Page 1
Lecture 1-b
Catenary Risers: Global Analysis
Dynamic Problem
equations and time scales
Celso P. Pesce
Professor of Mechanical Sciences
PhD in Ocean Engineering, MSc Marine Hydrodynamics, Naval Architect
[email protected]
LMO - Offshore Mechanics Laboratory
Escola Politécnica
University of São Paulo
Brazil
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Catenary lines
junta
flexível
riser de aço
bóia
intermediária
poita
enrijecedores de
flexão
TLPFPSO
flutuadores
restritor de
curvatura
flexible joint
Steel catenary riser
Bending restrictors
Subsurface buoyFloaters
Bending stiffener
Lazy-wave riser
Weight anchor
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Qv
Qw
bn
P’v
w
t=u
T
Mu
Mv
Mw
2
2
2
2
2
2
2
2
2
2
2
2
)(KQMMM
)(KQMMM
)(KMMM
)(fQTQ
)(fTQQ
)(fQQT
tIt
s
tIt
s
tIt
s
t
wmt
s
t
vmt
s
t
umt
s
w
wwwvuvvu
w
v
vvvwwuuw
v
u
uuuvwwv
u
wuvv
w
vwuw
v
uvwwv
General Kirshoff-Clebsh-Love Equations
(KCL equations)
Curved bars – large displacements, small deformations
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The planar static problem
with:
)(cos
)(sin
scqf
scqf
nn
tt
(s)
y
xi
j
k
uv
. 0
0
0
Qds
dM
fds
dT
ds
dQ
fds
dQ
ds
dT
n
t
Static forces due to
current
)();( scsc nt
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Perturbations around the
static equilibrium
configuration
2
2
2
2
cosΤQΤQ
sinQQ+TΤ
t
umqc
sds
d
s
t
umqc
sds
d
s
nnn
ttt
Hang-off
boundary-
layer
TDP
boundary-
layer (s,t)n t
yx
),()(),Q(
),()(),(Τ
),()(),(ε
),()(),(
tssQts
tssTts
tsests
tssts
eds
du
s
u
tssds
du
s
u
nt
tn
),())(1(
Kinematic relations
The planar dynamic problem
Oscillating hydrodynamic
forces
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2
2
2
2
Q
cos
Q+T
sin
t
um
sds
d
s
qcds
dT
s
Q
t
um
sds
d
s
qcds
dQ
s
T
nn
n
tt
t
Separating static and dynamic parts:
Static equilibrium,
tangential direction
Static equilibrium,
normal direction
0
0
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Linearized Dynamic Equations
Negleting second-order terms
Two dynamic equilibrium equations,
linearized around the static
equilibrium configurations
2
2
2
2
+
t
umT
s
ds
dQ
s
t
umQ
s
ds
dT
s
nn
tt
2
2
2
2
+
t
umT
sds
dQ
s
t
umQ
sds
dT
s
nn
tt
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Kinematic relations
Constitutive equations
Negleting
bending stiffness
effects:
gSSq
uuqtsEAets
ds
du
s
u
eds
du
s
u
t
umT
sds
d
t
um
ds
dT
s
ifoaf
ntf
tn
nt
nn
tt
)cossin(),(),(
1
2
2
2
2
Linearized Dynamic Equations: neglecting bending stiffness
Two dynamic equilibrium equations,
linearized around the static
equilibrium configurations
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)(sin)()(2
1)(
)(cos)()(2
1)(
2
2
sCsUsDUsc
sCsUsDUsc
Dan
Tat
Mean current hydrodynamic forces
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nn
n
tt
t
Ut
u
Ut
u
wsinv
wcosv
),(),(),( tststs invisc
ttsU
t
umts
ts
nta
in
n
in
t
wcos)(),(
0),(
2
2
Oscillating hydrodynamic forces
Parcelas dinâmicas das forças devido à correnteza e às ondas:
Relative velocity
components to the
flow
Viscous parcels
Inertial parcels
nnn
naD
visc
n
tnt
taT
visc
t
s
usU
t
usUDCts
s
usU
t
usUDCts
wcos)(sin)(2vsinal2
1),(
wsin)(cos)(2vsinal2
1),(
Gravitational waves
velocity filed
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s
cEI
ds
dEIQ
sEI
s
tscds
dEItsEI
2
2MQ
e
),(),(M
The dynamic equation in the normal direction may be written:
From the classic linear constituve equations:
The bending stiffness effect
2
2
2
2
cosT
Tt
umqc
sds
dEI
ssEI n
nn
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Second-order
term
The nondimensional dynamic equation in the normal direction reads:
Defining:
L
T
EI
0
0
0T
q
Flexural lenght at TDP
Static curvature
at TDP
amm
Tc
tL
ct
00
0ˆ
Transversal wave celerity
due to geometric stiffness,
at TDP
2
2
02
2
22
ˆ
ˆcosˆˆˆ
ˆ
ˆ
ˆˆ
ˆˆˆ
ˆ
ˆ
t
uc
ssd
d
ss
nnn
The bending stiffness effect
Small length
parameter
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Neglecting secon-order terms (bending stiffness):
Rigid risers (Steel): )10( 2O
Flexible risers: )10( 3 O
))(1(ˆ
ˆcosˆˆˆ
ˆ
ˆˆˆ 2
2
2
0
O
t
uc
s
nnn
The bending stiffness effect
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Time scales
)()(
sT
EIs
Wave celerity associated to
geometric rigidity
Wave celerity associated to
axial stiffness
a
i
f
i
i
f
i
g
g
c
Lt
ct
c
Lt
ct
c
Lt
5
)(
)(
4
)(
)(
3
2
1
Local flexural length
Wave celerity associated to
bending stiffness
m
EAc
mm
EIc
mm
Tc
a
a
i
f
i
f
a
g
)(
2
)(
)(
)(
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Model similarity and nondimensional group
[.
Number Symbol and definition Representation
Froude NumberDynamic motion in
waves
Reynolds NumberViscous forces
Strouhal NumberVortex shedding
frequency
Keulegan-
Carpenter Number
Inertial forces vs.
drag forces
Structural
Damping
Linear structural
damping
Reduced VelocityNormalized
velocity in VIV
Reduced Shedding
Frequency
Vortex shedding
normalized
frequency
Reduced MassRiser mass vs.
displaced mass
Added MassAdded mass vs.
riser mass
Bending Stiffness
Bending vs.
geometrical
stiffness
Axial Stiffness
Axial vs.
geometrical
stiffness
Soil Stiffness
Soil vs. bending
and geometrical
stiffness
gL
ArF
UDRe
U
Df stS
D
A2KC
cc
c
Df
UV
nr
rnn
ss V
Df
U
f
ff tt SS
Dm
mm
m
ma a
T
EI
LLK
f
f
1
T
EAKa
2T
EIkK s
s Rateiro et al
ISOPE2012
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Summary
• The global dynamics is governed by the geometric stiffness or
catenary stiffness.
• Bending stiffness effetcs are importante at the extremities and
TDP, or for high-order vibration modes for which the mode
vibrattion length is of same order of the local flexural length.
• There are several time scales that govern the overall dynamics
of a riser.
• A large nondimensional parameters group govern the overall
riser dynamics
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Acknowledgements
TPN
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FLUID-STRUCTURE INTERACTION AND
OFFSHORE MECHANICS LABORATORY