Thermodynamics

Thermal Conductivity Calculator

Back-solve material thermal conductivity from heat-flow data, or use a known k-value to estimate heat rate, heat flux, and thermal resistance.

Formula k = Q̇ L / (A ΔT)Reviewed Sep 7, 2026

Thermal conductivity, k, is the material property that tells you how easily heat conducts through a substance. Search intent for this calculator is usually practical: users either have a lab or field measurement and need k = Q̇L/(AΔT), or they know the material and want to estimate the heat flow through a simple slab. This page focuses on that material-property workflow, with common material presets, nearest-material comparison, heat flux, and resistance context alongside the headline k-value.

Calculation Bench
Solve for
01

Q̇ · Measured steady heat flow through the sample.

02

A · Cross-sectional area perpendicular to heat flow.

03

ΔT · Use a temperature difference, not absolute temperature.

04

L · Material thickness in the heat-flow direction.

Steady flat-layer conduction only. For multi-layer walls, surface films, and code-style U-values, use the U-Value Calculator instead.

Solution

Enter heat-flow data or pick a material conductivity to calculate thermal conductivity context.

k = Q̇ L / (A ΔT)

Formula Sheet

k=Q˙LAΔTk = \dfrac{\dot{Q}L}{A\Delta T}
Q˙=Qt\dot{Q} = \dfrac{Q}{t}
k=QLtAΔTk = \dfrac{QL}{tA\Delta T}
Q˙=kAΔTL\dot{Q} = \dfrac{kA\Delta T}{L}
q′′=kΔTLq'' = \dfrac{k\Delta T}{L}
  • kThermal Conductivity
  • Q̇Heat Transfer Rate
  • QHeat Energy
  • tTime
  • AArea
  • ΔTTemperature Difference
  • LThickness

Common Thermal Conductivity Values

MaterialTypical kUse
Dry air0.026 W/(m·K)Still air near room temperature
Rigid foam insulation0.03 W/(m·K)Typical closed-cell insulation range
Mineral wool0.04 W/(m·K)Common building insulation
Softwood0.12 W/(m·K)Across-grain building lumber estimate
Water0.6 W/(m·K)Liquid water near room temperature
Brick0.72 W/(m·K)Approximate masonry value
Glass1 W/(m·K)Soda-lime glass approximation
Concrete1.4 W/(m·K)Normal-weight concrete approximation
Carbon steel50 W/(m·K)Room-temperature engineering estimate
Aluminum237 W/(m·K)Common pure aluminum reference
Copper401 W/(m·K)High-conductivity metal reference

Variables & Units

SymbolVariableDescriptionCommon Units
kThermal ConductivityMaterial property describing heat conduction ability.W/(m·K), Btu/(h·ft·°F)
Q̇Heat Transfer RateSteady heat-flow rate through the sample or slab.W, kW, Btu/h
QHeat EnergyTotal heat transferred over the measurement interval.J, kJ, Btu
tTimeMeasurement interval for heat energy.s, min, h
AAreaArea normal to heat flow.m², ft², in²
ΔTTemperature DifferenceTemperature drop across the material thickness.K, °C, °F
LThicknessConduction path length through the material.mm, cm, m, in

How to Use This Calculator

  • 01Use Measured Rate when you already know heat-transfer rate in watts. Enter area, temperature difference, and thickness to solve for material conductivity.
  • 02Use Energy Over Time when your experiment reports heat energy over a time interval. The calculator first converts Q/t into watts, then solves k.
  • 03Use Known Material when you already know k or choose a material preset. The calculator estimates heat-transfer rate, heat flux, and thermal resistance for the slab.
  • 04Use a temperature difference, not absolute hot-side/cold-side temperatures. A 20 °C temperature difference equals a 20 K temperature difference.
  • 05Compare the result with the material table. If a measured k-value is far from any expected material, recheck thickness, area, heat-rate, contact losses, and units.

How the Formula Works

For steady one-dimensional conduction through a flat slab, Fourier's law reduces to Q̇ = kAΔT/L. Rearranging gives k = Q̇L/(AΔT).

If heat energy Q is measured over time t, the heat-transfer rate is Q̇ = Q/t before applying the conductivity formula.

The calculator also reports heat flux q'' = Q̇/A = kΔT/L, area-normalized resistance R' = L/k, and total resistance R = L/(kA). These extra outputs help users act on the result instead of seeing only a bare k-value.

Worked Example 01

Back-solve insulation conductivity from measured heat rate

Known

  • Heat transfer rate: 80 W
  • Thickness: 0.10 m
  • Area: 10 m²
  • Temperature difference: 20 K

Formula

k = Q̇ L / (A ΔT)

Substitution

k = 80 × 0.10 / (10 × 20)

Result

k = 0.04 W/(m·K)

That value is in the insulation range and close to mineral wool or similar building insulation.

Worked Example 02

Find k from heat energy over time

Known

  • Heat energy: 30,000 J
  • Time: 10 s
  • Thickness: 0.02 m
  • Area: 1 m²
  • Temperature difference: 30 K

Formula

k = Q L / (t A ΔT)

Substitution

Q̇ = 30000/10 = 3000 W; k = 3000 × 0.02 / (1 × 30)

Result

k = 2 W/(m·K)

The energy measurement is first converted into watts before applying Fourier's law.

Worked Example 03

Copper heat flow through a small bar

Known

  • Thermal conductivity: 401 W/(m·K)
  • Area: 4 cm²
  • Temperature difference: 80 K
  • Thickness: 0.20 m

Formula

Q̇ = k A ΔT / L

Substitution

Q̇ = 401 × 0.0004 × 80 / 0.20

Result

Q̇ = 64.16 W

Copper conducts heat strongly even through a relatively small cross-section.

Applications

  • 01Back-solving k from a guarded-hot-plate style measurement
  • 02Comparing an unknown material result against common insulation, masonry, liquid, and metal values
  • 03Estimating slab heat rate and heat flux from a known material k-value
  • 04Checking whether a material behaves more like an insulator, masonry, or conductor

Assumptions

  • 01Steady one-dimensional conduction through a uniform flat material layer.
  • 02Thermal conductivity is constant across the temperature range.
  • 03Heat flow is perpendicular to the entered area.
  • 04Temperature difference is entered as a positive magnitude.

Where This Model Stops

  • 01Does not include convection films, radiation, contact resistance, moisture, thermal bridges, anisotropic materials, or temperature-dependent property curves.
  • 02Measured conductivity can be badly skewed by heat loss around sample edges or poor sensor contact.
  • 03Use the U-Value Calculator for multi-layer assemblies and the Heat Conduction Calculator for general solve-any-variable Fourier-law work.

References

  1. [1]
    Thermal Conductivity - Online Converter

    Engineering ToolBox

    Reference for thermal conductivity units and common material-property framing.

  2. [2]
    Thermal Conductivity Calculator

    BYJU'S

    Reference for k = QL/(AΔT) educational calculator intent.

  3. [3]
    Thermal Conductivity Calculator

    CalculatorLib

    Reference for energy-over-time measurement workflow and resistance output.

Frequently Asked Questions

How is this different from the Heat Conduction Calculator?

Heat Conduction Calculator is the broad Fourier-law solver for heat rate, heat flux, area, thickness, and temperature difference. This page is focused on thermal conductivity as a material property, with material presets, nearest-material comparison, and resistance context.

Is thermal conductivity the same as R-value?

No. Thermal conductivity k measures how easily a material conducts heat. Area-normalized resistance is R' = L/k, so thicker layers and lower k-values create higher insulation resistance.

Can I use degrees Celsius for ΔT?

Yes, if it is a temperature difference. A 20 °C difference equals a 20 K difference. Do not enter absolute surface temperatures in this field.

Why does measured k not match the material table?

Common causes are heat leakage around the sample, wrong area or thickness units, transient rather than steady heat flow, moisture, contact resistance, or a material whose k changes with temperature.