The rate of change of temperature is given by the Stefan-Boltzmann law:
\[
\frac{dT}{dt} = -\frac{\sigma A \epsilon (T^4 - T_{\text{ambient}}^4)}{C_p \cdot m},
\]
where:
- \( \sigma = 5.67 \times 10^{-8} \, \text{Wm}^{-2}\text{K}^{-4} \) is the Stefan-Boltzmann constant,
- \( A \) is the surface area of the asteroid,
- \( \epsilon \) is the emissivity (assumed to be 1 for a blackbody),
- \( T \) is the temperature of the asteroid,
- \( T_{\text{ambient}} \) is the ambient temperature,
- \( C_p \) is the specific heat capacity,
- \( m \) is the mass of the asteroid.
We assume the asteroid cools down by 0.5 K, so \( \Delta T = 0.5 \).
The total time for cooling is:
\[
\text{Time} = \frac{C_p \cdot m \cdot \Delta T}{\sigma A \epsilon (T^4 - T_{\text{ambient}}^4)}.
\]
After substituting the values and performing the calculation, we get:
\[
\text{Time} = 39990 \, \text{seconds}.
\]
Thus, the time taken to reduce the average temperature is \( 39990 \, \text{seconds} \).