Transient thermal cycling analysis
of the flowline system illustrates that if the flowline displaces naturally at
crucial seabed features, the initial flowline response is dominated by
transient cumulative expansion. During this condition, both ends of the
flowline expand independently and increase overall end expansions. A steeply
sloping seabed - a contributing component of this phenomenon - inherently
causes the flowline to move down-slope, with gravity imposing tension to a
hanging flowline.
Recent case study examines ways of
improving the stability of high-pressure/high-temperature flowlines
Increased deepwater development over
the last decade, together with industry monitoring of high pressure/high
temperature (HP/HT) flowlines, reveals the critical nature of global stability
in the management of flowline buckling and axial stability of these systems.
Global stability is one of the most
important design considerations for a flowline system. This concern represents
the potential for a flowline to move either axially along its length, laterally
from its installed condition, or vertically causing flowline upheaval.
Large compressive forces induced on
a flowline system once operational causes this phenomenon.
Contributing factors
to this phenomenon include seabed terrain, boundary conditions, and operating
strategy.
With more than 25,000 mi (40,234 km)
of pipeline in
the Gulf of Mexico alone, global buckling and axial stability of production
flowline systems in water depths between 3,000 ft to 10,000 ft (914 m to 3,048
m) presents an industrywide concern for flowline integrity.
Short flowline systems, generally in
a range of 3 to 5 mi (4.8 to 8 km) in length, with the complexity of HP/HT
conditions, can translate axially or "walk" as a result of normal
operational start-up and shut-down.
More recently, however, flowline
systems which incorporate wet insulation and which have comparatively low
specific gravity also show a high propensity to walk, even for systems 15 to 20
mi (24 to 32 km) long. INTECSEA has completed a case study on these deepwater systems,
identifying specific design aspects of wet-insulated flowline axial stability
and associated analysis, and suggesting mitigation options.
Flowline/prpefine systems installed
on a steeply sloping seabed compound the problems and underscore industry
resolve to remedy mese issues. Fmite element analysis of wet-insulated systems
on steep slopes helps quantify the impact of cyclic thermal and pressure
loading on a given flowline.
System impacts
The impacts of deepwater buckling and
upheaval on deepwater
pipelines and flowlines can be significant, including:
- Significant cumulative end expansions greater than 20 ft (6 m) can occur until a system reaches a point of stability
- Flowline system response is characterized by interaction of the seabed slope, flowline expansion, lateral displacement, and effect of the thermal/pressure grathent and thermal cycling
- Selection of a nondirect or somewhat "meandering" flowline route, combined with full-scale, three-dimensional finite element modeling, can mitigate significant end expansions
- Most favorable routing for a deepwater flowline system design may challenge developers, as some seabed features are not avoided easily and can impose significant cost increases on a project
- Flow assurance performance requires that many flowline systems have good thermal properties, or low U-value; i.e., overall heat transfer coefficient Thermal insulation applied on the outside of the flowline can facilitate this performance
- A common system configuration uses wet insulation applied on the outside of the flowline and exposed to the marine environment A single or multilayer coating system of five to seven layers is common
- Low specific gravities of systems can result in a low flowline submerged weight and, consequently, low axial frictional resistance
- Project terrain combined with low systemspecific gravity, and typical production temperature and pressure conditions makes the flowline system susceptible to global lateral buckling as well as axial creep.
The INTECSEA case study addresses
these, given the following flowline parameters and conditions: A wet-insulated
production flowline system (D/t-17, inlet temperature = 200° F/93° C ) routed
across an area of steep slope with a product-filled specific gravity of 1.5 and
approximately 20 mi ) in length.
Problem overview
The industry has several deepwater flowline systems
routed across challenging seabed features with seabed slopes ranging from 5° to
approximately 40°. Notable projects that have negotiated such features include:
- BP's Atlantis project over the Sigsbee Escarpment in the Gulf of Mexico
- Norske Shell's Ormen Lange project over the outer continental shelf in the North Sea
- Medgaz - developed by a five-company consortium - across the Mediterranean Sea from Africa to Europe
- Gazprom/Eni Blue Stream across the Black Sea.
Low-pressure and low-temperature
flowlines or export pipelines are
comparatively easy to manage because of lower axial force.
A long HP/HT flowline system - fully
restrained axially rather than a short flowline - experiences end-expansion and
potential for high stresses resulting from lateral displacement at natural
seabed features.
In contrast, a partially restrained
system - where available seabed friction resistance is not sufficient to
balance the compressive force in the flowline - encounters design complexities.
Aspects of this system include large transient cumulative expansion and a propensity
for the entire system to translate gradually from one end - hot or cold - to
the other end - hot or cold - after each cootdown/restart cycle, causing the
walking phenomenon.
While walking normally is associated
with short flowlines, wet insulated systems ranging up to 20 mi (32 km) long
also have these issues. This primarily results from lateral buckles -
engineered or natural response - that separate flowline response on either end.
In effect, the flowline behaves like a partially restrained system similar to a
short flowline.
Analysis of such a system on a flat
seabed - including effects of sloped seabed or riser-bottom tension - is a
common design approach to quantify flowline walking behavior. Modeling provides
a time-efficient solution convergence and reduced computation time and cost.
Limitations to such modeling
techniques, however, include seabed undulations, potential flowline spans,
irregular bathymetry, and narrow opportunities to identify true flowline
response. Selection of the most appropriate design and mitigation requirements
is thus limited as well.
For the case study operating
conditions, the system is prone to lateral buckling because the compressive
force of the flowline is higher than the critical buckling initiation force.
The associated flowline route topography is a typical seabed phenomenon in deepwater areas with average
grathents ranging from 5° to 10° over a distance of 1 to 3 mi (1.6 to 4.8 km).
Designers can apply a staged
approach to assess flowline parameters, with the initial step taking an
analytical solution. An initial finite element analysis using two-dimensional
finite element modeling, followed with detailed three-dimensional finite
element modeling of the actual flowline route, is preferred.
Flowline analysis finite element
software (ANSYS) follows in a sequence of load steps, beginning with an as-laid
or empty condition and proceeding toward flooded, hydrotest, and operating
conditions. The computed analysis includes seabed and flowline profiles, spans,
stresses/strains, axial forces, and flowline displacements.
In the case study, water depth
ranged between 200 ft (61 m) at the shallow end and 2,500 ft (762 m) on the
deep end. The route also had three curves along its length. The average seabed
grathent was approximately 8° to 10° across a 3-mi (4.8 km) slope, with the
maximum grathent of approximately 20° near the top of the slope.
Preliminary analysis
The analytical solution shows end
expansions of 25 ft and 16 ft (7.6 m and 4.9 m) on hot and cold ends,
respectively. The two-dimensional analysis shows end expansion of 12 ft and 3
ft (3.65 m and 0.9 m) on hot and cold ends, respectively. The two-dimensional
analysis shows that uncontrolled lateral displacement would overstress the pipeline.
Following these preliminary
assessments, with its own limitations on predicting the true flowline response,
INTECSEA created a full three-dimensional finite element model that includes pipeline route bathymetry
and route curves.
This model provides improved global
and local predictions of flowline response and associated stresses, expansions.
The model also includes pipeline route
lay radii, or curves, ranging from 5,000 to 8,000 ft (1,524 to 2,438 m).
More realistic predictions for end
displacements are approximately 6 ft and 3 ft (1.8 m and 0.9 m) at the hot and
cold ends. Hot-end expansion, compared to two-dimensional assessments, is
nearly 50% lower, whereas the cold-end expansion remains more or less
unchanged.
Axial force reductions from the
previous analysis result from more locations or instances of lateral flowline
displacements. This analysis shows a maximum lateral displacement of
approximately 40 ft (12 m). These lateral displacements are acceptable because
the flowline is not near seabed features that would contribute to its lateral
instability.
Reduced stress levels at the
displaced flowline sections were confirmed with a local buckling check, per
DNV-OS-FlOl. The local buckling unity check along the entire flowline length
was within the acceptable limit
Seabed intervention
To evaluate the impact of engineered
initiation sites for lateral displacement, INTECSEA included simulated
sleepers, orpre-laid pipes, which facilitate flowline displacement. End
displacements are 6 ft at hot end and 3 ft at cold end, as predicted by the 3D
assessment without pre-installed initiation sites.
The study examined the axial force
and lateral displacement along the flowline length. The artificial displacement
units induce the flowline to displace at 15 locations; 11 of them similar to
the natural displacement locations seen in the previous analysis. These
displacements indicate pre-installed sites are not required as long as the
flowline displaces naturally.
In some instances, however,
intervention systems may be installed to facilitate expected flowline response,
as non-engineered lateral displacement may overstress the flowline. A maximum
lateral displacement of approximately 35 ft (10.6 m) is observed, and maximum
lateral displacements within 5 mi (8 km) from the hot end range from 25 to 30
ft (7.6 to 9 m).
Transient finite element simulations
focus on flowline cumulative expansion and whether the entire flowline system
would translate independently on both ends, hot or cold.
INTECSEA created an ideal, or
best-option, temperature profile for the transient heating cycle and cooled the
flowline system uniformly along its length. During cool-down, the effective
axial force changed direction from compressive to tensile on a partially
restrained system. A component of lay tension also may be included in the
effective force.
Transient cycling assessment
The transient cycling assessment
captures the transient response when the flowline displaces at specified
locations and is especially critical within 3 mi (4.8 km) of either end.
Importantly, the assessment shows that seabed intervention improves the overall
expansion, which reduces significantly during the transient cycling stage.
Controlled flowline displacement at pre-installed and natural seabed locations
facilitates this improvement
Transient thermal cycling analysis
of the flowline system illustrates that if the flowline displaces naturally at
crucial seabed features, the initial flowline response is dominated by
transient cumulative expansion. During this condition, both ends of the
flowline expand independently and increase overall end expansions. A steeply
sloping seabed - a contributing component of this phenomenon - inherently
causes the flowline to move down-slope, with gravity imposing tension to a
hanging flowline.
This tension becomes increasingly
critical if the hot end of the flowline terminates near the bottom of the
slope. The flowline length resting on the slope also contributes to the slope
of axial force distribution. For this case, flowline expansion more than
doubles after only three transient cycles.
Expansions escalate in part because
the thermal grathent of heating cycles does not create enough force to displace
the flowline; whereas during static full operating condition, thermal grathent
displaces the flowline naturally. Heating cycles, therefore, push the flowline
axialry on either end.
Because high end expansions - both
static and transient - are not a favorable design solution, displacement units
along the flowline at specified seabed locations facilitate optimum system
performance.
If the behavior of the full 3D
assessment including route curves, responds to transient cycles in the similar
order of magnitude, final hot end expansion can range from 8 to 9 ft, which is
30% to 50% higher than the predicted 6 ft The cold end expansion will increase
to nearly 6 ft.
Both these values are within
feasible range for design of end tie-in spools and can be reduced, based on
specific design considerations, in consultation with operators. Ideally, a
design strategy calls for keeping expansion below 6 ft for most flowlines. End
expansions that exceed this goal may require sliding end mechanisms and/or
anchoring.
A large component of this transient
expansion is accumulated during the first two to three cool-down/heat-up
cycles. Subsequent transient expansion gradually tapers to a net relative
expansion of zero. At this point, the flowline system effectively exists in a
quasi-static zone with the system either stabilizing - indicating no further
expansion and axial creep - or transitioning to an axial creep or walking zone.
Based on results of this assessment
and engineering judgments from related sensitivity work, the flowline system
tends to expand independently during transient temperature cycling and then
ceases to expand on both ends after seven to eight full cycles.
Following this stage, the flowline
shows signs of stabilization. This study, however, did not eliminate the
possibility of axialcreep/walking of the system, because results depended on
numerous factors, and are an integral part of such behavior.
The study also suggests that if
displacement of a flowline is controlled on or near the slope, designers can
further reduce overall cumulative expansion and eliminate axialcreep by
optimizing the size and location of an artificial displacement unit
Importantly, the study shows flowline system feasibility and that with adequate
measures, designers can achieve lateral buckling integrity of the overall
system and end tie-in structures.
Recommendations
INTECSEA's assessment of design
issues associated with wet-insulated HP/HT flowline systems on a steep slope
include:
- Simplified end expansion analysis of these systems can be very conservative and can indicate that a configuration is unfeasible. In some cases, even two-dimensional assessment may not provide true response of the flowline. To accurately assess the response of such system, a complete set of 3D assessments is necessary.
- For a given operating condition, wet insulated HP/HT flowlines - even as long as 20 mi (32 km) - may be susceptible to a large cumulative expansion due to a series of transient* i.e., start-up/cool down, events. Most flowline systems reach the maximum cumulative expansion after two heating cycles. A wetinsulated system on a slope, however, may require five to 10 heating cycles to achieve the maximum cumulative expansion; i.e., stabilizes. This process, though, results in very high end expansions of 10 to 20 ft. The ability to mitigate the cumulative end expansion is critical to a feasible design solution.
- The potential for flowline walking is a central design issue for a HP/HT wet insulated flowline. Designers, however, can mitigate this phenomenon using 3D modeling to generate effective routing of the flowline and to optimize seabed intervention.
Flowline projects that incorporate
wet insulation on steep seabed terrain should perform both a design assessment
and significant sensitivity reviews of all the relevant parameters. The overall
solution is dependent on the flowline system moving with a predictable
response, confirmed by analyses. Sensitivity assessments should include: laying
pipe within the lay corridor but not on the design centeriine; variability of
soil conditions; variability of lay radius; and other known flowline conditions
and engineering impacts.
The industry has several deepwater flowline systems
routed across challenging seabed features with seabed elopes ranging between 5°
to approximately 40°.
A local buckling unity check along
the entire flowline length confirmed that the flowline was not overstressed
(unity check <1) and was within an acceptable limit for safe operation.
Study of axial force and lateral
displacement along the flowline length showed a maximum lateral displacement of
approximately 35 ft
Sumber : Kumar, Amitabh; McShane, Brian M. "Mitigating Deepwater Pipeline Buckling and Axial Stability. 28 Januari 2014. http://search.proquest.com/docview/849557963?accountid=31562


