an investigation on an alternative approach to compute the

57
AN INVESTIGATION ON AN ALTERNATIVE APPROACH TO COMPUTE THE 100-YEAR LOAD RESPONSES FOR TURRET MOORED SYSTEMS Guilherme Viana Rosa e Silva Valsa Projeto de Gradua¸c˜ ao apresentado ao Curso de Engenharia Naval e Oceˆanica da Escola Polit´ ecnica, Universidade Federal do Rio de Janeiro, como parte dos requisitos necess´ arios ` aobten¸c˜ ao do t´ ıtulo de Engen- heiro. Orientador: Paulo de Tarso Themistocles Es- peran¸ca Rio de Janeiro Novembro de 2019

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Page 1: AN INVESTIGATION ON AN ALTERNATIVE APPROACH TO COMPUTE THE

AN INVESTIGATION ON AN ALTERNATIVE APPROACH TO COMPUTE THE

100-YEAR LOAD RESPONSES FOR TURRET MOORED SYSTEMS

Guilherme Viana Rosa e Silva Valsa

Projeto de Graduacao apresentado ao

Curso de Engenharia Naval e Oceanica da

Escola Politecnica, Universidade Federal do

Rio de Janeiro, como parte dos requisitos

necessarios a obtencao do tıtulo de Engen-

heiro.

Orientador: Paulo de Tarso Themistocles Es-

peranca

Rio de Janeiro

Novembro de 2019

Page 2: AN INVESTIGATION ON AN ALTERNATIVE APPROACH TO COMPUTE THE

AN INVESTIGATION ON AN ALTERNATIVE APPROACH TO

COMPUTE THE 100-YEAR LOAD RESPONSES FOR TURRET

MOORED SYSTEMS

Guilherme Viana Rosa e Silva Valsa

Orientador:

Prof. Paulo de Tarso Themistocles Esperanca, D.Sc

Examinador:

Prof.Claudio Alexis Rodrıguez Castillo, D. Sc

Examinador:

Prof. Luis Volnei Sudati Sagrilo, D.Sc

2019

Page 3: AN INVESTIGATION ON AN ALTERNATIVE APPROACH TO COMPUTE THE

Viana Rosa e Silva Valsa, Guilherme

An Investigation on an Alternative Approach to Compute the 100-

Year Load Responses for Turret Moored Systems/Guilherme Viana

Rosa e Silva Valsa. - Rio de Janeiro: UFRJ/Escola Politecnica,

2019.

XV, 44p.:il.;29,7cm

Orientador: Paulo de Tarso Themistocles Esperanca

Projeto de Graduacao - UFRJ/Escola Politecnica/Curso de Engen-

haria Naval e Oceanica, 2019.

Referencias Bibliograficas: p.43-44.

1.Hidrodynamics. 2.Seakeeping. 3.Reliability. 4.Extreme Analy-

sis. 5.Mooring. I. Themistocles Esperanca, Paulo de Tarso. II.

Universidade Federal do Rio de Janeiro, Escola Politecnica, Curso

de Engenharia Naval e Oceanica. III.An Alternative Approach to

Compute the 100-Year Load Responses for Turret Moored Systems.

iii

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ACKNOWLEDGEMENTS

Primeiramente gostaria de agradecer a minha famılia por todo apoio fornecido nao so

durante o perıodo de graduacao, mas por todo o suporte antes do inıcio da faculdade e

por todo apoio que, sem duvida, sera prestado apos a graduacao. Teria sido impossıvel

sem voces.

Gostaria de agradecer aos meus colegas de curso e amigos. Obrigado pelos mo-

mentos, risadas e ajuda nas materias. A amizade de voces foi fundamental durante os

anos de curso e espero reve-los sempre que possıvel. Os levarei para sempre comigo.

Gostaria de agradecer a UFRJ, que me forneceu nao somente a possibilidade de

aprender e me tornar um profissional de engenharia como tambem a inesquecıvel ex-

periencia de intercambio. A dupla titulacao foi um patamar alcancado que certamente

moldou e que ainda molda minha vida. Aproveito a oportunidade para agradecer a todos

que conheci no exterior, amigos, professores e colegas.

Agradeco ao Prof. Paulo de Tarso por aceitar ser meu orientador e pela ajuda

ao longo do trabalho e a Prof. Marta Tapia por ter possibilitado minha participacao no

programa de intercambio da UFRJ.

iv

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Resumo do Projeto de Graduacao apresentado a Escola Politecnica/UFRJ como parte

dos requisitos necessarios para obtencao do grau de Engenheiro Naval e Oceanico.

An Investigation on an Alternative Approach to Compute the 100-Year Load Responses

for Turret Moored Systems

Guilherme Viana Rosa e Silva Valsa

Novembro/2019

Orientador: Paulo de Tarso Themistocles Esperanca

Curso: Engenharia Naval e Oceanica

O metodo de analise de valores extremos para calcular a resposta de perıodo de retorno

de 100 anos ja e bem estabelecido. Para se contabilizar a variacao de longo prazo das res-

postas, usam-se condicoes ambientais equivalentes a um perıodo de retorno de 100 anos.

Enquanto para a variabilidade de curto prazo, usam-se percentis equivalentes a 37% ou

50% nas simulacoes. Uma investigacao de um metodo alternativo usando condicoes ambi-

entais equivalentes de um perıdo de retorno de 40 anos com um percentil de 90% para as

simulacoes de curto prazo e um fator de correcao [1] e usado para o calculo de tensoes em

linhas de ancoragem em um sistema de torre. Os valores obtidos pelo metodo proposto

obtiveram resultados cerca de 30% maiores que o padrao. Por motivos de limitacao tem-

poral, o calculo da resposta exata que forneceria uma ferramenta efetiva de comparacao

entre os metodos nao foi realizado.

Palavras-Chave: Hidrodinamica, Seakeeping, Confiabilidade, Analise Extrema, Ancor-

agem

v

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Abstract of Undergraduate Project presented to POLI/UFRJ as a partial fulfillment of

the requirements for the degree of Engineer.

An Investigation on an Alternative Approach to Compute the 100-Year Load Responses

for Turret Moored Systems

Guilherme Viana Rosa e Silva Valsa

November/2019

Advisor: Paulo de Tarso Themistocles Esperanca

Course: Naval and Oceanic Engineering

The reliability investigations that compute the 100-year responses follow a standard

practice. The 100-year environmental conditions are used to account for the long-term

variability of the responses while the MPM or 50% quantile values are used for the

short-term variability. A new method using a 40-year return period with the use of 90%

quantile values for the short-term simulations and a correction factor of 1.04 [1] is tested

to verify its applicability to the turret loads. The values obtained from the alterantive

method are over 30% higher than those of the standard method. The computation of

the exact response would give a comparison tool between the responses. Due to time

and computational issues this response is not computed, leaving opportunities for future

research.

Key-words: Hidrodynamics, Seakeeping, Reliability, extreme analysis, mooring

vi

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Nomenclature

Fdiff Diffraction Forces

FK Froude-Krylov Forces

Frad Radiation Forces

CoG Center of Gravity

DOF Degree of Freedom

Ln Natural Logarithm

LT Long-term

MBL Minimum Breaking Load

MPM Most Probable Maximum

PFE ”Projet des fins d’Etudes”

Q Quantile

QTF Quadratic Transfer Function

RAO Response Amplitude Operator

RMS Root Mean Square

RP Return Period

RV Response Value

ST Short-term

TLP Tension Leg Platforms

vii

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TMS Turret Moored System

α Wave Phase

β Gumbel Scale Parameter

βLT Variable in Gaussian Space Related to the Long-term Variable in the Physical

Space

βST Variable in Gaussian Space Related to the Short-term Variable in the Physical

Space

χ Wave Direction

ε Phase Angle

κ Wave Number

λ Gumbel Location Parameter

µ Response Parameter Evaluated

ω Wave Frequency

x Data Average Value

Φ Standard Normal Distribution

φD Diffraction Potential Flow

φI Incident Potential Flow

φR Radiation Potential Flow

φt Total Potential Flow

ρ Density [ tonsm3 ]

ξ Shape Parameter for the Long-term Probabilistic Distribution

A∞ Fluid Added Mass at Infinite Frequency

Aj Wave Amplitude

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Fh Total Horizontal Force applied onto the Chain Table

FLT Long-term Probabilistic Distribution of the Responses

Frad Total Horizontal Force applied onto the Turret

fST Short-term Probabilistic Distribution of the Responses

FXCT Mooring and Riser Forces Applied along the Turret x-axis

FXrad Mooring, Riser, Inertia and Entrapped Water Forces Applied along the Turret

x-axis

FY CT Mooring and Riser Forces Applied along the Turret y-axis

FY rad Mooring, Riser, Inertia and Entrapped Water Forces Applied along the Turret

y-axis

TMax Maximum Tension of the Mooring Lines

Vi Fluid Velocity in the i Direction

C Damping Matrix

K Stiffness Matrix

M Added Mass Matrix

Fx Cumulative Probabilistic Function for a Specific Response Parameter

Cs Current Speed

h Acceleration Impulse Function Matrix

Hs Significant Wave height

I Index Number used in the Gumbel Fit

M Mass

N Total Number of seeds

P Probability

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PI Probability of a Specific Index I in a Data Distribution

Tp Modal Peak Period

Ws Wind Speed

g Gravity[ms2

]

x

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Contents

List of Figures xii

List of Tables xiii

1 Introduction 1

1.1 Context . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 2

1.2 Problem Statement and Objectives . . . . . . . . . . . . . . . . . . . . . 2

1.3 Structure of the report . . . . . . . . . . . . . . . . . . . . . . . . . . . . 3

2 Project Presentation 4

2.1 Reference Systems . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 5

2.2 Mooring Lines . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 6

2.3 Risers . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 7

2.4 Turret . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 7

2.5 Environmental Data . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 7

3 Theoretical Formulation 9

3.1 Diffraction/Radiation Analysis . . . . . . . . . . . . . . . . . . . . . . . . 9

3.1.1 First-order Approach . . . . . . . . . . . . . . . . . . . . . . . . . 9

3.1.2 Second-Order Approach . . . . . . . . . . . . . . . . . . . . . . . 11

3.1.3 Radiation forces . . . . . . . . . . . . . . . . . . . . . . . . . . . . 12

3.2 Line Dynamics . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 14

3.3 Turret Loads . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 15

3.4 Extreme Analysis . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 16

3.4.1 Random/Stochastic Process . . . . . . . . . . . . . . . . . . . . . 16

3.4.2 Seed Number . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 17

3.4.3 Short-term Variability . . . . . . . . . . . . . . . . . . . . . . . . 18

xi

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3.4.4 Gumbel Probabilistic Model . . . . . . . . . . . . . . . . . . . . . 19

3.4.5 Return Period . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 21

3.4.6 Long-term Variability . . . . . . . . . . . . . . . . . . . . . . . . . 21

3.4.7 Methodology for the 100-year RP Responses . . . . . . . . . . . . 24

3.4.8 Exact Response . . . . . . . . . . . . . . . . . . . . . . . . . . . . 25

3.4.9 IFORM Contour . . . . . . . . . . . . . . . . . . . . . . . . . . . 26

3.4.10 Reference Article/New Method summary . . . . . . . . . . . . . . 29

4 Numerical Studies 30

4.1 Software Versions . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 30

4.2 Hydrostar-ARIANE-OrcaFlex Methodology . . . . . . . . . . . . . . . . 30

4.3 100-year Return Period Configuration . . . . . . . . . . . . . . . . . . . . 32

4.4 40-year Return Period Configuration . . . . . . . . . . . . . . . . . . . . 33

4.4.1 Design Points . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 34

5 100-year RP Turret Loads Investigations 35

5.1 Hydrostar-ARIANE-OrcaFlex Investigations . . . . . . . . . . . . . . . . 35

5.1.1 Standard Method Investigations . . . . . . . . . . . . . . . . . . . 36

5.1.2 Prosed Method Investigations . . . . . . . . . . . . . . . . . . . . 36

5.1.3 Conclusion . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 39

6 Conclusion 41

6.1 Perspective . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 42

xii

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List of Figures

2.1 Bird’s eye view of the mooring and riser systems. . . . . . . . . . . . . . 4

2.2 Vessel reference system. . . . . . . . . . . . . . . . . . . . . . . . . . . . 6

3.1 Example of a Gumbel fit. . . . . . . . . . . . . . . . . . . . . . . . . . . 20

3.2 Example of an environmental contour [6]. . . . . . . . . . . . . . . . . . . 22

3.3 Standard practice flow chart . . . . . . . . . . . . . . . . . . . . . . . . . 24

3.4 Example of a circle in gaussian space defined by two independent variables

[6] . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 27

3.5 IFORM Contour . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 29

4.1 Summary chart describing the work flow of the Hydrostar-ARIANE-OrcaFlex

investigations. The square boxes represent the software used. The rounded-

edged boxes represent the type of computation performed. The ellipses

represent the output from the computations. . . . . . . . . . . . . . . . . 32

5.1 OrcaFlex model. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 35

xiii

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List of Tables

2.1 Summary of the reference systems . . . . . . . . . . . . . . . . . . . . . . 5

2.2 Segment Lengths Summary . . . . . . . . . . . . . . . . . . . . . . . . . 6

2.3 Environmental Characteristics Main Parameters Summary . . . . . . . . 8

3.1 Description of turret loads . . . . . . . . . . . . . . . . . . . . . . . . . . 16

3.2 Example of table that relates the response values with their indexes and

cumulative probability values. This table exemplifies one condition ran

with 50 different seeds. . . . . . . . . . . . . . . . . . . . . . . . . . . . 19

3.3 Summary of the RP values and their probabilities considering 2920 simu-

lations of 3h in one year interval . . . . . . . . . . . . . . . . . . . . . . . 21

3.4 Joint frequency of significant wave height and spectral peak period [2] . . 23

3.5 IFORM Summary table values . . . . . . . . . . . . . . . . . . . . . . . . 28

4.1 Table that summarizes the loads taken into account when computing the

motions in ARIANE [11]. This is a general table that indicates ARIANE’s

computational capacities. It does not represent all loads computed in this

study. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 31

4.2 100-year return period turret loads reference environmental conditions . . 33

4.3 Summary of Metocean Return Periods. . . . . . . . . . . . . . . . . . . . 33

4.4 40-year return period design environmental conditions . . . . . . . . . . . 34

5.1 Fh and Frad values obtained with the standard approach. . . . . . . . . 36

5.2 40-year return period turret load responses . . . . . . . . . . . . . . . . . 36

5.3 Summary of environmental directions evaluated for design points 1 and 2. 37

5.4 Summary of turret load values with all environmental directions evaluated

for design points 1 and 2. . . . . . . . . . . . . . . . . . . . . . . . . . . . 38

5.5 Results comparison with the two proposed methods. . . . . . . . . . . . . 39

xiv

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Chapter 1

Introduction

FPSOs are largely used for oil and gas production. The environmental conditions

for this kind of activity can be very aggressive. Waves, wind and current play an impor-

tant role in defining the vessels’ motions and the loads that are applied to them. When

severe sea conditions are added into the equation, the problem becomes even more com-

plex. It is therefore vital for oil companies to accurately predict the vessel’s behavior in

open waters.

The seakeeping performance of offshore units is a crucial part when studying the

development of an oil and gas exploration field. A ship’s seakeeping performance can be

tied to its capacity to withstand external environmental loads and its motions response.

Comfort and damage to the ship and its cargo being the most used parameters for quality

standards. The investigations presented in this report relate to both seakeeping and to

the ability of the mooring system to keep the FPSO on station i.e station-keeping. This

is highly important when studying the chaintable loads.

The offshore unit analyzed in the investigations here presented is an internally

turret-moored FPSO vessel. This means that it is a floating system and that it requires

mooring lines to keep it in place, or within an imposed range of offsets. In addition to

these underwater cables, there are also risers that connect the seabed to the vessel. These

pipes are responsible for transferring fluids and information. More notably, the crude oil

from the wells.

The use of the Return Period (RP) responses is a standard practice to determine

which sea conditions the offshore unit might have to withstand during its lifetime. The

Return Period characterizes the probability of exceedance of an event during a previously

determined time frame. The most common RP analyzed in the industry nowadays are the

1

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1, 10, 100 and 10.000 years. The 1-year RP being the least severe, while the 10.000-year

RP is the most extreme case.

Usually, the 100-year RP environment is the main criteria to assess the vessel’s

seakeeping and mooring system station-keeping performaces. Since the environment is

described as a probabilistic model, the actual sea conditions vary from one study to

the other. Therefore, a wide number of 3h time-domain simulations is done, each of

them giving a different response. For every 3-hour environmental conditions, the Most

Probable Maximum (MPM) or the median reponse (50% Quantile) value of the response

is computed. The highest MPM or Q50% of all simulations performed is considered to

be the 100-year RP response.

Despite being a consolidated practice in the industry, an article [1] from BV pro-

poses a new method to better model the 100-year RP response. They use a 40-year RP

with a 90% quantile for the short-term variability, instead of the current 100-year RP

with a 50% quantile. They also propose a 1.04 correction factor. This new method is

investigated. The main variables analyzed in the investigations are the loads applied to a

turret mooring system. These efforts are the ones applied to the turret and are primarily

due to the mooring lines restoring forces.

1.1 Context

The study presented in this report is part of the internship activities done in

the context of a double degree program in France. This internship, called ”Projet des

Fins d’Etudes”or ”PFE” in French, lasted for 5 months and a half. This is a vital and

mandatory step for students at ENSTA-Bretagne to finish their studies and obtain their

diploma.

The nature of the work is mainly in the field of Hydrodynamics, with focus on

seakeeping. The offshore unit in question is an internally moored FPSO.

1.2 Problem Statement and Objectives

Even though the current practice for calculating the 100-year return period re-

sponse is well established in the offshore industry, there are other ways of computing this

response. A recent BV paper[1] tackled this issue. Their new proposed method indicates

2

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an approach to better estimate the 100-year RP response. However, their analyses focus

on the mooring lines maximum tensions (TMax). It is unknown if this approach can be

applied to other parameters (such as offset, mooring forces etc.).

If such approach is proven to be more precise than the one largely used in the

industry, it may (depending on the outcome of future research) indicate a need to update

the current long-term analysis methodology. The precision of the answer is indicated by

how far it is from the exact 100-year response (see Section 3.4.8 Exact Response).

The main activities consist of the computation of the 100-year RP response of

the tensions on the mooring turret using dedicated software. Several simulations are

performed to compute the reponses using the standard and the proposed methods.

1.3 Structure of the report

• Chapter 2 summarizes the characteristics of the Turret Moored Systems (TMS)

and its components.

• Chapter 3 details the theoretical formulations and hypotheses used to compute the

desired response values.

• Chapter 4 introduces the software used to do the computations and focuses on the

methodology used to obtain the 100-year RP responses. In addition, it describes

initial investigations important for the setup of the project.

• Chapter 5 details the investigations made and results obtained using the method-

ology described in Chapter 4.

• Chapter 6 is dedicated to the final conclusions of the project.

3

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Chapter 2

Project Presentation

As previously mentioned, the vessel being studied is a FPSO. Even though the

seabed studied has a slight slope, the seabed is considered as a flat surface. The mean

water depth is over 250m . The vessel has an internal turret system that allows it to

weathervane. The turret is connected to all mooring lines and risers. There is a total of

3 bundles composed of 5 mooring lines each, which makes a total of 15 mooring lines. In

addition, there are 21 risers. In total, there are 36 lines in the model. Figure 2.1 shows

the complete system.

Figure 2.1: Bird’s eye view of the mooring and riser systems.

4

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2.1 Reference Systems

There are three main reference systems to be considered: the global earth-fixed

reference system, the vessel axis system and the turret axis system. The origin (O) of the

earth-fixed system corresponds to the turret reference position at the mean water line. A

summary of the reference systems can be seen in Table 2.1 and Figure 2.2. The software

used during design have their own definition of the reference systems. As a result the

turret system has an orientation towards west, while the earth-fixed system is towards

east.

Table 2.1: Summary of the reference systems

Earth-Fixed Reference System

Axis Origin Positive Direction

X Turret CoG Towards North

Y Turret CoG Towards East

Z Mean Water Line Downwards

Vessel Axis System

Axis Origin Positive Direction

X FPSO Aft Perpendicular (AP) From AP to bow

Y FPSO Center Line (CL) From CL to Port Side

Z FPSO Base Line (BL) From BL upwards

Turret Axis System

Axis Origin Positive Direction

X Turret Center Line (CL) Towards North

Y Turret Center Line (CL) Towards West

Z FPSO Base Line (BL) From BL upwards

5

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Figure 2.2: Vessel reference system.

2.2 Mooring Lines

Each mooring line is composed of different segments, each of them with different

properties. They all possess a bottom chain, which is the part in contact with the seabed,

thus subjected to friction forces. In addition, they have a chain-steel wire component

(SSSW) and a top chain. Finally, they also have a small connector component that is

considerably heavier than the others and is used as the connection segment with the

fairleads. The mooring lines composition can be seen in Table 2.2.

Table 2.2: Segment Lengths Summary

Segment Unit Bundle 1 Bundle 2 Bundle 3

Bottom Chain m 520 420 720

SSSW m 355 355 355

Top Chain m 50 50 50

Connector m 3.5 3.5 3.5

Total Length m 1125 1025 1325

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2.3 Risers

The system operates with 21 risers when in full capacity, this condition is the one

considered for the computations. All risers have a buoyancy section dedicated to the

creation of underwater arches. This pliant-wave configuration seeks to lower the overall

tensions on the pipes. The risers are implemented on the computation model only for the

line dynamics computation. They do not take part on the computation of the Response

Amplitude Operators (RAOs).

2.4 Turret

The turret is a crucial component for this system. Besides grouping all risers and

mooring lines, it also allows the FPSO to weathervane. This ability is very important

when the system is subject to severe environmental conditions that can also come from

multiple directions. The main focus of the investigations presented is related to the turret

loads.

2.5 Environmental Data

The environmental data is obtained by a hindcast database. The metocean data

allows for the creation of long-term statistics that describe wave, current and wind char-

acteristics. The main aspects to be considered are the intensities (wave height and natural

period, wind and current speed) and their governing directions. Table 2.3 shows the main

characteristics of the environmental conditions studied.

7

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Table 2.3: Environmental Characteristics Main Parameters Summary

Parameter Symbol Unit

Waves Wave Height Hs [m]

Waves Spectral Peak Period Tp [s]

Waves Mean Wave Heading (-) [deg]

Wind Wind Speed Ws [m/s]

Wind Mean Wind Heading (-) [deg]

Current Current Speed at surface Cs [m/s]

Current Mean Current Heading (-) [deg]

Current Current Profile (-) [m/s] and [m]

8

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Chapter 3

Theoretical Formulation

3.1 Diffraction/Radiation Analysis

The radiation and diffraction analysis is a method that seeks to predict the re-

sponse of offshore structure forces/motions due to wave excitation. The first-order or

linear approach limits the analysis of the excitation efforts with the same frequencies as

the incoming waves, while the second-order approach allows the evaluation of loads with

frequencies besides those of the waves.

3.1.1 First-order Approach

The wave theory is important to predict sea induced loads on ships and offshore

structures as well as wave-induced motions. This approach considers that these efforts

and motions oscillate with the same frequency as the waves that excite the structures.The

linear theory allows the modelling of irregular waves by the simple addition of waves with

different amplitudes, lengths and directions. The wave elevation can be described as seen

in Equation 3.1 [2].

ζ =∞∑j=1

Aj sin(ωjt− κjx+ εj) (3.1)

Where Aj is the wave amplitude, ω the wave frequency, κ the wave number and ε the

phase angle.

Due to the linearity of the problem, the potential flow can be divided in three

parts, as shown in Equation 3.2. This assumption is not valid for large waves.

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φt = φI + φD + φR (3.2)

Where φI is the incident potential flow, φD the diffraction potential flow and φR the

radiated potential flow.

Considering the linear behaviour of the problem, the incident wave can be modelled

as the Airy wave. One main assumption is that the body does not affect the incoming

wave, more precisely its pressure field. It discards the diffraction contribution, therefore

only the incoming wave component is considered. From the incoming wave it is possible

to determine the loads that are applied on the body. These efforts are known as the

Froude-Krylov forces, as shown in Equation 3.3.

FK = −ρ∫∫

∂φI∂t

n dS (3.3)

Where ρ is the fluids’ density.

The diffraction phenomenon consists of the reflection and scattering of waves once

they encounter the body. The structure does not move, it is considered as a fixed body.

Diffraction originates excitation forces. The radiation problem takes into consideration

the waves created by the body without the contribution of the incoming wave. The body

oscillates and originates waves independently of any external excitation. The resulting

forces from this phenomenon are the added-mass and radiation damping contributions.

The contributions from the diffraction and radiation loads are shown in Equations 3.4

and 3.5.

Fdiff = −ρ∫∫

∂φD∂t

n dS (3.4)

Fradj = −ρ∫∫

∂φradj∂t

n dS j = 1, ... 6 (3.5)

Where ρ is the fluids’ density.

For the linear approach to be used, the fluid’s viscosity is neglected. In the linear

approach the dynamic responses of the structures (motions and loads) are excited with

the same frequency as those of the external waves.

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3.1.2 Second-Order Approach

The second-order approach allows the evaluation of loads that cannot be analyzed

with the linear approach since the latter works at a limited frequency range. Some of the

forces applied at the offshore structures are not at the same frequency of the incoming

waves. Therefore, the excitation loads can be close to the natural frequency of the

horizontal planar motions of the body, which may cause resonance issues.

The frequencies of these efforts can be smaller or higher than the wave frequency.

The most common effect analyzed at second-order is the wave drift load, an horizontal

effort linked to the structure’s capacity of creating waves. There is also a resonating

phenomenon known as springing that is observed at high frequencies in moored structures

such as TLPs.

The external forces can be developed as seen in Equation 3.6. [3]

F = F (0) + εF (1) + ε2F (2) + ε3F (3)... (3.6)

Where ε is a small linear parameter related to the wave amplitude. The ε2F (2) component

is the second-order term.

As shown in [2] the non-linear effects can be obtained by analyzing the Bernoulli’s

equation for the fluid pressure, as shown in Equation 3.7.

−ρ2

(V 21 + V 2

2 + V 23 ) =

−ρ2|∇φ|2 (3.7)

Where Vi is the fluid velocity at the i direction. An approximation of the velocity vector

for an idealized sea state composed of two distinct wave components ω1 and ω2 is proposed

[2], as shown in Equation 3.8.

V1 = A1 cos (ω1t+ ε1) + A2 cos (ω2t+ ε2) (3.8)

By analyzing only the V1 component, Equation 3.7 can be expanded as shown in Equation

3.9.

−ρ2

(V 21 ) =

−ρ2

(A2

1

2+A2

2

2+A2

1

2cos (2ω1t+ 2ε1)+

A22

2cos (2ω2t+ 2ε2) + A2

1A22 cos ((ω1 − ω2)t+ ε1 − ε2)+ (3.9)

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A21A

22 cos ((ω1 + ω2)t+ ε1ε2))

Through this analysis a constant term appears : −ρ2

(A2

1

2+

A22

2). This effort is the

mean drift load and its contribution is only noticeable by doing this second-order analysis,

this component is called wave drift load. Another term that appears is the (ω1−ω2) which

represents the difference wave frequencies. This factor represents a pressure contribution

that oscillates with a frequency equal to the difference of both wave frequencies. When

modelling more complex and realistic sea conditions, the velocity component can be

described as the sum of N different waves. Therefore, there will be several combinations

of difference wave frequencies. As a result, the difference frequency force components

oscillate at other frequencies than those of the waves. Thus, the combination of incoming

waves might introduce resonating forces and moments on the body [2].

This example demonstrates that the first-order analysis simplifies the problem by

not taking into consideration terms of higher order. By doing a second order analysis

other components such as the wave drift load and the difference frequencies come into

play. These efforts can impact greatly the movement and integrity of the structures since

the efforts being applied might be in the same range as that of their natural frequencies.

The higher-order approaches are not limited to the second-order analysis, they can

be a third-order, fourth-order approach or even higher. However, the more the order is

increased the more the solution becomes complex. Therefore, the study can become very

expensive since it takes larger amounts of time to solve a high-order problem. Besides,

approaches of order higher than two introduce terms that can be neglected because their

impact on the structure is small in comparison to first and second-order components.

Equation 3.9 also introduces a sum of frequencies. However, they are more specific to

TLP and taut moored structures that have oscillating periods of no more than 4 seconds.

3.1.3 Radiation forces

The radiation problem solution consists of forcing the ship to oscillate for the six

degrees of freedom in calm water. The system is excited with the same frequency as

the excitation waves. The equation of motion of the system can be written as shown in

Equation 3.10.

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MX(t) + CX(t) + KX(t) = F(t) (3.10)

Where M is the added mass matrix, C the damping matrix, K the stiffness matrix and

F(t) the external forces.

The added mass matrix and the hydrodynamic damping in the damping matrix are

frequency dependant. Since this method considers that external forces (such as mooring

and riser loads) do not affect motions in a significant manner at wave frequency, it does

not evaluate the full problem. In some cases this assumption may be correctly applied,

in others not. This approach computes the radiation forces as shown in Equation 3.11

[4].

[F (t)]rad =∑

Re{am(ωi)

[ω2i (A(ωi)− A0) + iωiB(ωi)

][u(ωi)]e

i[−ωit+ki(x cosχ+y sinχ)+αi]}

(3.11)

Where A(ωi) and B(ωi) are the added mass and damping matrix at the i-th wavelet

frequency, [u(ωi)] is the translation or rotation motion RAO. A0 is the added mass at

drift frequency. ωi is the encounter wave frequency, ki the wave number, χ the wave

direction and αi the wave phase of the i-th wavelet.

3.1.3.1 Convolution

The equation of motion is solved in the frequency domain. This is not compatible if

the external forces (wind, waves . . . ) are in time domain. The convolution options allows

for a more precise result since it computes the radiation forces by taking into account

all frequency values. The convolution integration method is an alternative approach to

compute the radiation forces.

The convolution method uses the system’s added mass and damping information

to compute a time domain response. The equation of motion of the system (Equation

3.10) is slightly modified. This approach is shown in Equation 3.12 [4].

(M + A∞)X(t) + CX(t) + KX(t) +

∫ t

0

h(t− τ)X(τ) dτ = F (t) (3.12)

Where M is the structural mass matrix, A∞ is the fluid added mass matrix at infinite fre-

quency, B is the damping matrix, K is the total stiffness matrix, and h is the acceleration

impulse function matrix, as shown in Equation 3.13 [4].

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h(t) =2

π

∫ ∞0

B(ω)sin(ωt)

ωdω =

2

π

∫ ∞0

{A(ω)−A(∞)} cos(ωt)dω (3.13)

Equation 3.12 is the equation of motion expressed in convolution integral form.

In the computations that do not consider convolution, the radiation forces are restricted

to the excitation wave frequencies. However, the convolution method is capable of cal-

culating the forces and their impacts on the structure motions to all frequencies by the

usage of the integral form of the radiation forces. It passes the parameters from frequency

domain to time domain.

The convolution considers then, that the radiation forces are analyzed as a separate

force in time domain. The convolution method basically means that frequency dependant

parameters such as the added mass and damping are treated in time domain instead of

the frequency domain by the means of a numerical computation, which is represented by

the integral in Equation 3.12.

3.2 Line Dynamics

Offshore units are either fixed or moored structures. Moored vessels and platforms

are subjected to forces originated from the interaction of the mooring lines and the

environment: friction force with the seabed, wave and current loads, inertia etc. This is

true for all underwater cables, therefore also for risers as well.

The vessels possess a large mass in comparison to the risers and moorings. Never-

theless, the dynamic response of the cables to external loads affect the vessels’ motions,

specially the lines drag forces. There are different approaches to consider the effects of

the mooring lines on a numeric model [5].

One approach is the use of the quasi-static method. This method solves the

mooring lines contributions by solving the catenary equations at each time step. With this

approach, the low frequency motions due to environmental excitation and the dynamic

effects of the lines are difficult to be solved.

In order to properly take into account the impact of the lines into the vessels’

motions, a full dynamic solution is to be used. This method allows for the computation

of the full effects of the moorings in the analysis by solving the motion equation at each

time step. This approach considers:

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• Seabed effects - The contact between the lines and the seabed create friction

forces. These loads are nonlinear. Besides, the portion of the lines that is in

contact with the floor changes as the vessel moves. As a result, there is also a

nonlinear geometrical factor to be considered.

• Drag forces - The Morison equation is commonly used to take into account the

fluid contributions on the underwater cables. The drag force is of nonlinear be-

haviour, it is proportional to the square of the velocity (relative velocity between

line and fluid).

3.3 Turret Loads

The objective of this study is to investigate the loads applied onto the turret. There

are two parameters investigated: the chain table loads and the turret loads. The former

takes into account the mooring lines and risers contributions, while the latter considers

also the entrapped water and the inertia contributions of the turret. The design load at

the chain table level is called Horizontal Force (Fh). See Equation 3.14.

Fh =√

(FXCT )2 + (FY CT )2 (3.14)

Where FXCT represents the mooring and riser forces along the turret x-axis and FY CT

represents the mooring and riser forces along the turret y-axis. Fh is then, the total

horizontal force applied onto the chain table. The turret axes are in accordance with the

previously defined turret reference system.

The turret load contributions have the same components as Fh. Moreover, it also

considers the turret inertia and entrapped water for its computations. The entrapped

water is the amount of water in the turret cylinder. This entrapped water does not

impact the static analysis. However, when the vessel moves, the turret accelerations also

impose accelerations on the entrapped water. Therefore, the water generates loads onto

the turret due to its inertia. The total horizontal forces applied onto the turret are called

turret loads (Frad). See Equation 3.15.

Frad =√

(FXrad)2 + (FY rad)2 (3.15)

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Where FXrad is the mooring and riser forces along the turret x-axis plus the turret inertia

and entrapped water loads along this axis. FY rad is the mooring and riser forces along the

turret y-axis plus the turret inertia and entrapped water loads along this axis. Frad is

then, the total horizontal force applied onto the turret. The turret axes are in accordance

with the previously defined turret reference system.

Table 3.1 summarizes the loads that are taken into consideration for each variable

investigated. These loads depend on the motions of the vessel and therefore are time-

dependent.

Table 3.1: Description of turret loads

Load Types Chain Table Loads Turret Loads

Dynamic Mooring Loads√ √

Dynamic Risers Loads√ √

Turret Mass Inertia Load ×√

Entrapped Water Inertia Load ×√

3.4 Extreme Analysis

The extreme analysis study is used to estimate the response values of the vari-

ables being studied. In this case, this analysis is focused on the 100-year Return Period

responses of the turret loads.

This analysis is made by computing several 3h numerical simulations using ded-

icated software. Each simulation gives a response value. These values can be used to

create a probabilistic distribution that gives in return the response desired according

to the Return Period being studied. The metodology and concepts of this study are

explained in this section.

3.4.1 Random/Stochastic Process

The random process field of study evaluates the random changes in numerical

values that compose the system being analyzed. Unlike the deterministic processes, in

the stochastic processes the behaviour of the variables being studied cannot be determined

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by the use of equations and so forth. A stochastic process is characterized by an ensemble

of empirical data. In this case, the empirical data is obtained through the simulations

ran.

The procedure for the simulations in this report consists of the definition of wave

and wind spectra and the realization of time domain evaluations. The waves are defined

by a significant wave height, spectral peak period and direction. The wind is characterized

by wind speed and direction. When transformed into the physical space of time domain

simulations, these spectra are responsible for the definition of the wave elevations and

wind behaviour with time in a simulation. They define how the environment behaves and

therefore the structure in it.

These random processes are then classified as stationary since the statistical pa-

rameters do not change with time. Another important concept is the ergodic theory.

An ergodic process is a class of random process as well as a sub-type of the stationary

process. In this type of analysis, the mean values for the time domain responses for a

specific sample are the same as the mean statistic values of the data ensemble.

3.4.2 Seed Number

The seed is a random number used to give the initial conditions for a pseudo-

random generator. The waves and wind are characterized as spectra, which are in fre-

quency domain. The wind or waves will have different time-domain behaviour depending

on the seed first used to ”populate” their spectra. In other words, every seed number

used to characterize a spectrum will give a different time-domain behaviour for the waves

and the wind. In this study, every 3h short-term simulation has a different seed number.

The seed number is computationally represented by the εj in Equation 3.1. The

spectrum used to represent the waves is the Jonswap spectrum. Due to the different wave

elevations and wind behaviour, the offshore systems being analyzed will have different

response values (ex. motions, turret loads) for each seed used. This means that even

though the spectra used are statistically similar (same significant wave height and spectral

peak period), the physical response encountered in each simulation is different from the

others.

Since the environmental characteristics are described by a probabilistic model, a

simulation emulating a specific environment does not necessarily output the same re-

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sponses every time it is run. This happens because the waves and wind are defined as

spectra. By using a different seed for each simulation, a different time-domain response is

obtained. The variation in results for the same sea state is called short-term variability.

3.4.3 Short-term Variability

The short-term variability is the term used to indicate that environmental condi-

tions that possess constant statistical parameters give different response values in accor-

dance to the seed that populates the spectra.

For instance, the statistical parameters that characterize a wave spectra are usually

the spectral peak period, the main direction and the wave height. For each simulation

run with a different seed number, the offshore unit will also respond differently in time

domain.

In this study several 3h simulations with different seeds for the same sea state are

run. By doing this procedure, it is possible to establish a probabilistic function that gives

the likelihood of obtaining a certain response value.

For each 3h simulation, the maximum response value is taken to create the curve.

The used method for building the probabilistic function out of empirical data is a Gumbel

fit that describes the probability of obtaining a response value for a specific sea state.

The number of 3h simulations to be run indicates the precision obtained to fit

the probabilistic curve. In other words, the larger the number of simulations ran, the

larger the number of points that were evaluated to create the curve. This is useful to get

a better understanding of the extreme values that define the probabilistic distribution

since its tail will be better discretized.

Convergence is an important aspect when doing a probabilistic function fit with

empirical data. Response values related to large quantiles, require a larger number of

simulations to be precise. For example, response values for the mean response may require

about twenty simulations, whereas values related to high quantile values i.e Q80% may

require more than fifty runs. In this study, the convergence criterium used is of a 1%

difference in value of the turret loads for Q90%. This translates into about 100 seeds.

This leads to the conclusion that investigations using this methodology can become

very expensive (CPU time) due to the number of simulation runs they require.

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3.4.4 Gumbel Probabilistic Model

The Gumbel distribution is a common probabilistic model used in engineering to

predict extreme values based on empirical data. After running the required number of

seeds for the environmental conditions to ensure convergence of the results, the Gumbel

fit can be made. Equation 3.16 shows the probabilistic density function of the Gumbel

distribution.

F (x;λ, β) = e−e−(x−λ)/β

(3.16)

Where λ is the location parameter and β is the scale parameter.

In the approach used for the calculations, the parameters are obtained from the

empirical data. In other words, they vary according to the data being analyzed. By

ordering the empirical values in increasing order, it is possible to create a distribution

of data. An index number is given to each response value as shown in Table 3.2. The

cumulative probability value in respect to the index is defined in Equation 3.17.

Table 3.2: Example of table that relates the response values with their indexes and

cumulative probability values. This table exemplifies one condition ran with 50 different

seeds.

Index Sorted response values Cumulative probability

1 2.11 E+4 0.010

2 2.28 E +4 0.030

. . . . . . . . .

50 5.56 E+4 0.990

PI =I − 0.5

N(3.17)

Where I is the index number and N the total number of seeds used.

After the variable values and their probabilities are correlated, a linear regression

is performed. The objective of the linear regression is to predict a response value from

an empirical data set. In this study, this is done by the fit of the values obtained through

the simulations and their corresponding probability as exemplified in Table 3.2. In order

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to properly do a linear regression, it is necessary that the variables behave linearly to the

the probabilities. That is why the regression is actually made by analyzing the logarithm

of the probability. This is obtained by the linearization of Equation 3.16. See Equation

3.18.

X = λ− β · ln(ln(P )) (3.18)

Where X is one response value and P the probability attached to this value.

If well behaved, the distribution takes the shape of a line - y = ax + b. The

shape and scale parameters can be obtained once the linear regression is fit. The shape

parameter is the slope of the line (a) and the scale parameter the intercept in the y-axis

(b). Figure 3.1 shows an example of distributed data in increasing values.

Finally, the response values can be obtained by using Equation 3.18. The cumu-

lative probability shown in Table 3.2 represents the quantile. For instance, the value

5.56E+4 represented in the table is linked to the cumulative probability of 0.990 or Q

99%.

Therefore, the MPM would correspond to the value of the Q 37%, the median to

the Q 50%. The proposed method is then related to Q 90% of the probabilistic fit done

with this method.

Figure 3.1: Example of a Gumbel fit.

The x-axis corresponds to the ln(ln(P)), where P is the probability of the sorted

max value in the Gumbel distribution and the y-axis corresponds to the sorted values

themselves.

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3.4.5 Return Period

The Return Period is a theoretical concept that can be understood as the inverse of

the average frequency of occurence of a given variable. For instance, a 100-year response

value represents a 1/100 chance of this value being exceeded in a year time.

In the analysis here made, the 100-year responses are evaluated based on an anual

event. In other words, an 100-year return period response has 1% chance of exceedence

in a year time.

The simulations made in this study are 3h-long. By considering an one year’s

time, there are 2920 ”pieces” of 3h. See Equation 3.19.

1 Year = 365 days = 365 days · 24hours

days= 8760 hours −→ 8760 hours

3 hours= 2920 (3.19)

Therefore, by considering the 100-year response (or 1% chance of exceendence) of

2920 groups of 3h, the likelihood for a specific RP event to happen can be described as

seen in Equation 3.20. Table 3.3 shows examples of probabilities of different RP values

for 2920 groups.

PRP =1

RP · 2920(3.20)

Table 3.3: Summary of the RP values and their probabilities considering 2920 simulations

of 3h in one year interval

Return Period Probability Probability

1 year 1/(1 · 2920) 3.42 E−4

10 years 1/(10 · 2920) 3.42 E−5

100 years 1/(100 · 2920) 3.42 E−6

10.000 years 1/(10.000 · 2920) 3.42 E−8

3.4.6 Long-term Variability

The short-term variability describes the variation in response within the same

environmental conditions. However, the sea states are in constant change. The long-

term variability is the term used to take into account such changes.

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The sea states are considered to be constant for a 3h period. After such time has

passed, the environmental conditions are changed, thus the mean response values are also

changed. By grouping all the sea states in 3h constant conditions, there is a total of 2920

conditions for a one-year period.

The long-term variability can be better exemplified by the use of environmental

countours. Figure 3.2 [6] is an example of a significant wave height and spectral period

contour used to characterize the different combinations possible for the design

Figure 3.2: Example of an environmental contour [6].

Each curve of this contour represents a specific return period environmental condi-

tion. The contour in the middle (red line) is representative of the 100-year return period

wave characteristics. Each point on this contour represents a possible (Significant wave

heigt, Spectral peak period) combination to characterize the waves. As a result, every

possible combination on this line has the same probability of occurence. In this case,

3.42E−6 as seen in Table 3.3.

The computation of all possible points of the contour prove to be a very demanding

procedure since there are several possible combinations to be evaluated. This is further

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emphasized by the need of several runs of the same 3h conditions to ensure that the

short-term variability is properly taken into consideration.

However, it is evident that some environmental conditions are more severe than

others. These not necessarily mean the waves with the largest significant heights but

also those that have peak periods close to the structure’s natural frequencies. Therefore,

only simulations for specific design points from the wave contour are actually considered

in the simulations. This ensures that the worst conditions are taken into account while

trying to minimize global computational time.

The environmental contours are created by the collection and analysis of metocean

data. This data is collected on the desired offshore installation sites. These empirical

statistical data are obtained throughout the years. Companies specialized in these type of

data collection and analysis are usually hired to give information about the environmental

conditions of the installation sites.

Table 3.4 correlates significant wave heights and spectral peak periods and indi-

cates the frequency each combination happens (or wave-period joint frequency). By using

a probabilistic analysis it is possible to obtain the 100-year RP Hs-Tp contours from the

metocean data. The procedure for computing such results is explained in [2].

Table 3.4: Joint frequency of significant wave height and spectral peak period [2]

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3.4.7 Methodology for the 100-year RP Responses

The standard practice in the industry nowadays to compute the 100-year response

uses the 100-year environmental contours to pick the design points. All of these points

characterize the 100-year condition and are likely to yield the maximum response. A 3h

simulation is run for each design point in time-domain and the MPM or 37% value of

non-exceedance or Q 37% is computed. The highest MPM over all desing points is taken

as the 100-year return period. In some cases the Q 50% value is used.

Even though this method considers the long-term variability of the environmental

conditions, it may not fully take into account the sensibility of the short-term variability

for the 3h simulations. Which means that the response values obtained to describe the

100-year RP response may not be properly estimated. This does not mean that the

systems will necessarily fail due to the big safety factors involved in offshore projects.

Figure 3.3 summarizes the standard practice procedure. This procedure is applied for

each design point being evaluated on the contour. See Figure 3.2.

Figure 3.3: Standard practice flow chart

The convergence criterium varies with each project. For this project the conver-

gence criterium is explained in Section 3.4.3 Short-Term Variability. The metodology

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used for the proposed method follows the same philosophy of the flow chart with the

exception that instead of the use of the MPM values for the computation of the tur-

ret loads, the Q 90% is used. In addition, the input environmental conditions are not

those characterizing the 100-year conditions but those of the 40-year RP environmental

conditions.

3.4.8 Exact Response

The exact response is a value used for the comparison with the results found

with the methodology explained in Figure 3.3 for all the design points evaluated on the

environmental contours (Figure 3.2).

The computation of the exact response can be done by using Equation 3.21 [1].

F (x) =

∫fLT (µ)FST (x|µ)dµ (3.21)

Where FST is the conditional short-term distribution of the environmental conditions and

fLT the long-term distribution that characterizes the environmental conditions.

This approach requires the computation of the long-term distribution fLT = fTp|Hs

of all possible combinations of the metocean data. This means running simulations for

all values in Table 3.4. In addition, it is necessary to compute the conditional short-term

responses to each environmental condition. This can be represented as FST = FX|TpHs.

With X being the response desired (ex. Turret loads).

Besides, it is necessary to run each condition several times to ensure the correct

accountability of the short-term variability. It is therfore a very demanding and time

consuming approach. This response is not computed in this report. Only the comparison

between the standard and proposed method is done.

It is important to mention that even with the name of exact response, the value

obtained by this method is not necessarily what the offshore unit will encouter during its

service life. This happens because the tools used to obtain this value are based on em-

pirical observations (Table 3.4) and may not correspond to the real values. Nevertheless,

it is a very robust approach that serves to give a anchor point for research studies.

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3.4.9 IFORM Contour

An alternative approach to compute the exact response is the FORM (First-Order

Reliability Method) [6]. With this approach the integral (Equation 3.21) is transformed

to the Gaussian space where three independant variables are defined: U1, U2 and U3. See

Equation 3.22[6].

FHs(h) = φ(U1)

FTp|Hs(t|h) = φ(U2) (3.22)

FX|TpHs(t|h) = φ(U3)

Where φ() is the standard Gaussian distribution function.

These variables form a sphere in the Gaussian space. The radius of the sphere β

defines points which the probability density is constant. See Equation 3.23 [6].

β =

√∑i

U2i (3.23)

Where β is the radius of the sphere in the gaussian space and Ui are the three independent

variables that define the sphere.

With this method it is possible to obtain the extreme values for a specific X

variable. The specific extreme response for a given probability of exceedence or return

period is obtained through an iterative procedure. See [6] for a full explanation of the

method.

The IFORM (Inverse First-Order Reliability Method)[7] is an approach that uses a

similar concept from the FORM method but instead, it seeks to find the extreme values

from an already defined probability of failure. For instance, for the 100-year RP the

probability of exceedence of 2920 periods of 3h in a year is 3.42 · 10−6 as shown in Table

3.3.

The IFORM contour is defined by a circle in the Gaussian space when considering

two variables. See Figure 3.4. Every point within a given radius distance of the circle

represents a combination between two independent variables. Every point within the

same radial distance defines points of the same probability of exceedence or return period

(RP1, RP10, RP100 etc.). By transforming the Gaussian space circle into the physical

space, it is possible to obtain a curve that defines the responses for a given RP. Each

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response (motion, tensions etc.) has its own curve, therefore the IFORM contour is result

dependant.

Figure 3.4: Example of a circle in gaussian space defined by two independent variables

[6]

An alternative application of the IFORM contour [1] relates the short-term sim-

ulations maximum responses with their respective return periods. All the points in the

contour correspond to an equivalent (Q,RP) combination that simulate the 100-year re-

sponse. This approach relates then, the RP directly with the short-term simulations’

quantiles. The objective of this study is to give an indication of which (Q,RP) combina-

tion to use. By doing this analysis, it is possible to arrive at the proposed combination

by [1] of using (Q,RP) = (90%,40-year RP). This approach [1] relates the Q and RP with

the Gaussian Variables U1 and U2 as shown in Equations 3.24 and 3.25.

RP =1

2920(1− Φ(U1))(3.24)

Q = Φ(U2) (3.25)

Where Φ is the standard normal distribution. The terms U1 and U2 correspond to the

variables in the Gaussian space. These variables are independent from one another.

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As stated before, β (Equation 3.23) represents the radius of the sphere in which

all points possess the same probability of exceedence. By computing the inverse of of

the normal distribution using the probability of exceedence as the input, it is possible to

find the value of the radius in the gaussian space that represents the 100-year RP in the

physical space.

In the Gaussian space, the combinations between Φ(U1) and Φ(U2) have the shape

of a circle. A circle with the radius 4.50 indicates then, that all combinations of U1 and

U2 possible in this radius give the 100-year response period. See Equation 3.26[1] and

Table 3.5.

β =√U21 + U2

2 = Φ−1(

1− 1

292000

)≈ 4.5 (3.26)

Table 3.5: IFORM Summary table values

Gaussian Space Physical Space

Combination # Φ(U1) Φ(U2) RP Q

1 3.396 2.952 1 99.842%

2 3.581 2.725 2 99.678%

. . . . . . . . . . . . . . .

100 4.500 0.000 100 50%

All U1 and U2 possible combinations are then calculated. Φ(U1) gives information

about the RP, while Φ(U2) the associated Q for a specific RP. By reverting these com-

binations from the Gaussian space (U1, U2) to the physical space (RP, Q) it is possible

to create an IFORM contour that relates the short-term variability with the RPs. See

Figure 3.5.

This approach is useful as the contour is valid for all responses. Otherwise, there

would be a different plot for every response being evaluated. Every point on the contour

express a different combination of RP and Q that gives the 100-year response. Any

possible combination of (Q,RP) is a valid point for computing the 100-year response.The

bigger the quantile, the more severe is the response value for the system. Likewise, the

bigger the return period, the more severe are the environmental conditions.

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Figure 3.5: IFORM Contour

Figure 3.5 is coherent with the choice of using a Q 90% with 40-year return period

for environmental conditions [1]. As previously stated, simulating all possible combina-

tions is time consuming both due to the large number of points but also because for higher

Q values, it is necessary to run several 3h simulations to guarantee results convergence.

3.4.10 Reference Article/New Method summary

An alternative (Q,RP) combination the 100-year return period response compu-

tation is proposed by BV [1]. This method proposes the use of the 40-year return period

environmental condition. In addition, it uses a Q 90% for the short-term simulations,

which is in accordance with the IFORM contour, see Figure 3.5. Finally, they also propose

a 1.04 correction factor on the response.

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Chapter 4

Numerical Studies

4.1 Software Versions

The software versions used during the project are stated below:

• HydroStar For Experts V7.22 [8]

• ARIANE 7.0.2 [9]

• OrcaFlex 10.2 [10]

4.2 Hydrostar-ARIANE-OrcaFlex Methodology

The geometry file is used as an input in Hydrostar. This software performs radia-

tion/diffraction computations and creates the vessel’s hydrodynamics database, including

RAOs and QTFs. The output is used as input in ARIANE.

After importing the database into ARIANE, the mooring lines are set. Besides, the

user inputs the parameters that describe the environmental parameters (waves, wind and

current). After the correct configuration of these parameters, the equilibrium position

and time domain simulations can be run. The outputs (first-order motions) are used in

OrcaFlex.

ARIANE solves the time-domain motions for the FPSO’s six degrees of freedom.

However, some assumptions are made: line-dynamics are not considered, lines stay in the

vertical plane and environmental conditions (waves, current and wind) are not applied

to the lines. In ARIANE, it is possible to compute the motions based on the low-

frequency excitation values. However, it also offers the possibility of using a unified

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low-high frequency resolution [11]. This approach considers the coupling of both the

low frequency and the wave frequency motions, which gives a more accurate response.

This is the chosen approach. Table 4.1 shows the parameters taken into account in its

computations when considering only the low-frequency motions or the total motion.

Table 4.1: Table that summarizes the loads taken into account when computing the

motions in ARIANE [11]. This is a general table that indicates ARIANE’s computational

capacities. It does not represent all loads computed in this study.

It is necessary to use the OrcaFlex software because ARIANE does not use line

dynamics in its computations. Therefore, line loads are not accurate enough. By imposing

the time domain motions obtained in ARIANE into the OrcaFlex model, the software is

capable of calculating the turret loads while taking into account the line dynamics. The

entrapped water contribution is also implemented in the OrcaFlex model.Figure 4.1 shows

the numerical work flow procedures of the Hydrostar-ARIANE-OrcaFlex investigations.

The simulations performed in ARIANE and OrcaFlex are time domain simulations

that last for three hours. A transient of 30 minutes is used to take into account a steady

sea-state. A total of 100 seeds with the same environmental conditions are used for every

return period. This allows for Fh and Frad results to converge.

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Figure 4.1: Summary chart describing the work flow of the Hydrostar-ARIANE-OrcaFlex

investigations. The square boxes represent the software used. The rounded-edged boxes

represent the type of computation performed. The ellipses represent the output from the

computations.

4.3 100-year Return Period Configuration

The 100-year environmental contours are ready-to-use at the beginning of the

project. As a result, there are several design points that can be picked from this contour.

Since the investigations are centered on the turret loads, the environmental conditions

that give the biggest responses for Fh and Frad are the conditions that will be chosen as

the 100-year design point.

Table 4.2 indicates the governing environmental conditions that are chosen as the

100-year RP environmental desing points.

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Table 4.2: 100-year return period turret loads reference environmental conditions

Wave Heading [deg] 240

Hs [m] 14.0

Tp [s] 14.3

Wind Heading [deg] 210

Ws [m/s] 32.0

Current Heading [deg] 195.0

Cs [m/s] 1.23

4.4 40-year Return Period Configuration

The usual way of defining the environmental contours is by using the hindcast

data. However, due to the limited time available it is chosen to interpolate between the

1, 10, 100 and 10.000 year contours are already defined to create the 40-year RP wind

and wave contour. This approach is not standard and a more criterious evaluation of the

40-year RP contours should be done in future works.

The environmental conditions calculated consider mainly a wave/wind governing

condition. As a result, the current RP of 10 years is maintained for the alternative

approach as well. Table 4.3 summarizes the RP used for each environmental parameter.

Table 4.3: Summary of Metocean Return Periods.

Parameter Standard Method Proposed Method

Waves 100-year RP 40-year RP

Wind 100-year RP 40-year RP

Current 10-year RP 10-year RP

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4.4.1 Design Points

Once the waves, wind and current design points for the 40-year RP environment

are defined, it is possible to compute the turret load responses and compare with the

standard approach. Table 4.4 summarizes the environmental design point for the 40-year

RP environmental conditions. The environmental headings correspond to the same as

those of the 100-year RP as seen in Table 4.2.

Table 4.4: 40-year return period design environmental conditions

Parameter Design Point 1 Design Point 2 Design Point 3

Wave Heading [deg] 240 240 240

Hs [m] 11.9 12.7 11.0

Tp [s] 13.0 14.0 12.0

Wind Heading [deg] 210

Ws [m/s] 31.3

Current Heading [deg] 195

Cs [m/s] 1.23

Since the 1-year and the 100-year RP conditions have the same wave, wind and

current directions that give the maximum values for the turret loads, it is chosen to

conserve these environmental headings. As previously stated, it is also chosen to keep

the 10-year RP condition for the current parameter.

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Chapter 5

100-year RP Turret Loads

Investigations

5.1 Hydrostar-ARIANE-OrcaFlex Investigations

The main goal of this section is the computation of the 100-year turret load re-

sponses with the standard and proposed methods. Figure 5.1 shows the OrcaFlex model

comprising the turret and underwater cables.

Figure 5.1: OrcaFlex model.

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5.1.1 Standard Method Investigations

The design point used to characterize the 100-year RP environmental conditions is

described in Table 4.2. This combination of environmental conditions simulate the most

critical environmental characteristics that give the maximum response for the turret loads.

It is chosen to run a batch with 100 different seeds in ARIANE to ensure con-

vergence (1% difference in value) for Frad. Then, the motions from every simulations

are inputted in OrcaFlex. After running all 3h simulations taking the line dynamics into

account, a Gumbel fit is made. The statistical analysis allows the computation of the

MPM value for the Fh parameter and the Q90% for Frad. Table 5.1 gives the values

found with the 100 seeds computed.

Table 5.1: Fh and Frad values obtained with the standard approach.

Parameter Quantile Investigations

Fh [kN] 37% 3.07 E+04

Frad [kN] 37% 2.99 E+04

5.1.2 Prosed Method Investigations

The design points used to characterize the 40-year RP environmental conditions

are shown in Table 4.4. A total of 100 seeds are used to obtain the Fh and Frad responses.

Table 5.2 summarizes the findings from the OrcaFlex simulations.

Table 5.2: 40-year return period turret load responses

Parameter Q Design Point 1 Design Point 2 Design Point 3

Fh [kN] 37% 2.48 E+4 2.58 E+4 1.95 E+4

Fh [kN] 90% 3.86 E+4 3.77 E+4 2.69 E+4

Frad [kN] 37% 2.53 E+4 2.49 E+4 2.18 E+4

Frad [kN] 90% 3.65 E+4 3.49 E+4 2.64 E+4

It can be seen that the design point 1 gives the most extreme responses with the

exception of Fh Q 37%. Therefore, design point 2 is chosen for Fh, otherwise design point

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1 is used. Design point 3 is not used.

Another investigation that is done is the variation of the mean environmental

heading direction. This check looks for the wind, wave and current directions that give

the maximum turret loads responses. Two additional investigations are made for design

points 1 and 2. For each point, the environmental parameters are shifted ±15 degrees.

Table 5.3 summarizes the environmental directions analyzed. These give a package of

four simulations : ±15 deg for design point 1 and ±15 deg for design point 2.

Table 5.3: Summary of environmental directions evaluated for design points 1 and 2.

Environmental parameter Initial directions + 15 degrees - 15 degrees

Waves 240 255 225

Wind 210 235 195

Current 195 210 180

A total of 100 seeds are used for each investigation with design points 1 and 2.

Results can be seen in Table 5.4. This Table contains all turret load values obtained from

both design points 1 and 2 and it also considers the variation in environmental direction

shown in Table 5.3.

The values in bold represent the maximum values obtained for each parameter.

All maximum values are obtained with the initial direction case, except for Frad - Q

90%. However, the difference in value between the +15 degrees and the initial value is

of 0.97%. So as to simplify the procedure and due to this small discrepancy, the initial

direction is considered to give the maximum response.

As a result, all maximum values are obtained when the environment has the same

directions as in the reference. Likewise, all maximum values are obtained with design

point 1, except for Fh - Q37%.

The Fh Q37% and Frad Q90% give values smaller than the reference since they

consider the same quantile value for the short-term simulations but a less severe sea state

condition. However, by comparing the Fh Q90% for 40 RP with Fh Q37% for 100 RP

the new found values are indeed larger.

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Table 5.4: Summary of turret load values with all environmental directions evaluated for

design points 1 and 2.

Initial direction

Load parameter Q Design point 1 Design point 2

Fh [kN] 37% 2.48 E+4 2.58 E+4

Fh [kN] 90% 3.86 E+4 3.77 E+4

Frad [kN] 37% 2.53 E+4 2.49 E+4

Frad [kN] 90% 3.65 E+4 3.49 E+4

-15 degrees

Load parameter Q Design point 1 Design point 2

Fh [kN] 37% 2.29 E+4 2.33 E+4

Fh [kN] 90% 3.35 E+4 3.54 E+4

Frad [kN] 37% 2.35 E+4 2.33 E+4

Frad [kN] 90% 3.19 E+4 3.32 E+4

+15 degrees

Load parameter Q Design point 1 Design point 2

Fh [kN] 37% 2.47 E+4 2.47 E+4

Fh [kN] 90% 3.83 E+4 3.60 E+4

Frad [kN] 37% 2.56 E+4 2.43 E+4

Frad [kN] 90% 3.54 E+4 3.47 E+4

To fully apply the method proposed by [1], there is still a correction factor of 1.04

to be applied to the answers. Table 5.5 compares the reference values with the results

from the OrcaFlex simulations with the correction factor. The discrepancy is calculated

according to Equation 5.1. Where the reference values used are the ones obtained with

the standard method for comparison reasons.

Discrepancy =Result− ReferenceValue

ReferenceValue(5.1)

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Table 5.5: Results comparison with the two proposed methods.

Standard Method Proposed method

Variable Q Values Q Results Discrepancy

Fh [kN] 37% 3.07 E+4 90% 4.01 E+4 +31%

Frad [kN] 37% 2.99 E+4 90% 3.79 E+4 +27%

For Fh, the new method evaluates the 100-year response as 31% larger than the

reference value. Likewise, new method predicts a 27% larger response value for Frad if

compared with the 100 RP MPM method.

For Frad, the 40-year RP using Q90% and the 1.04 correction factor give bigger re-

sponse values than the 100-year RP Q37%. This could indicate that the current practices

underestimate the 100-year RP responses as claimed in [1]. However, their conclusion is

only drawn and supported for the maximum line tensions.

5.1.3 Conclusion

In the BV article, they used Equation 3.21 with all environmental conditions

representing the 100-year responses and several short-term simulations to compute the

exact response. The values found with the new approach were compared with this exact

response. Furthermore, their approach only evaluates the TMax for the mooring lines, not

the turret loads.

When computing the maximum tensions for the mooring line, the BV article found

errors up to +30% in their computations using the standard design point method (RP

100, Q50%) and the exact response values. Similarly, the error found between the BV

method and the standard practice for our case is +31% for Fh. The fact that both [1] and

our simulations found similar values for the discrepancies between the different calculation

methods could indicate that the 40-year RP responses computed for the turret loads are

also closer to the exact response values. However, this consistency in the discrepancy

value may as well be a coincidence.

To properly verify if the new found 100-year response value is a more suited ap-

proach, the exact response is to be computed. If the reference value is closer to the exact

response, then the standard practice is the better option. Otherwise, the new approach is

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the most suited method among the two. It does not mean however, that the new method

is the best method for the 100-year response prediction since that there may be other

points on the IFORM contour that better estimate the searched answer.

It is also possible that the design point may change with the evaluated offshore

system and the response parameters being searched. The BV article found a good design

point for the maximum tension of the mooring lines. The exact answer is to be calculated

as shown in Equation 3.21. This answer requires the computation of 3h short-term

simulations for all possible environmental conditions. Besides, there is also the need

to compute several seeds for every condition to ensure convergence. This approach is

extremely time consuming and can not be completed within the limited time frame of

the internship. Therefore, assuming that the approach proposed in the BV article can be

applied to the turret loads, the new method offers indeed a better design point. However,

this is still to be verified in the future by the comparison of the standard practice and

new method answers with the exact response.

Besides, the 40-year environmental contours are interpolated between known con-

tours (RP 1, 10, 100, 10.000). To simulate the exact 40-year RP conditions it is necessary

to derive the contour from a hindcast database.

Even though simplifications were made during the process and the response values

found can not be considered as the final 100-year response values, the investigations

created the opportunity for the subject to be further developed. Should this study be

picked up in the future and the more time consuming tasks performed, it will be possible

to verify or not the new approach for turret loads responses. Should the method be

confirmed as more precise than the standard practice, response values would be the

closest to the exact computation values, thus creating a more precise method of the

100-year RP responses computations.

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Chapter 6

Conclusion

The objective of this study is to investigate the use of an alternative approach to

compute the 100-year Return Period response for turret loads. A design point approach

based on the IFORM contour is tested. This method proposed by BV [1] advises the

use of a 40-year RP environment for long-term conditions and the use of Q90% for the

short-term simulations, as well as a correction factor of 1.04.

The procedures are done with a combination of software: Hydrostar, ARIANE

and OrcaFlex.Three design points are picked based on the environmental contours avail-

able.Also, the environmental directions are varied for each design point to ensure that

the maximum response is found. These simulations use a 90% quantile value for the

short-term simulations, thus the decision to use 100 seeds for each case to ensure the

results converge.

On one hand, the investigations lead to a response that is coherent with the BV

claim of the new method, in other words, bigger than the reference values. On the other

hand, it is not possible to claim that this response gives the closest response value to the

100-year response.

To do a full evaluation of the values found, it is necessary to compute the exact

100-year response [6] (Equation 3.21). This computation requires the study of all envi-

ronmental conditions to take into account the long-term variability. Furthermore, it is

necessary to run each condition several times to account for the short-term variability.

This procedure is extensive and requires time. The initial goal was to perform this inves-

tigation but the time reserved for these calculations were not enough to pursue the inital

plan.

Extreme analysis studies are very comprehensive and even if the initially set goals

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were not all fulfilled, progress was made. A preliminary study of the new method is

already made. The 40-year RP responses gave larger values than the standard 100-year

practice. However, in the current state of affairs it is an assumption to claim that the

new method gives indeed a more precise answer. To properly evaluate results, the exact

response must be computed.

6.1 Perspective

• The first procedure to be done is the computation of the exact 100-year RP response

based on the hindcast database. This would solve the question whether the new

approach is applicable to the turret loads and if they do indeed give a closer response

value to the exact computation.

• Computation of the 40-year RP environmental contour using the hindcast database.

• In the long-term, if the work done during the internship proves itself to be a better

method to compute the responses, it could maybe question the current standard

practices in these type of studies.

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