Upload
esraates44
View
226
Download
6
Embed Size (px)
Citation preview
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 1/113
T H E U N I V E R S I T Y O F T U L S A
THE GRADUATE SCHOOL
NUMERICAL SIMULATION OF LAMINAR FLOW OF NON-NEWTONIAN
FLUIDS IN ECCENTRIC ANNULI
byYahya Hashemian Adariani
A thesis submitted in partial fulfillment of
the requirements for the degree of Master of Science
in the Discipline of Petroleum Engineering
The Graduate School
The University of Tulsa
2005
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 2/113
ii
T H E U N I V E R S I T Y O F T U L S A
THE GRADUATE SCHOOL
NUMERICAL SIMULATION OF LAMINAR FLOW
OF NON-NEWTONIAN FLUIDS IN ECCENTRIC ANNULI
by
Yahya Hashemian Adariani
A THESIS
APPROVED FOR THE DISCIPLINE OF
PETROLEUM ENGINEERING
By Thesis Committee
, Chair
Dr. Mengjiao Yu
Dr. Ramadan Ahmed
Dr. Siamack A. Sirazi
Dr. Stefan Miska
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 3/113
iii
ABSTRACT
Hashemian Adariani, Yahya (Master of Science in Petroleum Engineering)
Numerical Simulation of laminar Flow of non-Newtonian Fluids in Eccentric Annuli
Directed by Dr. Mengjiao Yu(113 pp., Chapter 4)
(229 words)
Accurate predictions of annular frictional pressure loss are important for optimal
well bore hydraulic program design. Inaccurate prediction of frictional pressure drop in
the annulus can result in an underestimation of the bottom hole pressure, which might
then exceed the strength of the formation, thus causing loss of drilling fluid and creating a
potentially dangerous situation due to the resulting loss of hydrostatic head.
In this study fully developed laminar axial flow of non-Newtonian fluids in
eccentric annuli has been investigated numerically. Effects of eccentricity on frictional
pressure loss in annulus for different fluids are presented. Numerical results are compared
with previous studies. Numerical investigation based on SIMPLE algorithm by Patankar-
Spalding (1972) has been presented for the case of Newtonian fluid flow in eccentric
annulus with inner pipe rotation.
Yield power-law rheology model is used as the constitutive equation of the flow.
Cartesian and boundary fitted coordinate system are utilized as two different approaches
to discretize the flow equations and generate mesh network. A minimum cut off value for
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 4/113
iv
the minimum shear rate is used to identify the plug (zero shear rate) region. Fluid flow
equations have been solved using an iterative successive over relaxation method.
Increasing eccentricity is found to lower frictional pressure drop for different
fluids. It was observed that for non-Newtonian fluids the effect of eccentricity on
pressure loss is less pronounced compared to Newtonian fluids.
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 5/113
ACKNOWLEDGEMENTS
The author thanks Dr. Mengjiao Yu, dissertation advisor, for his continuous
patience and assistance in this endeavor.
My special thanks to Dr. Ramadan Ahmed for his help and valuable suggestions.
I am thankful to Dr. Siamack Shirazi and Dr. Stefan Miska for their help,
suggestions and encouragement.
My appreciation extends to National Iranian Oil Company for providing me with
financial support.
I also thank TUDRP students and all my friends for their constant encouragementand support.
This work is dedicated to my parents.
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 6/113
vi
TABLE OF CONTENTS
Page
ABSTRACT...............................................................................................................iii
ACKNOWLEDGEMENTS .......................................................................................v
TABLE OF CONTENTS...........................................................................................vi
LIST OF FIGURES ...................................................................................................viii
CHAPTER 1: INTRODUCTION
1.1 Background ............................................................................................1
1.2 Significance of the Subject ....................................................................2 1.3 Contribution and Evaluation of This Study ........................................3
1.4 Scope of the Study ..................................................................................4
CHAPTER 2: LITERATURE REVIEW ...............................................................5
2.1 Annular Flow of Newtonian Fluid .......................................................52.2 Concentric No-Rotation Non-Newtonian ............................................92.3 Eccentric No-Rotation Non-Newtonian ..............................................11
2.4 Newtonian Fluid Flow in Annulus with Inner Pipe Rotation ............122.5 Concentric With Rotation Non-Newtonian .........................................13
2.6 Non-Newtonian Fluid Flow in Annulus with Inner Pipe Rotation ....13
CHAPTER 3: ANNULAR FLOW IN ECCENTRIC ANNULUS .......................15
3.1 Annular Flow in Eccentric Annulus .....................................................153.1.1 Assumptions ..............................................................................16
3.1.2 Continuity Equation .................................................................163.1.3 Momentum Equation.................................................................173.1.4 Drilling Fluid Rheology ............................................................18
General Model: .....................................................................19
3.1.5 Numerical Procedure ...............................................................203.1.6 Discretizing the Equation of Motion .......................................213.1.7 Solution Algorithm ....................................................................233.1.8 Minimum Shear Rate.................................................................23
3.1.9 Convergence Criteria................................................................243.1.10 Flow Rate Calculations...........................................................25
3.1.11 Using Boundary Fitted Coordinate System ............................253.1.12 Geometry Transformation.......................................................26
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 7/113
vii
3.1.13 Transformation of the Equations ............................................273.1.14 Discretization of the Equation of Motion................................28
3.1.15 Grid Refinement Analysis .......................................................293.1.16 Flow Rate Calculations...........................................................31
3.2 Newtonian Fluid Flow in Eccentric Annulus with Inner Pipe
Rotating .........................................................................................................32 3.2.1 Assumptions ..............................................................................33
3.2.2 Governing Equations ................................................................333.2.3 Boundary Conditions ................................................................34
3.2.4 Transformation of Equations ....................................................353.2.5 Numerical Procedure ................................................................383.2.6 Discretization of Momentum and Continuity Equation ............38
3.2.7 Pressure Correction Equation ..................................................423.2.8 Summary of SIMPLE Algorithm ...............................................45
CHAPTER 4: RESULTS AND CONCLUSIONS .................................................474.1 Newtonian Fluid .....................................................................................47
4.1.1 Results for Newtonian Fluid .....................................................474.1.2 Comparison of the Results for Newtonian ................................49
4.2 Power-Law Fluid....................................................................................514.2.1 Results for Power-Law Fluid ....................................................514.2.2 Comparison of the Results of Power-Law ................................54
4.3 Results and Comparison for Yield Power-Law Fluid ........................534.4 Comparison with Experimental data of Ahmed[1] .............................56
4.5 Conclusions .............................................................................................58
REFFERENCES ........................................................................................................56
APPENDIX A............................................................................................................64
APPENDIX B............................................................................................................67APPENDIX C ............................................................................................................73APPENDIX D............................................................................................................82
APPENDIX E ............................................................................................................91APPENDIX F.............................................................................................................95
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 8/113
viii
LIST OF FIGURES
Page
1.1 Schematic of Drilling Operation.........................................................................2
2.1.1 Newtonian fluid in concentric annulus ............................................................6
2.1.2 Eccentric Annulus............................................................................................6
2.1.3 Effects of eccentricity on frictional pressure loss for a Newtonian fluid with constant
rate using 7.1.2.eq . [ Secliter Q /1.0= , Sec Pa.00102.0=µ , m Ro 0889.0= ].....................9
3.1.1 Cartesian coordinate system.................................................................................17
3.1.2 Flow Curve for Different Fluids ...........................................................................19
3.1.3 Grid network in Cartesian coordinate with different grid sizes in x and y direction...21
3.1.4 Flow Rate Calculation at Grid Point i,j..................................................................25
3.1.5 Grid Network in Boundary Fitted Coordinate System............................................26
3.1.6 Geometry Transformation ....................................................................................27
3.1.7 Grid refinement in tangential direction (number of grids in radial direction=60).
Comparison of the value for volume flow rate of simulation with analytical solutions for
concentric annulus for a Newtonian (n=1) and a power-law (n=0.2) fluid. ........................30
3.1.8 Grid refinement in radial direction (number of grids in tangential direction=60).
Comparison of the value for volume flow rate of simulation with analytical solutions for
concentric annulus for a Newtonian (n=1) and a power-law (n=0.2) fluid. ........................31
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 9/113
ix
3.2.1 Boundary conditions for an eccentric annulus with rotating drill pipe............35
3.2.2 Staggered grid for velocity and pressure .........................................................39
3.2.3 Overall SIMPLE Algorithm .................................................................................46
4.1.1 Velocity profile of Newtonian fluid for concentric to fully eccentric annuli [ mOD 1778.0= ,
SecmQ /0001.0 3= , S Pa.00102.0=µ ] ........................................................ ...................47
4.1.2 Velocity profile of Newtonian fluid for concentric and fully eccentric annuli
[ mOD 1778.0= , SecmQ /0001.0 3= , S Pa.00102.0=µ ]..................................................48
4.1.3 Present study results for Newtonian fluid[ mOD 1778.0= , SecmQ /0001.0 3= ,
S Pa.00102.0=µ ]..........................................................................................................49
4.1.4 Eccentricity vs. error in pressure drop of the different studies compared with Piercy et al.
for a Newtonian fluid ..................................................... ...............................................50
4.2.1 Velocity profile of power-law fluid for concentric to fully eccentric annuli [ 5.0=o
i
R
R,
SecmQ /006.0 3= , nS Pa K .6.0= , 2.0=n ].....................................................................51
4.2.2 Velocity profile of power-law fluid for concentric and fully eccentric annuli [ 5.0=o
i
R
R,
SecmQ /006.0 3= , nS Pa K .6.0= , 2.0=n ].....................................................................52
4.2.3 Results for power-law fluid. [ 5.0=o
i
R
R, SecmQ /006.0 3= , nS Pa K .6.0= ] ............53
4.2.4 Results for power-law fluid. [ 5.0=n , SecmQ /006.0 3= , nS Pa K .6.0= ]................54
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 10/113
x
4.2.5 Comparison of Re. f predictions with previous studies [3,5]
for a power-law fluid with
[ 5.0=o
i
R
R, SecmQ /006.0 3= , nS Pa K .6.0= ].................................................................52
4.2.6 Comparison of Re. f predictions with previous studies[3,5]
for a power-law fluid with
[ SecmQ /006.0 3= , 5.0=n , nS Pa K .6.0= ] .................................................. ...................53
4.3.1 Comparison of the present study with Haciislamoglu[7]
[ inchOD 10= , inch ID 5= , SecmQ /012618.0 3= , 7.0=n , S Pa K .25.0= , Pa y 394.2=τ ] .....57
4.4.1 Comparison of the present study with experimental data of Ahmed[1]
[ mOD 035052.0= , m ID 01745.0= , %98.0=ty Eccentrici , 671.0=m ,
S Pa K .2610958.0= , Pa y 1.2=τ , m L 6576.3= ] ...................................................... ..........58
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 11/113
1
CHAPTER 1
INTRODUCTION
1.1 Background
During drilling operation of oil wells a fluid is pumped from a surface mud tank
down to the bottom of the well through drill pipe, through nozzles in the drill bit and then
back to the surface mud tank trough the annular space between the drill pipe and well
bore wall as shown in Fig.1.1. The drilling fluid has to satisfy several requirements such
as: supporting the well bore wall from collapsing, preventing formation fluid from
transferring to the well bore, cooling the drill bit, carrying cutting from bottom of the
well to the surface through annulus, etc.
The pump pressure is a function of pressure losses in surface equipment, in drill
pipe, across the bit nozzles, through the annulus, etc. Frictional pressure loss through
annulus is the main concern of this study.
Several factors can affect frictional pressure loss in annulus such as flow rate,
flow regime, mud rheology, well bore geometry, cuttings content, drill pipe rotation, drill
pipe lateral motion or swirling introduced by the rotation itself and/or fluid flow, etc. In
this study eccentricity is the main investigated issue along with rheology and drill pipe
rotation.
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 12/113
2
1.2 Significance of the Subject
In conventional drilling, frictional pressure loss accounts for about 10% of the
whole circulation pressure loss. [15]
In slim hole configurations, annular frictional pressure loss can contribute 30-50%
of the total fluid circulation pressure loss and some investigators have reported it to be as
high as 90%. [8]
Significant frictional pressure drop in the annulus can result in an increase of the
bottom hole pressure, which might then exceed the strength of the formation, thus
causing loss of drilling fluid and creating a potentially dangerous situation due to the
resulting loss of hydrostatic head. [15]
Fig.1.1 Schematic of Drilling Operation
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 13/113
3
1.3 Contribution and Evaluation of This Study
In this study effect of eccentricity of drill pipe and rheology of drilling fluid on
frictional pressure drop in annuli for Newtonian and non-Newtonian fluid is investigated.
A computer program in FORTRAN is developed to perform calculations.
Results of the program are compared with the present works of Azouz [3], Escudier [4, 5],
Piercy [17] and Haciislamoglu [7] and found to be all in good agreement. Also, numerical
simulation for a Newtonian annular flow in eccentric annulus with a rotational drill pipe
is performed.
1.4 Scope of the Study
A short review of the past works related to this study is the content of Chapter 2.
This review has categorized the previous studies according to the type of the problem.
Chapter 3 is an investigation of laminar flow of Newtonian and non-Newtonian
fluids in eccentric annulus. In the first part of this chapter, drill pipe is considered to be
stationary and fluid is Newtonian or non-Newtonian. The second part of the chapter
considers the drill pipe to be rotating and fluid to be Newtonian only. In the first part of
the chapter, two approaches are used to solve the problem. For the first approach a
rectangular mesh system is used to solve discretized flow equations in Cartesian system.
In the second approach, on the other hand, a boundary fitted coordinate system is utilized
to apply numerical technique to equations. Flow equations as well as geometry are
transformed into this new system and then discretized. Similar solution procedures are
used to solve the equations in Cartesian and boundary fitted coordinate system. The last
part of Chapter 3 is related to flow of Newtonian fluid in eccentric annulus with a rotating
drill pipe. Navier-Stokes equations of motion and continuity in a rectangular coordinate
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 14/113
4
system are transformed into a computational plane in a boundary fitted coordinate
system. SIMPLE algorithm by Patankar-Spalding [16] is chosen to solve the equations.
In chapter 4 results of numerical simulation are presented and compared with
other studies. Results are related to Newtonian and non-Newtonian fluid flow in eccentric
annulus with stationary drill pipe. Results for the case when drill pipe is in motion are not
presented due to instability of the numerical procedure.
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 15/113
5
CHAPTER 2
LITERATURE REVIEW
This chapter is a review of some the previous work about laminar annular flow.
Laminar annular flow is flow of a fluid in an annulus under laminar regime. In laminar
regime, fluid particles travel along well-ordered non-intersecting paths, or layers.
The determination of annular flow performance is important in the planning and
design of the hydraulic program for a well not only because of significant pressure losses
but also possible hole cleaning problems.
Laminar annular flow has been the subject of many investigations. With the
developments in computers and also computational fluid dynamics there is a high trend
of using numerical simulations.
2.1 Annular Flow of Newtonian Fluid
One of the first correlations for annular flow is given by Lamb (1932) [12]. In that
study, an equation is presented that correlates frictional pressure loss with flow rate in a
concentric annulus for a Newtonian fluid.
( )
−
−−=
1
2
221
224
142
ln8
r
r
r r r r
dl
dP q
µ
π 1.1.2.eq
Where,
1r : inner radius of the inner pipe
2r : inner radius of the outer pipe
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 16/113
6
dl
dP : pressure drop
µ : viscosity of the fluid
q : volumetric flow rate
Piercy et al. (1933) [17] presented an exact solution that correlates, frictional
pressure loss, flow rate and eccentricity. Considering Fig.2.21:
Where, o R and i R are the outer and inner cylinder radii and c is the displacement of the
two centers. Momentum equation in the rectangular Cartesian coordinates for this case to
be solved is:
Fig.2.1.1 Newtonian fluid in concentric annulus
R i
R o
c
X
Y
Fig.2.1.2 Eccentric Annulus
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 17/113
7
∂∂
+∂∂
+∂∂
−=2
2
2
2
0 y
v
x
v
z
P z z µ 2.1.2.eq
Where,
z
P
∂∂ : pressure drop in axial direction
µ : fluid viscosity
z v : fluid velocity in axial direction
Using below notation:
( )22 y xk v z +−=φ 3.1.2.eq
The mathematical problem now becomes:
02
2
2
2
=∂∂
+∂∂
y x
φφ 4.1.2.eq
subjected to the no-slip condition, )(
22
y xk w +−=φ on the solid boundaries, which is
Laplace’s equation.
They obtained exact solution by mapping the cross section conformally onto a
region where Laplace’s equation has a known solution. This technique is called” complex
variable” technique. By applying the transformation:
( )
+=+ ηξ i M iz y
2
1tan 5.1.2.eq
where,
2
2222
2 o
io Rc
c R R M −
+−=
z
P k
∂∂
=µ4
1:Where
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 18/113
8
the momentum equation ( 4.1.2.eq ) in the ( )ηξ , ??coordinate system will take the form:
02
2
2
2
=∂
∂+
∂
∂
η
φ
ε
φ 6.1.2.eq
Subject to:
βαηεη
η,01
coshcosh
cosh22 ==
−
+− at M K
Solving 6.1.2.eq :
( )io
n
n
io
R Rc for
nn
ne M c
M c R R
dl
dp−<<
−−
−−−
−=
∑∞
=
+−0,
)sinh(8
4
8
Q
1
)(22
2244
αβαβµ
π αβ 7.1.2.eq
Where,
c
c R R io
2F
222 +−=
22o R F M −=
−+
= M F
M F ln
2
1α
−−+−
= M c F
M c F ln
2
1β
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 19/113
9
0.4
0.5
0.6
0.7
0.8
0.9
1.0
0 0.2 0.4 0.6 0.8 1
Relative Eccentricity, [c/(Ro-Ri)]
d P / d L ( E c c e n . / C o n c e n . )
Ri/Ro=0.8
Ri/Ro=0.5
Ri/Ro=0.2
As can be clearly seen from Fig.2.1.3, the eccentricity of the drill pipe can cause a
substantial decrease in frictional pressure loss.
2.2 Concentric No Rotation Non-Newtonian
Bird and Fredrickson (1958) [6] obtain analytical correlation between flow rate and
frictional loss for Power-law fluids.
( ) ( )
−−−
∆
∆
+=
+−++
nnnnn
n
o
L K
P
n
RQ
1122
111
12
113
123
1 κβκβ
π 1.2.2.eq
Where,
K = fluid consistency index
Fig.2.1.3 Effects of eccentricity on frictional pressure loss for a Newtonian fluid with
constant flow rate using 7.1.2.eq . [ Secliter Q /1.0= , Sec Pa.00102.0=µ , m Ro 0889.0= ]
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 20/113
10
n = flow behavior index for power-law fluid
o
i
R
R=κ
L
P
∆
∆= pressure drop per unit length
And β can be calculated from the following equation:
∫ ∫
−=
−
11
2
1
2
β
β
κ
ξξ
βξξξ
ξ
βd d
nn
2.2.2.eq
In their paper, Bird and Fredrickson (1958) [6] also showed a correlation for
Bingham Plastic fluid flow in concentric annulus as follows:
( ) ( )( ) ( ) ( )
−++−−−−−
∆∆= +++ y y y y
p
o K K K L
P RQ ττλττλλ
µ
π 33242
23
11
3
4121
8 3.2.2.eq
Where,
K = fluid consistency index
pµ = plastic viscosity
o
i
R
R=κ
L
P
∆∆
= pressure
yτ = yield stress
And +λ can be calculated from the following:
( ) ( ) ( ) 0121ln22 =−+++−
−− +
+
+++ λττ
λ
τλτλλ y y
y y K
K 4.2.2.eq
Bird and Fredrickson [6] solved 4.2.2.eq numerically and presented the results in the
form of charts facilitating rapid application.
Skelland (1967) [8] presented another exact solution for Bingham plastic fluid as
follows:
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 21/113
11
( ) ( ) ( )( )
( ) ( )( ) ( )( )
( )( ) ( )( ) ( )33332222
2222222
22222224444
344
4416
816ln
2
16
2
io p
y y
oi
y
iooi y
io y
ioio
i
o p
io
p
R Rbaabbaab R R
R R R R R Rbaab L
P
R Rab L
P R R
L
P
bR
aRba R R
L
P Q
−−++
−++−+−
−++−+−−∆
∆−
−−
∆∆+−
∆∆−
+−+−
∆∆=
µ
πτττ
ττ
µ
π
µ
π
5.2.2.eq
Where, a and b could be calculated by solving the following equations:
( )
( )( )
+−−+=
=−
−−
∆∆
i
o
ioab R R
L P
y
bR
aR
R Rabab
ab
io
ln
2
2222
22
τ
6.2.2.eq
Hanks (1979)[9] presented analytical solution for yield power-law fluid. In that
study several charts are presented through computing theoretical solutions of the
equations of the motion for the concentric annular geometry using the Herschel-Bulkly
model. Using those charts to find some parameters and applying them to the equations,
one can compute volume flow rate through given pressure drop and also computing
pressure drop through given volume flow rate.
2.3 Eccentric No-Rotation Non-Newtonian
Haciislamoglu (1985) [7] and Azouz (1994) [3] used numerical simulation to solve
the governing equations of non-Newtonian fluid flow in eccentric annulus without pipe
rotation.
Nearly all of the analytical and numerical solutions for annular flow without pipe
rotation indicate that frictional pressure loss decreases with increasing eccentricity, at a
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 22/113
12
given flow rate. The reduction in pressure loss can be significant for instant can be in the
range of the pressure loss.
2.4 Newtonian Fluid Flow in Annulus with Inner Pipe Rotation
Yamada (1960) [22] described the experimental results for the resistance of water
flow through an annulus formed by two concentric cylinders, with the inner cylinder
rotating and the outer cylinder stationary. This study shows that when the flow is laminar,
the resistance of a flow is unaffected up to a certain rotational speed. But beyond this
speed the flow resistance increases as the Reynolds number increases.
Ooms et al. (1996) [15] performed numerical simulation of Newtonian fluids flow
in annulus to investigate effects of eccentricity and rotational speed of the inner pipe on
frictional pressure loss. Their study was more accurately followed by Escudier et al.
(1999) [4]. Theoretical and experimental study of Escudier et al. [4] suggested that in the
case of concentric annulus, rotation of the inner pipe does not influence frictional
pressure loss of the Newtonian fluids. However, in the case of eccentric annulus they
showed that when the inner pipe is rotating, for low eccentricities (less than 30%),
pressure drop remains approximately constant with increasing of eccentricity. For higher
eccentricities however, frictional pressure loss generally decreases with increasing of
eccentricity. Escudier et al. [4] also found that for a given radius ratio, as rotation speed of
the inner cylinder increases at any eccentricity, frictional pressure loss increases.
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 23/113
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 24/113
14
drop values for power-law fluids follow the trends observed by Escudier et al. (1999) [4]
for Newtonian fluids, including an increase with rotation of the inner pipe, an increase
with eccentricity at low and very high eccentricities but a decrease for intermediate
eccentricities. They showed that a power-law fluid generally exhibits lower pressure drop
as compared with the Newtonian liquid.
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 25/113
15
CHAPTER 3
ANNULAR FLOW IN ECCENTRIC ANNULUS
In this chapter laminar flow of Newtonian and non- Newtonian fluids through an
eccentric annulus is numerically simulated. In the first part of the chapter drill pipe is
considered to be stationary and fluid is Newtonian or non-Newtonian. In the second part
of this chapter inner pipe is rotating and fluid is Newtonian.
3.1 Annular Flow in Eccentric Annulus without Inner Pipe Rotating
To simulate fluid flow in an eccentric annulus when the drill pipe is stationary,
governing equations for flow in eccentric annulus are developed in the Cartesian
coordinate system. Yield Power Law model is used to represent the rheology of the fluid.
To solve the flow equations, two approaches are used. In the first approach a rectangular
mesh system is used to solve discretized flow equations in the Cartesian coordinate
system. In the second approach, on the other hand, a boundary fitted coordinate system is
utilized to apply numerical technique to equations.
In the first approach using a rectangular grid system, equations are discretized and
an iterative over relaxation method is used to solve for velocity field at each grid point
knowing frictional pressure loss in axial direction of the well bore. A relaxation technique
is used to speed up convergence of the solution. Calculation of relaxation factor is
presented and the treatment for the no shear region is discussed.
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 26/113
16
In the second approach similar solution procedure is used, but geometry as well as
equations are transformed into a computational domain in a boundary fitted coordinate
system.
3.1.1 Assumptions
1-Laminar and fully developed flow
2-Isothermal and steady state conditions
3-Flowing direction is in the annulus along the axial direction of the well bore.
4- Incompressible fluid
5- Flow domain is an eccentric annulus.
6- Drill pipe is stationary
7-No slippage at the walls
3.1.2 Continuity Equation
Navier-Stokes continuity equation for an isothermal laminar flow in Cartesian
coordinate system is:
∂∂
+∂
∂+
∂∂
−=∂∂
+∂∂
+∂∂
+∂∂
z
v
y
v
x
v
z v
yv
xv
t
z y x z y x ρ
ρρρρ 1.1.3.eq
Where, ρ is the density of the fluid and z y x vvv ,, are velocity components in
z y,, directions respectively. Coordinate system is shown in Fig.3.1.1.
Since the fluid is incompressible, all the terms on the left hand side of eq.3.1.1 are
zero. The first two terms in parenthesis on the right hand side of the same equation are
zero since the flow is purely axial (i.e. no flow in x and y directions). So, from 1.1.3.eq :
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 27/113
17
0=∂
∂ z
v z 2.1.3.eq
Fig.3.1.1 Cartesian coordinate system
3.1.3 Momentum Equation
For axial laminar flow, the equation of motion will take the form (Appendix A):
z
P
y
w
y x
w
x ∂
∂=
∂
∂
∂
∂+
∂
∂
∂
∂µµ 3.1.3.eq
Where, w is the fluid velocity in z direction and µ is the viscosity that is a
function of shear rate. The viscosity function depends on the rheology of the fluid. The
shear rate for axial flow can be expressed as:
22
∂∂+
∂∂=
y
w
x
wγ& 4.1.3.eq
In order to solve the above equations, the following boundary conditions are
applied:
1-Velocity at the drill pipe is zero
2- Velocity at the well-bore wall is zero.
X
Z
Y
F l o w
D i r e c t i o n
F l o w
D i r e c t i o n
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 28/113
18
3.1.4 Drilling Fluid Rheology
Flow behavior of a fluid can be described by a mathematical relationship between
shear stress and shear rate. Fluids are generally categorized as Newtonian and non-
Newtonian Fig.3.1.2. This classification is based on the relationship between shear rate
and shear stress. Drilling fluids are mostly non-Newtonian in character and almost
invariably shear thinning, and often exhibiting visco-elastic and thixotropic properties as
well as yield stress [2].
Newtonian Model:
γµτ = 5.1.3.eq
Bingham Plastic Model:
γµττ & p y +=
6.1.3.eq
Power Law Model:
→<→>
=FluidticPseudoplas1
FluidDilatant1
n
n K nγτ &
7.1.3.eq
Yield Power Law (Herschel-Bulkley) Model:
Pipe and annular flows of Yield Power-Law fluid is of great interests in drilling
applications. This model describes the rheological behavior of drilling muds more
accurately than Bingham Plastic and Power-Law models. The Yield Power-Law
rheological model for all time-independent fluids is given by:
n y K γττ &+=
8.1.3.eq
Where:
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 29/113
19
τ = Shear Stress
yτ = Yield Shear Stress
γ& = Shear Rate
K = Fluid Consistency Index
n = Flow Behavior Index
µ = Newtonian Viscosity
pµ = Plastic Viscosity
Fig.3.1.2 Flow Curve for Different Fluids
General Model:
All the above models can be expressed by the Yield Power Law model as follows:
→≠≠
=→=≠
→≠=
=→==
+=
Fluid Law Power Yield n If
K Model Plastic Binghamn If
Model Law Power n If
K Model Newtoniann If
K
y
p y
y
y
n y
1,0:
)(1,0:
1,0:
)(1,0:
τ
µτ
τ
µτ
γττ & 9.1.3.eq
Apparent Viscosity:
A non-Newtonian fluid does not have a constant viscosity like Newtonian. However, in
numerical modeling, the concept of viscosity is used for non-Newtonian fluids to make
the governing equations similar to Newtonian fluids. This viscosity is known as apparent
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 30/113
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 31/113
21
Fig.3.1.3 Grid network in Cartesian coordinate with different grid sizes in x and y direction
3.1.6 Discretizing the Equation of Motion
Equation of motion is a differential equation that can be approximated by a
discretized finite difference equation. A second-order central differencing scheme has
been used for all the grid points inside of the flow domain. This scheme establishes the
following system of algebraic equations:
∂∂
−++++++
= −+
+−+
++
z
P W AW AW AW A
A A A AW ji
n
ji
n
ji
n
ji
n
ji
n
1,
1
41,3,1
1
2,114321
,
1 1 13.1.3.eq
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 32/113
22
Where, coefficients are calculated based on 10.. Beq (Appendix B). In order to
speed up the rate of convergence an over relaxation factor is introduced to 1.6.3.eq thus:
( )
∂∂
−+++−
+++
++++= −
++−
++
+
z
P W A A A A
W AW AW AW A A A A A
W W
ji
n
ji
n
ji
n
ji
n
ji
n
ji
n
ji
n
,4321
1,
1
41,
3,1
1
2,1
14321
,,
1 ω
14.1.3.eq
Where:
ji
n
W ,
1+ : The value of the velocity field at node ji, at computational step (iteration) 1+n
ji
n
W , : The value of the velocity field at node ji, at computational step (iteration) n
Where, ω is over relaxation factor and is calculated following Azouz [3]at each
grid point and it is shown in (Appendix D):
( )
( )
<−++
≥−−+
=
0411
2
0411
2
2
3
2
12
23
21
2
ϕϕρ
ϕϕρ
ω
if
if
J
J
15.1.3.eq
Where:
+−+
+−
+=
1cos4
1cos4
2
1 24
22
23
21
21 N M J
πϕϕ
πϕϕ
ϕϕρ
appµϕ =1
appµϕ =2
x∂∂= µ
ϕ3
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 33/113
23
y∂∂
= µ
ϕ4
Where, N M , are number of grid points in y x, direction. Details of calculations
can be found in Appendix D.
Discretizing viscosity equation in 11.1.3.eq yields:
( ) 1,
,,
−+= n ji
ji
y
ji K γγ
τµ &
& 16.1.3.eq
Where:
2
1,1,
2
,1,1,
22
∆
−+
∆
−= −+−+
y
W W
x
W W ji ji ji ji jiγ& 17.1.3.eq
3.1.7 Solution Algorithm
Three systems of algebraic equations are solved iteratively. First, discretized
velocity equation ( 14.1.3.eq ) is solved at point ji, that is a point in the flow region. Then
viscosity equation ( 16.1.3.eq , 17.1.3.eq ) followed by relaxation factor calculation ( )15.1.3.eq
is evaluated. Iterations continue until convergence is achieved. Having velocity field,
flow rate is calculated through numerical integration over the flow region.
3.1.8 Minimum Shear Rate
Visco-plastic fluids encounter a problem for small shear rate in the un-yielded
region while calculating the apparent viscosity. This is the most difficult aspect for
numerical modeling of fluids with yield stress. Azouz [3] used a minimum cut off value of
the shear rate. It is better to determine a cut off value corresponding to the conditions. It
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 34/113
24
was experienced that if the cut of value is too small or too big, sometimes we need too
many unnecessary iterations or we may encounter instability problem. The following
equations can be used for calculating cut off value of minimum shear rate:
=− StressYiel without Fluids for
StressYield with Fluids for K
wall
n y
γ
τ
γ
&
&
8
1
8
min
10
10
18.1.3.eq
where, wall γ& can be calculated from 24.. Beq .Detailed derivations of the above equations
can be found in Appendix B.
Iteration begins with a relatively large value of cut off shear rate. When velocity
field reaches a convergence the cut off value must decrease and iterations continue with
the new cut off shear rate. This procedure continues until the smallest desired cut off
value is obtained. From then on, it will remain constant.
3.1.9 Convergence Criteria
When the values of velocity field do not change with more iteration and also
smallest calculated shear rate reaches the minimum desired shear rate, convergence is
achieved and calculations should be stopped.
Convergence of velocity is achieved when velocity field at new iterations is close
to the values of the previous iteration. This is defined by a relative value, called residual
of velocity:
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 35/113
25
( ) ( )
( )∑∑
∑∑
= =
= =
−
=max max
max max
1 1
,
1 1
,,
j
j
i
i
jiold
j
j
i
i
jiold
jinew
w
ww
Residual Velocity 19.1.3.eq
If the velocity residual is small enough 710.. − g e , convergence is achieved.
3.1.10 Flow Rate Calculations
Flow rate is integral of velocity times its associated area:
y xw AwwdAQ
j
j
i
i ji
j
j
i
i ji ji ∆∆=≈= ∑∑∑∑∫ = == =
max maxmax max
1 1,
1 1,, 20.1.3.eq
Fig.3.1.4 Flow Rate Calculation at Grid Point i,j
3.1.11 Using Boundary Fitted Coordinate System
One advantage the boundary fitted coordinate system compared to rectangular
coordinate system is its ability to conform to the boundaries of the system regardless of
i i+1i-1
j+1
j
j-1
y∆
x∆
jiw ,
y x A ji ∆∆=,
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 36/113
26
the shape. In another word grid generated can fit itself into the boundary of the system as
shown in Fig.3.1.4. This feature increases the accuracy of the solution developed.
Doing the transformation, physical Cartesian coordinates (x,y) becomes the
dependent variables and the curvilinear coordinates ( ηξ , ) becomes the independent
variables. A generated grid is then defined as a set of points formed by the intersections
of the lines of a boundary conforming curvilinear coordinate system.
Fig.3.1.5 Grid Network in Boundary Fitted Coordinate System
There is a uniform grid in this system in the sense that at each radius position the
angular width is constant and at each angular position, the radial width of the cells is also
constant.
x
y
e i R
o R ),(),(),( ji y x =≡ ηξ
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 37/113
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 38/113
28
e : Distance between the inner cylinder (drill pipe) and outer cylinder (well bore wall).
3.1.13 Transformation of the Equations
Equation of motion and apparent viscosity equation 12.1.3.eq are numerically
transformed from a Cartesian system to a computational domain. According to 43..C eq
(Appendix C):
( ) ( ) z
P J W W
J W W
J
appapp
∂∂
=
−
∂∂
+
−
∂∂
ξηηξ γβµ
ηγα
µ
ξ 22.1.3.eq
Where:
1−+= n y
app K γγ
τµ &
&
( )ηξηξ γβαγ W W W W J
21 22
2 −+=&
22ηηα x y +=
ηξξηγ x x y y +=
22ξξβ x y +=
ξηηξ y x y x J −=
Detailed derivations can be found in Appendix C.
3.1.14 Discretization of the Equation of Motion
The same way of discretizing as was used for the Cartesian coordinate system will
be used for the transformed equation:
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 39/113
29
0101,191,18,171,6
1,15,141,31,12,1
=−−−−
−−−−−
++−−++
+−−−−+
AW AW AW AW A
W AW AW AW AW A
ji ji ji ji
ji ji ji ji ji
23.1.3.eq
Where coefficients 101 A A − can be found in 16.. Deq (Appendix D) .
Solution algorithms will the same as well. Using relaxation factor:
+−+++
+++++=
++−−+
++
+−−+
−+
−++
10,11,191,1
1
8,171,6
1,15,1
1
41,
1
31,121
,,
1
AW AW AW AW AW A
W AW AW AW A A
W W
ji
n
ji
n
ji
n
ji
n
ji
n
ji
n
ji
n
ji
n
ji
n
ji
n
ji
n ω
24.1.3.eq
3.1.15 Grid Refinement Analysis
A gird refinement analysis showed that using grid numbers more than 100 in
radial and in tangential direction does not result in a significant change in flow rate. In
order to check the results for different grid numbers, a concentric annulus was considered
and the results of the numerical simulation was compared with the results of analytical
solution for Newtonian and non-Newtonian as it is shown in 6.1.3. Fig and 7.1.3. Fig .
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 40/113
30
0
0.2
0.4
0.6
0.8
1
1.2
1.4
1.6
1.8
0 100 200 300 400
Number of Grids in Tangential Direction
% E r r o r i n
f l o w r a t e ( c o m p a r e d w i t h a n a l y t i c a l
s o l u t i o n s )
n=1.0
n=0.5
Fig. 3.1.7 Grid refinement in tangentialdirection (number of grids in radial direction=60).Comparison of the value for volume flow rate of simulation with analytical solutions for
concentric annulus for a Newtonian (n=1) and a power-law (n=0.2) fluid.
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 41/113
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 42/113
32
( ) ( ) ( ) ( )1,11,11,11,11,11,11
2
1+++−+++++−++
∆−+−−= ji ji ji ji ji ji x x y y y x ABO 27.1.3.eq
( ) ( ) ( ) ( )1,11,11,11,11,11,112
1−+−−−+−+−−−+
∆−+−−= ji ji ji ji ji ji x x y y y xCDO 28.1.3.eq
( )( )( ) ( )( )
( )
−
−+−−
−
−+−−=
∆
2
2
2
2
1
1
2sin
1
1
2
1
JM
R i Ro j JM R o
CDO Arc
JM
R i Ro j JM R oCPDO 29.1.3.eq
( ) ( ) ( )( ) ( )1,11,11,11,11,11,12
12
21 −+−−−+−+−−−+∆ −
−−−−−−== ji ji ji ji ji ji x x y
JM je y y xCDO 30.1.3.eq
( )( )( ) ( )( ) ( )
( )
−
−+−−
−
−−−−=
∆
2
3
2
3
1
1
2sin
1
1
2
1
JM
R i Ro j JM R o
ABO Arc
JM
Ri R o j JM R o AQBO 31.1.3.eq
( ) ( )( )
( )1,11,11,11,11,11,1312
1+++−+++++−++
∆−
−
−−−−= ji ji ji ji ji ji x x y
JM
je y y x ABO 32.1.3.eq
Where, e JM IM ji ,,,, are shown in Fig.3.1.5.
3.2 Newtonian Fluid Flow in Eccentric Annulus with Inner Pipe Rotating
The objective of this section is to investigate laminar Newtonian fluid flow in a
concentric annulus with inner pipe rotation. Navier-Stokes equations for laminar flow of
a Newtonian fluid in Cartesian coordinate system are considered. All the equations are
transformed to a computational domain in the boundary fitted coordinate system.
Geometry, on the other hand is transformed algebraically. Having equations and
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 43/113
33
geometry in the computational domain, SIMPLE algorithm (Patankar –Spalding, 1972) is
applied to solve the equations.
3.2.1 Assumptions
1-Laminar and fully developed flow
2-Isothermal and steady state conditions
3-Flowing direction is in the annulus along the axial direction of the well bore.
4- Incompressible fluid
5- Flow domain is an eccentric annulus.
6- Drill pipe is rotating at a constant angular velocity
7-No slippage at the walls
3.2.2 Governing Equations
Considering Navier-Stokes equations in a Cartesian coordinate system for
Newtonian fluid, momentum equations in z y x ,, will be:
( ) ( ) x g
x
p
z
w
y
v
x
u
z
wu
y
vu
x
u
t
uρµρρ +
∂∂
−
∂
∂+
∂
∂+
∂
∂+
∂∂
+∂
∂+
∂∂
−=∂∂
2
2
2
2
2
22
1.2.3.eq
( ) ( ) y g
y
p
z
w
y
v
x
u
z
wv
y
v
x
uv
t
vρµρρ +
∂∂
−
∂
∂+
∂
∂+
∂
∂+
∂∂
+∂∂
+∂
∂−=
∂∂
2
2
2
2
2
22
2.2.3.eq
( ) ( ) z g z p
z w
yv
xu
z w
yvw
xuw
t w ρµρρ +
∂∂−
∂∂+
∂∂+
∂∂+
∂∂+
∂∂+
∂∂−=
∂∂
2
2
2
2
2
22
3.2.3.eq
And Continuity equation is:
0=
∂∂
+∂∂
+∂∂
+∂∂
z
w
y
v
x
u
t
ρ 3.2.3.eq
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 44/113
34
The first term on the left hand side of all the momentum equations is zero because
the flow is under steady state. Also on the right hand side of the same equations the last
term in the second parenthesis is zero due to flow is fully developed. Also the last term
on 1.2.3.eq and 2.2.3.eq is zero because there is not any gravity in x and y directions.
In continuity equation, the first term is also zero because of a steady state flow.
The last term on the left hand side of this equation is also zero because fluid is fully
developed.
Gravity in y x, directions is zero. Also we wish to eliminate gravity in z direction
in order to consider only frictional pressure loss so 4.2.321.3. −eq will take the new form:
( ) ( ) x
p
y
v
x
u
z
wu
y
vu
x
u
∂∂
−
∂
∂+
∂
∂=
∂∂
+∂
∂+
∂∂
2
2
2
22
µρ
5.2.3.eq
( ) ( ) y
p
y
v
x
u
z
wv
y
v
x
uv
∂∂
−
∂
∂+
∂
∂=
∂∂
+∂∂
+∂
∂2
2
2
22
µρ
6.2.3.eq
( ) ( ) z
P
y
v
x
u
z
w
y
vw
x
uw
∂∂
−
∂
∂+
∂
∂=
∂∂
+∂
∂+
∂∂
2
2
2
22
µρ
7.2.3.eq
0=∂∂
+∂∂
y
v
x
u
8.2.3.eq
3.2.3 Boundary Conditions
==
−=
===
0
:)(
0
:)(
..
w
Cosr v
Sinr u
boundaryinner string drill theOn
wvu
boundaryouter wall borewell theOn
Cs B
θω
θω
9.2.3.eq
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 45/113
35
Fig.3.2.1 Boundary conditions for an eccentric annulus with rotating drill pipe
3.2.4 Transformation of Equations
Using boundary fitted coordinates flow equations can be transformed from the
real domain onto a computational domain.
According to Hoffman [10] :
ξηηξ y x y x J −=1
10.2.3.eq
J
y x
ηξ =
11.2.3.eq
J
x y
ηξ −=
12.2.3.eq
J
y x
ξη −=
13.2.3.eq
J
x y
ξη =
14.2.3.eq
( )ξηηξ y f y f J f x
f x −==
∂∂
15.2.3.eq
θ
ωr
θω Cosr
θωSinr −
ω
x
y
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 46/113
36
( )ξηηξξη y f x f x f J f y
f y −−==
∂∂
16.2.3.eq
( )
( )( ){
( )( )}ξηηξηηξξηηξξξ
ηξξηηηξξηηξξξ
ηηξξηηξξξ
f y f y x y x y y x y
f x f x y y y y y y y J
f y f y y f y J x
f
n
n
n
−+−
+−+−
++−=∂
∂
22
223
222
2
2
2
2
2
17.2.3.eq
( )
( )( ){
( )( )}ξηηξηηξξηηξξξ
ηξξηηηξξηηξξξ
ηηξξηηξξξ
f y f y x x x x x x x
f x f x y x y x x y x J
f x f x x f x J x
f
n
n
n
−+−+
−+−+
+−=∂∂
22
223
222
2
2
2
2
2
18.2.3.eq
Applying 18.2.310.2.3. −eq to equations of motion and continuity, yields:
ξ -momentum equation:
)2( 1 ξηηηξηξξ ueducubuau J +++−
( ) ( ) ( ) 01
21432
22
1 =++++++ ηξξηηξρ
pa pauvauvauaua 19.2.3.eq
η -momentum equation:
)2( 1 ξηηηξηξξ vedvcvbvav J +++−
( ) ( ) ( ) 01
432
42
321 =++++++ ξηξηηξρ
pa pavavauvauva 20.2.3.eq
Z -momentum equation:
)2( 1 ξηηηξηξξ wedwcwbwaw J +++−
( ) ( ) ( ) ( ) 01
4321 =∂∂
−++++ Z
P
J vwavwauwauwa
µξηηξ 21.2.3.eq
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 47/113
37
Continuity Equation:
04321 =++++ ξηηξ vavauaua
22.2.3.eq
Where:
22ηη x ya +=
ηξηξ y y x xb +=
22ξξ x yc +=
ξηηξ y x y x J
−= 1
ηηξηξξα cxbxax +−= 2
ηηξηξξβ cybyay +−= 2
βα ξξ x y J d −= 23.2.3.eqs
αβ ηξ y x J e −=1
ηµ
ρ ya −=1
ξµ
ρ ya =2
ξµ
ρ xa −=3
ηµ
ρ xa =4
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 48/113
38
3.2.5 Numerical Procedure
This set of equations ( )2.22.319.2.3. −eqs exhibit a mixed elliptic-parabolic
behavior, and hence the standard relaxation technique which is widely used for those
types of equations is not particularly helpful.
To solve these kinds of equations, Patankar and Spalding (1972) proposed a
method called SIMPLE (Semi Implicit Pressure Linked Equation) algorithm. SIMPLE
algorithm is basically an iterative approach, where some innovative physical reasoning is
used to make the next iteration from the results of the previous iteration. The idea is to
start with discrete continuity equation and substitute into it the discrete u and v
momentum equations. Discrete momentum equations contain pressure differences hence
we can get an equation for the discrete pressures. SIMPLE algorithm actually solves for a
related quantity called the pressure correction.
3.2.6 Discretization of Momentum and Continuity Equation
Using ordinary discretization of equations in these types of equations may create a
checkerboarding problem as described by Patankar-Spalding [15]. A popular remedy for
checkerboarding is the use of a staggered mesh. The key feature here is to calculate
pressure and velocity at different grid points as shown in 2.2.3. Fig .
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 49/113
39
Fig.3.2.2 Staggered grid for velocity and pressure
The original formulation of the SIMPLE method by Patankar and Spalding
involved a finite-volume approach. In this study, a finite-difference approach is used
which would essentially give the same results as obtained by finite-volume method. We
choose to use a forward or backward differencing for the grid points close to the walls.
For other points, central differencing with second order accuracy is used. The
computational domain is assumed to have equal spaces in ηξ , direction meaning:
1=∆=∆ ηξ .
ξ -momentum equation after some arrangements will be:
( ) ( ) ( )[ ] ji ji ji ji ji P P a P P a
ca J AU ,2,2,2,12,1
2
1−+−
++= +−−
ρ 24.2.3.eq
Where:
( )ca J
A A
+=
2
12
( ) jη
( )iξ
i,j
i, , j-1
i-1, j
jiU ,1−
ji ji W P ,, ,
1, − jiV
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 50/113
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 51/113
41
And,
2
2
2
2
2,12,1
,1,1
2,1,1
2,1,1
−−−+∨∨
−+∨∨
−−−
−++
+=
+=
+=
+=
ji ji
ji ji
ji ji
ji ji
U U U
U U U
U U U
U U U
z -momentum equation:
2, C W ji = 26.2.3.eq
Where:
( )ca J
C C
+=
2
12
( ) ( )
( ) ( ) ( )
∂∂
−
−+
−
+
−+
−
+
−+−++
+
+−−−+=
−
≈
+−
∧∧
+
−
∧∧
+
∧
−−
≈
−+
−+−+−+
−−+−−+++−+
z
p
J W V W V
aW V W V
a
W U W U a
W U W U a
W W e
W W d
W W c
W W W W b
W W a J C
ji ji ji ji
ji ji ji ji
ji ji ji ji ji ji
ji ji ji ji ji ji
µ
1~
2
~
2
2
~
2
22
2
,2,24
2,2,3
2,2,2
1,21,21
,2,2
1
2,2,2,2,
2,22,22,22,2,2,21
2
2
~
2,12,1
2,12,1
−+−−≈
−+++
+=
+=
ji ji
ji ji
U U U
U U U
2
2
2,12,1
2,12,1
−+−−∧∧
+++−∧
+=
+=
ji ji
ji ji
U U U
U U U
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 52/113
42
2
2
~
1,21,2
1,21,2
−−+−≈
−+++
+=
+=
ji ji
ji ji
U V V
V V V
2
21,21,2
1,21,2
−−−+∧∧
+−++∧
+=
+=
ji ji
ji ji
U V V
V V V
Continuity equation:
01,21,41,1,32,1,12,1,11 =−+−+−+− −−−−+−−−−+ ji ji ji ji ji ji ji ji V V aV V aU U aU U a 27.2.3.eq
Where could be calculated from 23.2.3.eqs .
3.2.7 Pressure Correction Equation
The primary idea behind SIMPLE is to create a discrete equation for pressure (or
alternatively, a related quantity called the pressure correction) from the discrete
continuity equation( )27.2.3.eq . Since the continuity equation contains discrete face
velocities, we need some way to relate these discrete velocities to the discrete pressure
field. The SIMPLE algorithm uses the discrete momentum equations to derive this
connection. Let ** ,V U and *W be the discreteU ,V and W fields resulting from a solution of
the discrete V U , and W momentum equations. Let * P represent the discrete pressure field
which is used in the solution of the momentum equations. Thus 1,,1 , −− ji ji V U and jiW , satisfy:
( )
−+
−+
+= +−− ji ji ji ji ji P P a P P aca J
AU ,
*
2,
*
2,2
*
,
*
1
*
2,1
*
2
1
ρ 28.2.3.eq
( )
−+
−+
+= +−− ji ji ji ji ji P P a P P aca J
BV ,
*
,2
*
42,
*
,
*
3
*
21,
*
2
1
ρ 29.2.3.eq
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 53/113
43
2
*
,
*
C W ji = 30.2.3.eq
01,21,41,1,32,1,12,1,11 =−+−+−+− −−−−+−−−−+ ji ji ji ji ji ji ji ji V V aV V aU U aU U a 31.2.3.eq
If the pressure field * P is only a guess or a prevailing iterate, the discrete
**,V U and *
W obtained by solving the momentum equations will not, in general, satisfy the
discrete continuity equation( )31.2.3.eq . A correction is proposed to the starred velocity
field such that the corrected values satisfy continuity equation:
U U U ′+=*
32.2.3.eq
V V V ′+=*
33.2.3.eq
W W W ′+=*
34.2.3.eq
Correspondingly, we wish to correct the existing pressure field
*
p with
P P P ′+=*
35.2.3.eq
Subtracting 26.2.324.2.3. −eqs , from 30.2.328.2.3. −eqs , we obtain:
( ) ( ) ( )[ ] ji ji ji ji ji P P a P P a
ca J AU ,2,2,2,12,1
2
1 ′−′+′−′+
+′=′ +−−ρ
36.2.3.eq
( ) ( ) ( )[ ] ji ji ji ji ji P P a P P aca J
BV ,,242,,321,2
1
′−′+′−′++′=′ +−−ρ 37.2.3.eq
2, C W ji ′=′ 38.2.3.eq
We now make the main simplification of SIMPLE algorithm by doing following
approximation:
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 54/113
44
0
0
0
2
2
2
≅′≅′≅′
C
B
A
39.2.3.eqs
So, 38.2.336.2.3. −eqs will take the form
( ) ( ) ( )[ ]
( ) ( ) ( )[ ]
0
2
1
2
1
,
,,242,,31,
,2,2,2,1,1
=′
′−′+′−′+
=′
′−′+′−′+
=′
+−−
+−−
ji
ji ji ji ji ji
ji ji ji ji ji
W
P P a P P aca J
V
P P a P P aca J
U
ρ
ρ
40.2.3.eqs
We now consider the discrete continuity equation. The starred velocities**
, V U
obtained by solving the momentum equations using the prevailing pressure field*
P do
not satisfy the discrete continuity equation. Thus substituting 33.2.3.32.2.3. eqand eq into
continuity equation:
01,21,2
*
1,1,
*
41,1,
*
1,1,
*
3
2,12,1
*
,1,1
*
2,1,1
*
,1,1
*
1
=
′+−
′++
′+−
′++
′+−
′++
′+−
′+
−−−−−−−−++
−−−−−−++++
ji ji ji ji ji ji ji ji
ji ji ji ji ji ji ji ji
V V V V aV V V V a
U U U U aU U U U a
41.2.3.eq
Now substituting 37.2.3.30.2.3. eqand eq into 41.2.3.eq , after some arrangements it
yields:
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 55/113
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 56/113
46
Fig.3.2.3 Overall SIMPLE Algorithm
Correct pressure and velocities
32.2.3.*
eqU U U ′+=
33.2.3.*
eqV V V ′+=
35.2.3.*
eq P P P ′+=
Solve pressure correction equation
( ) ( ) ( )[ ] 42.2.3.1
2,2,42,22,23,2,221
, eq P P f P P f P P f f
P ji ji ji ji ji ji ji +−−−++−+ ′+′+′+′+′+′−=′
START
STOP
Convergence ?
Initial guess p*, u*, *
Solve discritized momentum equations
( )28.2.3.,
*
2,
*
2,2
*
,
*
1
*
2,1
*
2
1eq ji ji ji ji ji P P a P P a
ca J AU
−+
−+
+= +−−ρ
( )29.2.3.,
*
,2
*
42,
*
,
*
3
*
21,
*
2
1eq ji ji ji ji ji P P a P P a
ca J BV
−+
−+
+= +−−ρ
2
*
,
*
C W ji = 30.2.3.eq
Yes
No
Set:
U U =*
V V =*
W W =*
P P =*
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 57/113
47
CHAPTER 4
RESULTS AND CONCLUSIONS
4.1 Newtonian Fluid
4.1.1 Results for Newtonian Fluid
As eccentricity increases, frictional pressure drop decreases. This value could be
about 50% less than the pressure drop of a concentric annulus with the same flow rate.
When the annulus becomes eccentric, one side of annuls is wider than the other side.
Since fluid always tends to bulge through the wider area, most of the fluid flows through
the wider area of the annulus (as shown in Fig.4.1.1), where there is less restriction. In
other words the portion of the fluid that is taking the highest restriction of the geometry is
less than the portion under lower restriction. Figure.4.1.3 shows the results of the
simulation for Newtonian fluid in eccentric annuli.
Fig.4.1.1 Velocity profile of Newtonian fluid for concentric to fully eccentric annuli
[ mOD 1778.0= , SecmQ /0001.0 3= , S Pa.00102.0=µ ]
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 58/113
48
Fig.4.1.2 Velocity profile of Newtonian fluid for concentric and fully eccentric annuli
[ mOD 1778.0= , SecmQ /0001.0 3= , S Pa.00102.0=µ ]
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 59/113
49
0.4
0.5
0.6
0.7
0.8
0.9
1.0
0 0.2 0.4 0.6 0.8 1 1.2
Eccentricity
P r e s s . D
r o p ( E c c e n t r i c / C o n c e n t r i c )
(Ri/Ro)=0.8(Ri/Ro)=0.5
(Ri/Ro)=0.2
Fig.4.1.3 Present study results for Newtonian fluid [ mOD 1778.0= , SecmQ /0001.0 3= ,
S Pa.00102.0=µ ]
4.1.2 Comparison of the Results for Newtonian
Figure 4.1.4 shows the comparison of the present and past studies with the
analytical solution of Piercy et al. [17]. All the cases can predict quite reasonable results.
Considering the trend of the error for different studies, in the study of Azouz [3] error
seems to be quite constant for different eccentricities. However this is quite different for
the other two studies where with increasing of the eccentricity, error decreases. Since the
error can be generate from different sources, one can not explain the reason of these
discrepancies.
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 60/113
50
Present Study
0
0.1
0.2
0.3
0.4
0.5
0.6
0.7
0.8
0 0.2 0.4 0.6 0.8 1 1.2
Eccentricity
E r r o r %
Ri/Ro=0.8
Ri/Ro=0.5
Ri/Ro=0.2
Escudier et al.
0.00
0.10
0.20
0.30
0.40
0.50
0.60
0.70
0.80
0 0.2 0.4 0.6 0.8 1 1.2
Eccentricity
E r r o r %
Ri/Ro=0.8
Ri/Ro=0.5
Ri/Ro=0.2
Azouz
Fig.4.1.4 Eccentricity vs. error in pressure drop of the different studies compared with
Piercy et al. for a Newtonian fluid
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 61/113
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 62/113
52
Fig.4.2.2 Velocity profile of power-law fluid for concentric and fully eccentric annuli [ 5.0=o
i
R
R,
SecmQ /006.0 3= , nS Pa K .6.0= , 2.0=n ]
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 63/113
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 64/113
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 65/113
55
2
4
6
8
10
12
14
16
0 0.2 0.4 0.6 0.8 1
Eccentricty
f . R e
Escudier et al.
Azouz
Present Studyn=0.8
n=0.5
n=0.2
Ri/Ro=0.5
Figure 4.2.5 Comparison of Re. f predictions with previous studies
[3,5] for a power-law fluid
with [ 5.0=o
i
R
R, SecmQ /006.0 3= , nS Pa K .6.0= ]
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 66/113
56
3.5
4
4.5
5
5.5
6
6.5
7
7.5
8
0 0.2 0.4 0.6 0.8 1
Eccentricty
f . R e
Escudier et al.
Azouz
Present Study
Ri/Ro=0.2
Ri/Ro=0.5
Ri/Ro=0.8
n=0.5
Figure 4.2.6 Comparison of Re. f predictions with previous studies [3,5]
for a power-law fluid
with [ SecmQ /006.0 3= , 5.0=n , nS Pa K .6.0= ]
4.3 Results and Comparison for Yield Power- Law Fluid
Like power-law and Newtonian fluids, the same trend is observed for yield
power-law fluid. For the following case (Fig. 4.3.1), reduction in frictional pressure loss
for eccentric annulus compared to concentric case is 40%. A comparison between the
results of this study with Haciislamoglu[7]
for this case shows a good agreement between
the two studies and the differences is less than 2%.
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 67/113
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 68/113
58
0
10
20
30
40
50
60
70
0 5 10 15 20 25
Q[GPM]
P r e s s u r e D r o p [ i n c h o f w a t e r ]
Experimental Data
Present Study
Figure 4.4.1 Comparison of the present study with experimental data of
Ahmed[1]
[ mOD 035052.0= , m ID 01745.0= , %98.0=ty Eccentrici , 671.0=m ,
S Pa K .2610958.0= , Pa y 1.2=τ , m L 6576.3= ].
Note: Extensive numerical simulation using the program indicates that the
numerical procedure used in this study is not able to accurately predict the flow rate for
fluids with yield stress when the plug region is relatively large.
4.5 Conclusions
Ø For a given flow rate increasing eccentricity of the inner pipe decreases the
pressure drop in annuli;
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 69/113
59
Ø Pressure loss reduction due to eccentricity for highly shear thinning ( )2.0=n
non-Newtonian fluids is approximately 30%, while for Newtonian fluids can
be as high as 50%;
Ø The reduction of pressure loss due to eccentricity, is more significant at higher
radius ratios
→ 1..
o
i
R
Rei ;
Ø Using Cartesian grid networks simplifies the equation of motion and
numerical procedure, however at the same time less accuracy was observed;
Ø Due to complexity of the pipe rotation case, it is recommended to do more
simplification to find the source of instability.
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 70/113
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 71/113
61
[6] Fredrickson, A. G., Bird, R.B.: “Non-Newtonian Flow in Annuli,” Ind. And Chem.,
Vol. 50, March 1958,pp.347-352.
[7] Haciislamoglu, M. “Non-Newtonian Fluid Flow in Eccentric Annuli and Its
Application to Petroleum Engineering Problems.” Dec. 1989.
[8] Haige et al., “Experimental Study of Slim Hole Annular Pressure loss and Its Field
Applications.” SPE Paper No.59265
[9]Hanks, W.R., “The Axial Laminar Flow of Yield-Pseudoplastic Fluids in a Concentric
Annulus.” Ind. Eng. Chem. Process Des. Dev., Vol. 18, No. 3, 1979
[10]Hoffmann, K.A. “Computational Fluid Dynamics for Engineers.” Vol.1, 1993
[11]Hussain, Q.E. Sharif, M.A.R. “Analysis of Yield-Power-Law Fluid in Irregular
Eccentric Annuli.” Journal of Energy Resources Technology 120 (1998) 201-207
[12]Lamb, H., 1945, Hydrodynamics, 6th edn., Dover Publications, New York, pp. 585-
587.
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 72/113
62
[13] Luo, Y., Peden J. “Flow of Drilling Fluids Through Eccentric Annuli”, SPE 16692,
62nd Annual Technical Conference and Exhibition, Dallas, September 1987.
[14]Miska, S.Z. “Advanced Drilling”, Teaching Note, University of Tulsa, 2004.
[15]Ooms, G., Kampman-Reinhartz, B.E.,1996. “Influence of drill pipe rotation and
eccentricity on pressure drop over borehole during drilling”. Eur. J. Mech. B 15 (5), 695-
711.
[16]Patankar, S.V., 1980. “Numerical Heat Transfer and Fluid Flow Hemisphere”,
Bristol, PA, pp. 1-197.
[17]Piercy, N.A.V., Hooper, M.S., Winny, H.F. 1933. “Viscous flow through pipes with
core.” London Edinburgh Dublin Phil. Mag. J. Sci., 15 647-676.
[18]Pilehvari, A.: “Modeling of Laminar Helical Flow of A Power-Law Fluid Using the
Finite Element Method”, Technical Report, The University of Tulsa, 1989.
[19]Skelland, A. H. P. “Non-Newtonian Flow and Heat Transfer”, 1967, John Wiley &
Sons, Inc. New York.
[20]Wei, X., Miska S.Z., Takach N.E. “The Effect Of Drill Pipe Rotation On Annular
Frictional Pressure Loss”.
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 73/113
63
[21]Welty, J. R., Wicks, C. E. and Wilson, R. E., “Fundamentals of Momentum, Heat &
Mass Transfer”, New York, John Wiley & Sons, (1976).
[22]Yamada “Resistance of a flow through an Annulus with an Inner Rotating Cylinder”
Bulletin of JSME. May, 1960.
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 74/113
64
APPENDIX A
EQUATION OF MOTION IN CARTESIAN COORDINATES FOR LAMINAR
FLOW OF NON-NEWTONIAN FLUID IN ANNULUS
1.. Aeq
Flow
Direction
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 75/113
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 76/113
66
Because flow is only in one direction, 0== y x vv and also from continuity equation, 0=∂ z
v z
3.. Aeqs will take the form:
0=
∂∂
−=
∂∂−=
zz
z yz
z xz
y
v
xv
τ
µτ
µτ
5.. Aeq
Now substituting, 5.. Aeq into 3.. Aeq :
z
p
y
v
y x
v
x
z z
∂∂=
∂∂
∂∂+
∂∂
∂∂ µµ 6.. Aeq
Denoting: wv z = , 6.. Aeq will be:
z
p
y
W
y x
W
x ∂∂=
∂
∂∂∂+
∂
∂∂∂
µµ 7.. Aeq
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 77/113
67
APPENDIX B
DISCRETIZING EQUATION OF MOTION IN CARTESIAN COORDINATES
FOR LAMINAR FLOW OF NON-NEWTONIAN FLUID IN ANNULUS
Recalling equation of motion ( )AppendixA,A.7eq. :
0=∂∂−
∂∂∂∂+ ∂∂∂∂ z
P yw
y xw
xµµ 1.. Beq
The above finite differential equation can be app be approximated by a difference
equation. Beginning with the first term:
ji ji ji x
W
x
W
x
W
x,
2
1,
2
1, −+
∂∂
−
∂∂
≈
∂∂
∂∂
µµµ 2.. Beq
Also we can say:
2
,,1
,2
1
ji ji
ji
µµµ
+≈ +
+ 3.. Beq
2
,,1
,2
1
ji ji
ji
µµµ
+≈ −
− 4.. Beq
Now, using a second-order central differencing:
x
ww
x
W ji ji
ji ∆
−≈
∂∂ +
+
,,1
,
2
1 5.. Beq
x
W W
x
W ji ji
ji ∆
−≈
∂∂ −
−
,1,
,2
1 6.. Beq
Substituting 6.3.. B Beqs − into 2.. Beq yields:
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 78/113
68
( )( )( ) ( )( )[ ] ji ji ji ji ji ji ji ji
ji
W W W W x x
W
x,1,,,1,,1,,12
, 2
1−−++ −+−−+
∆≈
∂∂
∂∂
µµµµµ 7.. Beq
Similarly for y derivative in 2.. Beq :
( ) ( )( ) ( )( )[ ]1,,,1,,1,,1,2, 2
1 −−++ −+−−+∆
≈
∂∂
∂∂ ji ji ji ji ji ji ji ji
ji
W W W W y y
W y
µµµµµ 8.. Beq
Substituting equation 7.. Beq and 8.. Beq into 1.. Beq :
( )( )
( ) ( )
( )( )
( ) ( )
( )( )
( )( )
0
2
1
2
1,,
,1,2
,1,
,1,
2
,1,
,,12
,,1
,,1
=∂∂
−
∆
−+−
∆
−++
∆
−+−
∆
−+
−−
++
−−
++
z
P
y
W W
y
W W
x
W W
x
W W
ji ji
ji ji
ji ji
ji ji
ji ji
ji ji
ji ji
ji ji
µµµµ
µµµµ
9.. Beq
The above equation can be rearranges as:
( ) ( ) ( ) ( )
( ) ( )
( ) ( )0
22
22
2222
2
,1,
1,2
,1,
1,
2
,,1
,12
,,1
,1
2
,1,
2
,1,
2
,,1
2
,,1
,
=∂∂
−
∆
++
∆
++
∆
++
∆
++
∆
++
∆
++
∆
++
∆
+−
−−
++
−−
++
−+−+
z
P
yW
yW
xW
xW
y y x xW
ji ji
ji
ji ji
ji
ji ji
ji
ji ji
ji
ji ji ji ji ji ji ji ji
ji
µµµµ
µµµµ
µµµµµµµµ
10.. Beq
Or:
( ) 01,11,1,11,114321, =∂∂
−+++++++− −+−+ z
P W AW AW AW A A A A AW ji ji ji ji ji
11.. Beq
Where:
( )2
,,1
12 x
A ji ji
∆
+= + µµ
( )2
,,1
2
2 x
A ji ji
∆
+= − µµ
( )2
,1,
32 y
A ji ji
∆
+= + µµ
( )2
,1,
42 y
A ji ji
∆
+= − µµ
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 79/113
69
Rearranging 11.. Beq :
∂∂
−++++++
= −+
+−+
++
z
P W AW AW AW A
A A A AW ji
n
ji
n
ji
n
ji
n
ji
n
1,
1
41,3,1
1
2,114321
,
1 1 12.. Beq
Where 1, +nn are the old and the new computational steps (iterations)
respectively.
To apply relaxation factor to 12.. Beq , first we add ji
n
ji
n
W W ,, − to the right hand side of that
equation:
∂∂
−++++++
+−= −+
+−+
++
z
P W AW AW AW A
A A A AW W W ji
n
ji
n
ji
n
ji
n
ji
n
ji
n
ji
n
1,
1
41,3,1
1
2,114321
,,,
1 1 13.. Beq
Moving ji
n
W ,− into the parenthesis in 13.. Beq yields:
( )
∂∂
−+++−
+++
++++= −
++−
++
+
z
P W A A A A
W AW AW AW A A A A A
W W
ji
n
ji
n
ji
n
ji
n
ji
n
ji
n
ji
n
,4321
1,
1
41,3,1
1
2,114321
,,
1 1
14.. Beq
Equation 14. B can be represented as:
Residual,,
1
+=
+
ji
n
ji
n
W W 15.. Beq
Where:
( )
∂∂
−+++−
+++
+++= −
++−
++
z
P W A A A A
W AW AW AW A A A A A
ji
n
ji
n
ji
n
ji
n
ji
n
,4321
1,
1
41,3,1
1
2,11
4321
1Residual
16.. Beq
Residual in 15.. Beq will decrease as we approach the solution. And when the
convergence is achieved, value of residual will reach very close to zero. Based on this fact we can
increase/decrease rate of convergence by multiplying residual by an over/under relaxation factor
shown by ω . As a result, 14.. Beq will take the form:
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 80/113
70
( )
∂∂
−+++−
+++
++++= −
++−
++
+
z
P W A A A A
W AW AW AW A A A A A
W W
ji
n
ji
n
ji
n
ji
n
ji
n
ji
n
ji
n
,4321
1,
1
41,3,1
1
2,114321
,,
1 ω
17.. Beq
Minimum Shear Rate Calculation
Recalling YPL Rheology model equation:
n y K γττ &+= 18.. Beq
In the plug region, shear rate is very small. There for the contribution of the second term
on the right hand side of 18.. Beq is negligible compared to yτ .Denoting the shear rate in the plug
region by minγ& , we get:
yn K τγ <<min& 19.. Beq
Or,
yn K τγε <<min& 20.. Beq
As a reasonable estimation, ε in 19.. Beq can be approximated by
8
10 . Therefore,
19.. Beq takes the form :
n y K min
810 γτ &= 21.. Beq
Or,
n y
K
1
8min10
=
τγ& 22.. Beq
Equation 22. B can not be used for fluids without yield stress, because the value will be
zero. So a new cut off value has to be defined. For fluids with zero yield stress, wall shear rate
can be used as a value to estimate the cut off value. As a reasonable approximation:
wall γγ && 8min 10
−= 23.. Beq
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 81/113
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 82/113
72
=−
StressYield with Fluids for
K
StressYield without Fluids for
n y
wall
1
8
8
min
10
10
τ
γγ
&& 28.. Beq
Where, wall γ& can be calculated from 24.. Beq
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 83/113
73
APPENDIX C
TRANSFORMATION OF EQUATION OF MOTION FROM CARTESIAN
COORDINATES TO A BOUNDARY FITTED COORDINATE SYSTEM
Considering A.7eq. ( )AppendixA :
z
P
y
W
y x
W
x
appapp
∂
∂=
∂
∂
∂
∂+
∂
∂
∂
∂µµ
1..C eq
Where:
22
1
∂∂
+
∂∂
=
+= −
y
w
x
w
K n y
app
γ
γγ
τµ
&
&&
There has to be a corresponding relationship between each point in y x , coordinate to
boundary fitted ( )ηξ , system therefore,
( )
( )
( )
( ) y x
y x
y y
x x
,
,
,
,
ηη
ξξ
ηξ
ηξ
=
=
=
=
2..C eqs
x
f
x
f
x
f
∂∂
∂∂
+∂∂
∂∂
=∂∂ η
η
ξ
ξ 3..C eq
y
f
y y
f
∂∂
∂∂
+∂∂
∂∂
=∂∂ η
η
ξ
ξ 4..C eq
Now 1..C eq can be written as:
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 84/113
74
z
P
x
F
x
F
∂∂
=∂
∂+
∂∂ 21
5..C eq
Where:
x
W
F app ∂∂
= µ1 6..C eq
y
W F app ∂
∂= µ2
7..C eq
Applying the same procedure as in 3..C eqs to 5..C eqs :
z
P
y
F
y
F
x
F
x
F
∂∂
=∂∂
∂∂
+∂∂
∂∂
+∂∂
∂∂
+∂∂
∂∂ η
η
ξ
ξ
η
η
ξ
ξ2211 8..C eq
Defining J ′ as:
x y y x J
∂∂
∂∂−
∂∂
∂∂=′ ηξηξ
9..C eq
And multiplying 8..C eq by J ′1
, yields:
∂∂
′=
∂∂
∂∂
+∂∂
∂∂
+∂∂
∂∂
+∂∂
∂∂
′ z
P
J y
F
y
F
x
F
x
F
J
11 2211 η
η
ξ
ξ
η
η
ξ
ξ 10..C eq
According to chain rule:
∂∂
′∂∂+
∂∂
′∂∂+
∂∂
′∂∂+
∂∂
′∂∂+
∂∂
∂∂
′+
∂∂
∂∂
′+
∂∂
∂∂
′+
∂∂
∂∂
′
=
∂∂
′+
∂∂
′∂∂
+
∂∂
′+
∂∂
′∂∂
y J F
x J F
y J F
x J F
F
y J
F
x J
F
y J
F
x J
y J
F
x J
F
y J
F
x J
F
η
η
η
η
ξ
ξ
ξ
ξ
η
η
η
η
ξ
ξ
ξ
ξ
ηξ
η
ξξ
ξ
1111
1111
2121
2121
2121
11..C eq
Equation 11..C eq can be rearranged as:
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 85/113
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 86/113
76
Equation 15.C can be written as:
ξ
ξ
η
ηξ
η
η
ξ
x J
y J
x J
y J x
y
x
y
′=′−=
′−=
′=
16..C eqs
Consider the second bracket of the right hand side of 12..C eq :
∂∂
′∂∂
+
∂∂
′∂∂
+
∂∂
′∂∂
+
∂∂
′∂∂
y J y J F
x J x J F
η
η
ξ
ξ
η
η
ξ
ξ
111121 17..C eq
Now plugging 16..C eqs into it 17..C eq yields:
( ) ( ) ( ) ( ) [ ] [ ] 02121 =+−+−=
∂∂+−
∂∂+
−
∂∂+
∂∂ ηξηξηξηξξηξη
ηξηξ x x F y y F x x F y y F 18..C eq
Therefore 12..C eq reduces to:
∂∂
′+
∂∂
′∂∂
+
∂∂
′+
∂∂
′∂∂
=
∂∂
∂∂+
∂∂
∂∂+
∂∂
∂∂+
∂∂
∂∂
′
y J
F
x J
F
y J
F
x J
F
F
y
F
x
F
y
F
x J
ηη
η
ξξ
ξ
η
η
η
η
ξ
ξ
ξ
ξ
2121
21211
19..C eq
Plugging 19..C eq into 18..C eq , yields:
z
P
J y J
F
x J
F
y J
F
x J
F
∂∂
′=
∂∂
′+
∂∂
′∂∂
+
∂∂
′+
∂∂
′∂∂ 12121 ηη
η
ξξ
ξ 20..C eq
Now we need to write all derivatives in 20..C eq in terms of ηξ , only. So we need to
convert x∂
∂ξ,
y∂∂ξ
, x∂
∂η,
y∂∂η
into derivatives with respect to ηξ , .
Recalling form 2..C eqs :
( )ηξ , x x =
( )ηξ , y y =
( ) y x,ξξ =
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 87/113
77
( ) y x ,ηη =
According to chain rule:
=⇒
∂∂+
∂∂=
∂
∂+
∂
∂=
ηξη
ηξ
ξ
η
η
ξ
ξηξ
ηξd d y y x xdydx
d y
d y
dy
d x
d x
dx
=⇒
−
ηξηξ
ηξd d y y x xdydx
1
21..C eq
And similarly:
=
⇒
∂∂+
∂∂=
∂∂+
∂∂=
dydx
d d
dy y
dx x
d
dy y
dx x
d
y x
y x
ηη
ξξ
ηξ
ηηη
ξξξ
22..C eq
From 21..C eq and 22..C eq we deduce:
1−
=
ηξ
ηξ
ηη
ξξ
y y
x x
y x
y x 23..C eq
Extending 23..C eq results:
−−−
−−
−=
−
−−
=
ξηηξ
ξ
ξηηξ
ξ
ξηηξ
η
ξηηξ
η
ξξ
ηη
ξηηξηηξξ
y x y x
x
y x y x
y y x y x
x
y x y x
y
x y x y
y x y x y x
y x 1 24..C eq
And also 24..C eq in an extend form can be written as:
ξηηξ
ξ
ξηηξ
ξ
ξηηξ
η
ξηηξ
η
η
η
ξ
ξ
y x y x
x
y x y x
y
y x y x
x
y x y x
y
y
x
y
x
−=
−−=
−−=
−=
25..C eqs
Jacobean is defined as:
ξηηξ y x y x J −= 26..C eq
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 88/113
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 89/113
79
Comparing 27..C eqs and 16..C eqs we can say:
ξηηξ y x y x J
J −=′
=1
33..C eq
Utilizing 33..C eq in 32..C eq :
z
P J
J
xW xW x
J
yW yW y
J
xW xW x
J
yW yW y
appapp
appapp
∂∂
=
−+
−−
∂∂
+
−−
−
∂∂
ηξξη
ξ
ξηηξ
ξ
ηξξη
η
ξηηξ
η
µµη
µµξ
34..C eq
Rearranging 34..C eq :
( ) ( )
( ) ( ) z
P J x x y y yW
J x yW
J
x x y yW J
x yW J
app
appapp
appapp
∂∂
=
+−+
∂∂
+
+−+
∂∂
ηξξηξξξξη
ηξξηηηηξ
µµµ
η
µµ
ξ
22
22
35..C eq
Using following notations:
22
22
ξξ
ηξξη
ηη
β
γ
α
x y
x x y y
x y
+=
+=
+=
36..C eqs
Equation 35..C eq will take the form:
( ) ( ) z
P J W W
J W W
J
appapp
∂∂
=
−
∂∂
+
−
∂∂
ξηηξ γβµ
ηγα
µ
ξ 36..C eq
In 36..C eq we need to the transformation for appµ as well. Recalling appµ from 1..C eq
1−+= n y
app K γγ
τµ &
&
22
∂∂
+
∂∂
= y
w
x
wγ&
In order to transfer appµ , we need to transform γ& . According to 28..C eq and 29..C eq
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 90/113
80
J
yW yW
x
W ξηηξ −=
∂∂
37..C eq
J
xW xW
y
W ηξξη −=
∂∂
38..C eq
Substituting 37..C eq and 38..C eq into γ& , we get:
( )ξηηξηξξηξηηξξηηξ x xW W xW xW y yW W yW yW J y
W
x
W 22
1 22222222
2
22
−++−+=
∂
∂+
∂∂
39..C eq
Rearranging 39..C eq :
( ) ( ) ( )( )ξηξηηξξξηηηξ y y x xW W y xW y xW
J y
W
x
W +−+++=
∂∂
+
∂
∂2
1 222222
2
22
40..C eq
Utilizing notations form 36..C eqs into 40..C eq :
( )ηξηξ γβα W W W W J y
W
x
W 2
1 22
2
22
−+=
∂
∂+
∂∂ 41..C eq
Now plugging 41..C eq into 1..C eq :
1−+= n yapp K γ
γ
τµ &
&
Where:
( )ηξηξ γβαγ W W W W J
21 22
2 −+=& 42..C eq
So from 36..C eq and 42..C eq :
( ) ( ) z
P J W W
J W W
J
appapp
∂∂=
−
∂∂+
−
∂∂
ξηηξ γβµ
ηγα
µ
ξ 43..C eq
Where:
1−+= n yapp K γ
γ
τµ &
&
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 91/113
81
( )ηξηξ γβαγ W W W W J
21 22
2 −+=&
22ηηα x y +=
ηξξηγ x x y y +=
22ξξβ x y +=
ξηηξ y x y x J −=
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 92/113
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 93/113
83
Each term on the right hand side of 6.. Deq can be extended to:
+
≈
++ ji
ap p
ji
ap p
ji
ap p
J J J ,,1,
2
1 2
1 µαµαµα 7.. Deq
and
+
≈
−+− ji
ap p
ji
ap p
ji
ap p
J J J ,1,,
2
1 2
1 µαµαµα 8.. Deq
In 6.. Deq :
ji ji
ji
W W W
,,1
,2
1−≈
∂∂
++ξ
9.. Deq
And also
ji ji
ji
W W W
,1,
,2
1 −
+−
−≈
∂∂ξ
10.. Deq
Therefore:
( )
( )−
+
−−
+
≈
∂∂
∂∂
−−
++
ji ji
ji
ap p
ji
ap p
ji ji
ji
ap p
ji
ap p
ji
ap p
W W J J
W W J J
W
J
,1,
,1,
,,1
,,1,2
1
µαµα
µαµα
ξ
µα
ξ
11.. Deq
Similar to 11.. Deq , η derivative in 1.. Deq can be approximated as:
( )
( )
−
+
−
−
+
≈
∂∂
∂∂
−−
++
1,,
1,,
,1,
,1,,2
1
ji ji
ji
app
ji
app
ji ji
ji
ap p
ji
ap p
ji
ap p
W W J J
W W J J
W
J
µβµβ
µβµβ
η
µβ
η
12.. Deq
For the mixed derivation at node (i,j), we have:
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 94/113
84
( ) ( )
−
−−
≈
∂∂
∂∂
−−+−
−
−+++
+
1,11,1
,1
.
1,11,1
,1
.
,
.
4
1 ji ji
ji
ji ji
ji ji
W W J
W W J
W
J
γµγγµγ
η
γµγ
ξ 13.. Deq
( ) ( )
−−
−+−
≈
∂∂
∂∂
−−+−
−+++
1,1,1
1,
,11,1
1,,
114
1 ji ji
ji
app ji ji
ji
app
ji
ap pW W
J W W
J
W
J
µγµγ
ξ
µγ
η
14.. Deq
Plugging 14.11.. D Deqs − into 1.. Deq :
z
P J
W
J
W
J
W
J
W
J
appappappapp
∂∂=
∂∂
∂∂−
∂∂
∂∂+
∂∂
∂∂−
∂∂
∂∂
ξ
µγ
ηη
µβ
ηη
µγ
ξξ
µα
ξ
( )
( )
( ) ( ) +
−
−−
−
−
+
−−
+
−−+−−
−++++
−−
++
1,11,1
,1
1,11,1
,1
,1,
,1,
,,1
,,1
2
1
2
1
ji ji
ji
ap p
ji ji
ji
ap p
ji ji
ji
ap p
ji
ap p
ji ji
ji
ap p
ji
ap p
W W J
W W J
W W J J
W W J J
µγµγ
µαµα
µαµα
( )
( )
( ) ( ) z
P J W W
J W W
J
W W J J
W W
J J
ji ji ji
ji
ap p ji ji
ji
ap p
ji ji
ji
ap p
ji
ap p
ji ji
ji
ap p
ji
ap p
∂∂
=
−−
−+−
−
−
+
−−
+
−−+−
−+++
−−
++
,1,1,1
1,
,11,1
1,
1,,
1,,
,1,
,1,
114
1
2
1
µγµγ
µβµβ
µβµβ
15.. Deq
After some arrangements:
( )
−
−
−
−
−
−
−
−
−+
−+
1,,,1,
,1,,,1
,2
1
ji
ap p
ji
ap p
ji
ap p
ji
ap p
ji
ap p
ji
ap p
ji
ap p
ji
ap p ji
J J J J
J J J J W
µβµβµβµβ
µαµαµαµα
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 95/113
85
( )
−
−
−
−+−+
1,,1
1,14
1
ji
app
ji
ap p ji
J J W
µγµγ
( )
−
− −
−−
1,,
1,2
1
ji
app
ji
app ji
J J W
µβµβ
( )
−
−
−−
− ji
app
ji
app
ji J J
W
,1,
,12
1 µαµα
( )
−
−
−
+−+−
1,,1
1,14
1
ji
app
ji
app
ji J J
W µγµγ
( )
−
−
−
++
ji
app
ji
app
ji J J
W
,1,
1,2
1 µβµβ
( )
−
−
−
++
ji
app
ji
app
ji J J
W
,,1
,12
1 µαµα
( )
+
−
−−−−
1,,1
1,14
1
ji
app
ji
app
ji J J
W µγµγ
( ) 04
1,
1,,1
1,1 =∂∂−
+
−
++++
z
P J
J J W ji
ji
app
ji
app
ji
µγµγ 16.. Deq
Rearrangement and multiplying two sides of 16.. Deq by (-1):
( )
+
+
+
+
+
−+
−+
1,1,
,1,1,,
,
2
1
2
1
2
1
2
1
ji
ap p
ji
ap p
ji
ap p
ji
ap p
ji
ap p
ji
ap p ji
J J
J J J J W
µβµβ
µαµαµβµα
( )
+
−
−+−+
1,,1
1,14
1
ji
ap p
ji
ap p ji
J J W
µγµγ
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 96/113
86
( )
+
−
−−
1,,
1,2
1
ji
app
ji
app
ji J J
W µβµβ
( )
+
−
−−
ji
app
ji
app
ji J J
W
,1,
,12
1 µαµα
( )
+
−
+−+−
1,,1
1,12
1
ji
app
ji
app
ji J J
W µγµγ
( )
+
−
++
ji
app
ji
app
ji J J
W
,1,
1,2
1 µβµβ
( )
+
−
++
ji
app
ji
app
ji J J
W
,,1
,12
1 µαµα
( )
+
−
−−−−
1,,1
1,14
1
ji
app
ji
app
ji J J
W µγµγ
( ) 04
1,
1,,1
1,1 =∂∂
+
+
−
++++
z
P J
J J W ji
ji
app
ji
app
ji
µγµγ 16.. Deq
Denoting101 A A −
:
0101,191,18,171,6
1,15,141,31,12,1
=−−−−−
−−−−
++−−++
+−−−−+
AW AW AW AW A
W AW AW AW AW A
ji ji ji ji
ji ji ji ji ji
16.. Deq
Where:
1,1,
,1,1,,
1
2
1
2
1
2
1
2
1
−+
−+
+
+
+
+
+
=
ji
app
ji
app
ji
app
ji
app
ji
app
ji
app
J J
J J J J
A
µβµβ
µαµαµβµα
+
=
−+ 1,,1
24
1
ji
app
ji
ap p
J J A
µγµγ
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 97/113
87
+
=
−1,,
32
1
ji
app
ji
app
J J A
µβµβ
+
=
− ji
app
ji
app
J J A
,1,
42
1 µαµα
+
=
+− 1,,1
54
1
ji
app
ji
app
J J A
µγµγ
+
=
+ ji
app
ji
app
J J A
,1,
62
1 µβµβ
+
=
+ ji
app
ji
app
J J A
,,1
72
1 µαµα
+
=
−− 1,,1
84
1
ji
app
ji
app
J J A
µγµγ
+
=
++ 1,,1
94
1
ji
app
ji
app
J J A
µγµγ
z
P J A ji ∂
∂−= ,10
Applying Relaxation Factor:
Adding ji ji W W ,, − to the right hand side of 16.. Deq :
{
}101,191,18,171,6
1,15,141,31,12
1
,,,
1
AW AW AW AW A
W AW AW AW A A
W W W
ji ji ji ji
ji ji ji ji ji ji ji
+++++
++++−=
++−−++
+−−−−+
17.. Deq
Now jiW ,− taking into the braces:
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 98/113
88
{
}10,11,191,18,171,6
1,15,141,31,121
,,
1
AW AW AW AW AW A
W AW AW AW A A
W W
ji ji ji ji ji
ji ji ji ji ji ji
+−++++
++++=
++−−++
+−−−−+
18.. Deq
Now using relaxation factor we will have:
{
}10,11,191,18,171,6
1,15,141,31,12
1
,,
AW AW AW AW AW A
W AW AW AW A A
W W
ji ji ji ji ji
ji ji ji ji ji ji
+−++++
++++=
++−−++
+−−−−+ω
19.. Deq
Calculating Relaxation Factor
Following Azouz [3]:
J
appµα
ϕ =1 20.. Deq
J
appµβϕ =2 21.. Deq
( )
( )
−
−
−
=
−
=
−+
−+
1,1,
,1,1
3
5.0
5.0
ji
app
ji
app
ji
app
ji
appappapp
J J
J J J J
µγµγ
µαµαµγµαϕ
ηξ
22.. Deq
( )
( )
−
−
−
=
−
=
−+
−+
ji
app
ji
app
ji
app
ji
appappapp
J J
J J J J
,1,1
1,1,
4
5.0
5.0
µγµγ
µβµβµγµβϕ
ξη
23.. Deq
+−+
+−
+=
1cos4
1cos4
2
1 24
22
23
21
21 N M J
πϕϕ
πϕϕ
ϕϕρ 24.. Deq
If ( ) 042
32
1 ≥−ϕϕ , then:
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 99/113
89
211
2
J ρ
ω
−+= 25.. Deq
Otherwise,
211
2
J ρ
ω
++= 26.. Deq
Calculating Relaxation Factor in Cartesian Coordinate System
Following Azouz (1994):
ξηηξ
ξξ
ηξξη
ηη
β
γ
α
y x y x J
x y
x x y y
x y
−=
+=
+=
+=
22
22
27.. Deq
In this system, since there is not any transformation it can be said:
ξ
η
==
x
y 28.. Deq
As a result:
1
0
====
ξη
ξη
x y
y x 29.. Deq
So,
101
110
000
101
22
22
=−=−=
=+=+=
=+=+=
=+=+=
ξηηξ
ξξ
ηξξη
ηη
β
γ
α
y x y x J
x y
x x y y
x y
30.. Deq
( )
( ) app
appapp
J µ
µµαϕ ===
1
11 31.. Deq
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 100/113
90
( )
( ) app
appapp
J µ
µµβϕ ===
1
12 32.. Deq
( )
( )
( )
( )
( ) x
J J
app
appappappapp
∂∂
==
−
=
−
=
µµ
µµµγµαϕ
ξ
ηξηξ1
0
1
13
33.. Deq
( )
( )
( )
( )
( ) y
J J
app
appappappapp
∂∂==
−
=
−
=
µµ
µµµγµβϕ
η
ξηξη1
0
1
14
34.. Deq
+−+
+−
+=
1cos4
1cos4
2
1 24
22
23
21
21 N M J
πϕϕ
πϕϕ
ϕϕρ 35.. Deq
If ( ) 04 23
21 ≥−ϕϕ , then:
211
2
J ρ
ω
−+= 36.. Deq
Otherwise,
211
2
J ρ
ω
++= 37.. Deq
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 101/113
91
APPENDIX E
ALGEBRAIC GEOMETRY TRANSFORMATION
Algebraic Transformation of an Eccentric Annulus
Considering Fig3.8, Each point can be defined by a radius and an angle.
Fig.E.1 Determination of an arbitrary grid point
According to Fig.E.1 :
( ) ( )[ ]112
1l R ol Ro Roj −+−= 1.. E eq
From Fig.E.1 :
( )1
1 −
−+−=
JM
Rie Ro j JM l 2.. E eq
l
p
d
Ri ee
Ro Roj
C m
C j
C 1
rθ
Ro
Ri
Roj
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 102/113
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 103/113
93
Plugging 8.. E eqs into 7.. E eq :
( ) ( ) 222cossin oj j j j Rer r =−+ θθ 9.. E eq
Or,
θθ CoseSine Rr j joj j +−= 222 10.. E eq
Since the circle is decided into 1− IM divisions in tangential direction , where each
division will be represented by θ∆ , and half of the circle is used:
1−=∆
IM
πθ 11.. E eq
So θ can be calculated as:
( )1−∆= iθθ 12.. E eq
Substituting θ∆ from 11.. E eq
( )1
1
−−
= IM
iπθ 13.. E eq
Substituting 5.. E eq and 6.. E eq ,into 10.. E eq :
( )( )( )
( )( )
( ) ( )( )
( )
−−
−−
+
−−
−
−−
−
−−−=
1
1
1
1
1
1
1
1
1
222
IM
iCos
JM
je
IM
iSin
JM
je
JM
Ri Ro j JM Ror j
ππ
14.. E eq
Substituting 13.. E eq and 14.. E eq , into 8.. E eqs :
( ) ( )( )
( )( )
( )( ) ( )
( )( ) ( )
( ) ( )( )
( )( )
( )( ) ( )
( )( ) ( )
1
1
1
1
1
1
1
1
1
1
1,
1
1
1
1
1
1
1
1
1
1
1,
222
222
−−
−−
−−+
−−
−
−−
−
−−−=
−−
−−
−−+
−−
−
−−
−
−−−=
IM
iCos
IM
iCos
JM
je
IM
iSin
JM
je
JM
R i Ro j JM Ro ji y
IM
iSin
IM
iCos
JM
je
IM
iSin
JM
je
JM
R i Ro j JM Ro ji x
πππ
πππ
15.. E eq
Where:
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 104/113
94
JM j IM i <<<< 1,1
ji, : Grid points in tangential and radial direction respectively
1− IM : Number of divisions in tangential direction.
1− JM : Number of divisions in radial direction.
It should be mentioned that 15.. E eq is valid only for the half of the domain, and by
replacing π by π2 it can be used to transform a whole eccentric annulus from real
domain to a computational domain.
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 105/113
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 106/113
96
AQBDPC A A A A =+++ 4321 3.. F eq
From 2.. F eq , 3.. F eq :
AQBDPC
W
Q
ji
ji 4
,
, = 4.. F eq
Now, we need to find the area of AQBDPC .
Fig.F.2
A
B
C
D
P
Q
+1, j
i,j
+1, j+1
-1, j
+1, j-1
-1, , j-1
-1,j+1
, , j+1
, , j-1
A1
A2
A3
A3
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 107/113
97
Fig.F.3
According to FigF.3:
5611 A ACDO ABO AQBDPC +−−= ∆∆
5.. F eq
And also from the same figure:
∆−= CDOCPDO A 226 6.. F eq
∆−= ABO AQBO A 335
7.. F eq
Plugging, 6.. F eq , 7.. F eq into 5.. F eq :
∆∆∆∆−++−−= ABO AQBOCDOCPDOCDO ABO AQBDPC 332211 8.. F eq
From the mathematics books:
D
B
A
C
O1
A5
A6
O2
O3
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 108/113
98
Fig.F.4
( )( ) ( )( )323132313232
3131
2
1det
2
1 x x y y y y x x
y y x x y y x x
ABC −−−−−=
−−−−=
∆ 9.. F eq
Applying 9.. F eq to 8.. F eq :
( )( ) ( ) ( ) B A BO B A BO x x y y y y x x ABO −−−−−=∆
1112
1 10.. F eq
Substituting the coordinate of each point in 10.. F eq :
( ) ( ) ( ) ( )1,11,11,11,11,11,11 002
1+++−+++++−++
∆−−−−−= ji ji ji ji ji ji x x y y y x ABO 11.. F eq
Simplifying 11.. F eq :
( ) ( ) ( ) ( )1,11,11,11,11,11,112
1+++−+++++−++
∆−+−−= ji ji ji ji ji ji x x y y y x ABO 12.. F eq
Similarly for calculating the area of ∆CDO2 :
( )( ) ( )( ) DC DO DC DO x x y y y y x xCDO −−−−−=∆
2222
1 13.. F eq
( ) ( ) ( ) ( )1,11,11,111,11,11,12 021 −+−−−+−−+−−−+∆ −−−−−= ji ji ji j ji ji ji x x ye y y xCDO 14.. F eq
( ) ( ) ( ) ( )1,11,11,111,11,11,122
1−+−−−+−−+−−−+
∆−−−−−= ji ji ji j ji ji ji x x ye y y xCDO 15.. F eq
Substituting for 1− je from 10.. E eq , Appendix E:
A
B
C
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 109/113
99
( )( ) ( )
( )1
11,1 −
−+−−−+−= −−
JM
Rie Ro j JM R o Ree jo j 16.. F eq
Or,
( ) ( )( )11
1,1 −−++−−+−= −−
JM R ie Ro j JM R o Ree jo j 17.. F eq
Substituting for 1, − jo R from 10.. E eq , Appendix E:
( )( )
( )1
11, −
−+−−=−
JM
Ri R o j JM R o R jo 18.. F eq
Substituting 18.. F eq into 17.. F eq :
( ) ( )( )
( ) ( )( )11
11
1 −−++−−+
−−+−+−=−
JM Rie Ro j JM Ro
JM Ri Ro j JM Roee j 19.. F eq
Or,
( ) ( )( )
( ) ( )( )1
1
1
11 −
−++−−
−−+−
+=− JM
Rie Ro j JM
JM
Ri Ro j JM ee j 20.. F eq
Or,
( ) ( )( )1
11 −
+−−−+−+=− JM
Ri
e Ro
Ri
Ro
j JM
ee j 21.. F eq
Simplifying 21.. F eq
( )( )1
11 −
+−−=−
JM
j JM eee j 22.. F eq
Or,
( )
( )1
21
−
−=−
JM
jee j 23.. F eq
Substituting 23.. F eq into 15.. F eq :
( ) ( ) ( ) ( )1,11,11,111,11,11,122
1−+−−−+−−+−−−+
∆−−−−−= ji ji ji j ji ji ji x x ye y y xCDO
Or,
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 110/113
100
( ) ( ) ( )( )
( )1,11,11,11,11,11,121
2
2
1−+−−−+−+−−−+
∆−
−
−−
−−−= ji ji ji ji ji ji x x y JM
je y y xCDO 24.. F eq
After simplification:
( ) ( ) ( )( )
( )1,11,11,11,11,11,121
2
2
1−+−−−+−+−−−+
∆−
−
−−
−−−== ji ji ji ji ji ji x x y JM
je y y xCDO 25.. F eq
Calculating CPDO2 :
We know that:
( )2
2
1,
2
−= jo RCPDO
α 26.. F eq
From Sinus law for calculating the area of a triangle:
( ) αsin2
1 21,2 −
∆= jo RCDO 27.. F eq
As a result we can get:
( )
=
−
∆
21,
22sin
jo R
CDO Arcα 28.. F eq
Recalling for 1, − jo R from 10.. E eq , Appendix E:
( )( )
( )1
11, −
−+−−=−
JM
Ri R o j JM R o R jo 29.. F eq
Substituting 29.. F eq and 28.. F eq into 26.. F eq :
( )( )
( ) ( )( )( )
−−+−−
−
−+−−=
∆
2
2
2
2
11
2sin
1
1
2
1
JM Ri Ro j JM Ro
CDO Arc
JM
Ri Ro j JM RoCPDO 30.. F eq
Similarly, we can calculate∆CDO1 :
( )( ) ( )( ) DC DO DC DO x x y y y y x xCDO −−−−−=∆
1112
1 31.. F eq
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 111/113
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 112/113
102
( ) ( )( )
( )1,11,11,11,11,11,1312
1+++−+++++−++
∆−
−
−−−−= ji ji ji ji ji ji x x y
JM
je y y x ABO 39.. F eq
To calculate AQBO3 , similar procedure for calculating CPDO2 can be used as:
We know that:
( )2
2
1,
3
+= jo R AQBO
β 40.. F eq
From Sinus law for calculating the area of a triangle:
( )( )
=⇒=
+
∆
+
∆
2
1,
32
1,3
2sinsin
2
1
jo
jo R
ABO Arc R ABO ββ 41.. F eq
Or,
( )2
2
1,
3
+= jo R AQBO
β 42.. F eq
As a result:
( )
=
+
∆
2
1,
32sin
jo R
ABO Arcβ 43.. F eq
Recalling for 1, + jo R from 10.. E eq , Appendix E:
( )( )
( )1
11, −
−−−−=+
JM
Ri Ro j JM Ro R jo 44.. F eq
Substituting 44.. F eq and 43.. F eq into 42.. F eq :
( )( )( ) ( )( ) ( )
( )
−
−+−−
−
−−−−=
∆
2
3
2
3
1
1
2sin
1
1
2
1
JM
R i Ro j JM Ro
ABO Arc
JM
Ri R o j JM R o AQBO 45.. F eq
And finally from 4.. F eq , 3.. F eq , 12.. F eq , 25.. F eq , 30.. F eq , 32.. F eq , 39.. F eq , 45.. F eq
8/13/2019 Flow in Annulus
http://slidepdf.com/reader/full/flow-in-annulus 113/113
AQBDPC W
Q ji
ji2
,, = 46.. F eq
Where:
∆∆∆∆
−++−−= ABO AQBOCDOCPDOCDO ABO AQBDPC 332211
( ) ( ) ( ) ( )1,11,11,11,11,11,112
1+++−+++++−++
∆−+−−= ji ji ji ji ji ji x x y y y x ABO
( ) ( ) ( ) ( )1,11,11,11,11,11,112
1−+−−−+−+−−−+
∆−+−−= ji ji ji ji ji ji x x y y y xCDO
( )( )
( ) ( )( )( )
−
−+−−
−
−+−−=
∆
2
2
2
2
11
2sin
1
1
2
1
JM R i Ro j JM R o
CDO Arc
JM
R i Ro j JM R oCPDO
( ) ( ) ( )( )
( )1,11,11,11,11,11,121
2
2
1−+−−−+−+−−−+
∆−
−
−−
−−−== ji ji ji ji ji ji x x y JM
je y y xCDO
( )( )( ) ( )( ) ( )
( )
−
−+−−
−
−−−−=
∆
2
3
2
3
1
1
2sin
1
1
2
1
JM
R i Ro j JM Ro
ABO Arc
JM
Ri R o j JM R o AQBO 7.16.3.eq
( ) ( )( )
( )1,11,11,11,11,11,1312
1+++−+++++−++
∆−
−
−−−−= ji ji ji ji ji ji x x y
JM
je y y x ABO 8.16.3.eq