
622      Va.  Two-Phase Flow and Heat Transfer:  Two-Phase Flow Fundamentals  
Constants C
1
, C
2
, and C
3
 may be obtained from the Martinelli-Nelson or the Thom 
correlation.  Figure Va.2.3 gives the values of constants C
1
, C
2
, and C
3
 according 
to Thom’s correlation. 
Example Va.2.9.  Solve Example Va.2.8 based on the Separated Flow Model. 
Solution:  The same total pressure drop is applicable in the preheating section for 
both HEM and SFM. For the boiling section, we use Figure Va.2.3 for (∆P)
fric
,
(∆P)
acc
 and (∆P)
grav
 respectively.  These result in: C
1
≈ 8.5, C
2
≈ 14, and C
3
≈ 0.24. 
Substituting the constants in Equation Va.2.30, we find: 
)(
2
1
)(
1
2
,
C
LG
D
fP
sp
b
h
sptpfric
ρ
=∆ =
=×
××
5.8
2
00135.03)3.318(
02.0
1
0199.0
2
1.74 kPa 
)](/[)(
2
2
,
CGP
ftpacc
ρ
=∆  = (318.3)
2
× 0.00135 × 7.8 = 1.90 kPa 
)(cos)(
3,
CgLP
fbtpgrav
βρ
=∆  = 9.81 × (3/0.00135) × 0.24 = 5.2 kPa 
Therefore, total pressure drop over the tube is found as: 
∆P
total
 = (0.068 + 1.74) + (0.018 + 1.90) + (7.8 + 5.2) = 16.7 kPa 
This result is in reasonable agreement with the result obtained from the homoge-
nous model in Example Va.2.8. 
3.  Two Phase Critical Flow
Similar to the critical flow of compressible, single-phase fluid, as discussed in 
Chapter IIIc, flow of a two-phase mixture in a channel may also become critical.  
For cases where saturated water is contained under pressure, opening of a valve or 
sudden burst of a connecting pipe results in expulsion of the tank inventory.  In 
such a case, the saturated water may partially flash to steam as it approaches the 
break area, which is at much lower pressure.  We will seek an analytical solution 
for the two-phase critical flow of water and steam under the following conditions; 
flow is homogeneous (V
f
 = V
g
), thermodynamic equilibrium exists between the 
phases (T
f
 = T
g
), and the process is isentropic.  These assumptions lead to the de-
termination of critical flow for HEM.  Maintaining the assumption of an isentropic 
process, analytical solutions are also extended to two equilibrium non-homo-
genous cases.  The first case uses a slip ratio calculated from either the Moody or 
the Fauske model.  The second case uses models from Burnell and Henry-Fauske.  
These cases are summarized in Table Va.3.1 and then discussed in detail next.