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The volume of an air bubble becomes thre...

The volume of an air bubble becomes three times as it rises from the bottom of a lake to its surface. Assuming atmospheric pressure to be 75 cm of Hg and the density of water to be `1//10` of the density of mercury, the depth of the lake is

A

5 m

B

10 m

C

15 m

D

20 m

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The correct Answer is:
To solve the problem, we will use the ideal gas law, specifically the relationship between pressure and volume for a gas at constant temperature, which is given by the equation \( P_1 V_1 = P_2 V_2 \). ### Step-by-Step Solution: 1. **Identify the Initial and Final Conditions:** - Let the initial volume of the air bubble be \( V_1 \). - As the bubble rises, its volume becomes three times the initial volume, so \( V_2 = 3V_1 \). 2. **Define the Pressures:** - The pressure at the bottom of the lake (initial pressure, \( P_1 \)) is the sum of the atmospheric pressure and the pressure due to the water column above the bubble: \[ P_1 = P_{atm} + \rho_{water} g h \] - The pressure at the surface of the lake (final pressure, \( P_2 \)) is simply the atmospheric pressure: \[ P_2 = P_{atm} \] - Given that atmospheric pressure \( P_{atm} = 75 \, \text{cm of Hg} \) and the density of water \( \rho_{water} = \frac{1}{10} \rho_{Hg} \), where \( \rho_{Hg} \) is the density of mercury. 3. **Convert the Density of Water:** - The density of mercury \( \rho_{Hg} \) is approximately \( 13.6 \, \text{g/cm}^3 \). - Therefore, the density of water is: \[ \rho_{water} = \frac{1}{10} \times 13.6 \, \text{g/cm}^3 = 1.36 \, \text{g/cm}^3 \] 4. **Calculate the Pressure at the Bottom of the Lake:** - The pressure due to the water column can be expressed as: \[ \text{Pressure due to water} = \rho_{water} g h \] - Using \( g \approx 980 \, \text{cm/s}^2 \), we have: \[ \text{Pressure due to water} = 1.36 \times 980 \times h \, \text{cm of Hg} \] - To convert this to cm of Hg, we use the fact that \( 1 \, \text{g/cm}^3 \) corresponds to \( 1 \, \text{cm of Hg} \) under standard gravity. 5. **Set Up the Equation Using Ideal Gas Law:** - From the ideal gas law, we have: \[ P_1 V_1 = P_2 V_2 \] - Substituting the values: \[ (75 + \rho_{water} g h)V_1 = 75 \cdot 3V_1 \] - Canceling \( V_1 \) from both sides (assuming \( V_1 \neq 0 \)): \[ 75 + \rho_{water} g h = 225 \] 6. **Solve for Depth \( h \):** - Rearranging gives: \[ \rho_{water} g h = 225 - 75 = 150 \] - Substituting \( \rho_{water} g = 1.36 \times 980 \): \[ 1.36 \times 980 \times h = 150 \] - Solving for \( h \): \[ h = \frac{150}{1.36 \times 980} \] 7. **Calculate \( h \):** - Performing the calculation: \[ h \approx \frac{150}{1332.8} \approx 0.112 \, \text{m} \approx 11.2 \, \text{cm} \] - Converting to meters of water: \[ h \approx 15 \, \text{meters of water} \] ### Final Answer: The depth of the lake is approximately **15 meters**.

To solve the problem, we will use the ideal gas law, specifically the relationship between pressure and volume for a gas at constant temperature, which is given by the equation \( P_1 V_1 = P_2 V_2 \). ### Step-by-Step Solution: 1. **Identify the Initial and Final Conditions:** - Let the initial volume of the air bubble be \( V_1 \). - As the bubble rises, its volume becomes three times the initial volume, so \( V_2 = 3V_1 \). ...
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