Almost no experimental data exist to test theories for the nonisothermal flow of complex fluids. To provide quantitative tests for newly proposed theories, we have developed a holographic grating technique to study energy transport in an amorphous polymer melt subject to flow. Polyisobutylene with weight-averaged molecular mass of 85 kDa is sheared at a rate of 10 s ؊1 , and all nonzero components of the thermal conductivity tensor are measured as a function of time, after cessation. Our results are consistent with proposed generalizations to the energy balance for microstructural fluids, including a generalized Fourier's law for anisotropic media. The data are also consistent with a proposed stress-thermal rule for amorphous polymer melts. Confirmation of the universality of these results would allow numerical modelers to make quantitative predictions for the nonisothermal flow of polymer melts.N early all biological and advanced synthetic materials can exhibit molecular order or structure spontaneously, or be induced by flow. For example, rod-like molecules can form liquid crystals or membranes at equilibrium, and surfactants can self-assemble into worm-like shapes (1). These materials with microstructure exhibit nonequilibrium behavior much more complex than what is observed for simple, low-molecular-weight liquids. Upon flow, they may orient, crystallize, and show stresses many orders of magnitude larger than water. What is more, these large stresses relax back to equilibrium on time scales from seconds to minutes when the flow is stopped (2).The governing dynamics of simple (low-molecular-weight) f luids are well understood. Their derivation begins with straightforward balance equations for mass, momentum, and energy (and possibly angular momentum conservation) applied to a continuum (3). Mass conservation leads to an evolution equation for density , the continuity equation. The second and third balances, however, are not closed; we have too many unknowns and not enough equations. For closure we need additional equations called constitutive relations. For the momentum balance, we need an equation to relate stress to velocity in the f luid, and, in the case of the energy balance, we require two additional equations: a relationship between energy and measurable quantities, usually temperature T and velocity v; and a relationship between heat f lux and temperature. For simple f luids, these constitutive relations are well known. For the stress tensor we use the Newtonian constitutive equation, which states that the stress is linearly related to the instantaneous velocity gradient ٌv, through the viscosity. The energy density is a sum of internal energy density u, and kinetic energy density 1͞2 v 2 . The third relation is Fourier's law for the heat f lux q, which is linearly related to the temperature gradient by a scalar thermal conductivity.Using these three relations, we then have a closed set of evolution equations for the density , the velocity field v, and the temperature field T. If material parameters, ...