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Thermal conductivity and resistivity

Capacity of a material to conduct heat

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Through Thermodynamics, Thermal conduction and International System of Units

The reciprocal of thermal conductivity is called thermal resistivity.

Materials with high thermal conductivity transfer heat more efficiently than those with low thermal conductivity. Heat transport can arise from different microscopic mechanisms: In metals, thermal conductivity is typically dominated by free electrons, whereas in dielectric materials such as diamond it is largely due to lattice vibrations. Materials with high thermal conductivity are used in heat sink applications, while materials with low thermal conductivity, such as mineral wool or Styrofoam, are used for thermal insulation.

The defining equation for thermal conductivity is Fourier's law of heat conduction: q=−k∇T, where q is the heat flux, k is the thermal conductivity, and ∇T is the temperature gradient. Although k is commonly treated as a scalar, it can also be a second-rank tensor in the case of anisotropic materials.

Definition

Simple definition

Consider a solid material placed between two environments of different temperatures. Let T1 be the temperature at x=0 and T2 be the temperature at x=L, and suppose T2>T1. An example of this scenario is a building on a cold winter day; the solid material in this case is the building wall, separating the cold outdoor environment from the warm indoor environment.

According to the second law of thermodynamics, heat will flow from the hot environment to the cold one as the temperature difference is equalized by diffusion. This is quantified in terms of a heat flux q, which gives the rate, per unit area, at which heat flows in a given direction (in this case minus x-direction). In many materials, q is observed to be directly proportional to the temperature difference and inversely proportional to the separation distance L:

q=−k⋅T2−T1L.

The constant of proportionality k is the thermal conductivity; it is a physical property of the material. In the present scenario, since T2>T1 heat flows in the minus x-direction and q is negative, which in turn means that k>0. In general, k is always defined to be positive. The same definition of k can also be extended to gases and liquids, provided other modes of energy transport, such as convection and radiation, are eliminated or accounted for.

The preceding derivation assumes that the k does not change significantly as temperature is varied from T1 to T2. Cases in which the temperature variation of k is non-negligible must be addressed using the more general definition of k discussed below.

General definition

Thermal conduction is defined as the transport of energy due to random molecular motion across a temperature gradient. It is distinguished from energy transport by convection and molecular work in that it does not involve macroscopic flows or work-performing internal stresses.

Energy flow due to thermal conduction is classified as heat and is quantified by the vector q(r,t), which gives the heat flux at position r and time t. According to the second law of thermodynamics, heat flows from high to low temperature. Hence, it is reasonable to postulate that q(r,t) is proportional to the gradient of the temperature field T(r,t), i.e.

q(r,t)=−k∇T(r,t),

where the constant of proportionality, k>0, is the thermal conductivity. This is called Fourier's law of heat conduction. Despite its name, it is not a law but a definition of thermal conductivity in terms of the independent physical quantities q(r,t) and T(r,t). As such, its usefulness depends on the ability to determine k for a given material under given conditions. The constant k itself usually depends on T(r,t) and thereby implicitly on space and time. An explicit space and time dependence could also occur if the material is inhomogeneous or changing with time.

In some solids, thermal conduction is anisotropic, i.e. the heat flux is not always parallel to the temperature gradient. To account for such behavior, a tensorial form of Fourier's law must be used:

q(r,t)=−κ⋅∇T(r,t)

where κ is symmetric, second-rank tensor called the thermal conductivity tensor.

An implicit assumption in the above description is the presence of local thermodynamic equilibrium, which allows one to define a temperature field T(r,t). This assumption could be violated in systems that are unable to attain local equilibrium, as might happen in the presence of strong nonequilibrium driving or long-ranged interactions.

Other quantities

In engineering practice, it is common to work in terms of quantities which are derivative to thermal conductivity and implicitly take into account design-specific features such as component dimensions.

For instance, thermal conductance is defined as the quantity of heat that passes in unit time through a plate of particular area and thickness when its opposite faces differ in temperature by one kelvin. For a plate of thermal conductivity k, area A and thickness L, the conductance is kA/L, measured in W⋅K−1. The relationship between thermal conductivity and conductance is analogous to the relationship between electrical conductivity and electrical conductance.

Thermal resistance is the inverse of thermal conductance. It is a convenient measure to use in multicomponent design since thermal resistances are additive when occurring in series.

There is also a measure known as the heat transfer coefficient: the quantity of heat that passes per unit time through a unit area of a plate of particular thickness when its opposite faces differ in temperature by one kelvin. In ASTM C168-15, this area-independent quantity is referred to as the "thermal conductance". The reciprocal of the heat transfer coefficient is thermal insulance. In summary, for a plate of thermal conductivity k, area A and thickness L,

  • thermal conductance = kA/L, measured in W⋅K−1.
    • thermal resistance = L/(kA), measured in K⋅W−1.
  • heat transfer coefficient = k/L, measured in W⋅K−1⋅m−2.
    • thermal insulance = L/k, measured in K⋅m2⋅W−1.

The heat transfer coefficient is also known as thermal admittance in the sense that the material may be seen as admitting heat to flow.

An additional term, thermal transmittance, quantifies the thermal conductance of a structure along with heat transfer due to convection and radiation. It is measured in the same units as thermal conductance and is sometimes known as the composite thermal conductance. The term U-value is also used.

Thermal effusivity e is a combination of material thermal conductivity, density, and specific heat capacity:

e=kρCp

Thermal effusivity is the only thermophysical property that governs the interfacial temperature when two semi-infinite bodies come into contact. This implies that the thermoception of a material by the human skin is affected by the thermal effusivity of that material.

Finally, thermal diffusivity α combines thermal conductivity with density and specific heat:

α=kρcp.

As such, it quantifies the thermal inertia of a material, i.e. the relative difficulty in heating a material to a given temperature using heat sources applied at the boundary.

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