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Modern Engineering Thermodynamics

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654 CHAPTER 16: Compressible Fluid Flow<br />

h<br />

Isentropic<br />

stagnation<br />

state<br />

V 2<br />

2g c<br />

p os = constant<br />

p o = constant<br />

Actual<br />

stagnation<br />

state<br />

Increase in s due to<br />

irreversibilities in the<br />

real system<br />

p = constant<br />

h o<br />

h<br />

Initial state<br />

FIGURE 16.2<br />

An isentropic and a real deceleration to the stagnation state on a Mollier diagram.<br />

s<br />

and<br />

1<br />

ρ os<br />

ρ = 1 + V2 k−1<br />

2g c c p T<br />

(16.4)<br />

where the os subscript has been added to indicate the isentropic stagnation state condition. These states are shown<br />

schematically in Figure 16.2.<br />

EXAMPLE 16.2<br />

In Example 16.1, it was determined that the stagnation air temperature for air at 20.0°C traveling at 90.0 km/h = 25.0 m/s<br />

was 20.3°C. Now determine the isentropic stagnation pressure and isentropic stagnation density of this air when the atmospheric<br />

pressure is 0.101 MPa.<br />

Solution<br />

First, draw a sketch of the system (Figure 16.3).<br />

Air at 20.0°C<br />

and 90.0 km/h<br />

(25.0 m/s)<br />

Stagnation temperature gauge<br />

reads 20.3°C<br />

Atmospheric pressure = 0.101 MPa<br />

FIGURE 16.3<br />

Example 16.2.<br />

For air, the specific heat ratio is 1.40, and when p = 0.101 MPa, Eq. (16.3) gives the isentropic stagnation pressure as<br />

<br />

p os = p 1 + V 2<br />

k<br />

k−1<br />

2g c c p T<br />

0<br />

1<br />

ð25:0 m/sÞ 2 1 kJ/kg<br />

1000 m<br />

= ð0:101 MPaÞ 1 +<br />

2 /s 2<br />

B<br />

C<br />

@ 2ð1Þð1:004 kJ/kg.KÞð20:0 + 273:15 KÞA<br />

= 0:1014 MPa<br />

1:40<br />

1:40−1

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