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Modern Engineering Thermodynamics

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300 CHAPTER 9: Second Law Open System Applications<br />

and the series expansion for the logarithm of k for 0 < k < 2is<br />

ln k = ðk − 1Þ − ðk − 1Þ 2 /2 + ðk − 1Þ 3 /3 − <br />

clearly kR/c p > ln k, which produces the following result when the tanks are filled to the same pressure (but not<br />

with the same amount of mass):<br />

1ðS P<br />

<br />

Þ 2 ideal<br />

gas<br />

ðadiabaticÞ<br />

< 1 ðS P<br />

<br />

Þ 2 ideal<br />

gas<br />

ðisothermalÞ<br />

In the dissipative hydraulic flows studied earlier in this chapter, we find that less entropy is produced in both incompressible<br />

and ideal gas systems if the flows are carried out adiabatically as opposed to isothermally. The preceding<br />

analysis shows that this is also true in the filling of a rigid vessel. Note, however, that these two filling processes do<br />

not normally produce the same final system state. For example, adiabatic filling clearly produces a higher final temperature<br />

than isothermal filling when starting from the same initial temperature. A complete entropy production<br />

analysis has to include any additional processes required to reduce both systems to the same final state.<br />

EXAMPLE 9.8<br />

A 3.00 ft 3 rigid container is filled with oxygen entering at 70.0°F to a final pressure of 2000. psia. Assuming the container is<br />

initially evacuated and that the oxygen behaves as an ideal gas with constant specific heats, determine the amount of<br />

entropy produced when the container is filled<br />

a. Adiabatically by insulating it.<br />

b. Isothermally by submerging it in a water bath at 70.0°F while filling.<br />

Solution<br />

First, draw a sketch of the system (Figure 9.16).<br />

The unknowns are the amount of entropy produced when the<br />

container is filled adiabatically by insulating it and isothermally<br />

by submerging it in a water bath at 70.0°F while filling.<br />

The material is the oxygen gas in the tank.<br />

O 2 at 70.0°F<br />

O 2 at 70.0°F<br />

From Table C.13a of Thermodynamic Tables to accompany <strong>Modern</strong><br />

<strong>Engineering</strong> <strong>Thermodynamics</strong>, we find for oxygen c p = 0.219 Btu/<br />

(lbm·R), R = 48.29 ft·lbf/(lbm·R), k=1.39. The final temperature<br />

after filling adiabatically is given by Eq. (6.36) as<br />

ðT 2 Þ adiabatic<br />

filling<br />

= kT in = 1:39ð70:0 + 459:67 RÞ = 736 R = 277°F<br />

and, for isothermal filling,<br />

ðT 2 Þ isothermal<br />

filling<br />

= T in = 70:0 + 459:67 = 530: R<br />

∀=3.00 ft 3<br />

P final = 2000. psia<br />

FIGURE 9.16<br />

Example 9.8.<br />

∀=3.00 ft 3<br />

P final = 2000. psia<br />

Insulation<br />

Water at 70.0°F<br />

(a) 1 (S P ) 2 =? (b) 1 (S P ) 2 = ?<br />

The final mass of oxygen in the container can be found from the ideal gas equation of state as<br />

so<br />

and<br />

ðm 2<br />

ðm 2<br />

<br />

Þ adiabatic<br />

filling<br />

<br />

Þ isothermal<br />

filling<br />

=<br />

=<br />

p 2 V 2<br />

RðT 2 Þadiabatic<br />

filling<br />

p 2 V 2<br />

RðT 2 Þisothermal<br />

filling<br />

m 2 = p 2V 2<br />

RT 2<br />

ð2000: lbf/in:2Þ 144 in: 2 /ft 2 3:00 ft 3<br />

= = 24:3 lbm<br />

½48:29 ft.lbf/ ðlbm.RÞŠð736 RÞ<br />

ð2000: lbf/in:2Þ 144 in: 2 /ft 2 3:00 ft 3<br />

= = 33:8 lbm<br />

½48:29 ft.lbf/ ðlbm.RÞŠð530: RÞ

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