Equilibrium Temperature Formula:
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Equilibrium temperature is the temperature at which an object reaches thermal balance with its environment, where the rate of energy absorption equals the rate of energy emission through radiation.
The calculator uses the equilibrium temperature formula derived from the Stefan-Boltzmann law:
Where:
Explanation: This formula calculates the temperature at which an object's radiative heat loss equals the heat input, reaching thermal equilibrium.
Details: Calculating equilibrium temperature is crucial in thermodynamics, climate science, astronomy, and engineering applications where radiative heat transfer is significant.
Tips: Enter heat input in watts, Stefan-Boltzmann constant in W/m²K⁴ (default is 5.67e-8), and surface area in square meters. All values must be positive.
Q1: What is the Stefan-Boltzmann constant?
A: The Stefan-Boltzmann constant (σ) is a physical constant that describes the total intensity of radiation emitted by a black body per unit surface area.
Q2: Does this formula assume a black body?
A: Yes, this formula assumes an ideal black body with emissivity of 1. For real materials, the formula should include emissivity.
Q3: What are typical applications of this calculation?
A: This calculation is used in planetary science, climate modeling, thermal engineering, and designing radiative cooling systems.
Q4: Why is the temperature proportional to the fourth root of heat input?
A: This relationship comes from the Stefan-Boltzmann law, which states that radiant energy is proportional to the fourth power of temperature.
Q5: Can this calculator be used for objects with non-uniform temperature?
A: This calculator assumes uniform temperature distribution. For complex geometries or non-uniform heating, more advanced thermal analysis is needed.