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Basics of Fluid Mechanics, 2014a

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90 CHAPTER 4. FLUIDS STATICS<br />

The comparison <strong>of</strong> the right hand terms <strong>of</strong> equations (4.66) and (4.65) provides<br />

the conditions to determine the stability. From a mathematical point <strong>of</strong> view, to keep<br />

the inequality for a small dh only the first term need to be compared as<br />

gρ<br />

Pk > gρ<br />

P − C x<br />

T<br />

(4.67)<br />

After rearrangement <strong>of</strong> the inequality (4.67) and using the ideal gas identity, it transformed<br />

to<br />

C x<br />

T<br />

(k − 1) gρ<br />

><br />

kP<br />

C x < k − 1<br />

k<br />

g<br />

R<br />

(4.68)<br />

The analysis shows that the maximum amount depends on the gravity and gas<br />

properties. It should be noted that this value should be changed a bit since the k should<br />

be replaced by polytropic expansion n. When lapse rate C x is equal to the right hand<br />

side <strong>of</strong> the inequality, it is said that situation is neutral. However, one has to bear in<br />

mind that this analysis only provides a range and isn’t exact. Thus, around this value<br />

additional analysis is needed 9 .<br />

One <strong>of</strong> the common question this author has been asked is about the forces<br />

<strong>of</strong> continuation. What is the source <strong>of</strong> the force(s) that make this situation when<br />

unstable continue to be unstable? Supposed that the situation became unstable and<br />

the layers have been exchanged, would the situation become stable now? One has to<br />

remember that temperature gradient forces continuous heat transfer which the source<br />

temperature change after the movement to the new layer. Thus, the unstable situation<br />

is continuously unstable.<br />

4.3.5 Gravity Variations Effects on Pressure and Density<br />

Until now the study focus on the change <strong>of</strong> density<br />

and pressure <strong>of</strong> the fluid. Equation (4.11) has two<br />

terms on the right hand side, the density, ρ and<br />

the body force, g. The body force was assumed<br />

until now to be constant. This assumption must be<br />

deviated when the distance from the body source<br />

is significantly change. At first glance, the body<br />

force is independent <strong>of</strong> the fluid. The source <strong>of</strong><br />

the gravity force in gas is another body, while the<br />

gravity force source in liquid can be the liquid itself.<br />

Thus, the discussion is separated into two different<br />

issues. The issues <strong>of</strong> magnetohydrodynamics are<br />

r b<br />

P b ρ b<br />

g ∝ r 2<br />

Fig. -4.12. The varying gravity effects<br />

on density and pressure.<br />

too advance for undergraduate student and therefore,will not be introduced here.<br />

r<br />

9 The same issue <strong>of</strong> the floating ice. See example for the floating ice in cup.

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