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Ch 14: Fluids and Elasticity
Chapter 14, Problem 14

The deepest point in the ocean is 11 km below sea level, deeper than Mt. Everest is tall. What is the pressure in atmospheres at this depth?

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Key Concepts

Here are the essential concepts you must grasp in order to answer the question correctly.

Hydrostatic Pressure

Hydrostatic pressure is the pressure exerted by a fluid at equilibrium due to the force of gravity. It increases with depth in a fluid, calculated using the formula P = ρgh, where P is pressure, ρ is the fluid density, g is the acceleration due to gravity, and h is the depth. In the ocean, seawater has an average density of about 1025 kg/m³, which is essential for calculating the pressure at great depths.
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Atmospheric Pressure

Atmospheric pressure is the pressure exerted by the weight of the atmosphere above a given point. At sea level, this pressure is approximately 101.3 kPa, or 1 atmosphere (atm). When calculating pressure at depth in the ocean, it is important to consider that the pressure increases by about 1 atm for every 10 meters of water depth, adding to the atmospheric pressure at the surface.
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Pressure Conversion

Pressure conversion is the process of translating pressure measurements from one unit to another, such as from pascals (Pa) to atmospheres (atm). Since 1 atm is equivalent to 101,325 Pa, understanding how to convert between these units is crucial for interpreting pressure values at different depths. This conversion allows for a clearer understanding of the extreme conditions present in deep ocean environments.
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