How to use (3 steps)
- Select the mode: single object or mixing two substances.
- Enter mass, specific heat, temperatures, or heat. Keep units consistent (kg with J/(kg·K) or g with J/(g·K)).
- Press Compute to see the solved value, the full table, and the step-by-step energy balance. Copy URL shares the setup.
Default example: heat 0.10 kg of water from 20 °C to 80 °C (solve for Q). The initial calculation runs automatically.
Inputs
Results
Positive Q heats the sample; negative Q means the sample releases heat. Q > 0: heat absorbed.
| Mass m | 0.1 kg |
|---|---|
| Specific heat c | 4184 J/(kg·°C) |
| Temperature change ΔT | 60 °C |
| Heat Q | 25104 J |
How it's calculated
- Use mass
m = 0.1 kg, specific heatc = 4184 J/(kg·°C), initial temperature20 °C, and final temperature80 °C. - The temperature change is
ΔT = 80 − 20 = 60 °C. - Apply
Q = m c ΔT, givingQ = 0.1 × 4184 × 60 = 25104 J.
FAQ
Can this handle phase changes such as melting or boiling?
This calculator assumes constant specific heat and no phase change. To model melting or evaporation, add the latent heat separately.
How should I align the units?
Use matching units such as kg with J/(kg·K) or g with J/(g·K). Mixing units (e.g., kg with J/(g·K)) will give incorrect results. Temperatures may be in °C or K because only differences are used, so ΔT is identical.
Does it consider heat loss to the surroundings?
Mixing mode assumes an insulated system with no heat loss to the container or air. Real experiments may differ because of heat loss or the container's heat capacity.
What should I enter first for a calorimetry run?
Start with mass, temperature change, and the known heat or specific heat value. Keep units consistent so the calculated heat capacity or specific heat reflects the experiment setup.
Why can a calorimetry run results differ from nearby tools?
Differences usually come from mass, heat, temperature change, and heat-loss assumptions. Match those assumptions before comparing this result with another CalcBE page, spreadsheet, or external tool.
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