Heat transfer in the context of temperature change is a critical process in thermodynamics, describing how heat energy moves from one place to another. The formula for calculating the heat (\( Q \)) required for a temperature change involves a few variables: the mass of the substance (\( m \)), its specific heat (\( c \)), and the change in temperature (\( \Delta T \)). The equation is expressed as:
The specific heat acts like a coefficient to resist temperature change, while the mass and temperature difference define the overall capacity for heat absorption or release.
In the context of water,
if you need to increase the temperature of 10 kg of water from 24.6°C to 46.2°C:
- Mass (\( m \)) = 10,000 g
- Specific heat (\( c \)) = 4.18 J/g°C
- Temperature change (\( \Delta T \)) = 21.6°C
Inserting these in the formula gives:
- \( Q = 10,000 \,\text{g} \times 4.18 \,\text{J/g}^\circ\text{C} \times 21.6^\circ\text{C} \approx 903,360 \,\text{J} \)
This considerable amount of energy demonstrates how liquid water, with its high specific heat, demands substantial energy even for modest temperature changes.