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Thermal conductivity () is a fundamental thermophysical property that quantifies a material's inherent ability to conduct heat via conduction. It represents the rate of heat transfer () per unit area () per unit temperature gradient () under steady-state conditions. This definition arises directly from Fourier's Law of Heat Conduction:
where is the heat flux (heat transfer rate per unit area, W/m²) in the x-direction, and is the temperature gradient (K/m). The negative sign indicates heat flows from regions of higher temperature to lower temperature. Essentially, tells us how readily heat energy diffuses through a material due to molecular interactions (vibrations in solids, collisions in fluids).
Factors Influencing Thermal Conductivity:
Units: The SI unit is Watts per meter-Kelvin (W/m·K). Imperial units (Btu·in/hr·ft²·°F) are sometimes used; conversion is essential (1 W/m·K ≈ 6.933 Btu·in/hr·ft²·°F).
Distinction from Thermal Diffusivity: While thermal conductivity () measures how well a material conducts heat, thermal diffusivity ()) measures how fast heat propagates through it by incorporating density () and specific heat (). High enables more heat flow, but high means temperature changes occur more rapidly.