The heat energy transferred from the hotter water is equivalent to the heat energy absorbed by the cooler water. The relationship governing heat transfer is:
\[
Q = mc\Delta T
\]
Where:
- \( m \) represents the mass of the substance,
- \( c \) denotes the specific heat capacity of water (\( 4.18 \, \text{J/g}^\circ\text{C} \)),
- \( \Delta T \) indicates the variation in temperature.
Let \( T_f \) be the final equilibrium temperature.
For the hot water:
\[
Q_{\text{hot}} = 200 \times 4.18 \times (80 - T_f)
\]
For the cold water:
\[
Q_{\text{cold}} = 100 \times 4.18 \times (T_f - 20)
\]
Equating heat lost to heat gained:
\[
200 \times 4.18 \times (80 - T_f) = 100 \times 4.18 \times (T_f - 20)
\]
Simplifying the equation:
\[
200 \times (80 - T_f) = 100 \times (T_f - 20)
\]
\[
16000 - 200T_f = 100T_f - 2000
\]
\[
16000 + 2000 = 300T_f
\]
\[
18000 = 300T_f
\]
\[
T_f = \frac{18000}{300} = 60^\circ \text{C}
\]
Consequently, the mixture achieves a final temperature of \( 60^\circ \text{C} \).