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Modern Engineering Thermodynamics

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366 CHAPTER 11: More Thermodynamic Relations<br />

11.3 GIBBS PHASE EQUILIBRIUM CONDITION<br />

During a phase change process, the system pressure and temperature are not independent properties. This means<br />

that, if we hold one of them constant during a phase change, the other must also remain constant. Under the<br />

condition of constant pressure and temperature, dp = dT = 0, and Eq. (11.9) gives dg = 0. Since g = g f + xg fg ,we<br />

can then write<br />

dg = dg f + xdg fg + g fg dx = 0<br />

Again, Eq. (11.8) can be used to evaluate dg f = dg fg = 0. Since x can vary during the phase equilibrium, dx<br />

cannot be zero. Therefore, we are forced to conclude from the preceding equation that g fg = 0 at phase equilibrium,<br />

or g f = g g . Using the definition of the Gibbs function, Eq. (11.7), we see that, at phase equilibrium,<br />

or<br />

g f = g g = h f − ðT sat Þs f = h g − ðT sat Þs g<br />

or<br />

h g − h f = h fg = ðT sat Þðs g − s f Þ = ðT sat Þs fg<br />

s fg = h fg /T sat (11.10)<br />

This gives us an important relation between the entropy and the enthalpy of a phase change, but we need much<br />

more information to complete the process of determining the nonmeasurable properties u, h, ands from the<br />

measurable properties p, v, and T. The following example illustrates the use of Eq. (11.10).<br />

EXAMPLE 11.3<br />

Use Eq. (11.10) to calculate the phase change entropy s fg for water at exactly 1.00 MPa and compare the result with the<br />

value for s fg at exactly 1.00 MPa listed in Table C.2b in Thermodynamic Tables to accompany <strong>Modern</strong> <strong>Engineering</strong><br />

<strong>Thermodynamics</strong>.<br />

Solution 1<br />

The unknown is the phase change entropy of water. From (Eq. 11.10), we have<br />

and from Table C.2b at p = 1.00 MPa, we find that<br />

and<br />

then, Eq. (11.10) gives<br />

s fg = h fg<br />

T sat<br />

h fg = 2015:3 kJ/kg<br />

T sat = 179:90°C<br />

s fg = h fg 2015:3 kJ/kg<br />

=<br />

T sat 179:90 + 273:15 K = 4:4482 kJ/kg .K<br />

Comparing this with the value for s fg listed in Table C.2b at p = 1.00 MPa, we find that it is exactly the same.<br />

The following exercises illustrate some of the many uses of Eq. (11.10).<br />

Exercises<br />

7. Use Eq. (11.10) to compute the values of s fg for water at 0.0100 MPa and compare the result with the values listed in<br />

Table C.2b. Find h fg and T sat at 0.01 MPa from Table C.2b. Answer: (s fg ) calc = 7.5021 kJ/kg·K.<br />

8. Use Eq. (11.10) to compute the value of h fg for water at 100.°F and compare the result with the value listed in Table<br />

C.1a. Find values for s fg and T sat at 100.°F from Table C.1a. Answer: (h fg ) calc = 1036.96 Btu/lbm.<br />

9. Use the values for h fg and s fg found in Table C.2b for water at 10.0 MPa and Eq. (11.10) to calculate the value of T sat at<br />

this state. Answer: (T sat ) calc = 584.2 K = 311.06°C.<br />

1 To achieve the desired result, we need to carry a lot more significant figures than usual.

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