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Two Phase Flow

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: By GROUP : Abdul-Majeed et.al Two-Phase Flow
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Page 1: Two Phase Flow

:ByGROUP : Abdul-Majeed et.al

Two-Phase Flow

Page 2: Two Phase Flow

Tow- phase flow in horizontal pipes differs markedly from that in vertical pipes; except for the Beggs and Brill correlation (Beggs and Brill,1973) , which can be applied for any flow direction, completely different correlations are used for horizontal flow than for vertical flow.

Tow-Phase Flow:

Page 3: Two Phase Flow

The flow regime does not affect the pressure drop as significantly in horizontal flow as it dose in vertical flow, because there is no potential energy contribution to the pressure drop in horizontal flow.

The flow regime is considered in some pressure drop correlations and can affect production operations in other ways.

Figure 10-1 (Beggs and Brill, 1973) depicts the commonly described flow regimes in horizontal gas-liquid flow. These can be classified as three types of regimes: segregated flows, in which the two phases are for the most part separate; intermittent flows, in which gas and liquid are alternating; and distributive flows, in which one phase is dispersed in the other phase.

A : Flow regimes

Page 4: Two Phase Flow

: Figure (10-1)

:flow regimes in two phase horizontal flow

Page 5: Two Phase Flow

segregated flow is further classified as being stratified smooth, stratified wavy (ripple flow), or annular. At higher gas rates, the interface becomes wavy, and stratified wavy flow results. Annular flow occurs at high gas rates and relatively high liquid rates and consists of an annulus of liquid coating the wall of the pipe and a central core of gas flow, with liquid droplets entrained in the gas.

The intermittent flow regimes are slug flow and plug (also called elongated bubble)flow. Slug flow consists of large liquid slugs alternating with high-velocity bubbles of gas that fill almost the entire pipe. In plug flow, large gas bubbles flow along the top of the pipe.

Distributive flow regimes described in the literature include bubble, mist ,and froth flow.

Page 6: Two Phase Flow

Shown in fig. (10-2) The axes for this plot are Gl / λ and Gl λØ / Gg , where Gl and Gg are the mass fluxes of liquid and gas, respectively (lbm/hr-ft2) and the parameters λ and Ø are

 

λ= [ (ρg /0.075) (ρL /62.4) ]1/2

Ø= 73/σL [ μL (62.4/ρL )2 ]1/3

Where densities are in lbm/ft3 , μ is in cp, and σl is in dynes/cm.

Page 7: Two Phase Flow
Page 8: Two Phase Flow

The Beggs and Brill correlation : is based on a horizontal flow regime map

that divides the domain into the three flow regime categories, segregated, intermittent and distributed. This map, shown in Fig. 10-4, plots the mixture Froude number defined as

NFr= um2 / g D

Versus the input liquid fraction, λl.

Page 9: Two Phase Flow

Taitel and Dukler (1976): developed a theoretical model of the

flow regime transitions in horizontal gas-liquid flow; their model can be used to generate flow regime maps for particular fluids and pipe size. Figure 10-5 shows a comparison of their flow regime prediction with those of Mandhane et al. for air-water flow in a 2.5-cm pipe.

Page 10: Two Phase Flow
Page 11: Two Phase Flow

Using the Baker, mandhane, and Beggs and Brill flow regime maps, determine the flow regime for the flow of qo= 2000 bbl/day of oil and qg= 1MM scf/day of gas at 800 psia and 1750F in a 2-1/2 in. I.D. pipe. The fluids are Given:

-for liquid: ρ=49.92 lbm/ft3 ; μl=2 cp ;

σl=30 dynes/cm; ql=0.130 ft3/sec.

-for gas: ρ=2.61 lbm/ft3 ; μg=0.0131 cp ;

Z=0.935 ; qg=0.242 ft3/sec.

Example:

Page 12: Two Phase Flow

 

-cross sectional are = (π/4)*(D/12)2

=(π/4)*(2.5/12)2=0.0341 ft2

usl= ql/A = 0.13/0.0341 =3.812 ft/sec

usg= qg/A =0.242/0.0341=7.1 ft/sec

go to fig.(10-3): the flow regime is predicted to be slug flow.

um= usl+usg= 10.9 ft/sec

Solution:

Page 13: Two Phase Flow

for using Baker map, we calculation: Gl, Gg, λ, and Ø.

Gl= usl ρl= 3.81(ft/sec) * 49.92(lbm/ft3) * 3600(sec/hr)

= 6.84* 105 lbm/hr-ft2

Gg= usgρg= 7.11(ft/sec) * 2.6(lbm/ft3) * 3600(sec/hr)

= 6.65* 104 lbm/hr-ft2

λ =[(2.6/0.075)(49.92/62.4)]1/2 = 5.27 Ø =(73/30)[2(62.4/49.92)2]1/3 = 3.56

The coordinates for the baker map are Gg/λ =(6.65*104)/5.27 = 1.26*104

GlλØ/Gg= (6.84*105)(5.27)(3.56)/(6.65*104)= 193

Reading from fig. 10-2, the flow regime is predicted to be dispersed bubble, though the conditions are very near the boundaries with slug flow and annular mist flow.

Page 14: Two Phase Flow
Page 15: Two Phase Flow

For using Beggs and Brill, calculation NFr , λl .

NFr= (10.9 ft/sec)2/(32.17ft/sec2)[(2.5/12)ft]

=17.8

λl =usl/um

=3.81/10.9 = 0.35

From fig. (10-4): the flow regime is predicted to be intermittent.

Page 16: Two Phase Flow
Page 17: Two Phase Flow

Begs and brill correlation: The Beggs and Brill correlation presented in applied to horizontal flow. The correlation is somewhat simplified, since the angle Ѳ is 0, making the factor ψ equal to 1. This correlation is presented in section

∆Ptotal=∆Pf+∆Pel

:B: Pressure gradient correlations

Page 18: Two Phase Flow

Eaton correlation: The Eaton correlation (Eaton et al., 1967) was developed empirically from a series of tests in 2-in.- and 4-in.-diameter, 1700-ft-long lines. It consists primarily of correlations for liquid holdup and friction factor.

The friction factor( f ) is obtained from the correlation shown in Fig. 10-6 as a function of the mass flow rate of the liquid, ml, and the total mass flow rate, mm' For the constant given in this figure to compute the abscissa, mass flow rates are in Ibm/sec, diameter is in ft, and viscosity is in lbm/ft-sec.

Dg

upf

x

p

c

mmF

2)(

2

Page 19: Two Phase Flow

Two gas-condensate wells feed into a 4-in. gathering line 2.10 mi long. Well A will flow at the rate of 3 MMcfd, and well B will flow at the rate of 1 MMcfd. The following data are available on each well:

:Example 7.5

Page 20: Two Phase Flow

* Gallons per Mcf of gas The summation of the uphill rises in

the line is 143 ft. The initial pressure at the wells is 900 psig. What is the pressure drop in the line?

Page 21: Two Phase Flow

SOLUTION:

Gas: Line diameter = = 0.6667 ft. Line length = 5 × 5280 = 26400 ft.

= 833.3333 Mcf/hr.

Assume an average pressure in the pipeline of 1350 psig or 1365 psia. Assume an average temperature in the pipeline of 60 °F or 520 °R. Calculate the weighted average specific gravity of the commingled gas

stream: = 0.67

Calculate the gas viscosity. The molecular weight of the gas is: Ma = γg × 28.97 = 0.67 × 28.97 = 19.2099

From Fig.(2.10) μ1 = 0.0099 cp.

24

1000)4610( GSQ

12

8

)4610(

)80.04()70.06()60.010(

GS

97.28a

air

ag

M

M

M

Page 22: Two Phase Flow
Page 23: Two Phase Flow

= 170.5 + 307.3 × 0.67 = 376 °R.

= 709.6 – 58.7 × 0.67 = 670 psia.

= 1.38

= 2.04From Fig. (2.11) μ/μ1 = 1.36Calculate the gas viscosity at pipeline conditions:

= 0.013464 cp.From Fig. 2.4, Z = 0.755

376

520

pcpr T

TT

670

1365

pcpr P

PP

gpcT 3.3075.170

gpcP 7.586.709

36.10099.01

1 G

Page 24: Two Phase Flow
Page 25: Two Phase Flow

Calculate the gas volume at pipeline conditions:

=6.776 Mcf/hr = 6776

ft3/hr.

Calculate the density of the gas at pipeline conditions:

= 6.2919 Lbm/ft3.

ZT

pQQ GSGPL

520

7.14

755.0520

520

1365

7.143333.833

GPLQ

ZT

pSGG

701.2

755.0520

136567.0701.2

G

Page 26: Two Phase Flow

Liquid:Assume that the average composition of the

condensate is normal octane (n-C8H18).

From Table( 2-2):Tpc = 564.22 °R, Ppc = 360.6 psia, Ma = 114.232 and γL = 0.65.

=0.65 × 62.4 = 40.56 lbm/ft3

=0.9216 = 3.785

22.564

520

pcpr T

TT

4.62 LL

6.360

1365

pcpr P

PP

Page 27: Two Phase Flow
Page 28: Two Phase Flow

From Fig. (7.11) 0.014

= 0.1496 cp.

From a plot of GPM vs. pressure (Fig. 7.17), the GPM at 1350 psig is 4 for well A , 3.125 for well B and 3.437 for well C:

QLPL = 10000 × 4 + 6000 × 3.125 + 4000 × 3.437 = 72498 gal/day = 403.8155 ft3/hr

232.114014.0014.0 aL M

1 gal/day = 0.005570023 cuf/hr

Page 29: Two Phase Flow
Page 30: Two Phase Flow
Page 31: Two Phase Flow

Two-phase: Calculate λ, the input liquid-volume ratio: = 0.0562

Calculate , the mixture velocity:

=20566.5996 ft3/hr

= 5.7134 ft/s.

Calculate , the mixture velocity:

= 0.0211 cp = 0.0000142 Lbm/ft-s

6776403.8155

403.8155

GPLLPL

LPL

QQ

Q

MV

22 6667.04

6776403.8155

4

D

QQ

A

QV GPLLPLM

1 cuf / hr = 0.0002778 cuf / sec

TP

)0562.01( 0.0134640562.0 0.1496

)1(

GLTP

Page 32: Two Phase Flow

# Now, calculate the two-phase Reynolds number. This is a trial and error calculation. Assume a value for , the liquid hold-up.

Assume :

Calculate , the two-phase density:

=10.0481 Lbm/ft3.

03.0LR

03.01

)0562.01( 6.2919

03.0

0562.040.56

1

)1(

22

22

L

G

L

LTP RR

Page 33: Two Phase Flow

= 2695384.271

From Fig. (7.15) : This is not a close enough check, and the calculation must be repeated with the

new value of

0.0000142

10.0481 5.71346667.0Re

TP

TPMTP

VD

07.0LR

LR

Page 34: Two Phase Flow
Page 35: Two Phase Flow

= 7.8565 Lbm/ft3.

= 2107491.618

From Fig.( 7.15) : This checks.Calculate the single-phase friction factor:

= 0.00118

07.01

)0562.01(2919.6

07.0

0562.040.56

1

)1(

22

22

L

G

L

LTP RR

0.0000142

7.8565 5.71346667.0Re

TP

TPMTP

VD

07.0LR

32.032.0 )82107491.61(

125.000140.0

Re

125.000140.0

TP

of

Page 36: Two Phase Flow

Determine the friction factor ratio from Fig. (7.14):

  Calculate the two-phase friction factor: =

0.00298 Calculate the pressure drop due to friction:

= 13.0533 psi

516.2/ oTP ff

516.20.00118o

TPoTP f

fff

6667.02.32144

7.8565) 5.7134( 264000.002982

144

2

2

2

Dg

VLfp

c

TPMTPF

Page 37: Two Phase Flow
Page 38: Two Phase Flow

Next, the pressure drop due to elevation changes must be considered.

Calculate VSG , then superficial gas velocity:

=19409.8691 ft3/hr =

5.3916 ft3/s.

From Fig. (7.16): Calculate the elevation pressure drop:

=13.5482 psi

Calculate the total pressure drop:

=26.6015 psi.

22 6667.04

6776

4

D

QV GPLSG

37.0

144

13056.4037.0

144

Hp LE

0 13.5482 13.0533 AEFtotal pppp

Page 39: Two Phase Flow
Page 40: Two Phase Flow

Two-Phase Flow The Drama (2).flv

Page 41: Two Phase Flow

THANK YOU

FOR ALL

note :example two phase not found in.


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