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This video from The Efficient Engineer is
sponsored by Brilliant.
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One of the very first things you learn in
fluid mechanics is the difference between
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laminar and turbulent flow.
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And for good reason - these two flow regimes
behave in very different ways and, as we’ll
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see in this video, this has huge implications
for fluid flow in the world around us
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Here we have an example of the laminar flow
regime.
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It's characterised by smooth, even flow.
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The fluid is moving horizontally in layers,
and there is a minimal amount of mixing between
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layers.
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As we increase the flow velocity we begin
to see some bursts of random motion.
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This is the start of the transition between
the laminar and turbulent regimes.
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If we continue increasing the velocity we
end up with fully turbulent flow.
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Turbulent flow is characterised by chaotic
movement and contains swirling regions called
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eddies.
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The chaotic motion and eddies result in significant
mixing of the fluid.
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If we record the velocity at a single point
in steady laminar flow, we'll get data that
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looks like this.
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There are no random velocity fluctuations,
and so in general laminar flow is fairly easy
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to analyse.
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For turbulent flow we’ll get data that looks
like this.
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This flow is much more complicated.
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We can think of the velocity as being made
up of a time-averaged component, and a fluctuating
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component.
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The larger the fluctuating component, the
more turbulent the flow.
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Because of its chaotic nature, analysis of
turbulent flow is very complex.
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Since laminar and turbulent flow are so different
and need to be analysed in different ways,
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we need to be able to predict which flow regime
is likely to be produced by a particular set
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of flow condition
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We can do this using a parameter which was
defined by Osborne Reynolds in 1883.
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Reynolds performed extensive testing to identify
the parameters which affect the flow regime,
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and came up with this non-dimensional parameter,
which we call Reynolds number.
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It's used to predict if flow will be laminar
or turbulent.
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Rho is the fluid density, U is the velocity,
L is a characteristic length dimension, and
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Mu is the fluid dynamic viscosity.
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The equation is sometimes written as a function
of the kinematic viscosity instead, which
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is just the dynamic viscosity divided by the
fluid density.
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The characteristic length L will depend on
the type of flow we are analysing.
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For flow past a cylinder it will be the cylinder
diameter.
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For flow past an airfoil it will be the chord
length.
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And for flow through a pipe it will be the
pipe diameter.
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Reynolds number is useful because it tells
us the relative importance of the inertial
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forces and the viscous forces.
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Inertial forces are related to the momentum
of the fluid, and so are essentially the forces
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which cause the fluid to move.
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Viscous forces are the frictional shear forces
which develop between layers of the fluid
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due to its viscosity.
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If viscous forces dominate flow is more likely
to be laminar, because the frictional forces
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within the fluid will dampen out any initial
turbulent disturbances and random motion.
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This is why Reynolds number can be used to
predict if flow will be laminar or turbulent.
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If inertial forces dominate, flow is more
likely to be turbulent.
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But if viscous forces dominate, it’s more
likely to be laminar.
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And so smaller values of Reynolds number indicate
that flow will be laminar.
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The Reynolds number at which the transition
to the turbulent regime occurs will vary depending
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on the type of flow we are dealing with.
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These are the ranges usually quoted for flow
through a pipe, for example.
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Under very controlled conditions in a lab
the onset of turbulence can be delayed until
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much larger Reynolds numbers.
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Most flows in the world around us are turbulent.
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The flow of smoke out of a chimney is usually
turbulent.
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And so is the flow of air behind a car travelling
at high speed.
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The
flow of blood through vessels on the other
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hand is mostly laminar, because the characteristic
length and velocity are small.
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This is fortunate because if it were turbulent
the heart would have to work much harder to
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pump blood around the body.
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To understand why this is, let's look at how
the flow regime affects flow through a circular
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pipe.
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The flow velocity right at the pipe wall is
always zero.
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This is called the no-slip condition.
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For fully developed laminar flow, the velocity
then increases to reach the maximum velocity
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at the centre of the pipe.
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The velocity profile is parabolic.
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For turbulent flow the profile is quite different.
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We still have the no-slip condition, but the
average velocity profile is much flatter away
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from the wall.
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This is because turbulence introduces a lot
of mixing between the different layers of
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flow, and this momentum transfer tends to
homogenise the flow velocity across the pipe
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diameter.
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Note that I have shown the time-averaged velocity
here.
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The instantaneous velocity profile will look
something like this.
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In pipe flow one thing we are particularly
interested in is pressure drop.
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Across any length of pipe there will be a
drop in pressure due to the frictional shear
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forces acting within the fluid.
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The pressure drop in turbulent flow is much
larger than in laminar flow, which explains
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why the heart would have to work harder if
blood flow was mostly turbulent!
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We can calculate Delta-P along the pipe using
the Darcy-Weisbach equation.
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It depends on the average flow velocity, the
fluid density and a friction factor f.
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For laminar flow the friction factor can be
calculated easily.
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It is just a function of the Reynolds number.
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If we combine these two equations we can see
that the pressure drop is proportional to
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the flow velocity.
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But for turbulent flow calculating f is more
complicated.
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It is defined by the Colebrook equation.
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f appears on both sides of the equation, so
it needs to be solved iteratively.
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Unlike laminar flow, for which the pressure
drop is proportional to the flow velocity,
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it turns out that for turbulent flow it is
proportional to the flow velocity squared.
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And it also depends on the roughness of the
pipe surface.
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Epsilon is the height of the pipe surface
roughness, and the term Epsilon/D is
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called the relative roughness.
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Surface roughness is important for turbulent
flow because it introduces disturbances into
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the flow, which can be amplified and result
in additional turbulence.
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For laminar flow it doesn't have a significant
effect because these disturbances are dampened
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out more easily by the viscous forces.
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Since the Colebrook equation is so difficult
to use, engineers usually use its graphical
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representation, the Moody diagram, to look
up friction factors for different flow conditions.
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Where flow is laminar the friction factor
is only a function of Reynolds number, so
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we get a straight line on the Moody diagram.
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For turbulent flow you select the curve corresponding
to the relative roughness of your pipe, and
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you can look up the friction factor for the
Reynolds number of interest.
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So we know that if Reynolds number is large,
inertial forces dominate, and the flow is
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turbulent.
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But even for turbulent flow viscous forces
can be significant in the boundary layers
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that develop at solid walls.
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Because of the no-slip condition, shear stresses
are large close to a wall.
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This means that in a turbulent boundary layer
there remains a very thin area close to the
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wall where viscous forces dominate and flow
is essentially laminar.
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We call this the laminar, or viscous, sublayer.
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Its thickness decreases as Reynolds number
increases.
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Above the laminar sublayer there is the buffer
layer, where both viscous and turbulent effects
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are significant.
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And above the buffer layer turbulent effects
are dominant.
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If the roughness of a surface is contained
entirely within the thickness of the laminar
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sublayer, the surface is said to be hydraulically
smooth, because the roughness has no effect
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on the turbulent flow above the sublayer.
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This is important in pipe flow because, as
can be seen from the Moody diagram, flow in
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smooth pipe has a lower friction factor and
so smaller pressure drop than flow in rough
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pipe.
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We can see that for a given roughness the
friction factors converge to a constant value
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to the right of this dashed line, meaning
that at high Reynolds number the friction
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depends only on the relative roughness.
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At these high Reynolds numbers the thickness
of the laminar sublayer is extremely thin,
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and so the effect of the surface roughness
is governing.
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Modelling turbulent flow through a pipe is
fairly simple, but most scenarios are far
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more complex.
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It’s worth talking more about why analysis
of turbulent flow is so complicated, and a
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lot of it has to do with the turbulent eddies
we saw at the start of the video.
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Large eddies contain a lot of kinetic energy.
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Over time the energy in these large eddies
feeds the creation of progressively smaller
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eddies, until at the smallest scale the turbulent
energy in minuscule eddies dissipates as heat,
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due to frictional forces caused by the fluid
viscosity.
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We can think of the energy in the flow as
cascading from the largest to the smallest
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eddies, and so this concept is called the
energy cascade.
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The energy cascade was summarised in a very
elegant way by the physicist Lewis Fry Richardson,
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who wrote that "Big whirls have little whirls
that feed on their velocity, and little whirls
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have lesser whirls, and so on to viscosity".
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Because of this behaviour, turbulence involves
a huge range of length and time scales.
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This makes analysis of turbulent flow very
complex, to the point that it is probably
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the most significant challenge facing the
field of Fluid Mechanics.
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For complex scenarios like flow past an airfoil,
we can't accurately describe the fluid behaviour
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using simple equations.
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So to analyse the flow we have to use either
experimentation or numerical methods, or a
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combination of the two.
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Modelling flow using numerical methods is
the field of Computational Fluid Dynamics.
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It essentially involves using computational
power to solve the Navier-Stokes equations,
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which is a system of partial differential
equations that describes the behaviour of
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fluids, but is difficult to solve.
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To do this we model the fluid domain around
the airfoil as a mesh of discrete elements,
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define boundary conditions and fluid properties,
and apply an appropriate assessment technique
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to find a solution.
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I mentioned earlier that one of the main challenges
when dealing with turbulence is capturing
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the wide range of length scales associated
with the turbulent eddies.
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There are three main techniques which are
used to simulate flow in CFD, and they differ
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mainly in how they treat turbulence on these
different scales.
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First we have Direct Numerical Simulation.
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This involves solving the Navier-Stokes equations
down to even the smallest scales, and so all
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turbulent eddies are fully resolved, meaning
that they are simulated explicitly.
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This is very computationally expensive, and
isn’t a practical solution for the vast
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majority of fluid flow problems.
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Next we have Large Eddy Simulation.
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This technique resolves the large scale eddies
explicitly, but small scale eddies are filtered
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out and are modelled, using what is known
as a subgrid-scale model.
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LES is much less computationally expensive
than DNS.
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Finally we have the Reynolds-Averaged Navier-Stokes
technique,
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which is the least computationally expensive of the three techniques.
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This is a time-averaged method which doesn’t
resolve eddies explicitly at all.
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Instead it models the effect of eddies using
the concept of turbulent viscosity.
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Several different turbulence models exist,
like the K-Epsilon or K-Omega models, with
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different models being better suited to different
problem types.
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As is so often the case in engineering, experience
and intuition will need to be used to determine
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00:13:22,610 --> 00:13:27,230
which techniques and models are best suited
to a particular problem.
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00:13:27,230 --> 00:13:31,550
When it comes to troubleshooting problems
in the real world, the importance of engineering
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That's it for this look at laminar and turbulent
flow.
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00:14:50,040 --> 00:14:51,319
Thanks for watching.
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