A buoy is attached to the bottom of a river by an anchor chain. Due to a strong flood, the water level rises higher than the length of the anchor chain, so that the buoy gradually sinks into the flood. What happens when the waterline keeps rising?
Details and Assumptions: The buoy is open at the bottom, so that water can penetrate into the interior. However, the water is held back by an air bubble, which also causes the buoyancy of the buoy.
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The buoyancy force according to the Archimedean principle corresponds to the volume V of the displaced water: F = ρ g V with the density of the water, ρ , and the gravitational acceleration g . In our case, the volume V is approximately equal to the volume of the enclosed air. According to the ideal gas law, this volume is given by V = p n R T with the molar amount of substance, n , the general gas constant R , the temperature, T , and the pressure p . Since both the air quantity n and the temperature T are constant, the volume depends only on the pressure p . The pressure is due to the atmospheric pressure and the gravitational pressure of the water: p = p 0 + ρ g h with the height difference h between the river level and the water surface in the buoy. As the water level rises, so does the pressure in the buoy, compressing the air inside and decreasing the volume of displaced water. Finally, the buoyancy force is no longer sufficient for the buoy to float, causing the buoy to sink to the ground. It is crucial that the air in the buoy is compressible, while the surrounding water is virtually incompressible and therefore has a constant density.