Introduction to CFD Chapter 5: Introduction to Turbulence and RANS Modeling

This chapter introduces the physical nature of turbulent flows and explains why turbulence modeling is necessary in practical CFD. The statistical description of turbulence, the concept of scale separation, and the emergence of the Reynolds-averaged framework are discussed. The chapter concludes with an overview of the RANS–Boussinesq hypothesis and the role of eddy-viscosity models in engineering simulations.

 

Why Turbulence Dominates Engineering Flows

Most flows encountered in engineering applications operate at sufficiently high Reynolds numbers for turbulence to develop. Examples include internal duct flows, boundary layers on external surfaces, wakes behind bluff bodies, and mixing processes.

Turbulence strongly influences:

  • Pressure losses and drag

  • Heat and mass transfer rates

  • Mixing efficiency

  • Noise generation

  • Flow-induced vibrations

As a result, turbulence modeling often determines whether a CFD prediction is useful for design.


Qualitative Characteristics of Turbulent Flow

Turbulent flows exhibit a combination of features that distinguish them from laminar motion:

  • Three-dimensionality
    Velocity fluctuations evolve in all spatial directions, even when the mean flow appears two-dimensional.

  • Unsteadiness
    The instantaneous flow field changes continuously in time, across a wide range of time scales.

  • Wide range of scales
    Large, energetic structures coexist with much smaller, rapidly evolving eddies.

  • Enhanced transport
    Momentum, heat, and species are transported far more efficiently than by molecular diffusion alone.

Because of this complexity, turbulence is best described statistically rather than instantaneously.


Reynolds Number and the Onset of Turbulence

The balance between inertial effects and viscous damping governs whether turbulence can be sustained. At sufficiently high Reynolds numbers, nonlinear inertial mechanisms dominate and enable the formation of unsteady vortical structures.

In practice, the transition to turbulence depends on:

  • Geometry

  • Flow disturbances

  • Surface roughness

  • Free-stream turbulence levels

This explains why nominal Reynolds-number thresholds vary across different flow configurations.


Statistical Description of Turbulence

Since predicting exact instantaneous flow realizations is impractical, turbulence is approached through statistical averaging.

Reynolds introduced the idea of decomposing flow quantities into:

  • A mean (time-averaged or ensemble-averaged) component

  • A fluctuating component capturing turbulent motion

This decomposition allows engineers to focus on predictable mean quantities while accounting for the influence of fluctuations through additional modeled terms.


The Reynolds-Averaged Framework

Applying averaging procedures to the governing equations leads to transport equations for the mean flow. These equations retain the same structure as the laminar equations, with additional stress-like terms arising from velocity fluctuations.

These additional terms represent the momentum transport induced by turbulence and cannot be expressed directly using mean flow variables alone. This difficulty is known as the turbulence closure problem.


Physical Meaning of Reynolds Stresses

The Reynolds stresses describe how turbulent fluctuations transport momentum. Physically, they:

  • Redistribute momentum across the flow

  • Modify velocity profiles

  • Influence separation and reattachment

  • Control turbulent diffusion rates

Accurate turbulence modeling revolves around providing a reliable approximation for these stresses.


Energy Cascade and Turbulent Scales

Turbulence organizes itself through a hierarchical transfer of energy across scales:

Large scales

  • Comparable to geometric dimensions

  • Strongly influenced by boundary conditions and mean flow gradients

  • Responsible for most of the kinetic energy

Intermediate scales

  • Less dependent on geometry

  • Governed primarily by inertial interactions

Small scales

  • Weakly influenced by geometry

  • Dominated by viscous effects

  • Responsible for dissipating kinetic energy into heat

This cascade process explains why resolving all turbulent scales directly is computationally prohibitive for most engineering flows.


Implications for CFD

Fully resolving all turbulent scales requires extremely fine spatial and temporal resolution, which limits direct numerical simulation to research-scale problems.

Engineering CFD therefore, relies on approaches that:

  • Avoid resolving the smallest scales explicitly

  • Represent their influence through modeling assumptions

This leads naturally to averaged or filtered formulations.


Approaches to Turbulent Flow Simulation

Three broad strategies exist:

Direct Numerical Simulation (DNS)

  • Resolves all turbulent scales

  • Provides the most detailed information

  • Computationally infeasible for industrial applications

Scale-Resolving Simulations (SRS)

  • Resolve large-scale unsteadiness

  • Model only the smallest scales

  • Include LES, DES, and related methods

Reynolds-Averaged Navier–Stokes (RANS)

  • Solve equations for mean quantities

  • Model the full effect of turbulence

  • Enable steady-state simulations

  • Remain the dominant industrial approach

This chapter focuses on the RANS framework.


Motivation for Steady RANS Models

Although turbulence is inherently unsteady, many engineering questions involve:

  • Time-averaged forces

  • Mean pressure losses

  • Average heat transfer rates

RANS models enable:

  • Faster simulations

  • Reduced computational cost

  • Simplified post-processing

These advantages explain their widespread use despite known limitations.


Boussinesq Hypothesis and Eddy Viscosity

The Boussinesq hypothesis relates Reynolds stresses to mean velocity gradients through a modeled turbulent viscosity.

This assumption:

  • Treats turbulence as an enhanced momentum diffusion process

  • Preserves analogy with laminar stress–strain relationships

  • Greatly simplifies closure modeling

Its success stems from robustness and efficiency, though it cannot capture all anisotropic turbulence effects.


Families of RANS Turbulence Models

Within the Boussinesq framework, several model classes exist:

Algebraic and zero-equation models

  • Rely on local flow quantities

  • Very economical

  • Limited generality

One-equation models

  • Introduce a single transported turbulence variable

  • Well suited for attached wall-bounded flows

Two-equation models

  • Solve transport equations for turbulence energy and a scale variable

  • Balance robustness and accuracy

  • Form the backbone of most industrial simulations

More advanced closures relax the Boussinesq assumption and are addressed in later chapters.


Engineering Intuition

  • Turbulence modeling trades physical detail for computational feasibility

  • Mean-flow accuracy depends more on modeling assumptions than solver settings

  • Eddy-viscosity models perform best when turbulence is close to isotropic

  • Boundary layers, separation, and curvature challenge simple closures

A clear understanding of turbulence physics helps interpret RANS results realistically.


Study Priorities

If short on time, focus on:

  1. Physical characteristics of turbulent flow

  2. Statistical nature of turbulence

  3. Energy cascade concept

  4. Meaning of Reynolds stresses

  5. Purpose of RANS modeling

  6. Role of the Boussinesq hypothesis


Key Takeaways

  • Turbulence is a multiscale, three-dimensional, unsteady process.

  • Statistical descriptions enable practical modeling.

  • Reynolds averaging introduces unclosed stress terms.

  • Energy cascades from large to small scales.

  • RANS models remain essential for industrial CFD.

  • Eddy-viscosity closures balance robustness and efficiency.

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Introduction to CFD Chapter 6: Compressible Flow

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Introduction to CFD Chapter 4: Fundamentals of the Finite Volume Method