Intermediate

Thermal Diffusivity Calculator — α = k / (ρ · Cₚ)

Enter a material's thermal conductivity, density, and specific heat capacity to compute its thermal diffusivity — a measure of how fast temperature changes propagate through it.

W/(m·K)

e.g. 0.04 foam, 0.2 wood, 0.6 water, 50 steel, 385 copper

kg/m³

e.g. 1.2 air, 500 wood, 1000 water, 2700 aluminium, 7800 steel

J/(kg·K)

e.g. 1005 air, 2000 wood, 4182 water, 897 aluminium, 500 steel

s

Optional — used to compute thermal penetration depth δ = 2√(α·t)
Thermal diffusivity
12.8205mm²/s

α = k / (ρ · Cₚ) — higher means temperature changes spread faster

α in m²/s
0.00001282 m²/s
α in mm²/s
12.8205 mm²/s
Penetration depth (δ = 2√αt)
0.4297 m
Step-by-step: thermal diffusivity
1

Formula

α = k / (ρ × Cₚ)
2

Thermal conductivity

k = 50 W/(m·K)
3

Density

ρ = 7800 kg/m³
4

Specific heat capacity

Cₚ = 500 J/(kg·K)
5

Denominator

ρ × Cₚ = 7800 × 500 = 3900000 J/(m³·K)
=

Thermal diffusivity

α = 50 / 3900000 = 0.00001282 m²/s
Step by step
  1. 1

    Volumetric heat capacity ρ × Cₚ

    7,800 × 500 = 3,900,000
    Energy absorbed per unit volume per kelvin.
  2. 2

    α in m²/s

    50 ÷ 3,900,000 = 0.00001282
  3. 3

    α in mm²/s (× 10⁶)

    0.00001282 × 1,000,000 = 12.8205
Results are estimates for general information only and are not professional advice — always verify important results independently before relying on them. Read the full disclaimer.
Quick answer

How does this calculator work?

Thermal diffusivity α = k/(ρ·Cₚ) combines conductivity and volumetric heat capacity to quantify how fast temperature waves travel through a material. Steel ≈ 12.8 mm²/s (fast), water ≈ 0.14 mm²/s (slow). The thermal penetration depth after time t is δ = 2√(α·t).

Formula
α = k / (ρ · Cₚ) [m²/s] • δ = 2√(α · t) (penetration depth at time t)
How this is calculated

Thermal diffusivity α (m²/s) measures how quickly a temperature disturbance at one surface of a material propagates through its bulk. It combines two competing effects: high thermal conductivity k promotes fast heat transport, while high volumetric heat capacity ρ·Cₚ means the material absorbs heat without changing temperature much, slowing propagation. The formula α = k/(ρ·Cₚ) is a material property — independent of geometry and boundary conditions — and is the key parameter in the transient heat-conduction equation ∂T/∂t = α·∇²T.

Materials with high diffusivity (metals) equilibrate quickly after a temperature change. Copper (α ≈ 112 mm²/s) reaches thermal equilibrium far faster than wood (α ≈ 0.08–0.13 mm²/s) or water (α ≈ 0.143 mm²/s), which is why a metal spoon in hot coffee heats up faster than a wooden one. Building materials like concrete (α ≈ 0.7–1.0 mm²/s) have intermediate diffusivity — they store heat well and release it slowly, which is useful for thermal mass in passive-solar design.

The thermal penetration depth δ = 2√(α·t) is a practical derived quantity: it approximates how far a sudden temperature change at one surface has significantly penetrated into a semi-infinite material after time t. For example, after 1 hour (3,600 s) in steel (α = 12.8 mm²/s), the penetration depth is about 430 mm; in concrete (α = 0.75 mm²/s) it is about 104 mm. This formula is an order-of-magnitude estimate for semi-infinite geometry — actual penetration in finite-thickness slabs requires the full analytical or numerical solution.

Frequently asked questions

Thermal conductivity k (W/m·K) measures steady-state heat flow through a material at a given temperature gradient — useful for calculating heat losses through walls and pipes. Thermal diffusivity α (m²/s) measures how fast a temperature change propagates in transient conditions. A material can have high k but low α if it has a very high heat capacity (e.g. water: k = 0.6 W/m·K but α = 0.14 mm²/s). For steady-state calculations use k; for time-dependent problems use α.

Approximate values in mm²/s: still air ≈ 19, water ≈ 0.14, wood ≈ 0.10–0.13, concrete ≈ 0.7–1.0, glass ≈ 0.34, brick ≈ 0.5, ice ≈ 1.0, aluminium ≈ 97, copper ≈ 112, steel ≈ 12–14, silver ≈ 166. Higher diffusivity means faster thermal equilibration.

The penetration depth δ = 2√(α·t) is the approximate distance into a material at which the temperature has changed significantly after a step change applied at the surface. It is useful for estimating: how deep frost penetrates soil overnight, how fast a metal casting cools, or whether a thermal disturbance has reached the interior of a wall after a given time. It grows with the square root of elapsed time.

Also known as

thermal diffusivity calculator alpha k rho cp
heat diffusion material property
thermal diffusivity of materials
alpha equals k divided by rho cp
penetration depth thermal calculator
transient heat conduction diffusivity
thermal inertia calculator

APA

TG we-Calculate Editorial Team. (2026). Thermal Diffusivity Calculator — α = k / (ρ · Cₚ) [Online calculator]. TG we-Calculate. https://we-calculate.com/calculator/thermal-diffusivity-calculator

Chicago

TG we-Calculate Editorial Team. "Thermal Diffusivity Calculator — α = k / (ρ · Cₚ)." TG we-Calculate. 2026. https://we-calculate.com/calculator/thermal-diffusivity-calculator.

IEEE

TG we-Calculate Editorial Team, "Thermal Diffusivity Calculator — α = k / (ρ · Cₚ)," TG we-Calculate, 2026. [Online]. Available: https://we-calculate.com/calculator/thermal-diffusivity-calculator

BibTeX

@misc{wecalculate_thermal_diffusivity_calculator, title = {Thermal Diffusivity Calculator — α = k / (ρ · Cₚ)}, author = {{TG we-Calculate Editorial Team}}, howpublished = {\url{https://we-calculate.com/calculator/thermal-diffusivity-calculator}}, year = {2026}, note = {TG we-Calculate} }

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