Monday, March 9, 2026

Understanding Failure in Marine and Coastal Engineering

 


From Root Causes to the Unconscious Dimension of Engineering Judgment

Modern marine and coastal infrastructure operates within some of the most demanding environments on Earth. Offshore platforms, artificial islands, breakwaters, quay walls, pipelines, and marine terminals must withstand an intricate combination of environmental loading, geotechnical uncertainty, operational demands, and long-term material degradation.

In regions such as the Arabian Gulf and Red Sea, these challenges are intensified by:

  • Extremely high salinity and temperature, accelerating corrosion processes

  • Shallow shelf morphodynamics, affecting wave transformation and sediment transport

  • Soft marine soils and carbonate sediments, influencing foundation performance

  • Rapid mega-project development, compressing design and construction schedules

Within such environments, understanding not only how systems perform but how and why they fail becomes a central engineering responsibility.

Failures may arise from structural deficiencies, geotechnical instability, hydraulic misjudgment, material degradation, operational mismanagement, or a combination of these factors. Regardless of discipline or scale, every failure demands a systematic and disciplined investigation aimed at identifying its true root causes.


Failure Cause Characterization in Marine Systems

Failure triggers in complex engineering systems can generally be categorized into three fundamental domains, collectively referred to as Failure Cause Characterization (Márquez, 2007):

Human Causes

Errors of omission or commission originating from human actions or decisions.

Examples in marine infrastructure include:

  • Misinterpretation of metocean data

  • Incorrect application of wave transformation models

  • Improper construction sequencing in reclamation works

  • Inadequate inspection regimes for offshore structures

These human errors often manifest later as physical failures.


Physical Causes

The direct technical mechanisms that produce failure.

Typical examples in marine-coastal engineering include:

  • Scour development around piles or monopiles

  • Hydraulic instability of breakwater armour layers

  • Foundation settlement in carbonate soils

  • Fatigue cracking in offshore structural members

  • Liquefaction under cyclic wave loading

  • Progressive corrosion of steel components in high-salinity waters

Physical causes represent the observable mechanisms, but they rarely explain the entire failure chain.


Latent Causes

Deficiencies embedded within management systems, governance structures, or organizational practices that allow failures to emerge.

Examples frequently observed in large Gulf projects include:

  • Over-reliance on global datasets (e.g., ERA5) without local calibration

  • Insufficient site investigation density in reclaimed island developments

  • Design schedules driven by commercial pressures rather than technical validation

  • Fragmented coordination between hydrodynamic, geotechnical, and structural teams

Latent causes are particularly dangerous because they exist upstream of observable failures and often remain hidden until a major incident occurs.


The Asset Management Perspective

Failure analysis is inseparable from asset management. Within the ISO 55000 asset management framework, performance evaluation must address not only outcomes but also the decision processes that produced them.

ISO guidance emphasizes that asset performance should be assessed by asking:

Have the asset management objectives been achieved?
If not, why not?

This question directly invokes the investigation of latent causes and decision-making adequacy.

For marine infrastructure—where assets may operate for 30–50 years under aggressive environmental conditions—Root Cause Failure Analysis (RCFA) becomes an essential component of lifecycle management.

Comparable principles are embedded within quality management systems such as ISO 9001, which require structured reporting, investigation procedures, and continuous improvement mechanisms.


Failure Investigation in Marine Infrastructure

A rigorous failure investigation typically requires the following minimum components:

Investigation Team Definition

A multidisciplinary team including:

  • Structural engineers

  • Geotechnical specialists

  • Coastal and hydraulic engineers

  • Materials scientists

  • Operations personnel

  • Independent technical reviewers


Data Collection

Systematic documentation of the incident:

  • Date and time of failure

  • Operational conditions (wave, tide, current)

  • Structural loading conditions

  • GIS and location data

  • Inspection history


Impact Evaluation

Assessment of:

  • Structural damage

  • Operational disruption

  • Environmental consequences

  • Economic losses


Technical Description of the Asset

This includes:

  • Structural configuration

  • Foundation type

  • Materials used

  • Design assumptions and codes applied


Root Cause Identification

Identification of both direct and systemic causes.


Corrective and Preventive Recommendations

Actions addressing both:

  • Immediate technical issues

  • Long-term systemic improvements


Supporting Evidence

Including:

  • Photographs and inspection reports

  • Monitoring data

  • Construction records

  • Numerical model results


Lessons Learned

Formal documentation for integration into future design and operational procedures.


Root Cause Analysis and Validation

Modern engineering practice relies on standardized RCA frameworks such as BS EN 62740, which provide structured methodologies for identifying and validating root causes.

The most critical phase of this process is validation.

Validation ensures that the identified cause truly explains the failure mechanism and can guide corrective action.

Common validation approaches include:

Independent Technical Review

External experts assess the investigation to eliminate bias and confirm methodological rigor.


Experimental or Physical Testing

Hydraulic models, structural testing, or laboratory experiments reproduce the failure mechanism under controlled conditions.

For example:

  • Breakwater stability verification in physical wave flumes

  • Soil strength characterization through laboratory geotechnical testing


Numerical Simulation

Advanced simulations may include:

  • Finite element modeling of structural behavior

  • Computational fluid dynamics (CFD) simulations of hydraulic conditions

  • Monte Carlo simulations of reliability and probabilistic loading

However, simulation models must be used cautiously. If the model assumptions do not realistically represent the physical system, the conclusions may become misleading.


The Limits of Engineering Knowledge

Despite the sophistication of modern analytical tools, all investigations operate within the limits of human knowledge.

A useful conceptual framework divides knowledge into four categories:

Known Knowns

Established facts, validated theories, and verified observations.

Examples include:

  • Wave mechanics theory

  • Structural mechanics principles

  • Verified soil properties


Known Unknowns

Recognized uncertainties such as:

  • Parameter variability in soil models

  • Measurement errors in wave data

  • Modeling assumptions

These uncertainties can often be managed through safety factors and probabilistic design methods.


Unknown Unknowns

Completely unforeseen factors such as:

  • undocumented seabed anomalies

  • unexpected construction deviations

  • undocumented third-party interventions

These events often appear only after failure has occurred.


Unknown Knowns

A concept explored by philosopher Slavoj Žižek, referring to knowledge that exists within the unconscious.

These are insights accumulated through years of experience, pattern recognition, and professional exposure.

In engineering practice, this is often described as expert intuition.


The Unconscious Dimension of Engineering Judgment

Engineering decisions are not purely analytical. Beyond explicit calculations and models, expert judgment frequently relies on internalized knowledge structures formed through experience.

An experienced marine engineer may detect inconsistencies in a design report or modeling result before being able to formally articulate the reason.

What appears to be intuition is often a rapid synthesis of accumulated technical knowledge.

Maintaining a well-informed unconscious therefore becomes an intellectual responsibility. It is developed through:

  • Continuous reading and study

  • Field observations and inspections

  • Exposure to real failure cases

  • Interaction with multidisciplinary experts

Many significant engineering insights emerge not during formal analysis but during moments of reflection—when the mind processes information beyond conscious attention.


Conclusion

In marine and coastal engineering, failures rarely originate from a single cause. They emerge from a complex interaction of technical mechanisms, human decisions, and organizational structures.

Effective failure analysis therefore requires more than technical calculation. It demands:

  • systematic investigation

  • multidisciplinary collaboration

  • rigorous validation methods

  • and the cultivated intuition of experienced engineers

In this sense, engineering judgment operates at the intersection of science, experience, and reflection.

Intuition is not the opposite of rigor.

It is its long-term byproduct.


References

Márquez, A. C. (2007). The Maintenance Management Framework: Models and Methods for Complex Systems Maintenance. Springer.

ISO (2014). ISO 55000: Asset Management — Overview, Principles and Terminology. International Organization for Standardization.

BSI (2015). BS EN 62740: Root Cause Analysis (RCA). British Standards Institution.

PIANC (2014). Harbour Approach Channels Design Guidelines. PIANC.

BSI (2018). BS 6349 Series: Maritime Works. British Standards Institution.

DNV (2021). DNV-ST-N001: Marine Operations and Marine Warranty. Det Norske Veritas.

ISO (2019). ISO 19901-1: Metocean Design and Operating Considerations. International Organization for Standardization.

Žižek, S. (2012). Less Than Nothing: Hegel and the Shadow of Dialectical Materialism. Verso.

Understanding Random Waves in Breakwater Hydraulic Modelling

 

From Pierson–Moskowitz to JONSWAP — A Practical Explanation for Young Engineers

When engineers design coastal structures such as breakwaters, seawalls, and harbour protection systems, they rarely test them against a single perfect wave.

Real oceans do not produce regular waves.

Instead, they generate random wave fields composed of thousands of interacting wave components.

Because of this, modern hydraulic modelling uses wave spectra rather than individual waves.

A classic experimental study on this topic is the work of Kloppman and Van der Meer, who investigated random wave behaviour in front of reflective coastal structures using laboratory wave flumes. 

Their research shows how wave spectra change near structures and why engineers must carefully measure incident and reflected waves when testing breakwaters.

This article explains the core ideas behind that research in a practical way.


1 The difference between regular waves and random waves

In basic wave theory courses, we usually begin with a simple wave:

𝜂(𝑥,𝑡)=𝑎cos(𝑘𝑥𝜔𝑡)

Where:

  • 𝑎 = wave amplitude

  • 𝑘 = wave number

  • 𝜔 = angular frequency

  • 𝑥 = distance

  • 𝑡 = time

This represents a perfect sinusoidal wave.

However, the ocean is not composed of a single sine wave.

Instead, the sea surface is better described as a superposition of many waves with different frequencies and amplitudes.

Mathematically,

𝜂(𝑥,𝑡)=𝑖=1𝑁𝑎𝑖cos(𝑘𝑖𝑥𝜔𝑖𝑡+𝜙𝑖)

This means the water surface is the sum of many components.

Instead of tracking every wave individually, engineers describe the wave field using spectral energy distribution.




2 What is a wave spectrum?

A wave spectrum describes how wave energy is distributed across frequencies.

The spectrum function is written as

𝑆(𝑓)

Where

  • 𝑓 = frequency

  • 𝑆(𝑓) = wave energy density at that frequency

The total wave variance becomes

𝑚0=0𝑆(𝑓)𝑑𝑓

The significant wave height is related to this variance:

𝐻𝑠=4𝑚0

This is the fundamental relationship used in both numerical wave models and hydraulic laboratories.

The experimental work of Kloppman and Van der Meer used this spectral framework to analyze wave fields in front of reflective structures.


3 The Pierson–Moskowitz spectrum

The Pierson–Moskowitz spectrum represents a fully developed sea, meaning the wind has blown long enough for waves to reach equilibrium.

It is defined as

𝑆𝑃𝑀(𝑓)=𝛼𝑔2(2𝜋)4𝑓5exp(𝛽(𝑓𝑝𝑓)4)

Typical constants:

𝛼=0.0081
𝛽=0.74

Where:

  • 𝑓𝑝 = peak frequency

  • 𝑔 = gravity

This spectrum produces a smooth energy curve.

Physically this means

  • energy spreads over a wider range of frequencies

  • waves are less concentrated around the peak.

This behaviour was also observed in laboratory measurements where broad spectra damp standing-wave oscillations near reflective structures.


4 The JONSWAP spectrum

The JONSWAP spectrum modifies the Pierson–Moskowitz spectrum to represent fetch-limited seas, such as the North Sea or Arabian Gulf.

It introduces a peak enhancement factor.

The spectrum becomes

𝑆𝐽(𝑓)=𝑆𝑃𝑀(𝑓)𝛾exp[(𝑓𝑓𝑝)22𝜎2𝑓𝑝2]

Where

𝛾3.3

This parameter sharpens the spectral peak.

Typical values

𝜎={0.07𝑓𝑓𝑝0.09𝑓>𝑓𝑝

Physically this means:

  • wave energy is concentrated around the peak frequency

  • wave groups become stronger

  • wave heights fluctuate more intensely.

The hydraulic experiments showed that JONSWAP spectra produce clearer standing wave patterns near reflective structures than Pierson–Moskowitz spectra.


5 Why random waves create standing patterns near breakwaters

When waves hit a reflective structure, such as a vertical wall or breakwater, they reflect back toward the sea.

The incident and reflected waves interact.

Linear theory shows the total wave elevation becomes

𝜂(𝑥,𝑡)=𝑎cos(𝑘𝑥𝜔𝑡)+𝑎𝑅cos(𝑘𝑥+𝜔𝑡+𝜙)

Where

  • 𝑅 = reflection coefficient

This produces nodes and antinodes, forming a standing wave pattern.

Laboratory experiments measured these variations using wave gauges placed along the flume.

The measurements confirmed that

  • nodes occur where destructive interference happens

  • antinodes occur where wave energy concentrates.

The experiments also showed that the standing pattern is strongest near the structure and gradually fades offshore.


6 Hydraulic modelling experiment

The study performed tests in a glass-walled wave flume approximately

  • 45 m long

  • 1 m wide

A piston-type wave generator produced random waves.

More than 30 wave gauges were used to measure the spatial variation of the wave field.

Two reflective structures were tested:

  1. vertical wall

  2. rubble mound breakwater

Measurements showed

  • wave spectra change significantly near reflective structures

  • nodes and antinodes form in the significant wave height

  • the distance between these oscillations increases offshore.

These results match predictions from linear wave interference theory.


7 Why this matters for breakwater design

Understanding spectral waves is critical because

1️⃣ Breakwaters experience random waves, not regular waves.

2️⃣ Wave reflection can amplify local wave heights.

3️⃣ Standing wave patterns affect:

  • armour stability

  • toe scour

  • overtopping behaviour.

Hydraulic modelling therefore uses random wave spectra such as JONSWAP or Pierson–Moskowitz to realistically reproduce ocean conditions.


8 Key takeaway for young coastal engineers

If you remember only three ideas, remember these:

1. Real seas are random.
Engineers must model waves using spectra.

2. JONSWAP and Pierson–Moskowitz describe how wave energy is distributed.

3. When waves meet structures, reflection creates standing wave patterns that strongly influence hydraulic performance.

Understanding these ideas is the first step toward mastering breakwater hydraulic modelling.


Conclusion

Hydraulic modelling remains one of the most powerful tools in coastal engineering.

By combining

  • spectral wave theory

  • laboratory wave generation

  • precise measurements of reflection and interference

engineers can understand how real seas interact with coastal structures.

The experiments discussed here demonstrate that even complex random wave fields can be interpreted using relatively simple theoretical principles.

This combination of theory and physical modelling continues to guide the design of modern breakwaters around the world.


References

Kloppman, G., and Van der Meer, J. W.
Random Wave Measurements in Front of Reflective Structures.
Journal of Waterway, Port, Coastal, and Ocean Engineering.