The transfer of thermal energy between regions of different temperature.Heat flow, or heat transfer, is the spontaneous movement of thermal energy from a region of higher temperature to a region of lower temperature. It occurs through three mechanisms: conduction (direct contact), convection (fluid movement), and radiation (electromagnetic waves). Heat flow is a cornerstone of thermodynamics, governing everything from planetary climates to the operation of engines and refrigerators. The second law of thermodynamics dictates that heat naturally flows one way, from hot to cold, unless external work is applied.
The study of heat flow began with early thermometers in the 17th century, but the quantitative laws emerged in the 19th century. Joseph Fourier formulated his law of heat conduction in 1822, and Sadi Carnot's work on heat engines laid the foundation for thermodynamics.
At the microscopic level, heat is the kinetic energy of particles. In conduction, energetic particles collide with neighbors, transferring energy. Convection involves bulk motion of fluids carrying thermal energy. Radiation emits photons that carry energy across empty space. The rate of heat flow depends on temperature difference, material properties (thermal conductivity), and geometry, as described by Fourier's law for conduction and the Stefan-Boltzmann law for radiation.
Heat flow principles are used in designing heat exchangers, thermal insulation, cooling systems for electronics, and in understanding climate change and weather patterns.
Heat can flow 'backwards' in certain quantum systems, where energy moves from cold to hot due to quantum correlations, as demonstrated in recent experiments.











