Next, let's talk about 'specific heat capacity'. This is the amount of heat required to raise the temperature of one gram of a substance by one degree Celsius. The specific heat capacity of water is 4.18 J/g°C, one of the highest among common substances, which is why water heats up and cools down slowly.
When dealing with temperature changes in water, we use the formula:
- \( Q = m_{\text{water}} \times c \times \Delta T \)
Here, \(Q\) is the energy, \(m_{\text{water}}\) is the mass of the water, \(c\) is the specific heat capacity, and \(\Delta T\) is the change in temperature.
In the given problem, the water cools from \(8.0^{\circ} \text{C} \) to \(0.0^{\circ} \text{C} \), and the energy transfer is calculated as:
\( Q = 15030 \text{ J} = m_{\text{water}} \times 4.18 \text{ J/g°C} \times (8.0^{\circ} \text{C} - 0.0^{\circ} \text{C})\).
This formula helps us find out how much heat energy the water lost to melt the ice.