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Answer :
The absolute water pressure at point B, considering capillary actions, is determined to be 988 mm + 2.696 mm + 11.75 mm = 1002.446 mm of water.
At the given elevation ZB = 988 mm, we need to account for the capillary actions due to the inner diameter of 0.3 mm. Capillary rise in a tube can be calculated using the formula h = 2T cosθ / ρrg, where h is the capillary rise, T is the surface tension, θ is the contact angle, ρ is the density of the fluid, r is the radius of the tube, and g is the acceleration due to gravity.
For fluid 2 (mercury) with higher surface tension, the capillary rise (2.696 mm) should be subtracted from the elevation, while for fluid 3 (water) with lower surface tension, the capillary rise (11.75 mm) should be added.
The absolute pressure at point B is given by the hydrostatic pressure equation P = ρgh, where ρ is the fluid density, g is the acceleration due to gravity, and h is the height difference.
In the case of air at point A, it's open to the atmosphere, so its pressure is the atmospheric pressure (101.325 kPa).
To calculate the thickness of the atmosphere, we use the hydrostatic pressure formula and rearrange it to solve for h, considering the air density and the atmospheric pressure.
For the gauge pressure experienced by a driver at a depth of 10 m in seawater, we use the hydrostatic pressure equation with the given relative density of seawater.
For the piston problem, we can use the principle of hydraulic systems, where pressure is transmitted equally. The force on each piston is given by the product of pressure and piston area. Equating the forces on the two pistons gives the ratio of their areas, and we can then calculate the diameter of the smaller piston.
In the case of pumping oil from a well, we need to consider the pressure required to lift the oil to the pump's height. This pressure is a function of the oil's density, the pump's height, and gravity.
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