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Fourier's Law for Insulation Formula

HVAC Design and Engineering
Heat Transfer

Fourier's Law for Insulation Formula

Alternative resource for calculating heat loss or gain: Heat Loss from Ducts Equations and Calculator

Steady state, one-dimensional heat flow through insulation systems is governed by Fourier’s law:

Fourier's Law Equation

Q = –kA dT/dx

Where:

Q = rate of heat flow, Btu/h
A = cross-sectional area normal to heat flow, ft2
k = thermal conductivity of insulation material, Btu/h·ft·°F
dT/dx = temperature gradient, °F/ft

For flat geometry of finite thickness, the equation reduces to:

Q = kA(T1 – T2)/L

where L is insulation thickness, in ft.

For radial geometry, the equation becomes

Q = kA2(T1– T2)/[r2 ln(r2/r1)]

Where
r2 = outer radius, ft
r1 = inner radius, ft
A2 = area of outer surface, ft2

The term r2 ln( r2/r1 ) is sometimes called the equivalent thickness of the insulation layer. Equivalent thickness is the thickness of insulation that, if installed on a flat surface, would equal the heat flux at the outer surface of the cylindrical geometry.

Heat transfer from surfaces is a combination of convection and radiation. Usually, these modes are assumed to be additive, and therefore a combined surface coefficient can be used to estimate the heat flow to and from a surface:

hs = hc + hr

where

hs = combined surface coefficient, Btu/h·ft2·°F
hc = convection coefficient, Btu/h·ft2·°F
hr = radiation coefficient, Btu/h·ft2·°F

Assuming the radiant environment is equal to the ambient air temperature, the heat loss/gain at a surface can be calculated as

Q = hsA(Tsurf – Tamb)

The radiation coefficient is usually estimated as:

hr = ε σ ( T4surp - T4amb) / ( Tsurp - Tamb)

Where:

ε = surface emittance
σ = Stephen-Boltzmann constant, 0.1712 × 10-8 Btu/h·ft2·°R4

Related:

Reference:

  • ASHRAE Fundamental Handbook, 2019