Uploaded by khanacademy on 11.09.2009

Transcript:

SAL: The notion of a half-life is useful, if we're dealing

with increments of time that are multiples of a half-life.

For example, where time equals zero, we

have 100% of our substance.

Then after time equals one half-life, we'd have 50% of

our substance.

At time is equal to two half-lives, we'd have 25% of

our substance, and so on and so forth.

So if I say that three half-lives have gone by-- in

the case of carbon that would be, what, roughly 15,000

years-- I can tell you roughly, or almost exactly,

what percentage of my original element I still have. In the

case of carbon-14, I'll tell you what percentage of my

original carbon-14 has not decayed into nitrogen, as yet,

nitrogen-14.

And that's useful, but what if I care about how much carbon I

have after 1/2 a year, or after 1/2 a half life, or

after three billion years, or after 10 minutes?

What if I want a general function.

A general function, as a function of time, that tells

me the number, or the amount, of my decaying substance I

have. So that's what we're going to do in this video.

And it's going to be a little mathy, but I think the math is

pretty straightforward, especially if you've taken a

first-year course in calculus.

And this is actually a pretty neat application of it.

So let's just think a little bit about the rate of change,

or the probability, or the number particles that are

changing at any given time.

So if we say, the difference or change in our number of

particles, or the amount of particles, in any very small

period of time, what's this going to be dependent on?

This is the number particles we have in a

given period time.

This is our rate of change.

So one thing, we know that our rate of change is going down.

We know it's a negative number.

We know that, in the case of radioactive decay, I could do

the same exercise with compounding growth, where I

would say, oh no, it's not a negative number, that our

growth is dependent on how much we have. In this case the

amount we're decaying is proportional, but it's going

to be the negative of how much of the actual compound we

already have.

Let me explain that.

So what I'm saying is, look, our amount of decay is

proportional to the amount of the substance that we already

are dealing with.

And just to maybe make that a little bit more intuitive,

imagine a situation here where you have 1

times 10 to the 9th.

You have a billion carbon atoms. And let's say over here

you have 1 times 10 to the 6th carbon atoms. And if you look

at it at over some small period of time, let's say, if

you look at it over one second, let's say our dt.

dt as an infinitesimally small time, but let's say it's a

change in time.

It's a delta t.

And let's say over one second, you observe that this sample

had, I don't know, let's say you saw 1000 carbon particles.

You really wouldn't see that with carbon-14, but this is

just for the sake of our intuition.

Let's say over one second you saw 1000 carbon particles per

second here.

Well here you have 1000th of the number particles in this

sample as this one.

So, for every thousand particles you saw decaying

here, you'd really expect to see one carbon particle per

second here.

Just because you have a smaller amount.

Now I don't know what the actual constant is.

But we know that no matter what substance we're talking

about, this constant is dependent on the substance.

Carbon's going to be different from uranium, is going to be

different from, you know, we looked at radon.

They're all going to have different

quantities right here.

And we can see that.

We'll actually do it in the next video, you can actually

calculate this from the half-life.

But the rate of change is always going to be dependent

on the number of particles you have, right?

I mean, we saw that here with half-life.

When you have 1/2 the number of particles,

you lose 1/2 as much.

Here, if we start with 100 particles here, we went to 50

particles, then we went to 25.

When you start with 50, in a period of time you lose 25.

When you start with 100, you lose 50.

So clearly the amount you lose is dependent on the amount you

started with, right?

Over any fraction of time, and here it's

a very small fraction.

So what I set up here is really fairly simple, but it

doesn't sound so simple to a lot of people if you say it's

a differential equation.

We can actually solve this using pretty straightforward

techniques.

This is actually a separation of variables problem.

And so, what can we do?

Let's divide both sides by N.

We want to get all the N's on this side and all the t stuff

on the other side.

So if we have 1 over N, dN over dt is

equal to minus lambda.

I just divided both sides of this by N.

And then I can multiply both sides of this by dt, and I get

1 over N dN is equal to minus lambda dt.

Now I can take the integral of both sides of this equation.

And what do I get?

What's the antiderivative?

I'm taking the indefinite integral or the

antiderivative.

What's the antiderivative of 1 over N?

Well that's the natural log of N plus some constant-- I'll

just do that in blue-- plus some constant.

And then that equals-- What's the antiderivative of just

some constant?

Well it's just that constant times the

derivative, the variable.

We're taking the antiderivative

with respect to.

So minus lambda, times t, plus some constant.

These are different constants, but they're arbitrary.

So if we want, we can just subtract that constant from

that constant, and put them all on one side and then we

just get another constant.

So this boils down to our solution to our differential

equation is the natural log of N is equal to minus lambda-t,

plus some other constant, I call it c3, it doesn't matter.

And now if we want to just make this a function of N in

terms of t, let's take both of these, or both take e to the

power of both sides of this.

You can view that as kind of the inverse natural log.

So e to the power of ln of N, ln of N is just saying what

power do you raise e to to get to N?

So if you raise e to that power, you get N.

So I'm just raising both sides of this equation.

I'm raising e to both sides of this equation.

e to the ln of N is just N.

And that is equal to e to the minus lambda-t, plus c3.

And now this can be rewritten as, N is equal to e to the

minus lambda-t, times e to the c3.

And now once again this is an arbitrary constant, so we can

just really rename that as, I don't know, let me

rename it as c4.

So, our solution to our differential equation, N, as a

function of t, is equal to our c4 constant, c4e

to the minus lambda-t.

Now let's say, even better, let's say is N equals 0.

Let's say that N equals 0.

We have N sub 0 of our sample.

That's how much we're starting off with.

So let's see if we can substitute that into our

equation to solve for c4.

So we said N sub-0 is equal to, let's put 0 in here, so

let's see, that's equal to N sub naught.

And that's equal to c4 times e to the minus lambda, times 0.

Well, minus anything times 0 is 0.

So it's e to the 0.

So that's just 1.

So c4 is equal to N naught, our starting

amount for the sample.

So we've actually got an expression.

We have the number of particles, or the amount as a

function of t, is equal to the amount that we start off with,

at time is equal to 0, times e to the minus

lambda, times time.

And we just have to be careful that we're always using the

time constant when we solve for the different

coefficients.

So this seems all abstract.

How does this relate to half-life?

Well let's try to figure out this equation for carbon.

This'll be true for anything where we

have radioactive decay.

If we actually had a plus sign here it'd be exponential

growth as well.

We know that carbon, c-14, has a 5,700-year half-life.

So the way you could think about it, is if at time equals

0 you start off with t-- So time equals 0. t equals-- let

me write that down.

If at N of 0 is equal to-- and we could write

100 there if we want.

Actually why don't we do that?

If N of 0 we start off with 100.

And then at N of 5,700 years-- so we're going to take t to be

in years, you just have to be consistent with your units--

how much will we have left?

We'll have 50 left.

We could have written x and x over two here, and it would

have all have worked out in the end.

So let's see, let's apply that to this equation and try to

solve this for lambda.

So we know N of 0 is equal to 100.

So we immediately know that we can write this equation as N

of t is equal to 100e, to the minus lambda-t, at least in

this exact circumstance.

And we also know that N of 5,700-- so that means, N of

5,700-- that is equal to, we just said, that's one

half-life away.

So we have 1/2 as much of our compound left.

That's equal to 50, which is equal to the 5,700th power

times lambda.

So it's equal to 100 times e, to the minus

lambda, times 5,700.

And now we just solve for lambda.

Then we'll have a general equation for how much carbon

we have at any given moment in time.

So if you divide both sides of this by 100.

What do we get?

We get 0.5, we have 1/2, is equal to e to the-- let me

just write minus 5,700 lambda, and then we could take the

natural log of both sides.

So then we get-- scroll down a bit-- the natural log of 1/2

is equal to the-- the natural log of this is just minus

5,700 lambda.

To solve for lambda, you get lambda is equal to the natural

log of 1/2, over minus 5,700.

So let me see what that is.

Let's see what that is.

So 0.5 natural log is that, divided by minus 5,700.

5,700 negative is equal to 1.2 times 10 to the negative 4.

Is equal to 1.21 times 10 to the minus 4.

So there you have it, we figured out our lambda.

So the general equation for how much carbon-14 we can

expect at any moment in time, t, where t is in years, is N

of t is equal to the amount of carbon we start off with,

times e to the minus lambda.

The minus lambda is 1.21 times 10 to the minus

4, times t in years.

So now if you say after 1/2 a year, you just plug it in and,

you have to tell me how much you started off with, and then

I can tell you how much you have after 1/2 a year, or

after a billion years, or after a gazillion years.

And we'll do a lot more of these

problems in the next video.