PROFESSOR: So let's look at a little more detail
at the equilibrium size of respiratory droplets
that are emitted during breathing,
or coughing, or speaking.
And the key idea is that these droplets are not pure liquid.
As explained in the wells curve, pure droplets
that are small enough will shrink completely
and evaporate.
However, these droplets contain a significant amount
of solutes.
And those solutes, in the case of mucus coming from your lungs
or from your vocal cords, your nasal pharynx,
are full of proteins and other macromolecules, carbohydrates.
And also there are always in bodily fluids plenty
of dissolved salts such as sodium and chloride or calcium
or potassium ions.
Also, in saliva, many of these species are present,
although it's not quite as thick of a liquid.
And of course, virions as well will find themselves in here,
and it also constitutes solutes.
So the idea is that we don't just have a pure liquid.
So there is some initial volume fraction
of solute in the liquid.
And in addition to that, most of these liquids --
sorry, the solutes I should say are
charged and thus hygroscopic.
What that means is that, of course, the salt,
those ions are literally charged species, but also the proteins
and other macromolecules that many
charge residues and sites along the molecule, which
attract water.
And essentially, there is a layer
of bound water solvating all of these species I just mentioned,
including the virus.
So I'll just sketch that there's lots
of bound water, which is surrounding each species,
including the virus.
There's essentially a layer of water
mostly around these molecules here and other species.
So it's solutes plus the bound water
that's coming from solvation of these molecules in liquid.
So that water is pretty firmly attached.
And even if you dry the material, a lot of that water
will still be left over.
It takes a significant amount of energy to remove it.
And so if we think that --
if we describe there is initial volume of the droplet V_O,
and a radius R_0, so let's say it's initially
a circular droplet, there is an initial amount
of solid, V_s, which is phi_s^0 times V_0.
So there's a certain amount of solutes in there which cannot
be removed.
So the water can evaporate, but the solutes will not.
So let's think a little bit about what
the consequences of that are.
So let me do a brief derivation here
for looking at the thermodynamics of this system.
And the key idea is just to get to the final result.
I don't want to dwell on the details of thermodynamics.
But an important concept here is the relative humidity
of the air.
So there's moisture in the air.
There's water vapor.
And it's at a certain level.
So we often write that rh for relative humidity.
And that can be defined as the concentration of vapor,
water vapor in the air relative to the vapor concentration
that would be in equilibrium with pure liquid.
So when the concentration water vapor gets high enough,
eventually you start to nucleate water droplets.
And you start to have condensation water.
That's essentially how rain forms from the clouds.
So that's that ratio.
So relative humidity is telling you
how close you are to basically having, water liquid water come
out of the air.
OK, now, the relative humidity also tells us
something about how far you are from that phase transition
point.
And there's a very simple approximation.
I'll put approximate here.
We can also write that this is -- scales with, and is --
can be in fact close to the liquid volume
fraction in equilibrium inside the drop.
So that'll be the water volume fraction of water liquid
inside the droplet.
At least you can see here in this relationship when this
volume fraction is one -- in other words,
we have pure water --
then the relative humidity is 100%.
OK, and on the other hand, when you have, let's say, only 50%
water, over here, that's like having relative humidity 50%.
This can be derived by more careful consideration
of the ideal entropy of mixing where essentially
this term here is take into account the excluded
volume and the fact that all the sites in this droplet
are not available for the water.
So they're being excluded by all the solutes and the bound water
that are present.
And similarly, we have a buildup of free energy
in the bulk as well.
So basically, this comes from some thermodynamic
considerations of equilibrium between water vapor
and water liquid.
We can write this as 1 minus the volume fraction
in equilibrium of the solid.
OK, now the thing is that we can now write this.
So if we multiply through, we can write this as 1 minus the --
so what is the volume -- so when we get to equilibrium,
this droplet is going to change its shape.
It's going to reach a new shape, which
we're going to calculate our new volume, V_equilibrium.
And so what this would would be V_solid,
which is phi_s^0*V_0 divided by V_equilibrium.
So it's going to be new volume, V_equilibrium, which
will be achieved then.
And then we'll end up with the equilibrium volume fraction.
So if I take these equations here,
and I solve, I get a fundamental result, which
is that the equilibrium volume of the droplet
relative to the initial volume is equal to,
well, we have put this on the other side.
That'll be (1-RH).
And we divide that out.
And we find that it's the initial volume fractions
solutes divided by (1-RH).
That is our key result. And let's plot what this looks
like.
So if we prop the relative humidity
on the horizontal axis, from 0 to 100%, so at 100%,
the water vapor is saturating the air.
And you would start to nucleate and condensed water
liquid from that.
At 0, the air is completely dry.
And there is essentially no water vapor present.
So that's the range.
And typical comfortable rooms have a relative humidity
around 50%.
This is a typical number.
And let's plot on this axis the equilibrium volume.
It could also be the equilibrium radius
because I should say that if there are spheres,
that this is also equal to R_equilibrium divided by (R_0)^3.
So I can also take a cube root of this.
And I would have the ratio of radii.
So we would know if we started a certain radius, what's
the final radius.
OK, so we can talk about volume.
We can talk about radius.
So here is the initial size of the drop.
And somewhere down here is V_s,
which is the solute volume, which is phi_s^0*V_0.
Now what is this value?
It depends on the kind of liquid.
So saliva is mostly water with some salt
and a few other molecules.
But in saliva, the volume fraction phi_s^0
is 0.5% in saliva.
OK, so that's just gives you a sense.
So this is quite far down, right?
But then, if you look in mucus, it
depends which mucus you're talking about.
But the mucus that comes from the lungs or from the pharynx,
it can vary.
But what has also been measured in droplets
that are emitted by breathing is that this can range anywhere
from 5% to 10%.
So a fairly significant amount of the volume of the droplet
is containing all these molecules and the bound water
around that.
Now we know that because mucus is very sticky.
It's a non-Newtonian fluid.
It doesn't maintain a nice round shape even.
It can have a regular shape.
It flows slowly.
It has a high viscosity.
And that's because it has a large amount
of these hygroscopic solutes.
So mucus might be a little bit higher up.
But in any case, what you then find is
we can sketch different regions of this plot now.
So this curve this formula drive here,
when the relative humidity is zero, we start here.
So that's saying when there's no water in the air,
you completely dry the droplet.
And you're left just with the molecules, the solid molecules,
and possibly the bound water around it,
depending on how dry the air actually is.
And then it rises up and blows up at 100%.
So when you get to 100%, then droplets
are getting really large.
And if you actually hit 100%, then you
can't really speak of an equilibrium size
because you'll just start to get lots and lots of water.
So that's that limit.
And so now we can look at three different regimes
of the kinds of droplets that we'd expect to see.
So down here at 0% or close to zero,
we have a dried droplet nuclei as they're called
in the public health field.
These respiratory aerosols, if they completely dry out,
and you're left with just these solutes, then that's
called a droplet nucleus.
So it doesn't necessarily mean it's
a nucleus for phase transformation
as we use that term in, say, engineering or in physics.
But it's really just refers to the core
of just the hydrated solutes.
So if I could sketch what that looks like, that would be--
for example, all those molecules I just
sketched there might be condensed
into some little blob, which, by the way,
could include a virion.
In fact, it could even be just one virion
if that were all that were in there.
And you would have a little bit of bound water around it.
But you essentially have a dried up blob of just the solutes.
OK, and so that -- and then, of course,
the smallest volume you can get is just the initial solute
volume that you started with, plus the bound water.
On the other end, if we are near 100% relative humidity, then
the fact that these are hygroscopic solutes, which
like to have water near them, will form as a nucleation site
to actually cause more and more water
to grow and be absorbed into this droplet.
And not only do the droplets not shrink,
as predicted by the Wells curve for a pure liquid,
but they can actually grow.
So if the size here is small enough to begin with,
let's say it were a several-micron droplet to begin with,
but it contains a lot of solutes, and we're
at very high humidity, actually the particle can grow.
So over here, we could end up with an even larger droplet
than we started with where now because the humidity is
so high, and we have the same number of molecules in there
that I sketched before, that's more dilute now.
And there's maybe a virus or a virion here and there.
And of course, there's also some salt.
But basically, the droplet is growing.
So here we have hygroscopic growth
and also we have what's called deliquescence, which
refers to water that's absorbing around these salt molecules
and even causing some other molecules or charges
on these macromolecules to dissolve into solution
because it's more and more water present
and it can solvate more species.
And so whereas hygroscopic growth
refers to water being absorbed into a more
solid-like framework, you can also
be generating more aqueous solution, which is deliquescence.
So basically, the droplet can actually grow.
And that would be like when you're here, let's just say.
And this might be when you're here.
And then, of course, when you're at 50% relative humidity,
you can see the droplet has shrunken
but not all the way down to the initial solute volume fraction,
but something larger.
And in fact, if the relative humidity is 50%,
you end up at exactly twice the solid volume fraction.
So if the solid volume fraction of mucus is 10%,
you may end up with a droplet that
is maybe 20% of the volume.
So maybe it looks something like this.
OK, and so we have a little bit of shrinking going on.
And maybe there's even a virus in there as well.
But there is still plenty of water.
And so you can see also now the value of having solutes
in mucus in terms of making the virions more viable and more
easily transmittable because they hold onto the water.
So that the virion is in a stable environment.
So that when it ends up being inhaled into someone else's
lungs that it can then more easily
diffuse out of that region and infect the host cells.
In contrast, if you have a nearly pure liquid
that the virion is in, let's say pure water or even saliva,
which is actually mostly water, then
the droplet will shrink by a factor of 100.
And it might be just literally a virion with a [couple of
ions] just enveloped
with a tiny bit of water.
And maybe that, in some cases, would be not as viable
of a situation for the virions.
So basically the mucus fragments are
likely to be the more common source of the aerosols that
will stay in the air and remain infectious.