WHAT is being related? Two quantities that each need direction information:
Stressσij: force per area. First index = face normal, second index = force direction. 9 components (6 independent, since σij=σji by moment balance).
Strainεij: fractional deformation. Also symmetric, 6 independent.
WHY not just a matrix? Because at each point the state of loading is itself a 3×3 object. Relating one 3×3 tensor linearly to another requires an object with 4 indices:
σij=Cijklεkl(i,j,k,l∈{1,2,3})
Summation over repeated k,l (Einstein convention). This is Hooke's law in its most general linear-elastic form.
Why this form? Take two nearby points separated by dx. After deformation the separation becomes dxi+∂xj∂uidxj. The change in squared length, to first order, involves the symmetric part of ∂ui/∂xj. The antisymmetric part is pure rotation (no stretch), so we discard it — that's why we symmetrize. Rotation doesn't store elastic energy, so it must not appear in ε.
WHY does energy give the major symmetry? For a conservative elastic material stress is the gradient of a stored-energy density: σij=∂W/∂εij. Then Cijkl=∂2W/∂εij∂εkl, and mixed partials commute — hence swapping the ij and kl pairs leaves C unchanged.
Here εkk=ε11+ε22+ε33 is the volumetric strain (trace = fractional volume change). λ and μ are the Lamé parameters; μ≡G is the shear modulus.
Why only two building blocks? Isotropy means C must look the same after any rotation — an isotropic tensor. The only isotropic 4th-rank tensors are combinations of δijδkl, δikδjl, δilδjk. Minor symmetry forces the last two to appear together, leaving two coefficients.
Imagine a foam block. If you squeeze it from the top, it doesn't just get shorter — it also bulges out the sides. So "how much it squishes" depends on which sides you push and how hard, all at the same time. One number can't describe that. So we use a big table of numbers (a tensor) that says: "if you push this way, here's exactly how it changes in every direction." For most simple materials the whole giant table boils down to just two numbers: how stiff it is (E) and how much it bulges sideways (ν). That's the whole trick.
Dekho, 1D mein Hooke's law simple hai: σ=Eε, matlab jitna kheencho utna khinchta hai. Lekin real material — jaise spacecraft ka aluminium panel — ko aap ek saath multiple directions mein push aur shear kar sakte ho. Aur ek important baat: jab aap x direction mein kheencho, to material y aur z mein patla ho jaata hai — isko Poisson effect kehte hain. Isliye ek single number E kaafi nahi, humein ek tensor chahiye jo poora relationship bataaye: σij=Cijklεkl.
Ab Cijkl mein 34=81 components hote hain, lekin symmetries ki wajah se ye ghat ke 21 reh jaate hain (anisotropic material ke liye). Aur agar material isotropic ho — har direction mein same behaviour — to sirf do constants bachte hain: Lamé ke λ aur μ (jahan μ=G shear modulus hai). Iska clean form yaad rakho: σij=λεkkδij+2μεij. Yahaan εkk trace hai jo volume change batata hai.
Engineering form mein hum likhte hain εxx=E1[σxx−ν(σyy+σzz)] — ye −ν(...) wala part hi Poisson coupling hai. Ek trap yaad rakho: shear mein engineering shearγxy=2εxy use karna, warna factor-of-2 ki galti ho jaati hai aur answer double/half ho jaata hai.
Ye kyun important hai spacecraft ke liye? Jab pressure tank ko pressurize karte ho,