Thermodynamics

Newton's Law of Cooling

Rate of cooling proportional to temperature difference. Solution: T(t) = T_env + (T₀ - T_env)e^(-ht).

Variables

dT/dt
Rate of temperature change
Cooling rate
K/s
h
Cooling constant
Depends on surface and medium
1/s
T
Object temperature
Current temperature
K
T_env
Environment temperature
Ambient temperature
K

Derivation

Empirical law for convective cooling. Valid when temperature difference is small.

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