Useful in problems with wires and rods.

Spring-equivalent constant

k of a wire seen as a Hookean spring.

Strain energy / volume

Energy stored per unit volume in elastic deformation.

Y is a MATERIAL property — does NOT depend on the wire's size or shape.

Extension ΔL DOES depend on geometry: long thin wires extend more than short thick ones under the same load.

Steel (Y ≈ 200 GPa) is about 100,000× stiffer than rubber (Y ≈ 1-10 MPa).

Diamond has the highest Y (~1000 GPa) of any natural material.

Y varies slightly with temperature — usually decreases with rising T.

For ANISOTROPIC materials (wood, crystals), Y depends on direction of measurement.

Bulk Modulus

B = −ΔP/(ΔV/V) — cube compresses under hydrostatic pressure. 3D iso visual + live bar.

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Bulk modulus B (sometimes K) measures resistance to VOLUME change under hydrostatic pressure.

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Definition: B = −P/(ΔV/V). Negative sign because volume DECREASES as pressure INCREASES.

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Units: Pa, same as pressure.

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Typical values: steel ≈ 160 GPa, water ≈ 2.2 GPa, air ≈ 0.0001 GPa (at 1 atm). Solids are nearly incompressible; gases very compressible.

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Compressibility κ = 1/B — fractional volume change per unit pressure.

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Bulk modulus determines the speed of sound in fluids and solids: v = √(B/ρ) for longitudinal waves.

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For ideal gas: isothermal B_T = P (= 10⁵ Pa at 1 atm); adiabatic B_S = γP.

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Solids' bulk modulus is HIGH (~10² GPa) ⇒ they barely change volume even under enormous pressure.

Bulk modulus

Negative sign ensures B > 0 since ΔV < 0 for compressive P.

Compressibility

Fractional volume change per Pa.

Sound speed in a medium

Wave-speed depends on bulk modulus and density.

Ideal gas (isothermal vs adiabatic)

γ = c_p/c_v. Adiabatic bulk modulus governs sound speed in air.

Bulk modulus measures volumetric stiffness — solids are nearly incompressible (B ~ 100 GPa).

Sound speed in air ≈ 343 m/s comes from B_S = γP ≈ 1.4 × 10⁵ Pa and ρ ≈ 1.2 kg/m³.

Sound speed in water (~1500 m/s) is fast because B is large despite ρ being moderate.

For a gas: isothermal compression has lower B than adiabatic — that's why sound is approximately adiabatic.

B and Young's Y for the same material are DIFFERENT — Y for stretching, B for compression of all sides.

Compressibility κ is useful in geophysics, fluid mechanics — quantifies how much fluid 'gives' under pressure.

Shear Modulus

G = F/(Aφ) — block sheared into a parallelogram. Watch angle φ grow linearly with τ.

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Shear modulus G (also called rigidity modulus η or μ) measures resistance to SHAPE change at constant volume.

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Apply tangential force F to top face of a solid block (area A) while bottom is fixed: produces angular shear θ.

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Shear stress = F/A; shear strain = θ ≈ Δx/L (for small angles). G = shear stress / shear strain.

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Units: Pa. Typical values: steel ≈ 80 GPa, copper ≈ 45 GPa, rubber ~ MPa.

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Liquids and gases have G = 0 — they have no rigidity and cannot sustain shear stress at equilibrium.

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Shear modulus governs torsion of rods, propagation of TRANSVERSE waves in solids, etc.

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Torsion of a wire: torque τ = (πGr⁴/2L)·θ, where r = radius, L = length, θ = twist angle.

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Speed of transverse (shear) waves in solid: v_s = √(G/ρ).

Shear modulus

θ ≈ Δx/L for small shear angles.

Torsion of a wire

Used in torsion-balance experiments.

Transverse wave speed (solid)

S-waves in seismology.

Relation to Y, B, σ (isotropic)

σ_p = Poisson's ratio. Y, B, G all linked.

Fluids have G = 0 — they shear easily and continuously under any tangential force.

Shear modulus is typically 1/3 to 1/2 of Young's modulus for metals.

Earthquakes: P-waves (longitudinal) travel through everything; S-waves (shear) travel only through solids. This is how we know Earth's outer core is LIQUID — S-waves don't pass.

Torsion in mechanical engineering (drive shafts, springs) is governed by G.

G, B, and Y for an isotropic material are related — only two are independent.

Soft tissues and biological materials often have very low G — leading to specialized 'elastography' imaging.

Poisson's Ratio

ν = −ε_T/ε_L — rod extends axially, contracts laterally. See the grid deform.

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Poisson's ratio σ_p (often ν) measures lateral contraction during axial stretching: σ_p = −(lateral strain)/(longitudinal strain).

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When you stretch a rod axially, it gets THINNER laterally — both effects related by σ_p.

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Range: 0 ≤ σ_p ≤ 0.5 for isotropic materials. Most metals: 0.25-0.35. Cork: ~0. Rubber: ~0.5 (essentially incompressible).

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σ_p = 0.5: material is incompressible (volume unchanged when stretched). Rubber, soft tissues approach this.

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σ_p = 0: no lateral contraction at all. Cork has ~0.04 — useful for bottle stoppers.

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Some special materials (auxetics) have NEGATIVE Poisson's ratio — they expand laterally when stretched.

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Links Young's modulus, bulk modulus, and shear modulus: B = Y/[3(1−2σ_p)], G = Y/[2(1+σ_p)].

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Dimensionless quantity — pure number.

Poisson's ratio (definition)

D = diameter; positive value because lateral strain is opposite to longitudinal.

Relation to Y, B

Bulk modulus rises sharply as σ_p → 0.5.

Relation to Y, G

Shear modulus depends on Y and σ_p.

Volume change

Becomes zero for σ_p = 0.5 ⇒ incompressible.

σ_p is dimensionless and bounded between 0 and 0.5 for stable isotropic materials.

σ_p = 0.5 ⇒ incompressible (like rubber). At σ_p = 0.5, B → ∞.

When you stretch a wire, it gets thinner. Poisson's ratio quantifies how much.

Cork's near-zero σ_p makes it perfect for bottle stoppers — no lateral expansion when squeezed in.

Auxetic materials (negative σ_p) are man-made — used in protective equipment, exotic foams.

Two independent elastic constants describe an isotropic material — choose any two of {Y, B, G, σ_p}.

Elastic Potential Energy

U = ½σε·V — area under σ–ε curve fills as the wire stretches; energy bar grows live.

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Elastic potential energy is the energy stored in a deformed elastic body — recoverable when the body returns to its natural shape.

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For a spring or wire obeying Hooke's law: U = ½kx² (spring) or U = ½·F·ΔL (wire under tension F, extension ΔL).

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Energy per unit volume (energy density): u = ½·σ·ε = ½·Y·ε² = σ²/(2Y).

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All this is recovered when stress is released — provided you stay in the elastic region.

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Beyond the elastic limit, some energy goes into permanent (plastic) deformation, heat, or fracture.

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Springs in series and parallel: in series, k decreases (1/k_eq = Σ 1/k_i); in parallel, k increases (k_eq = Σ k_i).

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Application: bow-and-arrow stores elastic energy in the bow, transferred to KE of arrow.

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Earthquake faults store enormous elastic energy in stressed rocks — released suddenly during slip.

Spring/wire stored energy

Average force × distance — factor of ½ because F ramps up linearly.

Elastic energy density

Per unit volume; valid in linear regime.

Total energy in stretched wire

Energy = (F²L)/(2YA).

Springs (series / parallel)

Series gentle, parallel stiff (opposite of capacitors!).

Always factor of ½ — because force varies linearly from 0 to F during elongation.

Energy density u = σ²/(2Y): high stress + low Y stores lots of energy per unit volume (rubber, archery bows).

Beyond elastic limit, NOT all stored energy is recoverable — some heats the material, some causes plastic deformation.

Springs in series: like resistors in PARALLEL (k_eq < k_min).

Springs in parallel: like resistors in SERIES (k_eq = sum).

Stored elastic energy can be enormous — earthquake faults release built-up strain energy in seconds.

Mechanical Properties of Solids on sciphylab (also known as SciPhy, SciPhy Lab, SciPhy Labs). Free physics revision for Class 11, JEE Mains, JEE Advanced, NEET UG, AP Physics 1/2/C, SAT Subject Physics, and CUET-UG.