The rate of heat transfer \( Q \) is given by:
\[
Q = k A \frac{\Delta T}{d}
\]
where:
- \( k \) is the thermal conductivity,
- \( A \) is the surface area,
- \( \Delta T \) is the temperature difference,
- \( d \) is the thickness of the material.
The time to melt the ice is inversely proportional to the thermal conductivity:
\[
t \propto \frac{1}{k}
\]
Thus, the ratio of the times for containers P and Q is related to the square root of the ratio of their thermal conductivities:
\[
\frac{t_2}{t_1} = \sqrt{\frac{k_1}{k_2}}
\]
Thus, the ratio of conductivities is:
\[
\frac{k_1}{k_2} = \frac{t_1^2}{t_2}
\]