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Calculate the apprroximate change in density of water in a lake at a depth of `400 m ` below the surface. The density of water at the surface id `1030 kg//m^(3)` and bulk modulus of water is `2xx10^(9) N//m^(2)`.

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To calculate the approximate change in density of water in a lake at a depth of 400 m below the surface, we will follow these steps: ### Step 1: Understand the Problem We are given: - Density of water at the surface, \( \rho = 1030 \, \text{kg/m}^3 \) - Bulk modulus of water, \( B = 2 \times 10^9 \, \text{N/m}^2 \) - Depth, \( x = 400 \, \text{m} \) - Acceleration due to gravity, \( g \approx 10 \, \text{m/s}^2 \) ### Step 2: Calculate the Pressure at Depth The pressure at a depth \( x \) in a fluid is given by: \[ P = \rho g x \] Substituting the values: \[ P = 1030 \, \text{kg/m}^3 \times 10 \, \text{m/s}^2 \times 400 \, \text{m} = 4,120,000 \, \text{N/m}^2 \] ### Step 3: Calculate the Bulk Strain The bulk strain \( \epsilon \) is given by: \[ \epsilon = \frac{P}{B} \] Substituting the pressure calculated in Step 2: \[ \epsilon = \frac{4,120,000 \, \text{N/m}^2}{2 \times 10^9 \, \text{N/m}^2} = 0.00206 \] ### Step 4: Relate Bulk Strain to Change in Volume The change in volume \( \Delta V \) can be expressed in terms of the original volume \( V \): \[ \Delta V = \epsilon V \] ### Step 5: Calculate the Change in Density Since density is inversely proportional to volume, the new density \( \rho' \) at depth \( x \) can be calculated as: \[ \rho' = \frac{\rho V}{V - \Delta V} \] Substituting \( \Delta V = \epsilon V \): \[ \rho' = \frac{\rho V}{V - \epsilon V} = \frac{\rho}{1 - \epsilon} \] Substituting \( \epsilon \): \[ \rho' = \frac{1030 \, \text{kg/m}^3}{1 - 0.00206} \approx \frac{1030 \, \text{kg/m}^3}{0.99794} \approx 1032 \, \text{kg/m}^3 \] ### Step 6: Calculate the Change in Density The change in density \( \Delta \rho \) is: \[ \Delta \rho = \rho' - \rho = 1032 \, \text{kg/m}^3 - 1030 \, \text{kg/m}^3 = 2 \, \text{kg/m}^3 \] ### Final Result The approximate change in density of water at a depth of 400 m below the surface is: \[ \Delta \rho = 2 \, \text{kg/m}^3 \] ---

To calculate the approximate change in density of water in a lake at a depth of 400 m below the surface, we will follow these steps: ### Step 1: Understand the Problem We are given: - Density of water at the surface, \( \rho = 1030 \, \text{kg/m}^3 \) - Bulk modulus of water, \( B = 2 \times 10^9 \, \text{N/m}^2 \) - Depth, \( x = 400 \, \text{m} \) - Acceleration due to gravity, \( g \approx 10 \, \text{m/s}^2 \) ...
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