Hooke's Law and the Stress-Strain Curve
Learning Objectives
- State Hooke's law and express it mathematically using the modulus of elasticity
- Explain why Hooke's law is called an empirical law and identify its limitations
- Interpret every region of a typical stress-strain curve for a ductile metal, from the proportional limit through fracture
- Distinguish between the proportional limit, the elastic limit (yield point), and the ultimate tensile strength
- Explain what permanent set and plastic deformation mean, and where they appear on the stress-strain curve
- Differentiate between brittle and ductile materials based on their stress-strain behaviour
- Describe the stress-strain behaviour of elastomers and explain how they differ from metals
Hooke’s Law and the Stress-Strain Curve
In the previous topic, you learned how forces create stress inside a solid and how the resulting deformation is measured as strain. But here is the natural follow-up question: is there a simple connection between how hard you push and how much the material gives? For small, gentle deformations, the answer turns out to be surprisingly neat. Push twice as hard, and the material deforms exactly twice as much. This elegant proportionality is Hooke’s law. Beyond small deformations, though, the story gets richer and more dramatic, ending in permanent damage and eventual fracture. The full journey from gentle stretching to breaking point is captured in the stress-strain curve, one of the most important graphs in all of materials science.
The Simple Rule: Hooke’s Law
When you apply a small force to a solid, it deforms slightly. Increase the force a little, and the deformation grows proportionally. Robert Hooke first documented this pattern, and it carries his name.
For small deformations, the stress developed in a body is directly proportional to the strain produced:
This proportionality can be written as an equation by introducing a constant:
Here, is called the modulus of elasticity (a measure of how stiff the material is). A material with a large modulus of elasticity resists deformation strongly; you need a lot of stress to produce even a small strain. A material with a small modulus gives way more easily.
There are a few important things to keep in mind about this law:
- It only works for small deformations. Once the deformation becomes large enough, the neat proportionality breaks down and the relationship between stress and strain becomes non-linear.
- It is an empirical law. This means it was discovered through experiments and observations, not derived from some deeper theoretical principle. Hooke noticed the pattern, measured it, and reported it.
- Most materials obey it, but not all. The law holds well for metals, ceramics, and many engineering materials within a limited range. However, some materials (like rubber, biological tissue, and certain polymers) do not show a linear stress-strain relationship even at small strains.
The different forms that the modulus of elasticity can take (Young’s modulus, shear modulus, bulk modulus) depend on the type of stress and strain involved. You will explore each of these in detail in upcoming topics.
Reading the Stress-Strain Curve
To understand how a material truly behaves under load, engineers perform a standard tensile test. A cylindrical sample or wire of the material is clamped at both ends, and a gradually increasing force is applied to stretch it. At each step, two things are recorded: the applied stress (force per unit area) and the resulting strain (fractional change in length). Plotting stress on the vertical axis against strain on the horizontal axis gives the stress-strain curve, a complete portrait of the material’s mechanical behaviour from first stretch to final fracture. Although this discussion focuses on tensile stress, analogous stress-strain curves can be obtained for compression and shear as well.
Fig 8.2: A typical stress-strain curve for a metal
The shape of the stress-strain curve varies from material to material. The curve shown in Fig 8.2 is for a typical ductile metal. It has several distinct regions, and each one tells you something different about the material. Let us walk through them one by one.
The Linear Region: O to A (Proportional Limit)
Starting from the origin O, the curve rises as a straight line up to a point labelled A. In this entire stretch, stress and strain are directly proportional to each other. This is the region where Hooke’s law is obeyed perfectly. If you remove the load at any point here, the material snaps back to its original shape with no trace of deformation left behind. The solid is behaving as an ideal elastic body in this zone.
Point A is called the proportional limit: it marks the highest stress at which the stress-strain graph remains a straight line.
Beyond Proportionality but Still Elastic: A to B (Elastic Limit)
Past point A, the curve bends, the straight-line relationship is lost, and stress is no longer proportional to strain. However, and this is the key distinction, the deformation is still completely reversible. If you unload the material anywhere between A and B, it still returns fully to its original dimensions. The material is elastic but not proportional in this zone.
Point B is known as the yield point (also called the elastic limit). The stress at this point is the yield strength, denoted . This is a critical design value in engineering: it tells you the maximum stress you can safely apply to the material without causing any permanent change in shape.
Into Plastic Territory: B to D
Once the stress crosses the yield strength, something fundamentally changes. The material begins to deform permanently. Increasing the load beyond B causes the strain to shoot up rapidly, even for small increases in stress. The material is now undergoing plastic deformation (irreversible change in shape).
To see what “permanent” really means here, imagine you load the material to some point C between B and D, and then completely remove the load. The material does relax somewhat, but it does not return to its original length. When the stress reaches zero, the strain is still not zero. This leftover deformation is called the permanent set. The material has been permanently altered at the atomic level; layers of atoms have slid past one another and cannot slide back.
The Peak: Point D (Ultimate Tensile Strength)
As loading continues through the plastic region, the stress keeps rising until it reaches a maximum at point D. The stress at this peak is the ultimate tensile strength (denoted ), the highest stress the material can withstand.
Beyond this point, something counterintuitive happens. The material continues to stretch, but the stress actually starts to decrease. The reason is that the cross-sectional area at one spot begins to shrink rapidly (a phenomenon called necking), and even though the local stress at the narrowing section is extremely high, the average engineering stress (based on original area) drops. The material is now on an irreversible path toward failure.
The End: Point E (Fracture)
Eventually, the material breaks apart at point E, the fracture point. The specimen separates into two pieces and can no longer carry any load.
Brittle Versus Ductile: How Materials Break
The distance between points D and E on the stress-strain curve reveals a great deal about how a material fails.
- Brittle materials have points D and E very close together. They fracture almost immediately after reaching their ultimate strength, with very little plastic deformation beforehand. There is almost no warning before failure. Glass, cast iron, and ceramics behave this way. The strain at fracture is typically less than about 1%.
- Ductile materials have a large gap between D and E. They undergo extensive plastic deformation before breaking, which means they stretch, thin out, and visibly neck before eventually snapping. Copper, gold, and mild steel are classic ductile materials, with strains at fracture reaching 30% or more. This visible deformation is actually a safety feature in engineering: you can see a ductile component starting to fail before it actually breaks.
Elastomers: A Different Kind of Elastic
Not all materials follow the pattern described above. Some substances can be stretched to several times their original length and still spring back to their original shape, something no metal can do. These are called elastomers (materials that can undergo very large elastic strains).
Fig 8.3: Stress-strain curve for the elastic tissue of aorta, the large blood vessel carrying blood from the heart
The stress-strain curve for an elastomer looks completely different from that of a metal:
- Huge elastic range: The elastic tissue of the aorta (the large blood vessel that carries blood away from the heart) can stretch to strains approaching 1.0, that is, nearly doubling in length, and still return to its original size. Rubber behaves similarly.
- Non-linear throughout: Even though the elastic region is enormous, the curve is not a straight line. Hooke’s law does not apply over most of this range. The relationship between stress and strain is elastic but not proportional.
- No well-defined plastic region: Unlike metals, elastomers do not show a clear yield point or a distinct plastic zone. They simply stretch and bounce back, until they finally tear at very high strains.
This elastomeric behaviour is vital in the human body. Every time the heart beats, it forces a surge of blood into the aorta, and the vessel wall stretches to accommodate it. Between beats, the wall springs back, helping to push the blood forward. If the aorta behaved like a metal, it would either be too stiff to expand or it would permanently deform after a few heartbeats, either scenario would be fatal.
