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Basics of Fluid Mechanics, 2014a

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4.4. FLUID IN A ACCELERATED SYSTEM 97<br />

velocity liquid start to exit the U tube? If the rotation <strong>of</strong> U tube is exactly at the center,<br />

what happen the rotation approach very large value?<br />

Advance material can be skipped<br />

4.4.3 <strong>Fluid</strong> Statics in Geological System<br />

This author would like to express his gratitude to<br />

Ralph Menik<strong>of</strong>f for suggesting this topic.<br />

In geological systems such as the Earth provide cases to be used for fluid static for<br />

estimating pressure. It is common in geology to assume that the Earth is made <strong>of</strong><br />

several layers. If this assumption is accepted, these layers assumption will be used to<br />

do some estimates. The assumption states that the Earth is made from the following<br />

layers: solid inner core, outer core, and two layers in the liquid phase with a thin crust.<br />

For the purpose <strong>of</strong> this book, the interest is the calculate the pressure at bottom <strong>of</strong><br />

the liquid phase. This explanation is provided to understand how to use the<br />

Fig. -4.18. Earth layers not to scale. 10<br />

bulk modulus and the effect <strong>of</strong> rotation. In reality, there might be an additional effects<br />

which affecting the situation but these effects are not the concern <strong>of</strong> this discussion.<br />

Two different extremes can recognized in fluids between the outer core to the<br />

crust. In one extreme, the equator rotation plays the most significant role. In the<br />

10 The image was drawn by Shoshana Bar-Meir, inspired from image made by user Surachit

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