Plane Stress Transformation Equations
Find the normal and shear stresses on any rotated plane — the foundation of every stress-analysis tool that follows.
A beam cracks along a 45° angle under torsion not because the material is weak at 45°, but because the stress state looks completely different on that slanted plane. Stress transformation is how you rotate your point of view mathematically — and discover where the real danger lies.
Why stress changes with orientation
Stress is not a single number — it is a tensor, a complete description of how force is transmitted through a point in every possible direction. The three numbers you usually see (σx, σy, τxy) are just the components on the x and y faces of a conveniently oriented square element. If you slice that element at an angle, the same internal forces must still balance — but now they are resolved onto slanted faces, producing different normal and shear stresses.
The transformation equations come from cutting a tiny wedge at angle θ and enforcing equilibrium. They are not empirical fits; they are exact consequences of force balance, valid for any homogeneous, linear-elastic material and any plane-stress state.
Principal stresses and the principal angle
There is always some angle θ at which the shear stress τx′y′ drops to zero. Those planes — the principal planes — carry only normal stress, called the principal stresses σ1 and σ2. They are the maximum and minimum normal stresses attainable at that point under any rotation. Setting τx′y′ = 0 and solving gives the principal angle θp and the principal-stress formula below.
A quick sanity check: the sum of the principal stresses must equal the sum of the original normal stresses, because rotating the element cannot create or destroy normal force. That means σ1 + σ2 = σx + σy — a useful check after every calculation.
The largest shear stress in the x-y plane occurs on planes rotated 45° from the principal planes. Its magnitude equals the radius term in the principal-stress formula:
τmax(in-plane) = √[((σx − σy)/2)² + τxy²]
Crucially, the planes of maximum in-plane shear are not planes of zero normal stress. They carry the average normal stress σavg = (σx + σy)/2. This is one of the most common mistakes in introductory stress analysis — students often assume maximum-shear planes are 'pure shear' planes, but they only are when σavg happens to be zero.
- Average normal stress: σavg = (80 + 40)/2 = 60 MPa.
- Radius R = √[((80 − 40)/2)² + 30²] = √[20² + 30²] = √1300 ≈ 36.06 MPa.
- Principal stresses: σ1 = 60 + 36.06 = 96.06 MPa; σ2 = 60 − 36.06 = 23.94 MPa.
- Sanity check: σ1 + σ2 = 96.06 + 23.94 = 120 MPa = σx + σy — confirmed.
- Principal angle: tan(2θp) = τxy / ((σx − σy)/2) = 30/20 = 1.5 → 2θp = 56.31° → θp ≈ 28.2°.
- Maximum in-plane shear: τmax = R = 36.06 MPa, occurring on planes at θp + 45° ≈ 73.2°.
- Normal stress on those max-shear planes = σavg = 60 MPa (not zero).
- σx′ = (80+40)/2 + (80−40)/2·cos(60°) + 30·sin(60°) = 60 + 20·0.5 + 30·0.8660 = 60 + 10 + 25.98 = 95.98 MPa.
- R = √[((80−40)/2)² + 30²] = √[400 + 900] = √1300 ≈ 36.06 MPa.
- τmax(in-plane) = R ≈ 36.1 MPa.
Check your understanding
- Stress transformation resolves the same stress state onto rotated planes using equilibrium.
- Principal stresses are the maximum and minimum normal stresses; they occur on planes where shear is zero.
- Maximum in-plane shear equals the radius R and occurs on planes at 45° to the principal planes, carrying σavg.
- Always check: σ1 + σ2 = σx + σy.
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