Compute enthalpy change (ΔH) for heating, cooling, and phase change processes using Q = m·cp·ΔT + phase transition energy. Includes material database for water, air, metals, and custom inputs.
In thermodynamics, enthalpy (H) is a measure of the total heat content of a system. The change in enthalpy (ΔH) represents the heat absorbed or released at constant pressure, described by the fundamental equation ΔH = m · cp · ΔT + ΔHphase. This calculator integrates both sensible heat (temperature change without phase change) and latent heat (energy absorbed/released during melting, vaporization).
ΔH = m · cp,ice·ΔTice + m·Lfusion + m·cp,water·ΔTwater + m·Lvapor + m·cp,steam·ΔTsteam
where Lfusion = 334 kJ/kg, Lvapor = 2260 kJ/kg; cp,ice=2.09, cp,water=4.184, cp,steam=2.0 kJ/(kg·K).
A power plant boiler heats water from 25°C to superheated steam at 150°C. Using our calculator: mass = 10 kg water. The algorithm computes: (1) sensible heat 25→100°C: 10×4.184×75 = 3138 kJ; (2) vaporization: 10×2260 = 22600 kJ (positive, absorbed); (3) sensible heat 100→150°C steam: 10×2.0×50 = 1000 kJ. Total ΔH = 26738 kJ. For cooling from 150°C back to 25°C, all signs reverse – correctly handled.
All calculations are performed in double‑precision floating point. Latent heat values are referenced to IAPWS‑IF97 standards. For water, the calculator automatically uses segmented specific heats: ice (cp=2.09 kJ/(kg·K)), liquid (4.184), steam (2.0). For other materials, constant cp is assumed – accurate for moderate temperature ranges. The tool also validates that input temperatures are numeric and mass positive; errors are reported clearly.
| Material | cp [kJ/(kg·K)] | Typical application |
|---|---|---|
| Water (liquid) | 4.184 | Cooling systems, heat exchangers |
| Ice | 2.09 | Cold storage, cryogenics |
| Steam (superheated) | 2.0 | Power cycles, district heating |
| Air | 1.005 | HVAC, ventilation |
| Aluminum | 0.897 | Heat sinks, automotive radiators |
| Copper | 0.385 | Electrical conductors, heat pipes |
Enthalpy change is a state function, meaning only initial and final states matter – path independent. That’s why we can sum sensible and latent contributions linearly. The first law of thermodynamics at constant pressure gives ΔH = Qp. Our calculator respects this principle, making it reliable for everything from chemical reaction calorimetry to climate control sizing. For water, the high specific heat and latent heats explain its role as an outstanding thermal buffer in nature and industry.