- Mass m (kg)
- 1kg
- Specific heat c (J/(kg·K))
- 4186J/(kg·K)
- Temperature change ΔT (K)
- 10K
41,860.00J
Open with these values41,860.00J
Result: 41,860.00 JHeat energy is mass times specific heat times temperature change: 1 kg of water (c = 4186) warmed by 10 °C takes 41,860 J. The specific heat is yours to enter, so any substance works — water 4186, aluminium 900, copper 385. A negative temperature change means cooling, and the answer turns negative.
Held fixed: Mass m (kg) 1.000 kg, Specific heat c (J/(kg·K)) 4,186.0 J/(kg·K).
| Temperature change ΔT (K) (K) | Result (J) |
|---|---|
| 0.00 | 0.00 |
| 2.50 | 10,465.00 |
| 5.00 | 20,930.00 |
| 7.50 | 31,395.00 |
| 10.00Your value | 41,860.00 |
| 12.50 | 52,325.00 |
| 15.00 | 62,790.00 |
| 17.50 | 73,255.00 |
| 20.00 | 83,720.00 |
41,860.00J
Open with these values9,000.00J
Open with these values-41,860.00J
Open with these valuesQ = m × c × ΔT
A rise of ten kelvin and a rise of ten degrees Celsius are the same step, so nothing needs converting here. That sets this formula apart from the gas laws, which insist on an absolute temperature.
Water's specific heat shifts with temperature: 4185.5 from the 15 °C calorie, 4187 at 15 °C, and 4184 at 20 °C as the common figure. The field is yours — enter the value your own source gives.
Q = mcΔT covers warming and cooling only, while the substance stays solid, liquid or gas throughout. Melting or boiling needs the latent heat on top, which this calculator does not carry.
Water going from 20 °C to 30 °C entered as ΔT = 30.
ΔT is the difference, so it is 10. With 1 kg and c = 4186 that is 41,860 J, not 125,580 J.
ΔT converted to kelvin by adding 273.15.
A difference needs no offset — ten degrees of warming are ten kelvin. Entering 283.15 would print 1,185,266 J instead of 41,860 J.
Melting 1 kg of ice at 0 °C costs m × c × 0.
A phase change runs at constant temperature, so ΔT is zero and the formula returns zero. The energy sits in the latent heat, which is outside this calculator.
| Mass (kg), c (J/(kg·K)), ΔT (K) | Substance | Heat energy (J) |
|---|---|---|
| 1, 4186, -10 | Water, cooled | -41860 |
| 3, 500, 0 | Steel, no change | 0 |
| 0.5, 900, 20 | Aluminium, heated | 9000 |
| 1, 4186, 10 | Water, heated | 41860 |
| 2, 4186, 5 | Twice the water, half the rise | 41860 |
Heat energy is the mass times the specific heat times the temperature change. For 1 kg of water with c = 4186 heated by 10 °C, that is 1 × 4186 × 10 = 41,860 J. It tells you how much energy is needed to change a substance's temperature by a given amount.
Specific heat (c) is the energy needed to raise 1 kg of a substance by 1 kelvin, in J/(kg·K). Water is about 4186, aluminium about 900, copper about 385, and dry air about 1005. Look up the value for your material and enter it directly — it is an input, not a fixed constant.
Mass in kilograms, specific heat in joules per kilogram-kelvin, and temperature change in kelvin or degrees Celsius — one kelvin equals one degree Celsius in size. With these SI inputs the result comes out in joules, with no conversion needed.
A negative ΔT means the substance is cooling rather than heating. The formula then returns a negative heat energy, which is energy released by the substance instead of absorbed. Cooling 1 kg of water by 10 °C gives −41,860 J — the same magnitude, opposite sign.
It underpins heating and HVAC sizing, cooking, calorimetry in chemistry, and engine cooling. Water's high specific heat is why it makes such a good coolant and why oceans moderate the climate — they absorb huge amounts of energy for only a small temperature change.
Information, not professional advice.
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