The problem involves the relationship between pressure and volume for an air bubble as it rises to the surface of a lake. We can use Boyle's Law, which states that for a constant temperature, the product of pressure and volume remains constant, i.e., \( P_1V_1 = P_2V_2 \). Given:
\( V_2 = 2V_1 \)
Let \( P_1 \) be the pressure at the bottom of the lake and \( P_2 \) be the pressure at the surface.
Atmospheric pressure \( P_2 = 75 \) cm Hg.
Density of mercury \( \rho_{Hg} = 40 \times \) density of water \( \rho_w \).
The pressure at the bottom is the sum of atmospheric pressure and the pressure due to water column:
\( P_1 = P_2 + h \rho_w g \)
Using Boyle’s Law:
\( P_1V_1 = P_2 \cdot 2V_1 \)
Therefore:
\( P_1 = 2P_2 \)
Substitute in the pressure equation:
\( 2P_2 = P_2 + h \rho_w g \)
\( P_2 = h \rho_w g \)
Convert \( P_2 \) from cm of Hg to pascals:
\( P_2 = 75 \) cm Hg \( = 75 \) cm \( \times 1333 \) Pascal/cm (since 1 cm Hg = 1333 Pa)
\( P_2 = 99975 \) Pascal
Using the conversion of mercury to water density:
\( \rho_w = \rho_{Hg} / (40/3) \)
\( \rho_w = 13600 \) kg/m\(^3\) / (40/3)
Calculate pressure in water as \( h \cdot \rho_w \cdot g = P_2 \):
\( \rho_w g = 99975 \) Pascal
Finally, solve for \( h \):
\( h = 99975 \) Pascal \(/ (1000 \times 9.81)\)
\( h \approx 20 \) meters
Thus, the depth of the lake is 20 meters.