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PROFESSOR: Today I just want to
review some radiation basics.

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Now, it used to be that there
was a big pset on calculating

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the number of people who
die from a nuclear accident

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but I have, this semester,
taken out the psets.

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And so what we
will do is we will

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do this calculation in class
next Wednesday as a whole class.

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And this lecture was
previously to prepare

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you to do the pset because
there's a mix of backgrounds.

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I think I'm still
going to give it.

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And for a lot of you, this
will be a lot of review.

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There might be some
new information.

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And that's great.

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And maybe you learned something,
and maybe you know it all.

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All right, so let's just
have a quick review.

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Just to first
remind you, there's

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something called
non-ionizing radiation

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versus ionizing radiation.

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Non-ionizing is stuff like radio
waves and microwaves and so on,

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visible light.

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And when you get
towards the ultraviolet,

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the energies of the photons
becomes energetic enough

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that you can actually
liberate electrons from atoms.

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And that is what
makes it ionizing,

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and that's when you start to
get radiation effects that break

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down DNA and cause cancer.

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So photons are where we
normally start thinking,

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but there's also
charged particles.

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There's a lot of different ones.

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You have alpha particles,
which are basically

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a helium-4 nucleus, protons.

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Muons we don't
think of very much,

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but they show up in cosmic rays.

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And beta particles, which are
just basically-- beta plus

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and beta minus, either free
electrons or free positrons,

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positrons being the antimatter
analog of an electron.

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And you say, well,
where in the world

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is that going to come from?

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And actually you do get
it in these reactions.

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It does show up.

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These positrons, antimatter
does show up in these reactions.

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So these things
are being charged,

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have an electric field
associated with them.

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And as they move through
matter, those electric fields

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interact with the electric
fields of the atoms,

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of the electrons.

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And that allows them to interact
in a variety of ways, typically

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off the electron structure,
but sometimes off

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the nucleus itself.

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And then you have charged
neutral particles, namely

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the neutron, which is,
of course, only going

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to interact through
the strong force

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and thus will only interact
with the nucleus of the atom.

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But when those interactions do
happen and they're not very--

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these particles, they
fly through matter,

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and they're interacting
instantaneously.

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And they're slowing down
and depositing energy

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in just the thinnest
layers of matter.

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But these things can
penetrate quite deeply

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because they're not charged.

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But when they interact,
they're very dramatic.

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All right.

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So you've probably all
seen this from high school.

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Heavy charged particles get
stopped by things like paper.

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Lighter, thinner smaller
ones can go into your hand.

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But they'll be
stopped by something

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that has a high
density of electrons,

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so like metal, which
has a sea of electrons.

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Neutrons are absorbed in
water because they scatter off

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of like hydrogen. And
gamma radiation can easily

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penetrate all these things.

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And you need wind up basically
needing lead as a shield.

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It's a very simplified view.

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In reality, this is
what it looks like.

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You have just crazy number
of reactions occurring

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with matter of all kinds.

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Let's just talk about
these a little bit more.

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So the three principal
reactions that dominate

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are the photoelectric
effect, the Compton effect,

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and pair production.

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And all of these depend on the
energy of the incoming particle

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and on the z, or the atomic
number of the nucleus.

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So the first process
there on the top left

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is photoelectric effect,
and this is usually

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a dominant process when you
have a low-energy photon.

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So the photon is usually below
a few hundred keV in energy.

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And what it does is it transfers
all of its energy to an electron

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and kicks out the electron,
usually from an inner shell.

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And so now you have this
high-energy electron,

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which is traveling,
which is also charged.

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And that's going to transfer
further energy and so on.

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So this is what I think Einstein
received his Nobel Prize for.

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The probability of this
increases dramatically

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with atomic number, basically
somewhere between z cubed and z

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to the fifth.

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And it decreases dramatically
with the energy of the photon,

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about 1 over E to the--

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or E to the minus, dependence
on E being energy, obviously.

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The Compton effect is
the most common effect.

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So in the Compton effect,
you have a photon coming in.

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It looks like it's going to be
photoelectric, but actually what

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it does is it scatters off
of this so-called quasi-free

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electron.

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And it just gives up some of
the energy to the electron

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and kicks out the electron.

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And then a lower energy
photon continues,

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so you get this branching.

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And this is something
that basically leads

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to these kinds of showers.

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You see these branching events
in matter because of this.

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So essentially the Compton
cross-section is essentially

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proportional to the
number of atoms--

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sorry, the number of
electrons in an atom.

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So it basically just scales
with the atomic number.

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If you have a very
high-energy photon,

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it can interact with the
coulombic field of the nucleus

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and split into an
electron and a positron.

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So it goes from being a
mass-free, matter-less thing,

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and it creates matter.

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And then the positron
will touch something else

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and then annihilate and
create a photon back.

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And this is pair production.

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To do that, you have to have an
incoming photon whose energy is

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high enough that it's higher
than the rest mass of these two

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particles, and
that is 1.022 MeV.

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The probability
of this happening

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increases dramatically
as the photon energy

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goes above 1.02 MeV.

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And it increases
roughly as z squared.

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So this really is something that
happens in high-z materials,

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gold and so on.

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It's not going to be a dominant
process in human tissue,

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for example.

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So these things all
combine in this array.

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And you get basically
two types of behavior.

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If you have energies--
if you have radiation

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that originates either from
gamma radiation or electrons,

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you'll get these branching
phenomenon, where

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you have an interaction,
and then the particle

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travel some distance and so on.

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And we call this low LET,
which stands for linear energy

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transfer.

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And so you'll have
these events separated

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by hundreds of nanometers,
and you get these branches.

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If instead you have a
particle like a muon

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or an alpha particle, which is
heavy, it has a large field,

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you will get what we call
high LET event, radiation

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interaction.

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So basically this
is just like this

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has it's such a huge
massive particle

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and it has so much field.

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And it's just slowly
interacting, interacting,

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interacting and just leaves
this wake of destruction.

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And it doesn't go very far.

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But the damage it
does do is very dense.

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And so this kind
of radiation tends

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to lead to more
localized cell damage

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and is more likely to kill
a cell or do DNA damage.

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So actually that's
very useful if you're

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trying to treat cancers.

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And you can put that
radiation source like that

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right next to the tumor.

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Then it's really good
at not going very far

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into healthy tissue and
also just really doing

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a bad job on the
unhealthy tissue.

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All right.

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So these are obviously basic,
different rate of each.

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So radiation from the decay
of nucleotides, a key thing

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to remember is that
the activity level

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is equal to the rate of
decay for the isotope.

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And that means that
you can specify

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these things are all
proportional, the activity,

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the number of atoms
present in the isotope,

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and the mass of that isotope.

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If someone gives you
one-- they say, oh,

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there was a 100 becquerel--
that's a measurement

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of activity--

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of iodine.

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You can calculate
either of these

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because they're all
directly proportional.

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Does anyone know how to--

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I assume people
know how to do this.

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I will do it for if you
don't know how to do it.

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But basically, you
have these equations

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that give you the
rate change, which

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is the activity proportional
to the decay constant,

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times the number of atoms.

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The decay constant is
related to the half life

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by this relationship.

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You should basically
know all this.

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And then you can just
calculate forward.

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I think, unless someone has
not seen this, don't be shy.

00:10:29.230 --> 00:10:33.670 align:middle line:84%
All right, I will just
zoom through this.

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All right, so we have two
principal units for decay.

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In case you don't remember, the
CGS unit is a decay per second.

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We call it a Becquerel.

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Sometimes you'll see this
older unit called a Curie.

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And you have to remember
this number, which

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is really annoying,
3.7 times 10 to the 10.

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Decays per second is a Curie.

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So Yes, a Curie is
a lot of radiation

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compared to a Becquerel.

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All right, so sometimes,
you might think about--

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so in movies, you often
hear people say, oh, it

00:11:12.790 --> 00:11:16.130 align:middle line:90%
has a half life of 30 years.

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Therefore it won't be safe
to be there for 30 years.

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No, only half of the atoms
are decaying in 30 years.

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How long does it
take to get safe?

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Strictly speaking, almost never.

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But a nice couple orders
of magnitude reduction

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is often practical.

00:11:35.330 --> 00:11:37.710 align:middle line:84%
And so 7 half lives
is kind of a good rule

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of thumb for when
you're thinking

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of something being irrelevant.

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So you're just thinking
ahead, about contamination

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from fallout.

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And you think, oh, cesium-137,
big isotope in fallout,

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has a half life of 30 years.

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How long do I have
to worry about it?

00:11:56.580 --> 00:12:00.980 align:middle line:84%
Something like 30 times
7, a couple hundred years,

00:12:00.980 --> 00:12:02.900 align:middle line:90%
something like that.

00:12:02.900 --> 00:12:06.500 align:middle line:84%
All right, so of
course, there's a lot

00:12:06.500 --> 00:12:09.580 align:middle line:90%
of radiation in the environment.

00:12:09.580 --> 00:12:11.480 align:middle line:84%
There's basically,
in the United States,

00:12:11.480 --> 00:12:13.280 align:middle line:84%
roughly-- this is
the gamma dose.

00:12:13.280 --> 00:12:18.220 align:middle line:84%
This is measured 1 meter above
the ground, from all isotopes.

00:12:18.220 --> 00:12:21.500 align:middle line:84%
It comes from-- we
call this ground shine.

00:12:21.500 --> 00:12:25.180 align:middle line:84%
Ground shine also
includes fallout.

00:12:25.180 --> 00:12:26.740 align:middle line:84%
So when we do our
calculation class,

00:12:26.740 --> 00:12:31.800 align:middle line:84%
we will calculate the ground
shine from a nuclear accident.

00:12:31.800 --> 00:12:34.380 align:middle line:84%
But there's a naturally
occurring ground shine.

00:12:34.380 --> 00:12:38.300 align:middle line:84%
And this comes from, basically,
three sources, uranium

00:12:38.300 --> 00:12:43.250 align:middle line:84%
and its daughters, thorium and
its daughters, and potassium-40.

00:12:43.250 --> 00:12:45.270 align:middle line:84%
And these are the
principal things.

00:12:45.270 --> 00:12:47.650 align:middle line:84%
So potassium-40
tends to aggregate

00:12:47.650 --> 00:12:56.010 align:middle line:84%
in places that have silica,
or mica, or salt deposits,

00:12:56.010 --> 00:12:56.850 align:middle line:90%
and so on.

00:12:56.850 --> 00:12:59.490 align:middle line:84%
And then, you might
find uranium and thorium

00:12:59.490 --> 00:13:02.310 align:middle line:84%
in things like granite,
and so on and so forth.

00:13:02.310 --> 00:13:04.850 align:middle line:90%


00:13:04.850 --> 00:13:12.410 align:middle line:84%
So what can I say
about all these?

00:13:12.410 --> 00:13:15.850 align:middle line:84%
I think I'm going to
go through a level--

00:13:15.850 --> 00:13:18.850 align:middle line:90%
this is a level diagram.

00:13:18.850 --> 00:13:21.190 align:middle line:84%
But let me-- I'm going to
have one a little bit later.

00:13:21.190 --> 00:13:26.170 align:middle line:84%
I think I want to talk about
that a little bit later.

00:13:26.170 --> 00:13:28.640 align:middle line:84%
Basically, here's, just
briefly, an example

00:13:28.640 --> 00:13:31.430 align:middle line:84%
of potassium-40 decays
into argon and calcium.

00:13:31.430 --> 00:13:34.130 align:middle line:90%


00:13:34.130 --> 00:13:37.400 align:middle line:84%
Here are the uranium
decay chains.

00:13:37.400 --> 00:13:39.720 align:middle line:90%
You've probably seen these.

00:13:39.720 --> 00:13:43.820 align:middle line:84%
The issue with these is,
being a heavy isotope,

00:13:43.820 --> 00:13:47.240 align:middle line:84%
it, of course, has a lot of
things it can decay into.

00:13:47.240 --> 00:13:50.480 align:middle line:84%
Thorium goes to-- starts
out as uranium-238, becomes

00:13:50.480 --> 00:13:54.060 align:middle line:84%
thorium, protactinium,
protactinium, uranium, thorium,

00:13:54.060 --> 00:14:00.880 align:middle line:84%
radon, radium, polonium, and
so on and so forth, bismuth.

00:14:00.880 --> 00:14:05.560 align:middle line:90%
The worst of these is radon.

00:14:05.560 --> 00:14:10.680 align:middle line:84%
It has the issue that it has a
half life of almost four days,

00:14:10.680 --> 00:14:12.200 align:middle line:90%
and it's a gas.

00:14:12.200 --> 00:14:15.320 align:middle line:84%
So all this stuff is typically
happening underground,

00:14:15.320 --> 00:14:16.880 align:middle line:90%
in the rocks.

00:14:16.880 --> 00:14:17.900 align:middle line:90%
And it's fine.

00:14:17.900 --> 00:14:23.540 align:middle line:84%
But then, it produces this
radon, and that seeps out.

00:14:23.540 --> 00:14:25.280 align:middle line:84%
And actually, this
is responsible

00:14:25.280 --> 00:14:28.240 align:middle line:84%
for-- it's the biggest single
source of natural radiation

00:14:28.240 --> 00:14:30.440 align:middle line:90%
exposure for most Americans.

00:14:30.440 --> 00:14:33.720 align:middle line:84%
And it's comparable
to the average dose

00:14:33.720 --> 00:14:35.470 align:middle line:84%
that an average
American receives

00:14:35.470 --> 00:14:38.790 align:middle line:84%
from diagnostic medical
X-rays and procedures.

00:14:38.790 --> 00:14:40.470 align:middle line:90%
It's a big source of dose.

00:14:40.470 --> 00:14:43.270 align:middle line:84%
And depending on where you
live, and what kind of rock

00:14:43.270 --> 00:14:46.870 align:middle line:84%
is under you, and how
close it is to the surface,

00:14:46.870 --> 00:14:48.570 align:middle line:90%
this can be a big problem.

00:14:48.570 --> 00:14:50.130 align:middle line:90%
What happens is it's a gas.

00:14:50.130 --> 00:14:51.310 align:middle line:90%
It floats into the air.

00:14:51.310 --> 00:14:52.890 align:middle line:90%
It collects in your basement.

00:14:52.890 --> 00:14:53.910 align:middle line:90%
You Inhale it.

00:14:53.910 --> 00:14:58.470 align:middle line:84%
And then, it decays
in your lungs.

00:14:58.470 --> 00:15:01.690 align:middle line:84%
And the rest of this decay chain
then happens in your lungs.

00:15:01.690 --> 00:15:04.050 align:middle line:90%
And that's not a great thing.

00:15:04.050 --> 00:15:08.110 align:middle line:90%


00:15:08.110 --> 00:15:10.710 align:middle line:84%
The other thing to point
out, I guess, with these

00:15:10.710 --> 00:15:15.310 align:middle line:90%
is that-- this is thorium.

00:15:15.310 --> 00:15:16.670 align:middle line:90%
Thorium is common.

00:15:16.670 --> 00:15:20.870 align:middle line:84%
You find it a lot in
different kinds of sand.

00:15:20.870 --> 00:15:22.830 align:middle line:84%
It's not such a big
thing for Americans

00:15:22.830 --> 00:15:25.130 align:middle line:84%
unless you have a brick
house or something.

00:15:25.130 --> 00:15:27.830 align:middle line:90%


00:15:27.830 --> 00:15:33.140 align:middle line:84%
But it goes to show how the
chemistry really matters.

00:15:33.140 --> 00:15:35.040 align:middle line:84%
Actually, there's
also a radon here.

00:15:35.040 --> 00:15:38.900 align:middle line:84%
But this is less of
a problem, this one.

00:15:38.900 --> 00:15:41.060 align:middle line:84%
The chemistry of
these things affect

00:15:41.060 --> 00:15:44.540 align:middle line:84%
where they are aggregated,
how they are transported

00:15:44.540 --> 00:15:46.420 align:middle line:90%
into different kinds of water--

00:15:46.420 --> 00:15:49.740 align:middle line:84%
into different kinds of minerals
by water-- and so forth.

00:15:49.740 --> 00:15:51.740 align:middle line:84%
And I think this is
a good opportunity

00:15:51.740 --> 00:15:55.220 align:middle line:84%
to bring up the idea
of secular equilibrium.

00:15:55.220 --> 00:15:59.540 align:middle line:84%
So if we just look at the
half lives, at the top there,

00:15:59.540 --> 00:16:02.300 align:middle line:84%
you see that the half
life of thorium-232

00:16:02.300 --> 00:16:06.120 align:middle line:84%
is 10 to the 10 years,
1.4 times 10 to the 10.

00:16:06.120 --> 00:16:08.060 align:middle line:90%
It's a very long time.

00:16:08.060 --> 00:16:12.200 align:middle line:84%
And then, everything else is
short-- five years, six hours,

00:16:12.200 --> 00:16:16.840 align:middle line:84%
one year, three days, 55
seconds, tenth of a second,

00:16:16.840 --> 00:16:21.900 align:middle line:84%
10 hours, 60 minutes,
0.229 microseconds.

00:16:21.900 --> 00:16:25.140 align:middle line:84%
So what does this
look like in practice?

00:16:25.140 --> 00:16:33.010 align:middle line:84%
In practice, you have
this reservoir of thorium.

00:16:33.010 --> 00:16:34.890 align:middle line:90%
Nothing is happening.

00:16:34.890 --> 00:16:38.570 align:middle line:84%
And then, if we
just speed up time,

00:16:38.570 --> 00:16:40.195 align:middle line:84%
one thorium atom
decays, and then goes,

00:16:40.195 --> 00:16:42.237 align:middle line:84%
doo, doo, doo, doo, doo,
doo, doo, doo, doo, doo.

00:16:42.237 --> 00:16:43.850 align:middle line:84%
And you have all
these other decays.

00:16:43.850 --> 00:16:47.010 align:middle line:84%
So essentially, all
of these isotopes

00:16:47.010 --> 00:16:52.570 align:middle line:84%
are present with the same
rate as the thorium atom.

00:16:52.570 --> 00:16:55.130 align:middle line:84%
That's the rate at
which they show up.

00:16:55.130 --> 00:16:58.130 align:middle line:84%
And you can treat all of
these subsequent decays

00:16:58.130 --> 00:17:02.570 align:middle line:84%
as basically happening
almost simultaneously

00:17:02.570 --> 00:17:05.450 align:middle line:90%
with the rate of thorium.

00:17:05.450 --> 00:17:08.290 align:middle line:84%
So this is an important factor
when you're-- or an important

00:17:08.290 --> 00:17:11.170 align:middle line:84%
concept when you're doing
calculations of dose.

00:17:11.170 --> 00:17:14.410 align:middle line:84%
Because you might have one
really long-lived isotope, which

00:17:14.410 --> 00:17:17.339 align:middle line:84%
is really controlling
everything that's going on.

00:17:17.339 --> 00:17:19.089 align:middle line:84%
And so you just want
to keep this in mind,

00:17:19.089 --> 00:17:22.450 align:middle line:84%
because it can ease
the calculations.

00:17:22.450 --> 00:17:26.609 align:middle line:84%
You would add up all
of these energies

00:17:26.609 --> 00:17:28.850 align:middle line:84%
and all of these
decay paths, and just

00:17:28.850 --> 00:17:35.090 align:middle line:84%
attribute it to that
mother isotope decay time.

00:17:35.090 --> 00:17:41.450 align:middle line:84%
You can, I guess-- yes,
there it is, written out.

00:17:41.450 --> 00:17:46.530 align:middle line:84%
You can figure out
the exact amount

00:17:46.530 --> 00:17:49.808 align:middle line:84%
of every one of
these given this--

00:17:49.808 --> 00:17:51.850 align:middle line:84%
think of this as a set of
differential equations,

00:17:51.850 --> 00:17:55.730 align:middle line:84%
where you have one bucket slowly
filling into another bucket,

00:17:55.730 --> 00:17:56.950 align:middle line:90%
pouring into another bucket.

00:17:56.950 --> 00:18:00.410 align:middle line:84%
And you can solve that
bucket for an arbitrary

00:18:00.410 --> 00:18:02.130 align:middle line:90%
number of buckets.

00:18:02.130 --> 00:18:04.930 align:middle line:84%
And this is called
the Bateman equation.

00:18:04.930 --> 00:18:07.450 align:middle line:90%
So there it is.

00:18:07.450 --> 00:18:10.930 align:middle line:84%
And this will tell you the
activity of any given isotope

00:18:10.930 --> 00:18:14.630 align:middle line:90%
I at time t for a chain.

00:18:14.630 --> 00:18:17.270 align:middle line:84%
And you would follow this-- you
have to work out this equation.

00:18:17.270 --> 00:18:19.020 align:middle line:84%
But you don't have to
write this down now.

00:18:19.020 --> 00:18:21.730 align:middle line:84%
If you really want to know this,
just remember the name "Bateman

00:18:21.730 --> 00:18:23.410 align:middle line:90%
equation," and go look it up.

00:18:23.410 --> 00:18:28.080 align:middle line:84%
And there is a closed form
way of figuring all this out.

00:18:28.080 --> 00:18:30.160 align:middle line:90%
All right?

00:18:30.160 --> 00:18:34.000 align:middle line:84%
So secular equilibrium,
important concept to just keep

00:18:34.000 --> 00:18:36.520 align:middle line:90%
in the back of your head.

00:18:36.520 --> 00:18:41.197 align:middle line:84%
All right, so next week,
when we do the calculation,

00:18:41.197 --> 00:18:43.780 align:middle line:84%
we're not going to be interested
in naturally occurring stuff.

00:18:43.780 --> 00:18:46.000 align:middle line:84%
We're going to be
interested in radiation that

00:18:46.000 --> 00:18:48.120 align:middle line:90%
comes from nuclear reactors.

00:18:48.120 --> 00:18:55.985 align:middle line:84%
And most of that
comes from fission.

00:18:55.985 --> 00:18:57.360 align:middle line:84%
Of course, when
you have fission,

00:18:57.360 --> 00:19:01.680 align:middle line:84%
you have two radioactive
nuclear fragments.

00:19:01.680 --> 00:19:05.880 align:middle line:84%
And if you remember
back to your basics,

00:19:05.880 --> 00:19:11.240 align:middle line:84%
this isotope is stabilized
by a high number of neutrons

00:19:11.240 --> 00:19:13.000 align:middle line:90%
because it's a heavy isotope.

00:19:13.000 --> 00:19:18.120 align:middle line:84%
And you need those extra
neutrons to hold it together,

00:19:18.120 --> 00:19:22.320 align:middle line:84%
more strong force against
the coulombic repulsion.

00:19:22.320 --> 00:19:25.020 align:middle line:84%
What happens is, now these
fragments are smaller,

00:19:25.020 --> 00:19:27.230 align:middle line:90%
there's an excess of neutrons.

00:19:27.230 --> 00:19:32.470 align:middle line:84%
And so you have,
principally, a mode

00:19:32.470 --> 00:19:39.490 align:middle line:84%
of decay that is beta radiation,
where these neutrons convert--

00:19:39.490 --> 00:19:42.310 align:middle line:84%
they pop and they convert
themselves into protons.

00:19:42.310 --> 00:19:48.030 align:middle line:84%
And then, the charge
balance is maintained

00:19:48.030 --> 00:19:52.590 align:middle line:84%
by then ejecting an electron
and an antineutrino.

00:19:52.590 --> 00:19:54.770 align:middle line:90%
And that is beta decay.

00:19:54.770 --> 00:19:56.670 align:middle line:84%
And that's the
principal mode of decay

00:19:56.670 --> 00:20:00.910 align:middle line:84%
that we really see from
these fission products.

00:20:00.910 --> 00:20:03.510 align:middle line:84%
So instantaneously,
fission is just

00:20:03.510 --> 00:20:06.350 align:middle line:84%
giving off a few neutrons,
which is obviously radiation.

00:20:06.350 --> 00:20:08.730 align:middle line:84%
But it's actually the decay
of the fission products,

00:20:08.730 --> 00:20:12.950 align:middle line:84%
which happens later, that
is the concern for reactors.

00:20:12.950 --> 00:20:18.790 align:middle line:84%
There are, in spent fuel,
still sources of neutrons.

00:20:18.790 --> 00:20:21.870 align:middle line:84%
Some of these fission
products have a mode where

00:20:21.870 --> 00:20:24.180 align:middle line:90%
they will eject the neutron.

00:20:24.180 --> 00:20:29.180 align:middle line:84%
And also, you have neutron
capture, where you have

00:20:29.180 --> 00:20:30.780 align:middle line:90%
what are called transuranics.

00:20:30.780 --> 00:20:35.020 align:middle line:84%
So you start with uranium-235 or
238, and it absorbs a neutron,

00:20:35.020 --> 00:20:36.880 align:middle line:90%
and becomes uranium-239.

00:20:36.880 --> 00:20:41.260 align:middle line:84%
You can keep absorbing
neutrons, and just by luck,

00:20:41.260 --> 00:20:45.900 align:middle line:84%
not get fissioned, and
be in the spent fuel.

00:20:45.900 --> 00:20:49.220 align:middle line:84%
And then, some of
those transuranics

00:20:49.220 --> 00:20:51.600 align:middle line:90%
want to decay by a neutron.

00:20:51.600 --> 00:20:54.820 align:middle line:84%
So you will have a neutron
source in spent nuclear fuel

00:20:54.820 --> 00:20:56.820 align:middle line:84%
that you have to worry
about when you're

00:20:56.820 --> 00:21:00.680 align:middle line:84%
talking about dealing
with spent nuclear fuel,

00:21:00.680 --> 00:21:04.220 align:middle line:84%
not so much, as it turns out,
dealing with reactor accidents.

00:21:04.220 --> 00:21:08.380 align:middle line:84%
And that's because those
heavy isotopes don't typically

00:21:08.380 --> 00:21:11.020 align:middle line:90%
come out during the accident.

00:21:11.020 --> 00:21:15.100 align:middle line:84%
It's really the lighter
fission products.

00:21:15.100 --> 00:21:17.280 align:middle line:84%
So which fission
products are there?

00:21:17.280 --> 00:21:20.000 align:middle line:84%
Well, in principle, almost
anything can be there.

00:21:20.000 --> 00:21:21.940 align:middle line:90%
Here's the table of isotopes.

00:21:21.940 --> 00:21:25.930 align:middle line:84%
And you break up that
uranium, and you just wind up

00:21:25.930 --> 00:21:30.330 align:middle line:84%
in two spots on the chart,
where the number of protons

00:21:30.330 --> 00:21:34.610 align:middle line:84%
and neutrons adds up
to the number that

00:21:34.610 --> 00:21:38.730 align:middle line:84%
is in u-235 minus 2 or
3 neutrons that came out

00:21:38.730 --> 00:21:40.050 align:middle line:90%
during fission.

00:21:40.050 --> 00:21:43.810 align:middle line:84%
And that makes
everything complicated.

00:21:43.810 --> 00:21:47.290 align:middle line:84%
Because you have basically
every single element

00:21:47.290 --> 00:21:52.710 align:middle line:84%
in there, and that makes
it a pain to work with.

00:21:52.710 --> 00:21:55.187 align:middle line:84%
There is a reliable
statistical distribution.

00:21:55.187 --> 00:21:56.270 align:middle line:90%
Have you probably seen it?

00:21:56.270 --> 00:21:59.330 align:middle line:84%
It looks like an M. I
should have put a plot of it

00:21:59.330 --> 00:22:02.290 align:middle line:84%
in here, that tells
you which isotopes

00:22:02.290 --> 00:22:05.090 align:middle line:90%
are more likely to come out.

00:22:05.090 --> 00:22:09.250 align:middle line:84%
But basically, you do have
to deal with everything.

00:22:09.250 --> 00:22:16.170 align:middle line:84%
All right, so let's just look
at the situation in what's

00:22:16.170 --> 00:22:18.090 align:middle line:90%
going on in the fuel.

00:22:18.090 --> 00:22:24.100 align:middle line:84%
So because of this, all of
these fission fragments,

00:22:24.100 --> 00:22:31.440 align:middle line:84%
which are undergoing decay over
time scales of between minutes

00:22:31.440 --> 00:22:35.320 align:middle line:84%
and hundreds of years,
thousands of years,

00:22:35.320 --> 00:22:39.160 align:middle line:84%
we have to keep
the cool-- sorry,

00:22:39.160 --> 00:22:46.160 align:middle line:84%
keep the fuel cool so it doesn't
heat up from the decay and melt.

00:22:46.160 --> 00:22:49.800 align:middle line:84%
And so all of this, of
course, happens under water.

00:22:49.800 --> 00:22:54.600 align:middle line:84%
Here's a picture of a fuel
machine unloading a PWR pressure

00:22:54.600 --> 00:22:55.600 align:middle line:90%
vessel.

00:22:55.600 --> 00:23:00.160 align:middle line:84%
Here is a fuel bundle being
inserted into the spent fuel

00:23:00.160 --> 00:23:00.960 align:middle line:90%
pond.

00:23:00.960 --> 00:23:05.560 align:middle line:84%
These barriers here, which
make these little casks,

00:23:05.560 --> 00:23:10.400 align:middle line:84%
are neutron-absorbing so that we
can squeeze more fuel bundles,

00:23:10.400 --> 00:23:14.960 align:middle line:84%
and they won't start
reacting with each other.

00:23:14.960 --> 00:23:16.480 align:middle line:84%
Most of the blue
light in this photo

00:23:16.480 --> 00:23:19.970 align:middle line:84%
is just blue because of Rayleigh
scattering of the light.

00:23:19.970 --> 00:23:25.350 align:middle line:84%
But you can see, right here,
the Cherenkov radiation

00:23:25.350 --> 00:23:29.030 align:middle line:84%
on this freshly
unloaded fuel bundle.

00:23:29.030 --> 00:23:33.190 align:middle line:90%
So how spicy are these things?

00:23:33.190 --> 00:23:37.390 align:middle line:84%
So here's a good way
to understand that.

00:23:37.390 --> 00:23:40.790 align:middle line:84%
This is a function of
the time after discharge

00:23:40.790 --> 00:23:42.350 align:middle line:90%
of a single bundle.

00:23:42.350 --> 00:23:45.090 align:middle line:90%
And we have two bundles for you.

00:23:45.090 --> 00:23:49.050 align:middle line:84%
The old fuel, 33 megawatt
days per kilogram,

00:23:49.050 --> 00:23:53.190 align:middle line:84%
that's kind of where we were in
the '70s in terms of how far we

00:23:53.190 --> 00:23:54.550 align:middle line:90%
would burn the fuel.

00:23:54.550 --> 00:23:57.330 align:middle line:84%
Now we burn the
fuel much further,

00:23:57.330 --> 00:24:01.050 align:middle line:84%
so there's more radiation in it,
50 megawatt days per kilogram.

00:24:01.050 --> 00:24:03.750 align:middle line:90%
So that's the solid green line.

00:24:03.750 --> 00:24:07.190 align:middle line:84%
And you can just
see, immediately,

00:24:07.190 --> 00:24:09.950 align:middle line:84%
you have a dose rate
of something like 100,

00:24:09.950 --> 00:24:14.630 align:middle line:84%
or more than 100,
sieverts per hour 1 meter

00:24:14.630 --> 00:24:16.770 align:middle line:84%
from the center of
the fuel bundle.

00:24:16.770 --> 00:24:21.310 align:middle line:84%
So it's like, if the bundle is
there, and I'm standing here,

00:24:21.310 --> 00:24:23.990 align:middle line:84%
I'm going to get 100
sieverts per hour.

00:24:23.990 --> 00:24:25.990 align:middle line:90%
The LD50 for that is--

00:24:25.990 --> 00:24:28.270 align:middle line:84%
I will have a 50%
probability of dying

00:24:28.270 --> 00:24:31.390 align:middle line:90%
if I stand there for 2 minutes.

00:24:31.390 --> 00:24:35.250 align:middle line:84%
But you can see it
cools down pretty fast.

00:24:35.250 --> 00:24:38.630 align:middle line:84%
It's down to a factor
of 10 times cooler

00:24:38.630 --> 00:24:40.950 align:middle line:90%
after about 15 years.

00:24:40.950 --> 00:24:45.830 align:middle line:84%
And it gets to another 10 times
cooler after about 100 years.

00:24:45.830 --> 00:24:47.510 align:middle line:84%
But even then,
we're still talking

00:24:47.510 --> 00:24:50.830 align:middle line:90%
about an LD50 in 3 to 4 hours.

00:24:50.830 --> 00:24:55.870 align:middle line:84%
So if I were trying to
steal this fuel bundle

00:24:55.870 --> 00:25:00.510 align:middle line:84%
and manipulate it, I don't have
a good chance of surviving.

00:25:00.510 --> 00:25:02.890 align:middle line:84%
No matter what, I'm going
to get radiation illness.

00:25:02.890 --> 00:25:05.430 align:middle line:90%


00:25:05.430 --> 00:25:06.650 align:middle line:90%
It's a big thing.

00:25:06.650 --> 00:25:11.270 align:middle line:84%
And it's actually part of
our protection against theft.

00:25:11.270 --> 00:25:14.470 align:middle line:84%
The IAEA has this definition
of self-protecting.

00:25:14.470 --> 00:25:21.900 align:middle line:84%
And I think the self-protecting
definition is roughly out here.

00:25:21.900 --> 00:25:25.800 align:middle line:84%
So what we don't
want, of course,

00:25:25.800 --> 00:25:29.660 align:middle line:84%
is to get any of this
inside of our body,

00:25:29.660 --> 00:25:34.020 align:middle line:84%
because that's really
seriously problematic.

00:25:34.020 --> 00:25:36.980 align:middle line:84%
And so we don't want any
of this being dispersed.

00:25:36.980 --> 00:25:39.980 align:middle line:84%
So how does this
stuff get dispersed?

00:25:39.980 --> 00:25:43.720 align:middle line:84%
Mostly, this happens because
the field bundles get too hot,

00:25:43.720 --> 00:25:46.580 align:middle line:84%
because they haven't been
maintained cool in the pool,

00:25:46.580 --> 00:25:49.740 align:middle line:84%
or some event happens,
which melts the fuel.

00:25:49.740 --> 00:25:54.380 align:middle line:84%
And that causes the isotopes,
which are more volatile--

00:25:54.380 --> 00:25:57.380 align:middle line:84%
which is to say they have a
lower melting and vaporization

00:25:57.380 --> 00:26:00.120 align:middle line:84%
temperature-- to
start boiling away.

00:26:00.120 --> 00:26:03.260 align:middle line:84%
And then, they vaporize,
and they travel in the air.

00:26:03.260 --> 00:26:04.680 align:middle line:84%
And this can
happen, for example,

00:26:04.680 --> 00:26:08.260 align:middle line:84%
if have a fire, various
things like that.

00:26:08.260 --> 00:26:16.630 align:middle line:84%
So the principal isotopes that
we worry about in an accident

00:26:16.630 --> 00:26:24.890 align:middle line:84%
are these, cesium-137,
americium, cesium-134,

00:26:24.890 --> 00:26:28.050 align:middle line:90%
and then these transuranics--

00:26:28.050 --> 00:26:30.490 align:middle line:84%
or americium is a transuranic--
plutonium, americium,

00:26:30.490 --> 00:26:33.070 align:middle line:84%
and these other
plutonium isotopes.

00:26:33.070 --> 00:26:36.490 align:middle line:84%
These are the ones
that really contribute

00:26:36.490 --> 00:26:40.090 align:middle line:90%
a lot to nuclear accident dose.

00:26:40.090 --> 00:26:42.190 align:middle line:84%
There are some other
things in here as well,

00:26:42.190 --> 00:26:47.050 align:middle line:84%
but they tend to be daughters of
these things, bismuth and so on.

00:26:47.050 --> 00:26:50.610 align:middle line:90%
Barium is another one.

00:26:50.610 --> 00:26:53.190 align:middle line:84%
So when we do our
calculation next Wednesday,

00:26:53.190 --> 00:26:58.730 align:middle line:84%
we're going to really
focus on cesium-137

00:26:58.730 --> 00:27:00.390 align:middle line:90%
as the principal isotope.

00:27:00.390 --> 00:27:04.530 align:middle line:84%
Because you can see
how This is something

00:27:04.530 --> 00:27:07.070 align:middle line:90%
that is high for a long time.

00:27:07.070 --> 00:27:09.470 align:middle line:90%
This is a log chart.

00:27:09.470 --> 00:27:13.020 align:middle line:84%
So big difference if you're a
little further up on this chart.

00:27:13.020 --> 00:27:15.080 align:middle line:84%
This thing tends
to really dominate.

00:27:15.080 --> 00:27:18.680 align:middle line:84%
So it's kind of a good
first order calculation.

00:27:18.680 --> 00:27:21.560 align:middle line:84%
But when you do talk
about spent fuel,

00:27:21.560 --> 00:27:25.840 align:middle line:84%
and you're talking about
hundreds or thousands of years,

00:27:25.840 --> 00:27:28.840 align:middle line:84%
then these transuranics
begin to matter more.

00:27:28.840 --> 00:27:33.360 align:middle line:84%
And that's what matters
in the very long run.

00:27:33.360 --> 00:27:39.660 align:middle line:84%
All right, so how does
this accident occur?

00:27:39.660 --> 00:27:42.040 align:middle line:84%
So this is the
inside of a reactor.

00:27:42.040 --> 00:27:46.340 align:middle line:84%
The pressure vessel, the
reactor core is over here.

00:27:46.340 --> 00:27:48.560 align:middle line:84%
That's just the
edge of the well.

00:27:48.560 --> 00:27:50.280 align:middle line:90%
It goes like this.

00:27:50.280 --> 00:27:52.160 align:middle line:84%
And the reactor
is roughly there.

00:27:52.160 --> 00:27:53.600 align:middle line:84%
So the first thing
that can happen

00:27:53.600 --> 00:27:56.340 align:middle line:84%
is you have some kind of
loss of cooling accident.

00:27:56.340 --> 00:28:00.120 align:middle line:84%
And inside the core, you have
some fuel that is exposed.

00:28:00.120 --> 00:28:03.220 align:middle line:84%
And that fuel will then
not be locally cooled.

00:28:03.220 --> 00:28:07.120 align:middle line:84%
And just from the radiation
decay, it will heat up,

00:28:07.120 --> 00:28:10.400 align:middle line:90%
and the cladding can blister.

00:28:10.400 --> 00:28:13.217 align:middle line:84%
And you can have
melting of the fuel,

00:28:13.217 --> 00:28:15.550 align:middle line:84%
and-- we talked about this
in the last class-- something

00:28:15.550 --> 00:28:18.190 align:middle line:84%
called corium, which is
basically a molten fuel,

00:28:18.190 --> 00:28:21.290 align:middle line:84%
dripping down to the bottom
of the pressure vessel.

00:28:21.290 --> 00:28:25.190 align:middle line:90%
That's your principal concern.

00:28:25.190 --> 00:28:28.270 align:middle line:84%
But we also have to
worry about this thing.

00:28:28.270 --> 00:28:31.750 align:middle line:84%
This is the spent fuel pool,
where all the spent fuel goes.

00:28:31.750 --> 00:28:36.390 align:middle line:84%
And there can be
decades of fuel in here.

00:28:36.390 --> 00:28:37.930 align:middle line:90%
This fuel has been cooling.

00:28:37.930 --> 00:28:40.390 align:middle line:84%
This fuel is fresh
and extra spicy.

00:28:40.390 --> 00:28:45.110 align:middle line:84%
But there's a lot more fuel
here than there is over here.

00:28:45.110 --> 00:28:48.630 align:middle line:84%
So what happens is you have this
machine that pulls out the fuel,

00:28:48.630 --> 00:28:51.390 align:middle line:84%
and it transfers it
through this sluice gate.

00:28:51.390 --> 00:28:55.130 align:middle line:84%
And then it brings it and sticks
it into one of these slots,

00:28:55.130 --> 00:28:57.670 align:middle line:90%
as I showed you earlier.

00:28:57.670 --> 00:29:01.190 align:middle line:84%
And then it sits in this
pool for some period of time,

00:29:01.190 --> 00:29:02.250 align:middle line:90%
until it's cool enough.

00:29:02.250 --> 00:29:04.670 align:middle line:84%
And then you put a
concrete cask in here.

00:29:04.670 --> 00:29:07.910 align:middle line:84%
And then you transfer the fuel
into the cask, seal the cask,

00:29:07.910 --> 00:29:08.910 align:middle line:90%
and you can take it out.

00:29:08.910 --> 00:29:11.780 align:middle line:84%
And then once it's cool enough,
it can go into this cask

00:29:11.780 --> 00:29:13.280 align:middle line:90%
and just be air cooled.

00:29:13.280 --> 00:29:17.660 align:middle line:84%
And then you stick it outside
the reactor on a platform.

00:29:17.660 --> 00:29:22.860 align:middle line:84%
So there's about 6.5 meters
of water, 20 feet of water,

00:29:22.860 --> 00:29:24.580 align:middle line:90%
above this fuel.

00:29:24.580 --> 00:29:26.520 align:middle line:90%
And it's there for two reasons.

00:29:26.520 --> 00:29:29.900 align:middle line:84%
One is, it's a lot of mass that
acts as a biological shield-- it

00:29:29.900 --> 00:29:32.160 align:middle line:84%
protects the people who
are in the plant-- and two,

00:29:32.160 --> 00:29:36.260 align:middle line:84%
obviously, to keep
that water cool.

00:29:36.260 --> 00:29:42.360 align:middle line:84%
In 1979, Sandia
National Laboratory,

00:29:42.360 --> 00:29:44.660 align:middle line:84%
which one of our
government labs,

00:29:44.660 --> 00:29:46.500 align:middle line:84%
realized that one
of the scenarios

00:29:46.500 --> 00:29:48.460 align:middle line:84%
for a potential
reactor accident was

00:29:48.460 --> 00:29:52.220 align:middle line:84%
not just what was happening
over here in the core,

00:29:52.220 --> 00:29:57.860 align:middle line:84%
but that you could have the
water leak out of this pool

00:29:57.860 --> 00:29:59.220 align:middle line:90%
somehow.

00:29:59.220 --> 00:30:01.780 align:middle line:84%
And that could
cause the zirconium

00:30:01.780 --> 00:30:05.980 align:middle line:84%
clad on the outside of the
fuel to heat up to the point

00:30:05.980 --> 00:30:08.910 align:middle line:84%
where it would
spontaneously ignite.

00:30:08.910 --> 00:30:12.170 align:middle line:84%
It would undergo an
autocatalytic reaction.

00:30:12.170 --> 00:30:16.570 align:middle line:84%
Even if there's some water,
and there's steam coming up,

00:30:16.570 --> 00:30:21.010 align:middle line:84%
at a certain temperature, it
will rip off the oxygen molecule

00:30:21.010 --> 00:30:23.690 align:middle line:84%
from the water
atoms in the steam

00:30:23.690 --> 00:30:27.970 align:middle line:84%
and basically have
a runaway oxidation

00:30:27.970 --> 00:30:30.390 align:middle line:90%
reaction, which is burning.

00:30:30.390 --> 00:30:34.570 align:middle line:84%
So it will spontaneously catch
on fire if it gets too hot.

00:30:34.570 --> 00:30:36.810 align:middle line:84%
And then, of course,
you will boil away

00:30:36.810 --> 00:30:40.350 align:middle line:84%
all of these encased
radionuclides.

00:30:40.350 --> 00:30:43.930 align:middle line:84%
And you could have
a very big problem.

00:30:43.930 --> 00:30:46.850 align:middle line:84%
That, so far, has
never happened.

00:30:46.850 --> 00:30:51.170 align:middle line:84%
But it is considered to
be a hypothetical concern.

00:30:51.170 --> 00:30:53.810 align:middle line:90%
It receives some attention.

00:30:53.810 --> 00:30:56.570 align:middle line:84%
But actually, during
the Fukushima accident,

00:30:56.570 --> 00:30:59.490 align:middle line:84%
we had a loss of
offsite power event

00:30:59.490 --> 00:31:04.850 align:middle line:84%
that got us pretty close to this
particular scenario happening.

00:31:04.850 --> 00:31:08.080 align:middle line:84%
So let me just tell you a little
bit more of what happened.

00:31:08.080 --> 00:31:12.400 align:middle line:84%
Basically, because there was no
offsite power to the reactor,

00:31:12.400 --> 00:31:16.640 align:middle line:84%
all the systems that
regulate the water level

00:31:16.640 --> 00:31:21.040 align:middle line:84%
and pump in the water to
maintain the safety of this pool

00:31:21.040 --> 00:31:22.520 align:middle line:90%
were disabled.

00:31:22.520 --> 00:31:27.360 align:middle line:84%
And very slowly, the
pool began to heat up.

00:31:27.360 --> 00:31:32.040 align:middle line:84%
And you can see, in this
photo, this steam coming off

00:31:32.040 --> 00:31:33.680 align:middle line:90%
of the reactor pool.

00:31:33.680 --> 00:31:35.920 align:middle line:84%
It's boiling the
water in the pool

00:31:35.920 --> 00:31:40.200 align:middle line:84%
because there's no cool water
being circulated into the pool.

00:31:40.200 --> 00:31:44.320 align:middle line:84%
This photo was actually
taken after TEPCO

00:31:44.320 --> 00:31:49.760 align:middle line:84%
was able to deliver fresh
emergency water into the pool

00:31:49.760 --> 00:31:50.940 align:middle line:90%
using fire trucks.

00:31:50.940 --> 00:31:52.660 align:middle line:84%
So they were able
to raise the level.

00:31:52.660 --> 00:31:54.520 align:middle line:90%
But you can see here--

00:31:54.520 --> 00:31:58.760 align:middle line:84%
you can see kind of
see the rust line here.

00:31:58.760 --> 00:32:03.800 align:middle line:84%
And so the level is still kind
of like 8 to 10 inches below

00:32:03.800 --> 00:32:05.220 align:middle line:90%
where it normally was.

00:32:05.220 --> 00:32:10.280 align:middle line:90%


00:32:10.280 --> 00:32:12.280 align:middle line:84%
The other thing to
see in this photo

00:32:12.280 --> 00:32:15.920 align:middle line:84%
is you can see
daylight, up here.

00:32:15.920 --> 00:32:23.040 align:middle line:84%
Because the reactor building had
exploded because of hydrogen.

00:32:23.040 --> 00:32:27.140 align:middle line:84%
And so what happened is
this radiolysis of water

00:32:27.140 --> 00:32:28.900 align:middle line:90%
produces hydrogen gas.

00:32:28.900 --> 00:32:34.320 align:middle line:84%
It accumulates in the
building, and then it ignites.

00:32:34.320 --> 00:32:37.000 align:middle line:84%
And it blew the
reactor building apart.

00:32:37.000 --> 00:32:41.240 align:middle line:84%
So this spent fuel pool was just
open to the outside environment,

00:32:41.240 --> 00:32:43.740 align:middle line:90%
and this boiling off the water.

00:32:43.740 --> 00:32:47.640 align:middle line:84%
And they were worried
that the water

00:32:47.640 --> 00:32:51.240 align:middle line:84%
was going to reach the
point where the fuel would

00:32:51.240 --> 00:32:52.680 align:middle line:90%
become uncovered.

00:32:52.680 --> 00:32:54.840 align:middle line:84%
So they kept bringing
in fire trucks,

00:32:54.840 --> 00:32:56.942 align:middle line:84%
and shooting hoses,
and hoping that--

00:32:56.942 --> 00:32:59.400 align:middle line:84%
on the top of the building,
and hoping that-- it would rain

00:32:59.400 --> 00:33:02.550 align:middle line:90%
into this pool to refill it.

00:33:02.550 --> 00:33:05.750 align:middle line:84%
Despite all that
effort, actually, they

00:33:05.750 --> 00:33:08.270 align:middle line:84%
thought they were
hosed, no pun intended.

00:33:08.270 --> 00:33:13.390 align:middle line:84%
So this is a chart from
the National Academies

00:33:13.390 --> 00:33:15.870 align:middle line:84%
that shows, basically,
what happened.

00:33:15.870 --> 00:33:20.190 align:middle line:84%
The official prediction of the
water level was the black line.

00:33:20.190 --> 00:33:23.830 align:middle line:90%
So here's the accident.

00:33:23.830 --> 00:33:26.310 align:middle line:84%
They thought that the
water was basically

00:33:26.310 --> 00:33:29.310 align:middle line:84%
evaporating at a constant
rate because of the heat.

00:33:29.310 --> 00:33:32.388 align:middle line:84%
And then they realized that they
need to do something about it,

00:33:32.388 --> 00:33:33.930 align:middle line:84%
so they kept bringing
in fire trucks.

00:33:33.930 --> 00:33:36.390 align:middle line:84%
And they got really desperate,
and they kept hosing in.

00:33:36.390 --> 00:33:38.223 align:middle line:84%
And they thought they
had gotten some water,

00:33:38.223 --> 00:33:40.110 align:middle line:90%
but then there were some issues.

00:33:40.110 --> 00:33:42.810 align:middle line:84%
And once it reached
this red line--

00:33:42.810 --> 00:33:46.030 align:middle line:90%
this is the height of the water.

00:33:46.030 --> 00:33:49.190 align:middle line:84%
So 4 meters is the height
of the fuel bundle.

00:33:49.190 --> 00:33:53.470 align:middle line:84%
The water is at 6.5
meters above that.

00:33:53.470 --> 00:33:57.470 align:middle line:84%
And they thought, basically,
they were exposing the fuel,

00:33:57.470 --> 00:33:59.390 align:middle line:90%
and things were going wrong.

00:33:59.390 --> 00:34:02.620 align:middle line:84%
And they were waiting
for the fire to start.

00:34:02.620 --> 00:34:05.300 align:middle line:90%
That, turns out, didn't happen.

00:34:05.300 --> 00:34:11.900 align:middle line:84%
The reality is that
this sluice gate

00:34:11.900 --> 00:34:17.659 align:middle line:84%
here, that is supposed to seal
off this chamber that contains

00:34:17.659 --> 00:34:20.179 align:middle line:84%
the reactor pressure
vessel, had gotten

00:34:20.179 --> 00:34:22.500 align:middle line:90%
damaged in the earthquake.

00:34:22.500 --> 00:34:28.020 align:middle line:84%
And as a result, water was
leaking from that vessel

00:34:28.020 --> 00:34:31.780 align:middle line:84%
into the reactor, cooling--
into the spent fuel pond.

00:34:31.780 --> 00:34:35.340 align:middle line:84%
And that is what-- this
is the actual water level.

00:34:35.340 --> 00:34:38.500 align:middle line:90%
And so they were able to--

00:34:38.500 --> 00:34:43.820 align:middle line:84%
they basically got lucky because
of a leak that leaked water

00:34:43.820 --> 00:34:46.300 align:middle line:90%
into the spent fuel pool.

00:34:46.300 --> 00:34:49.880 align:middle line:84%
You can imagine what would
have happened if, in fact,

00:34:49.880 --> 00:34:53.672 align:middle line:84%
the leak occurred the other way,
and there was a crack somewhere

00:34:53.672 --> 00:34:55.380 align:middle line:84%
in the structure of
that spent fuel pool,

00:34:55.380 --> 00:34:56.820 align:middle line:90%
and it was leaking out.

00:34:56.820 --> 00:34:59.990 align:middle line:84%
Then it would have been
a much worse situation.

00:34:59.990 --> 00:35:01.210 align:middle line:90%
So here you can see--

00:35:01.210 --> 00:35:03.390 align:middle line:84%
these are photographs
from the reactor accident.

00:35:03.390 --> 00:35:07.170 align:middle line:84%
You can see a bunch of broken
concrete sitting on top

00:35:07.170 --> 00:35:09.290 align:middle line:90%
of the fuel bundles there.

00:35:09.290 --> 00:35:10.490 align:middle line:90%
Here's a top view.

00:35:10.490 --> 00:35:13.530 align:middle line:90%


00:35:13.530 --> 00:35:17.170 align:middle line:84%
That's what, basically, the
fuel looked like in the pool.

00:35:17.170 --> 00:35:19.110 align:middle line:84%
And this is why
the leak occurred.

00:35:19.110 --> 00:35:22.570 align:middle line:84%
This green thing here is
the fuel handling machine

00:35:22.570 --> 00:35:25.830 align:middle line:84%
that reaches into the pond
and moves the bundles around.

00:35:25.830 --> 00:35:29.430 align:middle line:84%
So right here is
where the pond is,

00:35:29.430 --> 00:35:31.730 align:middle line:84%
and that's the steam
coming off the pond.

00:35:31.730 --> 00:35:36.370 align:middle line:90%
So we got really lucky.

00:35:36.370 --> 00:35:38.330 align:middle line:84%
You could ask, well,
how bad would this

00:35:38.330 --> 00:35:45.410 align:middle line:84%
have been if this had become
uncovered and caught on fire?

00:35:45.410 --> 00:35:48.850 align:middle line:84%
So the Nuclear Regulatory
Commission did a calculation.

00:35:48.850 --> 00:35:51.410 align:middle line:84%
And they said that
the radiation releases

00:35:51.410 --> 00:35:56.130 align:middle line:84%
would have been about 100
times higher than they were,

00:35:56.130 --> 00:35:59.480 align:middle line:84%
which, if you do the math,
is about 25 times worse

00:35:59.480 --> 00:36:01.400 align:middle line:90%
than Chernobyl.

00:36:01.400 --> 00:36:04.560 align:middle line:84%
So even though this
is a reactor that

00:36:04.560 --> 00:36:09.000 align:middle line:84%
has a containment
and everything else,

00:36:09.000 --> 00:36:11.320 align:middle line:84%
it still could have
been really bad.

00:36:11.320 --> 00:36:15.840 align:middle line:84%
And just, we got lucky
because of the broken gate,

00:36:15.840 --> 00:36:19.800 align:middle line:84%
and no cracks anywhere
else in the pool.

00:36:19.800 --> 00:36:25.680 align:middle line:84%
So do not take away the
idea that Chernobyl was bad

00:36:25.680 --> 00:36:29.600 align:middle line:84%
because it was a bad design,
and all modern reactors can't

00:36:29.600 --> 00:36:30.900 align:middle line:90%
have those types of accidents.

00:36:30.900 --> 00:36:34.360 align:middle line:90%
That's not the case.

00:36:34.360 --> 00:36:39.640 align:middle line:84%
A really bad accident was
basically just luck away.

00:36:39.640 --> 00:36:50.280 align:middle line:84%
So let's talk about how
you would calculate dose

00:36:50.280 --> 00:36:52.720 align:middle line:90%
if such a thing were to occur.

00:36:52.720 --> 00:36:56.930 align:middle line:90%
So we talked about these units.

00:36:56.930 --> 00:36:59.470 align:middle line:90%
Those are units of decay.

00:36:59.470 --> 00:37:03.990 align:middle line:84%
What we want to know for dose is
energy deposited per unit mass,

00:37:03.990 --> 00:37:05.510 align:middle line:90%
per unit matter.

00:37:05.510 --> 00:37:10.030 align:middle line:84%
And so we have these other
units of a gray and a rad.

00:37:10.030 --> 00:37:12.910 align:middle line:90%
The gray is the kgs unit.

00:37:12.910 --> 00:37:19.710 align:middle line:84%
And in the United States,
historically, we used CGS units.

00:37:19.710 --> 00:37:21.990 align:middle line:84%
They're not imperial
units, but it's

00:37:21.990 --> 00:37:25.670 align:middle line:84%
ergs per gram, which
is CGS version.

00:37:25.670 --> 00:37:33.630 align:middle line:84%
And then, you can calculate,
essentially, the dose per decay.

00:37:33.630 --> 00:37:35.570 align:middle line:90%
And that gives you a dose rate.

00:37:35.570 --> 00:37:38.430 align:middle line:90%
So you have your decay rate.

00:37:38.430 --> 00:37:43.510 align:middle line:84%
And then, you need some
measure of your dose per decay.

00:37:43.510 --> 00:37:47.030 align:middle line:84%
And we'll talk about how
we get that in a second.

00:37:47.030 --> 00:37:52.950 align:middle line:84%
So this energy is not
just random kinetic energy

00:37:52.950 --> 00:37:56.780 align:middle line:84%
that is just heating
things up homogeneously.

00:37:56.780 --> 00:38:00.220 align:middle line:84%
This energy is being emitted in
these charged particles, which

00:38:00.220 --> 00:38:03.300 align:middle line:84%
interact in all those
photoelectric and other

00:38:03.300 --> 00:38:05.760 align:middle line:84%
phenomenon that I
showed you earlier.

00:38:05.760 --> 00:38:09.380 align:middle line:90%
So the simple way--

00:38:09.380 --> 00:38:11.900 align:middle line:84%
basically, it's very complex
to calculate it exactly,

00:38:11.900 --> 00:38:15.180 align:middle line:84%
so we have developed these
simple, back of the envelope

00:38:15.180 --> 00:38:16.202 align:middle line:90%
ways of doing it.

00:38:16.202 --> 00:38:17.660 align:middle line:84%
And what we use is
something called

00:38:17.660 --> 00:38:21.260 align:middle line:84%
the relative biological
effectiveness.

00:38:21.260 --> 00:38:24.220 align:middle line:84%
And so what this does
is it just attributes

00:38:24.220 --> 00:38:29.780 align:middle line:84%
a number that allows us to
convert from actual energy

00:38:29.780 --> 00:38:33.260 align:middle line:84%
deposited to effective
energy deposited

00:38:33.260 --> 00:38:39.760 align:middle line:84%
depending on how the radiation
interacts with the matter.

00:38:39.760 --> 00:38:44.260 align:middle line:84%
So the dose will be based
just on the electron energy,

00:38:44.260 --> 00:38:46.060 align:middle line:90%
or on the photon energy.

00:38:46.060 --> 00:38:49.820 align:middle line:84%
But then, we multiply it by
some effectiveness number.

00:38:49.820 --> 00:38:53.340 align:middle line:84%
And we have something called
equivalent dose, which

00:38:53.340 --> 00:38:56.580 align:middle line:84%
has exactly the same units,
because we are multiplying it

00:38:56.580 --> 00:38:58.490 align:middle line:90%
by a unitless scaling factor.

00:38:58.490 --> 00:39:00.240 align:middle line:84%
But it doesn't at all
mean the same thing.

00:39:00.240 --> 00:39:01.780 align:middle line:84%
Once we're in
effective dose, this

00:39:01.780 --> 00:39:06.320 align:middle line:84%
is basically a proportionality
to dose from photons.

00:39:06.320 --> 00:39:07.120 align:middle line:90%
That's the idea.

00:39:07.120 --> 00:39:09.260 align:middle line:84%
We'll set photons
at 1, and then we'll

00:39:09.260 --> 00:39:11.580 align:middle line:84%
have these multiplying
factors for everything other

00:39:11.580 --> 00:39:12.740 align:middle line:90%
than photons.

00:39:12.740 --> 00:39:15.580 align:middle line:90%
And that's what we do.

00:39:15.580 --> 00:39:18.340 align:middle line:84%
So generally, electrons
are also 1, and then

00:39:18.340 --> 00:39:20.780 align:middle line:84%
neutrons of different
energy, 5, 10, 20.

00:39:20.780 --> 00:39:22.240 align:middle line:90%
You can see how crude this is.

00:39:22.240 --> 00:39:25.980 align:middle line:84%
It's very rough--
heavier ions, and so on.

00:39:25.980 --> 00:39:29.040 align:middle line:84%
So once we do that, in
order to prevent confusion,

00:39:29.040 --> 00:39:30.720 align:middle line:90%
we change the name of the unit.

00:39:30.720 --> 00:39:35.740 align:middle line:84%
We go from grays, which is
literally joules per kilogram,

00:39:35.740 --> 00:39:39.720 align:middle line:84%
to sieverts, which has units
of joules per kilogram,

00:39:39.720 --> 00:39:42.500 align:middle line:84%
but it also contains
this multiplier.

00:39:42.500 --> 00:39:46.400 align:middle line:84%
So if it's sieverts of
neutron dose, in fact,

00:39:46.400 --> 00:39:51.050 align:middle line:84%
the actual energy deposited
would be a lot less.

00:39:51.050 --> 00:39:54.770 align:middle line:84%
And the equivalent one
for rad is rem, which

00:39:54.770 --> 00:39:57.690 align:middle line:90%
stands for rad equivalent man.

00:39:57.690 --> 00:40:00.010 align:middle line:84%
And you have this
conversion factor,

00:40:00.010 --> 00:40:05.010 align:middle line:84%
because we're going from
CGS to KGS, of, basically,

00:40:05.010 --> 00:40:09.750 align:middle line:84%
100 rem is 1 sievert,
100 rad is 1 gray.

00:40:09.750 --> 00:40:12.570 align:middle line:90%


00:40:12.570 --> 00:40:14.010 align:middle line:84%
If you can never--
sometimes it's

00:40:14.010 --> 00:40:15.510 align:middle line:90%
hard to remember what that is.

00:40:15.510 --> 00:40:18.170 align:middle line:84%
So a stupid thing
you can remember

00:40:18.170 --> 00:40:21.010 align:middle line:84%
is, you should have 100 rad
experiences before you're

00:40:21.010 --> 00:40:25.970 align:middle line:84%
gray, 1 per year, just
to help get your unit

00:40:25.970 --> 00:40:29.930 align:middle line:90%
conversion in your mind.

00:40:29.930 --> 00:40:34.010 align:middle line:84%
All right, so the
average annual dose

00:40:34.010 --> 00:40:35.730 align:middle line:84%
that we accumulate
from background

00:40:35.730 --> 00:40:38.770 align:middle line:84%
is about a
millisievert, excluding

00:40:38.770 --> 00:40:43.930 align:middle line:90%
radon, which is a big source.

00:40:43.930 --> 00:40:46.530 align:middle line:84%
This is a very crude
way of doing it.

00:40:46.530 --> 00:40:50.240 align:middle line:84%
It's not how you would do it
if you worked in a hospital

00:40:50.240 --> 00:40:53.180 align:middle line:84%
and you wanted to calculate
a dose for a patient

00:40:53.180 --> 00:40:55.680 align:middle line:84%
that you were going to give
them for some kind of treatment.

00:40:55.680 --> 00:40:58.440 align:middle line:84%
In that case, you would do
something much more fancy.

00:40:58.440 --> 00:41:01.140 align:middle line:84%
You would have a tissue
weighting factor.

00:41:01.140 --> 00:41:05.400 align:middle line:84%
You would have a dose
rate weighting factor.

00:41:05.400 --> 00:41:08.120 align:middle line:84%
And you would have all
of these adjustments

00:41:08.120 --> 00:41:11.440 align:middle line:84%
for how fast the radiation
comes in, what tissue.

00:41:11.440 --> 00:41:15.720 align:middle line:84%
Different tissues have different
vulnerabilities, and so on.

00:41:15.720 --> 00:41:20.080 align:middle line:84%
These numbers are very
poorly understood.

00:41:20.080 --> 00:41:22.520 align:middle line:84%
There's a lot of
subjectivity in this.

00:41:22.520 --> 00:41:25.720 align:middle line:84%
And basically, this is
way too fine of a process

00:41:25.720 --> 00:41:27.580 align:middle line:84%
if we're just doing
reactor accidents,

00:41:27.580 --> 00:41:30.600 align:middle line:84%
and it's just like people being
exposed in all different ways.

00:41:30.600 --> 00:41:33.000 align:middle line:84%
So we typically
don't actually do

00:41:33.000 --> 00:41:37.120 align:middle line:84%
this for the types of problems
that we're interested in.

00:41:37.120 --> 00:41:40.320 align:middle line:84%
All right, let me talk
about the level diagram.

00:41:40.320 --> 00:41:44.180 align:middle line:84%
All right, so who knows how
to read all these things?

00:41:44.180 --> 00:41:47.470 align:middle line:90%


00:41:47.470 --> 00:41:51.150 align:middle line:90%
All right, one person.

00:41:51.150 --> 00:41:52.870 align:middle line:90%
Let me go through it then.

00:41:52.870 --> 00:41:59.510 align:middle line:84%
So this is a level
diagram for cesium.

00:41:59.510 --> 00:42:03.550 align:middle line:90%
This is the atomic number.

00:42:03.550 --> 00:42:06.030 align:middle line:90%
And this is the half life.

00:42:06.030 --> 00:42:13.270 align:middle line:90%
A stands for annum, 30.07 years.

00:42:13.270 --> 00:42:15.690 align:middle line:90%
It decays via two paths.

00:42:15.690 --> 00:42:18.030 align:middle line:84%
Both of them are
beta minus, meaning

00:42:18.030 --> 00:42:21.550 align:middle line:90%
it gives off an electron.

00:42:21.550 --> 00:42:26.070 align:middle line:84%
Beta plus would be
giving off a positron.

00:42:26.070 --> 00:42:31.430 align:middle line:84%
This path produces an
electron with 0.512 MeV.

00:42:31.430 --> 00:42:35.190 align:middle line:84%
This path produces an
electron with 1.174 MeV.

00:42:35.190 --> 00:42:37.910 align:middle line:84%
The probability of it going
down this path is that.

00:42:37.910 --> 00:42:40.230 align:middle line:84%
Probability of it going
down this path is that.

00:42:40.230 --> 00:42:44.110 align:middle line:84%
So it's just a roll of the dice
depending on where it goes.

00:42:44.110 --> 00:42:45.620 align:middle line:84%
If it goes down
this path, it turns

00:42:45.620 --> 00:42:51.440 align:middle line:84%
into barium-136, atomic number
656, half life of 2.55 minutes.

00:42:51.440 --> 00:42:56.800 align:middle line:84%
If it runs up here, then
100%-- well, actually, 85.1%.

00:42:56.800 --> 00:43:00.620 align:middle line:84%
I don't know what the rest
is-- basically decay by--

00:43:00.620 --> 00:43:02.020 align:middle line:90%
oh, this is actually--

00:43:02.020 --> 00:43:04.620 align:middle line:90%


00:43:04.620 --> 00:43:07.280 align:middle line:84%
I'll have to go double-check
what that number is.

00:43:07.280 --> 00:43:11.860 align:middle line:84%
But basically, this now decays
by gamma, with this energy.

00:43:11.860 --> 00:43:16.860 align:middle line:84%
So this energy plus this
energy equals that energy.

00:43:16.860 --> 00:43:18.940 align:middle line:84%
It all winds up
in the same place.

00:43:18.940 --> 00:43:21.540 align:middle line:90%


00:43:21.540 --> 00:43:23.040 align:middle line:90%
Those energies, we call them.

00:43:23.040 --> 00:43:23.940 align:middle line:90%
Qs.

00:43:23.940 --> 00:43:29.740 align:middle line:90%
That's the reaction energy.

00:43:29.740 --> 00:43:33.380 align:middle line:90%
So let me ask you a question.

00:43:33.380 --> 00:43:36.740 align:middle line:84%
Can I just say, OK, well
essentially, they're all

00:43:36.740 --> 00:43:39.460 align:middle line:90%
going to wind up as barium-137.

00:43:39.460 --> 00:43:47.050 align:middle line:84%
So why don't I just assume that
all the decays give 1.174 MeV?

00:43:47.050 --> 00:43:49.030 align:middle line:90%
Can I do that?

00:43:49.030 --> 00:43:49.530 align:middle line:90%
Why?

00:43:49.530 --> 00:43:57.530 align:middle line:90%


00:43:57.530 --> 00:44:01.150 align:middle line:84%
One's a beta, one's an
electron, and one is a photon,

00:44:01.150 --> 00:44:02.990 align:middle line:90%
but they both have an RBE of 1.

00:44:02.990 --> 00:44:26.530 align:middle line:90%


00:44:26.530 --> 00:44:28.090 align:middle line:90%
I start out here.

00:44:28.090 --> 00:44:30.290 align:middle line:84%
I either go straight to
here, or I go, do, do.

00:44:30.290 --> 00:44:33.970 align:middle line:84%
And I have two decays, two
particles versus one particle.

00:44:33.970 --> 00:44:36.750 align:middle line:84%
But these two particles,
the levels add up.

00:44:36.750 --> 00:44:41.680 align:middle line:84%
So that level plus that level
is the same as this level.

00:44:41.680 --> 00:44:47.435 align:middle line:84%
Can I just treat them
all as having 1.174?

00:44:47.435 --> 00:44:49.060 align:middle line:84%
STUDENT: I'd have to
double-check this,

00:44:49.060 --> 00:44:50.810 align:middle line:84%
but the lower energy
beta probably doesn't

00:44:50.810 --> 00:44:53.420 align:middle line:90%
have enough to penetrate that.

00:44:53.420 --> 00:44:54.100 align:middle line:90%
Maybe it does.

00:44:54.100 --> 00:44:56.320 align:middle line:90%
No, that's 500 [INAUDIBLE].

00:44:56.320 --> 00:44:59.000 align:middle line:84%
R. SCOTT KEMP: Penetration is
not really actually considered

00:44:59.000 --> 00:45:01.120 align:middle line:90%
at all here.

00:45:01.120 --> 00:45:02.400 align:middle line:90%
You still multiply.

00:45:02.400 --> 00:45:04.108 align:middle line:84%
And the way you do
this is-- you wouldn't

00:45:04.108 --> 00:45:05.608 align:middle line:84%
say-- if it touches
your skin, if it

00:45:05.608 --> 00:45:08.340 align:middle line:84%
was exposed to the outside, then
there could be some adjustment.

00:45:08.340 --> 00:45:09.720 align:middle line:84%
But let's just say
you ingest this.

00:45:09.720 --> 00:45:10.220 align:middle line:90%
STUDENT: OK.

00:45:10.220 --> 00:45:11.678 align:middle line:84%
R. SCOTT KEMP:
Yeah, so penetration

00:45:11.678 --> 00:45:12.620 align:middle line:90%
doesn't really matter.

00:45:12.620 --> 00:45:22.572 align:middle line:90%


00:45:22.572 --> 00:45:23.780 align:middle line:90%
I'm not going to answer this.

00:45:23.780 --> 00:45:25.113 align:middle line:90%
I'm going to wait for an answer.

00:45:25.113 --> 00:45:28.760 align:middle line:90%


00:45:28.760 --> 00:45:29.920 align:middle line:90%
All right.

00:45:29.920 --> 00:45:33.743 align:middle line:84%
STUDENT: You can treat them
as both having the 1.174.

00:45:33.743 --> 00:45:36.160 align:middle line:84%
R. SCOTT KEMP: Who agrees that
we can treat them the same,

00:45:36.160 --> 00:45:39.360 align:middle line:84%
we can treat everything
as having 1.174?

00:45:39.360 --> 00:45:41.680 align:middle line:90%
All right, who disagrees?

00:45:41.680 --> 00:45:42.975 align:middle line:90%
All right, why?

00:45:42.975 --> 00:45:44.600 align:middle line:84%
STUDENT: Well, wouldn't
it be different

00:45:44.600 --> 00:45:48.353 align:middle line:84%
because you have gamma that's
on i versus another gamma?

00:45:48.353 --> 00:45:50.020 align:middle line:84%
R. SCOTT KEMP: That's
what the RBE does.

00:45:50.020 --> 00:45:51.580 align:middle line:90%
It's supposed to adjust.

00:45:51.580 --> 00:45:53.560 align:middle line:84%
And you see here, the
photon and the electron

00:45:53.560 --> 00:45:56.880 align:middle line:84%
is both assigned,
essentially, unity.

00:45:56.880 --> 00:45:57.580 align:middle line:90%
So you're right.

00:45:57.580 --> 00:45:59.460 align:middle line:84%
Technically, it's
not exactly the same,

00:45:59.460 --> 00:46:02.040 align:middle line:90%
but it's almost the same, yeah.

00:46:02.040 --> 00:46:03.180 align:middle line:90%
Yeah?

00:46:03.180 --> 00:46:06.920 align:middle line:84%
STUDENT: Are we assuming,
now, that that 85% is 100%.

00:46:06.920 --> 00:46:10.440 align:middle line:84%
R. SCOTT KEMP: Yeah,
assume that's 100%, yeah.

00:46:10.440 --> 00:46:13.400 align:middle line:84%
Just probably
different levels, yeah.

00:46:13.400 --> 00:46:21.200 align:middle line:90%


00:46:21.200 --> 00:46:31.440 align:middle line:84%
Antineutrinos-- so this
level change is 1.174.

00:46:31.440 --> 00:46:34.480 align:middle line:84%
But remember, beta minus
decay includes an electron

00:46:34.480 --> 00:46:36.640 align:middle line:90%
and an antineutrino.

00:46:36.640 --> 00:46:40.590 align:middle line:84%
The antineutrino basically
doesn't interact with matter.

00:46:40.590 --> 00:46:46.630 align:middle line:84%
And roughly-- we could derive
it, but I'm not going to.

00:46:46.630 --> 00:46:53.070 align:middle line:84%
Roughly 1/3 of the energy is
in the beta minus particle.

00:46:53.070 --> 00:46:57.730 align:middle line:84%
So if you were going to do
this calculation, you would do.

00:46:57.730 --> 00:47:05.190 align:middle line:90%


00:47:05.190 --> 00:47:33.470 align:middle line:84%
0.054 times 1/3 times 1.17 MeV
plus 0.512 times 1/3 plus 0.946

00:47:33.470 --> 00:47:35.330 align:middle line:90%
times 1 point--

00:47:35.330 --> 00:47:49.220 align:middle line:90%


00:47:49.220 --> 00:47:50.620 align:middle line:90%
like that.

00:47:50.620 --> 00:47:53.660 align:middle line:84%
You would multiply the
electron decays by 1/3,

00:47:53.660 --> 00:47:58.260 align:middle line:90%
and 100% for the photon decays.

00:47:58.260 --> 00:48:01.860 align:middle line:84%
Because the antineutrino is
taking away approximately 2/3

00:48:01.860 --> 00:48:02.520 align:middle line:90%
of the energy.

00:48:02.520 --> 00:48:05.100 align:middle line:84%
So in fact, this decay
is a lot less damaging

00:48:05.100 --> 00:48:06.660 align:middle line:90%
than this decay path.

00:48:06.660 --> 00:48:11.340 align:middle line:84%
And the barium-137m
is your enemy.

00:48:11.340 --> 00:48:16.020 align:middle line:90%
All right, so don't forget.

00:48:16.020 --> 00:48:18.620 align:middle line:84%
You can estimate the
beta energy exactly

00:48:18.620 --> 00:48:21.540 align:middle line:84%
if you want to,
using Fermi theory.

00:48:21.540 --> 00:48:24.660 align:middle line:84%
But I assume that
this is annoying.

00:48:24.660 --> 00:48:27.420 align:middle line:90%
So just use this.

00:48:27.420 --> 00:48:29.240 align:middle line:90%
This is good enough, 1/3.

00:48:29.240 --> 00:48:32.500 align:middle line:90%


00:48:32.500 --> 00:48:38.530 align:middle line:84%
All right, so cesium-137
is a very big problem.

00:48:38.530 --> 00:48:42.450 align:middle line:84%
Another one that we have
to worry about is iodine.

00:48:42.450 --> 00:48:45.130 align:middle line:84%
Iodine is not typically
produced in large quantities

00:48:45.130 --> 00:48:49.290 align:middle line:84%
directly from fission products,
but it is a decay product

00:48:49.290 --> 00:48:50.810 align:middle line:90%
of things that are.

00:48:50.810 --> 00:48:52.730 align:middle line:84%
And the reason we
worry about iodine

00:48:52.730 --> 00:48:58.410 align:middle line:84%
is because when we ingest it,
it accumulates in our thyroid.

00:48:58.410 --> 00:49:04.290 align:middle line:84%
So it typically comes
from either indium or tin,

00:49:04.290 --> 00:49:08.210 align:middle line:90%
and there are these decay paths.

00:49:08.210 --> 00:49:11.010 align:middle line:84%
Indium has a low
melting temperature,

00:49:11.010 --> 00:49:14.050 align:middle line:90%
but a very high boiling point.

00:49:14.050 --> 00:49:19.930 align:middle line:84%
So it will tend to melt, but
not vaporize if there's a fire.

00:49:19.930 --> 00:49:21.470 align:middle line:90%
The same is true for tin.

00:49:21.470 --> 00:49:26.810 align:middle line:84%
And does anyone
remember what Sb is?

00:49:26.810 --> 00:49:28.750 align:middle line:90%
What?

00:49:28.750 --> 00:49:32.370 align:middle line:90%
Antimony-- wow, that's great.

00:49:32.370 --> 00:49:40.080 align:middle line:84%
Yeah, tin and antimony, both
are unlikely to vaporize.

00:49:40.080 --> 00:49:47.040 align:middle line:84%
But iodine and tellurium--
but iodine vaporizes

00:49:47.040 --> 00:49:52.880 align:middle line:84%
at about 184 C, which is like
your kitchen oven temperature.

00:49:52.880 --> 00:49:58.840 align:middle line:84%
So this stuff all comes
boiling out of the reactor.

00:49:58.840 --> 00:50:02.440 align:middle line:84%
Even after the accident
is over, the fuel

00:50:02.440 --> 00:50:04.640 align:middle line:90%
is easily still this hot.

00:50:04.640 --> 00:50:06.760 align:middle line:84%
And so this is
how-- then it gets

00:50:06.760 --> 00:50:08.360 align:middle line:90%
released into the environment.

00:50:08.360 --> 00:50:14.320 align:middle line:84%
And you have eight days, 20
hours, and 6.5-hour half lives.

00:50:14.320 --> 00:50:17.060 align:middle line:84%
The eight-day stuff is the
stuff that's really problematic.

00:50:17.060 --> 00:50:20.840 align:middle line:84%
Because eight days is
long enough for a plume

00:50:20.840 --> 00:50:24.000 align:middle line:84%
to go into the air, to travel
through the atmosphere,

00:50:24.000 --> 00:50:26.720 align:middle line:90%
and to slowly settle.

00:50:26.720 --> 00:50:29.340 align:middle line:84%
And what happens is
once it vaporizes,

00:50:29.340 --> 00:50:32.390 align:middle line:84%
it cools, but then
it forms aerosols.

00:50:32.390 --> 00:50:36.350 align:middle line:84%
And then they have a very
slow settling based on what--

00:50:36.350 --> 00:50:38.870 align:middle line:84%
you've heard it called the
Stokes settling velocity.

00:50:38.870 --> 00:50:41.090 align:middle line:84%
So you can calculate,
depending on the particle size,

00:50:41.090 --> 00:50:43.110 align:middle line:84%
how fast these things
will fall to the ground.

00:50:43.110 --> 00:50:45.488 align:middle line:84%
And eventually, they'll
land on something.

00:50:45.488 --> 00:50:47.030 align:middle line:84%
You'll either inhale
them, or they'll

00:50:47.030 --> 00:50:48.670 align:middle line:90%
land on something you eat.

00:50:48.670 --> 00:50:53.470 align:middle line:84%
And because this thing
stays around eight days,

00:50:53.470 --> 00:50:56.030 align:middle line:84%
there's a good chance, in
the immediate aftermath,

00:50:56.030 --> 00:51:00.590 align:middle line:84%
that you might ingest
some of this iodine.

00:51:00.590 --> 00:51:01.750 align:middle line:90%
And that becomes a problem.

00:51:01.750 --> 00:51:05.270 align:middle line:84%
Because then it
decays inside you.

00:51:05.270 --> 00:51:10.670 align:middle line:84%
Once it decays, it
typically decays to xenon.

00:51:10.670 --> 00:51:14.910 align:middle line:84%
The long-lived xenon isotopes
actually are less problematic,

00:51:14.910 --> 00:51:16.430 align:middle line:84%
because they're
noble gases, and you

00:51:16.430 --> 00:51:19.130 align:middle line:84%
have a high chance of them
escaping from your body.

00:51:19.130 --> 00:51:22.450 align:middle line:84%
But some of these
shorter-lived xenons,

00:51:22.450 --> 00:51:26.110 align:middle line:84%
whether that atom will
escape within 15 minutes,

00:51:26.110 --> 00:51:28.390 align:middle line:90%
probably unlikely.

00:51:28.390 --> 00:51:33.740 align:middle line:90%
So this is the other source of--

00:51:33.740 --> 00:51:36.420 align:middle line:90%
big source of dose after cesium.

00:51:36.420 --> 00:51:38.020 align:middle line:84%
This is really only
something we worry

00:51:38.020 --> 00:51:41.740 align:middle line:84%
about in the immediate
aftermath of an accident.

00:51:41.740 --> 00:51:43.720 align:middle line:84%
We don't worry about it
when we do long-term.

00:51:43.720 --> 00:51:48.260 align:middle line:84%
So we will do an adjustment
next Wednesday, for iodine.

00:51:48.260 --> 00:51:51.460 align:middle line:84%
But most of the calculation
we're going to focus on

00:51:51.460 --> 00:51:54.700 align:middle line:90%
is cesium.

00:51:54.700 --> 00:51:59.140 align:middle line:84%
That's basically all
I have in the review.

00:51:59.140 --> 00:52:00.800 align:middle line:84%
Since we have a
little bit of time,

00:52:00.800 --> 00:52:04.320 align:middle line:84%
I will just show you
a couple of things.

00:52:04.320 --> 00:52:07.440 align:middle line:84%
So here, if we go back to
remembering low-LET radiation,

00:52:07.440 --> 00:52:09.260 align:middle line:84%
which is like photons
and electrons,

00:52:09.260 --> 00:52:11.933 align:middle line:84%
you're going to have
this kind of behavior,

00:52:11.933 --> 00:52:13.600 align:middle line:84%
where you have some
kind of interaction,

00:52:13.600 --> 00:52:16.500 align:middle line:84%
and then the particle can
travel some distance before it

00:52:16.500 --> 00:52:18.620 align:middle line:90%
reaches another interaction.

00:52:18.620 --> 00:52:25.420 align:middle line:84%
That distance is large compared
to the size of your DNA strands,

00:52:25.420 --> 00:52:28.540 align:middle line:84%
which are wrapped onto these
things called histones.

00:52:28.540 --> 00:52:32.300 align:middle line:84%
And so the DNA is coiled
into this coil of coils.

00:52:32.300 --> 00:52:36.300 align:middle line:84%
But the high-LET,
like alpha particles,

00:52:36.300 --> 00:52:39.980 align:middle line:84%
they're just interacting
all over the place.

00:52:39.980 --> 00:52:45.165 align:middle line:84%
And so you have a high
probability of getting what are

00:52:45.165 --> 00:52:47.540 align:middle line:84%
called double-strand breaks,
which I'll talk a little bit

00:52:47.540 --> 00:52:52.740 align:middle line:84%
more about next class,
where you basically--

00:52:52.740 --> 00:52:56.900 align:middle line:84%
a single-strand break
is where you have--

00:52:56.900 --> 00:52:58.160 align:middle line:90%
there's your DNA.

00:52:58.160 --> 00:53:01.940 align:middle line:90%


00:53:01.940 --> 00:53:04.280 align:middle line:90%
And you have all these bases.

00:53:04.280 --> 00:53:06.100 align:middle line:90%
So this is your sugar backbone.

00:53:06.100 --> 00:53:07.580 align:middle line:84%
So typically, what
will happen is

00:53:07.580 --> 00:53:09.700 align:middle line:84%
you'll have some
reaction come in,

00:53:09.700 --> 00:53:12.580 align:middle line:84%
and it'll interact
with an atom here.

00:53:12.580 --> 00:53:15.220 align:middle line:90%
And it will lyse that.

00:53:15.220 --> 00:53:18.980 align:middle line:84%
And then, your body has
a process to repair that.

00:53:18.980 --> 00:53:22.100 align:middle line:84%
But if you have
high-LET radiation,

00:53:22.100 --> 00:53:24.680 align:middle line:84%
it's interacting, interacting,
interacting, interacting,

00:53:24.680 --> 00:53:26.250 align:middle line:90%
interacting, interacting.

00:53:26.250 --> 00:53:29.690 align:middle line:84%
And so you can get cuts
in multiple places.

00:53:29.690 --> 00:53:33.330 align:middle line:84%
And then you can get a bigger,
more dramatic separation

00:53:33.330 --> 00:53:34.410 align:middle line:90%
of the DNA.

00:53:34.410 --> 00:53:37.890 align:middle line:84%
And that typically results
in a bigger problem.

00:53:37.890 --> 00:53:40.330 align:middle line:84%
The problems don't
arise from the cutting

00:53:40.330 --> 00:53:42.450 align:middle line:90%
of the DNA themselves.

00:53:42.450 --> 00:53:46.250 align:middle line:84%
The problems arise
from the DNA repair.

00:53:46.250 --> 00:53:52.630 align:middle line:84%
And that's a really, really,
really important thing to know.

00:53:52.630 --> 00:53:54.850 align:middle line:84%
It's, in fact, the
misrepair of DNA

00:53:54.850 --> 00:53:57.030 align:middle line:84%
that leads to
mutations, aberrations,

00:53:57.030 --> 00:53:59.850 align:middle line:84%
genomic instability,
and cell death.

00:53:59.850 --> 00:54:04.550 align:middle line:84%
So we'll talk a little bit
about this in the next class.

00:54:04.550 --> 00:54:07.090 align:middle line:90%


00:54:07.090 --> 00:54:13.310 align:middle line:84%
The fact that your body heals
itself does not fix the problem,

00:54:13.310 --> 00:54:16.490 align:middle line:90%
it is the problem.

00:54:16.490 --> 00:54:18.690 align:middle line:84%
Otherwise, if you
just slice the genome,

00:54:18.690 --> 00:54:20.850 align:middle line:84%
and the DNA did
not repair itself,

00:54:20.850 --> 00:54:23.570 align:middle line:90%
the cell dies, and that's it.

00:54:23.570 --> 00:54:29.280 align:middle line:84%
It either just dies, or becomes
senescent and doesn't replicate.

00:54:29.280 --> 00:54:32.920 align:middle line:84%
It's only when the DNA
repairs itself, basically,

00:54:32.920 --> 00:54:35.000 align:middle line:90%
that it's an issue.

00:54:35.000 --> 00:54:37.480 align:middle line:84%
All right, I'm
going to stop there

00:54:37.480 --> 00:54:41.920 align:middle line:84%
because I won't have
content for the next class.

00:54:41.920 --> 00:54:48.000 align:middle line:84%
But we will pick up on this
talk about dose response models,

00:54:48.000 --> 00:54:51.040 align:middle line:84%
how to estimate the
probability of cancer given

00:54:51.040 --> 00:54:54.630 align:middle line:90%
some dose in the next class.

00:54:54.630 --> 00:55:23.000 align:middle line:90%