A polymer melt has an observation-time-dependent response because chains need time to rearrange. Short compared with their terminal relaxation time, entangled chains constrain one another and can store elastic free energy. Long compared with that time, chains escape their original constraints by reptation and the uncrosslinked melt flows. A permanently crosslinked elastomer instead retains a long-time elastic modulus.
A single-time approximation is the Maxwell fluid: a spring of shear modulus and a viscous dashpot of viscosity in series. Their common stress and additive shear strains give , with relaxation time . For sinusoidal deformation proportional to , the storage modulus and loss modulus are
At low frequency dominates; at high frequency within this coarse-grained model dominates. Real melts have a spectrum of relaxation times and additional segmental or glassy regimes, so the single-time model does not describe every frequency. A step-strain experiment measures the decay of stress, whereas oscillatory rheometry separates stored energy from dissipated energy through the phase of the response.

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