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Physics & Engineering
Entropy Calculator
Calculate entropy change of a system
Process Type

Positive for heat added, negative for heat removed

Entropy Formula

ΔS = Q / T

ΔS = Entropy change (J/K)

Q = Heat transferred (J)

T = Absolute temperature (K)

Common Entropy Values
Ice melting at 273 K+22.0 J/mol·K
Water vaporizing at 373 K+109 J/mol·K
Ideal gas expansion+nR·ln(V₂/V₁)
What is Entropy?

Entropy is a fundamental thermodynamic property that measures the degree of disorder or randomness in a system. Introduced by Rudolf Clausius in 1865, entropy quantifies the amount of thermal energy in a system that is unavailable for doing useful work. The Second Law of Thermodynamics states that the total entropy of an isolated system can only increase over time, which explains why many natural processes are irreversible.

In practical terms, entropy helps engineers understand energy efficiency, predict the direction of spontaneous processes, and design more efficient thermal systems. Higher entropy means more disorder and less available energy for work, while lower entropy indicates a more ordered state with greater potential for useful work.

Disclaimer: Entropy calculations assume ideal or reversible processes. Real systems may have additional irreversibilities. Consult thermodynamics references for precise analysis.

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