two phase in pipes

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Two-Phase Flow Correlations Vertical Upward Flow Pipeline (Duns & Ros) 1- Flow regimes boundaries: The flow regimes map is shown in Figure 3-10 . The flow regimes boundaries are defined as a functions of the dimensionless quantities: N gv , N Lv , N d , N L , L 1 , L 2 , L s and L m where: N gv , N Lv , N d and N L are the same as Hagedorn & Brown method. L s = 50 + 36 N Lv and L m = 75 + 84 N Lv 0.75 L 1 and L 2 are functions of N d as shown in Figure 3-11 .

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Page 1: Two Phase in pipes

Two-Phase Flow CorrelationsVertical Upward Flow Pipeline (Duns & Ros)

1- Flow regimes boundaries: The flow regimes map is shown in Figure 3-10. The flow regimes boundaries are defined as a functions of the dimensionless quantities: Ngv, NLv, Nd, NL, L1, L2, Ls and Lm where:

- Ngv, NLv, Nd and NL are the same as Hagedorn & Brown method.

- Ls= 50 + 36 NLv and Lm= 75 + 84 NLv0.75

- L1 and L2 are functions of Nd as shown in Figure 3-11.

Bubble Flow Limits: 0 ≤ Ngv ≤ L1 + L2 NLv

Slug Flow Limits: L1 + L2 NLv ≤ Ngv ≤ Ls

Transition (Churn) Flow Limits: Ls < Ngv <Lm

Annular-Mist Flow Limits: Ngv > Lm

Page 2: Two Phase in pipes

Two-Phase Flow CorrelationsVertical Upward Flow Pipeline (Duns & Ros)

2- Pressure gradient due to elevation change: The procedure for calculating the pressure gradient due to elevation change in each flow regimes is:

- Calculate the dimensionless slip velocity (S) based on the appropriate correlation

- Calculate vs based on the definition of S:

- Calculate HL based on the definition of vs :

- Calculate the pressure gradient due to elevation change:

s

sLssmmsL

L

sL

L

sgs v

vvvvvvH

H

v

H

vv

2

4)(

1

5.02

4 /)( LLs gSv

ggLLsscelevation

HHwhereg

g

Z

P

d

d

Page 3: Two Phase in pipes

Two-Phase Flow CorrelationsVertical Upward Flow Pipeline (Duns & Ros)

Correlations for calculating S in each flow regimes:Bubble Flow:

F1 , F2 , F3 and F4 can be obtained from Figure 3-12.

Slug Flow:

F5 , F6 and F7 can be obtained from Figure 3-14.

Mist Flow: Duns and Ros assumed that with the high gas flow rates in the mist flow region the slip velocity was zero (ρs= ρn).

dLv

gvLv N

FFFwhere

N

NFNFFS 4

3'

3

2

'321 1

6'

627

'6

982.0

5 029.0)1(

)1( FNFwhereNF

FNFS d

Lv

gv

Page 4: Two Phase in pipes

Two-Phase Flow CorrelationsVertical Upward Flow Pipeline (Duns & Ros)

3- Pressure gradient due to friction:

Bubble Flow:

f1 is obtained from Moody diagram ( ), f2 is a correction

for the gas-liquid ratio, and is given in Figure 3-13, and f3 is an

additional correction factor for both liquid viscosity and gas-liquid

ratio, and can be calculated as:

Slug Flow: The same as bubble flow regime.

321 /2d

dffffwhere

dg

vvf

Z

Ptp

c

msLLtp

friction

sL

sg

v

vff

501 13

L

sLL dvN

Re

Page 5: Two Phase in pipes

Two-Phase Flow CorrelationsVertical Upward Flow Pipeline (Duns & Ros)

Annular-Mist Flow: In this region, the friction term is based on the gas phase only. Thus:

As the wave height on the pipe walls increase, the actual area through which the gas can flow is decreased, since the diameter open to gas is d – ε.

After calculating the gas Reynolds number, , the two-

phase friction factor can be obtained from Moody diagram or rough

pipe equation:

2

22

,2d

d

d

dvvddwhere

dg

vf

Z

Psgsg

c

sggtp

friction

g

sgg dvN

Re

05.0067.0)/27.0(log4

14

73.1

2

10

dfor

ddftp

Page 6: Two Phase in pipes

Two-Phase Flow CorrelationsVertical Upward Flow Pipeline (Duns & Ros)

Duns and Ros noted that the wall roughness for mist flow is affected by the wall liquid film. Its value is greater than the pipe roughness and less than 0.5, and can be calculated as follows (or Figure 3-15):

Where

Duns and Ros suggested that the prediction of friction loss could be refined by using d – ε instead of d. In this case the determination of roughness is iterative.

dv

NN

dNNfor

dvdNNfor

sgg

WeLWe

sgg

LWe

2

302.0

2

)(3713.0:005.0

0749.0:005.0

LL

L

L

sggwe N

vnumberWeberN

22

,)(

Page 7: Two Phase in pipes

Two-Phase Flow CorrelationsVertical Upward Flow Pipeline (Duns & Ros)

4- Pressure gradient due to acceleration:

Bubble Flow: The acceleration term is negligible.

Slug Flow: The acceleration term is negligible.

Mist Flow:

Pg

vvEWhere

E

ZP

ZP

Z

P

orZ

P

Pg

vv

Z

P

c

nsgmk

k

fele

total

totalc

nsgm

acc

1

dd

dd

d

d

d

d

d

d

Page 8: Two Phase in pipes

Two-Phase Flow CorrelationsVertical Upward Flow Pipeline (Duns & Ros)

Transition Flow: In the transition zone between slug and mist flow, Duns and Ros suggested linear interpolation between the flow regime boundaries, Ls and Lm , to obtain the pressure gradient, as follows:

Where

Increased accuracy was claimed if the gas density used in the mist

flow pressure gradient calculation was modified to :

MistSlugTransition Z

PB

Z

PA

Z

P

d

d

d

d

d

d

ALL

LNB

LL

NLA

sm

sgv

sm

gvm

1,

m

gvgg L

N '

Page 9: Two Phase in pipes

Two-Phase Flow CorrelationsVertical Upward Flow Pipeline (Orkiszewski)

Orkiszewski, after testing several correlations, selected the Griffith and Wallis method for bubble flow and the Duns and Ros method for annular-mist flow. For slug flow, he proposed a new correlation.

Bubble Flow

1- Limits: vsg / vm < LB

2- Liquid Holdup:

Where the vs have a constant value of 0.8 ft/sec.

13.0and/2218.0071.1Where 2 BmB LdvL

ssgsm

s

mL vvvv

v

vH /4)/1(15.01 2

Page 10: Two Phase in pipes

Two-Phase Flow CorrelationsVertical Upward Flow Pipeline (Orkiszewski)

3- Pressure gradient due to friction:

Where ftp is obtained from Moody diagram with liquid

Reynolds number: 4- Pressure gradient due to acceleration: is negligible in bubble

flow regimes.

Slug Flow

1- Limits: vsg / vm > LB and Ngv < Ls

Where Ls and Ngv are the same as Duns and Ros method.

dg

vf

Z

P

c

LLtp

friction 2d

d2

L

LL dvN

Re

Page 11: Two Phase in pipes

Two-Phase Flow CorrelationsVertical Upward Flow Pipeline (Orkiszewski)

2- Two-phase density:

The following procedure must be used for calculating vb:

1- Estimate a value for vb. A good guess is vb = 0.5 (g d)0.5

2- Based on the value of vb , calculate the

3- Calculate the new value of vb from the equations shown in the

next page, based on NReb and NReL where

4- Compare the values of vb obtained in steps one and three. If they

are not sufficiently close, use the values calculated in step three as

the next guess and go to step two.

Lbm

sggbsLLs vv

vvv

)(

L

bL dvN

b

Re

L

mL dvN

L

Re

Page 12: Two Phase in pipes

Two-Phase Flow CorrelationsVertical Upward Flow Pipeline (Orkiszewski)

Use the following equations for calculation of vb:

30001074.8546.0 ReRe6

bLNfordgNvb

80001074.835.0 ReRe6

bLNfordgNvb

5.0

5.02 59.13

5.0d

vwhereL

Lb

800030001074.8251.0 ReRe6

bLNfordgN

Page 13: Two Phase in pipes

Two-Phase Flow CorrelationsVertical Upward Flow Pipeline (Orkiszewski)

The value of δ can be calculated from the following equations depending upon the continuous liquid phase and mixture velocity.

Continuous Liquid Phase

Value of vm Equation of δ

Water < 10

Water >10

Oil <10

Oil >10

)log(428.0)log(232.0681.0)log(013.0

38.1dv

d mL

)log(888.0)log(162.0709.0)log(045.0

799.0dv

d mL

)log(113.0)log(167.0284.0)1log(0127.0

415.1dv

d mL

)log(63.0397.0)1log(01.0

)log(

)log(569.0161.0)1log(0274.0

571.1

371.1

dd

vX

Xdd

Lm

L

Page 14: Two Phase in pipes

Two-Phase Flow CorrelationsVertical Upward Flow Pipeline (Orkiszewski)

Data from literature indicate that a phase inversion from oil continuous to water continuous occurs at a water cut of approximately 75% in emulsion flow.

The value of δ is constrained by the following limits:

These constraints are supposed to eliminate pressure discontinuities between equations for δ since the equation pairs do not necessarily meet at vm=10 ft/sec.

L

s

bm

bm

mm

vv

vvForb

vvFora

1:10)

065.0:10)

Page 15: Two Phase in pipes

Two-Phase Flow CorrelationsVertical Upward Flow Pipeline (Orkiszewski)

3- Pressure gradient due to friction:

Where ftp is obtained from Moody diagram with mixture

Reynolds number: 4- Pressure gradient due to acceleration: is negligible in slug

flow regime.

Transition (Churn) Flow Limits: Ls < Ngv <Lm

The same as Duns and Ros method.

Annular-Mist Flow Limits: Ngv > Lm

The same as Duns and Ros method.

bm

bsL

c

mLtp

friction vv

vv

dg

vf

Z

P

2d

d2

L

mL dvN

Re

Page 16: Two Phase in pipes

Two-Phase Flow CorrelationsBeggs and Brill

Beggs and Brill method can be used for vertical, horizontal and inclined two-phase flow pipelines.

1- Flow Regimes: The flow regime used in this method is a correlating parameter and gives no information about the actual flow regime unless the pipe is horizontal.The flow regime map is shown in Figure 3-16. The flow regimes boundaries are defined as a functions of the following variables:

738.64

4516.13

4684.242

302.01

2

5.0,10.0

10252.9,316,

LL

LLm

Fr

LL

LLgd

vN

Page 17: Two Phase in pipes

Two-Phase Flow CorrelationsBeggs and Brill

Segregated Limits:

Transition Limits:

Intermittent Limits:

Distributed Limits:

2

1

and 01.0or

and 01.0

LN

LN

FrL

FrL

32 and 01.0 LNL FrL

43

13

and 4.0or

and 4.001.0

LNL

LNL

FrL

FrL

4

1

and 4.0or

and 4.0

LN

LN

FrL

FrL

Page 18: Two Phase in pipes

Two-Phase Flow CorrelationsBeggs and Brill

2- Liquid Holdup: In all flow regimes, except transition, liquid holdup can be calculated from the following equation:

Where HL(0) is the liquid holdup which would exist at the same conditions in a horizontal pipe. The values of parameters, a, b and c are shown for each flow regimes in this Table:

For transition flow regimes, calculate HL as follows:

LLcFr

bL

LLL HN

aHHH )0()0()0()( :constraintwith ,

Flow Pattern a b c

Segregated 0.98 0.4846 0.0868

Intermittent 0.845 0.5351 0.0173

Distributed 1.065 0.5824 0.0609

ABLL

NLAHBHAH Fr

LLL

1,,23

3ent)(intermittd)(segregaten)(transitio

Page 19: Two Phase in pipes

Two-Phase Flow CorrelationsBeggs and Brill

The holdup correcting factor (ψ), for the effect of pipe inclination is given by:

Where φ is the actual angle of the pipe from horizontal. For vertical upward flow, φ = 90o and ψ = 1 + 0.3 C. C is:

The values of parameters, d’, e, f and g are shown for each flow regimes in this Table:

)8.1(sin333.0)8.1sin(1 3 C

.0n that restrictio with ,ln)1( CNNdC gFr

fLv

eLL

Flow Pattern d' e f g

Segregated uphill 0.011 -3.768 3.539 -1.614

Intermittent uphill 2.96 0.305 -0.4473 0.0978

Distributed uphill No correction C = 0 , ψ = 1

All patterns downhill 4.70 -0.3692 0.1244 -0.5056

Page 20: Two Phase in pipes

Two-Phase Flow CorrelationsBeggs and Brill

3- Pressure gradient due to friction factor:

fn is determined from the smooth pipe curve of the Moody

diagram, using the following Reynolds number:

The parameter S can be calculated as follows:

For and for others:

Sntp

c

mntp

f

effdg

vf

L

P

,

2d

d2

42 )(ln01853.0)(ln8725.0ln182.30523.0

ln

yyy

yS

n

mn dvN

Re

)2.12.2ln(2.1/1 2)( ySHy LL

Page 21: Two Phase in pipes

Two-Phase Flow CorrelationsBeggs and Brill

4- Pressure gradient due to acceleration: Although the

acceleration term is very small except for high velocity flow,

it should be included for increased accuracy.

sin,

1

dd

dd

d

d

d

d

d

d

scelec

ssgmk

k

fele

total

totalc

sgms

acc

g

g

dL

dP

Pg

vvEWhere

E

LP

LP

L

P

orL

P

Pg

vv

L

P

Page 22: Two Phase in pipes

Figure 3-10. Vertical two-phase flow regimes map (Duns & Ros).

Page 23: Two Phase in pipes
Page 24: Two Phase in pipes

F4

F4

F3

F2

Page 25: Two Phase in pipes

F6

F5

Page 26: Two Phase in pipes
Page 27: Two Phase in pipes
Page 28: Two Phase in pipes

Figure 3-16. Beggs and Brill, Horizontal flow regimes map.