Video Transcript
In this video, we’re talking about
steady and turbulent flow. These two types of flow are
opposites of one another. And we may already have an
intuitive sense for what they mean. We might guess, for example, that
the flow in this river, where the boat currently is, is more steady, while the flow
farther on after the water has gone down this incline is more turbulent. That’s accurate. And in this lesson, we’re going to
see what makes for steady and turbulent flows.
Now, as we mentioned, these two
types of flow are opposites. The steadier a flow of fluid is,
the less turbulent it is, and vice versa. But then what did these terms
steady and turbulent really mean? The way we define these terms comes
down to how the speed and direction of the fluid in these flows changes. We can say that steadier flow
occurs when fluid’s speed and direction change less, while we would say more
turbulent flows occur when speed and direction change more.
It’s important to see that these
terms refer to the change in the speed and direction of flowing fluid. To see why this is so, imagine that
we have a stream of water. We can say that we’re looking down
on this stream, flowing along from left to right, as indicated by this velocity
vector. And let’s say further that all the
water in this stream is moving along with this same speed in the same direction,
left to right. Because neither the speed nor the
direction of the water in the stream is changing, we can say that this is a very
steady flow.
But then let’s compare this
original stream of water with this one shown here. In the second stream, the water is
again moving in the same direction, but this time with a much greater speed. Now, here’s a question. Which of these two flows is
steadier?
Well, that’s kind of a trick
question because both flows are actually equally steady. Even though water moves at
different speeds in the two flows, that speed, as well as the direction the water
moves, doesn’t change within each one. So then, what would be an example
of flow where speed does change?
We can think of it this way. Before, we were looking at this
stream here and this stream here from an aerial perspective. It was like looking down on a flow
of water as it moved along the ground, say. But now let’s imagine that these
are layers of fluid flow stacked on top of one another and that there are three
layers. We could think of this as looking
from the side on as water flows by, where this up here is the surface of the
water. And then as we go down, we increase
our depth until we reach the bottom.
So we have these three vertically
stacked layers of water. And each layer is moving at its own
particular speed. The layer on top is moving
slowest. And then speed increases as we
increase our depth. So what does this increase in speed
as we increase our depth cause?
Well, imagine being at the
interface between two of these three layers. At that location, the water in the
lower layer is moving faster than the water in the upper layer. And these two layers are in
contact. We can imagine what happens
here. There’s friction between these two
layers moving at different speeds. The faster-moving water tries to
speed up the slower-moving water, while the slower water tries to slow down the
faster water. This friction between layers causes
the flow of water to be disrupted. Both the speed and the direction of
the water near these layers changes. And we start to see signs of
turbulent fluid flow.
Whenever we see fluid direction
changing rapidly and especially when we see fluid moving in closed loops, those are
signs of strong change in fluid direction, which indicate turbulent flow. In a qualitative sense, it’s
possible to identify steady and turbulent flow by looking at what we can could the
streamlines of the fluid as it moves along.
To see this, let’s change our
perspective once more and imagine that now we’re looking downward on the surface of
a smoothly flowing river. These lines we’ve drawn in
represent streamlines of the water in the river as it flows along. And we can see that there’s no
change in the spacing between these lines at any point. So if we also assume that the flow
is at a steady rate from left to right, then we can say that what we’re looking at
now is an example of a very steady fluid flow.
But then, let’s say that we drop a
rock into the river, right here. If we do that, we know that this
will disrupt the streamlines. Rather than looking like this, the
lines would change to look something like this. Notice that now these streamlines
are no longer straight. That is, they do change
direction. And right behind the rock in the
stream, there’s even a closed loop. This indicates water that’s going
through an extreme change in direction as it moves through this loop. And we saw earlier that this is a
hallmark of turbulent flow.
It’s important to see though that
the level of turbulence is not the same everywhere in this section of the river
we’re looking down on. If we were to focus in on the
region right behind the stone in the river, this would indeed be the
highest-turbulence part of the flow we see. But what about another section,
say, this one over here?
In this case, we see streamlines
entering and leaving this section we’ve highlighted, basically moving in the same
direction. And the spacing between the
streamlines doesn’t change much at all, indicating that the speed is fairly constant
as well.
Just to explain that last point a
bit, about the distance between streamlines staying fairly constant, indicating a
fairly constant speed, let’s imagine that the speeds of the water moving along these
two streamlines was in fact very different. Let’s say, for example, that the
speed of the water in this streamline — we’ll call it 𝑆 sub 𝑡 for the top of the
two streamlines — is much greater than the speed of the water in this bottom
streamline — we’ll refer to it as 𝑆 sub 𝑏.
If this is true, if the water on
the top streamline is moving much faster than the water on the bottom one, then just
like we saw in our last example, there will be friction between these sections of
water moving at different speeds. The faster-moving section would
exert a stronger frictional force and tend to push its way downward towards the
lower streamline. This push would have an effect on
the direction of the lower streamline. But, nonetheless, if there was this
large speed difference between the fluid and each one, then over this patch of area
that we’ve identified, that would show up as a change in the distance between these
streamlines.
We see this going on by the way in
the more turbulent section of our flow. All that to say, when we see
streamlines, which keep the same distance apart from one another as they flow along,
this means that there’s very little or no speed difference between the fluid flowing
along those lines. Now that we know that steadier
fluid flow happens when fluid speed and direction change less, while more turbulent
flow occurs when these properties change more, let’s look at an example exercise
about steady and turbulent flow.
The diagram shows the flow of the
fluid past a circular obstacle. The gray lines represent the
direction of the fluid flow. Black regions represent solid
obstacles to the flow. In which of the two regions within
the dashed lines is the fluid flow faster?
So we’re imagining here that the
fluid in this diagram is flowing left to right. And as it does so, a solid obstacle
to that flow, right here, comes up. We could imagine this as being
something like a rock in a riverbed. And we know that such a rock causes
the fluid around it to flow differently. And indeed, we see that the gray
lines indicating the direction of fluid flow do change as the fluid avoids this
solid obstacle. Downstream of that obstacle, we see
these two regions marked out one and two. And we want to know in which of
them is the fluid flow faster on average.
Before we answer this question
though, of in which region the fluid flow is faster, let’s consider in which of the
two regions is the fluid flow more turbulent. We can recall that fluid flow is
more turbulent when a fluid’s speed and direction change more. So if we wanna figure out in which
region, one or two, the flow is more turbulent, we can look to see in which one do
the fluid speed and direction change more.
We can figure this out by
considering the gray lines, what we could call the streamlines of the fluid in this
flow. Notice how, in region one, these
two flow lines approach one another across this region, while in region two, the
flow lines are nearly parallel with one another. This might seem like a small
difference. But the changes in fluid direction
we see in region one greater than the direction changes we see in region two
indicate a more turbulent flow in region one. And indeed, this agrees with our
intuition.
We would expect a region in our
fluid right behind a large solid obstacle to be more turbulent, whereas farther
downstream, farther away from this obstacle, we expect the flow to smooth out. Okay, so if the flow in region one
is more turbulent than that in region two, how does that help us answer this
question of in which region does the fluid flow faster?
Consider again the streamlines in
region one. If we were to draw exaggerated
velocity vectors for parts of these streamlines in this region, they might look like
this. These vectors that we’ve drawn in,
even though they may overstate the motion of the fluid in this dimension, show us
that, nonetheless, because of these streamlines getting closer and closer together,
fluid in one part of this region will be pushing against fluid in the other
part. That is, fluid on this side of our
dashed line will be pushing on fluid on this side of the line, and vice versa.
Because the fluid in region one
isn’t only moving left to right but is instead also moving up and down we could say
from this perspective, some of that fluid velocity will be negated as the fluid
flows against itself. This will lead on average across
the whole region to a slowing down of this fluid. This is in contrast to the fluid in
region two. Instead of some fluid in the region
pushing against fluid in other parts of it, it’s all essentially moving in lockstep
and therefore fairly rapidly from left to right. Because the fluid in region one
resists its own motion more than the fluid in region two, we can say that it’s the
fluid in region two which flows faster.
Let’s look now at a second example
exercise.
The diagram shows the flow of a
fluid past a line perpendicular to the flow. The gray lines represent the
direction of fluid flow. Black regions represent solid
obstacles to the flow. In which of the regions within the
dashed lines is the fluid flow faster? In which of the regions within the
dashed lines is the fluid flow steadier?
Okay, so we see in our diagram
fluid flowing along. And we can say that it’s moving
from left to right as we’re looking at it. As the fluid moves along, there’s
an obstacle in its path right here, something solid in the way that won’t move. In response, and we can see this in
the flow lines, the fluid changes direction to avoid this obstacle. Downstream of the obstacle, we have
these two regions marked out one and two. We want to know, first, in which of
the two regions is the fluid flow faster and, secondly, in which of the two is it
steadier.
Now, actually, it’s a bit easier to
answer this second part of this question before we answer the first. Let’s consider whether fluid flow
is steadier in region one or in region two. And to help us figure that out, we
can recall that fluid flow is steadier when the fluid’s speed and direction change
less. So in a given region, if the fluid
there isn’t changing much in speed or direction, then that indicates a fairly steady
fluid flow.
If we look at region one in our
diagram, we can see right away that the fluid direction is changing significantly in
this region. In this region, there is part of a
closed loop of fluid flow. These closed loops show the
direction of fluid changing drastically and are hallmarks of turbulent flow. By contrast, the streamlines in
region two are nearly parallel with one another. They don’t change direction much at
all and also show us that the speed of fluid in this region doesn’t change much
either.
This clarifies our answer to the
second part of this question. We can say that it’s in region two
that the fluid flow is steadier because it’s in this region that fluid speed and
direction change less.
And now for the first part of our
question, which asks in which of the two regions the fluid flow is faster, now it’s
a bit counterintuitive. But actually, there’s a correlation
between steady fluid flow and faster fluid speed. The reason for this is that when
fluid is flowing steadily along, that means its direction isn’t changing very
much. It’s not interfering with
itself. The effect of that interference,
the fluid pushing against itself, would be to slow down the average speed of the
fluid.
For example, consider the fluid in
region one in our diagram. We can assume that in this closed
loop we see, the fluid is flowing in one direction in one part of the loop and in
the other direction in the other part. The fact that within this region
some fluid is flowing one way and some is flowing in the opposite direction shows us
that fluid in this region is strongly interfering with itself. It’s not able to establish a steady
flow. And therefore, it doesn’t have much
opportunity to pick up speed. And that means that the average
speed of the fluid in this region is lower than that of a region within the same
flow but where the fluid is not pushing against itself quite so much.
So not only is region two the place
where fluid flow is steadier, it’s also the region where fluid flow is faster. In general, the steadier a fluid
flow is, the faster it can move along.
Let’s summarize now what we’ve
learned about steady and turbulent flow. In this lesson, we saw that steady
and turbulent fluid flows are opposites. We saw further that steady flow
happens when fluid speed and direction change less, that is, are fairly constant,
while turbulent flow is indicated where fluid speed and direction change more. Along with this, we saw that in
diagrams of fluid flow, regions that display closed loops, closed streamlines
indicating fluid direction, are likely to be regions where turbulent flow is taking
place, whereas regions with nearly parallel flow lines that don’t change direction
much indicate regions of relatively steady fluid flow.
And lastly, we emphasized that
these two types of flows, steady and turbulent, are defined in terms of the changes
that do or do not occur in fluid speed and direction. This is a summary of steady and
turbulent flow.