I usually like to start a lecture with something new,
but this time I'm going to make an exception,
and start with the finishing up on Friday because it involves a
little more practice with complex numbers.
I think that's what a large number of you are still fairly
weak in. So, to briefly remind you,
it will be sort of self-contained,
but still, it will use complex numbers.
And, I think it's a good way to start today.
So, remember, the basic problem was to solve
something with, where the input was sinusoidal
in particular. The k was on both sides,
and the input looked like cosine omega t.
And, the plan of the solution consisted of transporting the
problem to the complex domain. So, you look for a complex
solution, and you complexify the right hand side of the equation,
as well. So, cosine omega t
becomes the real part of this complex function.
The reason for doing that, remember, was because it's
easier to handle when you solve linear equations.
It's much easier to handle exponentials on the right-hand
side than it is to handle sines and cosines because exponentials
are so easy to integrate when you multiply them by other
exponentials. So, the result was,
after doing that, y tilda turned out to be one,
after I scale the coefficient, one over one plus omega over k
And then, the rest was e to the
i times (omega t minus phi),
where phi had a certain meaning.
It was the arc tangent of a, it was a phase lag.
And, this was then, I had to take the real part of
this to get the final answer, which came out to be something
like one over the square root of one plus the amplitude one omega
/ k squared, and then the rest was cosine omega t plus minus
phi.
It's easier to see that that part is the real part of this;
the problem is, of course you have to convert
this. Sorry, this should be i omega
t, in which case you don't need the parentheses,
either. So, the problem was to use the
polar representation of this complex number to convert it
into something whose amplitude was this, and whose angle was
minus phi. Now, that's what we call the
polar method, going polar.
I'd like, now, for the first few minutes of
the period, to talk about the other method,
the Cartesian method. I think for a long while,
many of you will be more comfortable with that anyway.
Although, one of the objects of the course should be to get you
equally comfortable with the polar representation of complex
numbers. So, if we try to do the same
thing going Cartesian, what's going to happen?
Well, I guess the same point here.
So, the starting point is still y tilde equals one over,
sorry, this should have an i here, one plus i times omega
over k, e to the i omega t.
But now, what you're going to
do is turn this into its Cartesian, turn both of these
into their Cartesian representations as a plus ib.
So, if you do that Cartesianly,
of course, what you have to do is the standard thing about
dividing complex numbers or taking the reciprocals that I
told you at the very beginning of complex numbers.
You multiply the top and bottom by the complex conjugate of this
in order to make the bottom real.
So, what does this become? This becomes one minus i times
omega over k divided by the product of this in its complex
conjugate, which is the real number, one plus omega over k
squared
So, I've now converted this to the a plus bi form.
I have also to convert the right-hand side to the a plus bi
form. So, it will look like cosine
omega t plus i sine omega t.
Having done that,
I take the last step, which is to take the real part
of that. Remember, the reason I want the
real part is because this input was the real part of the complex
input. So, once you've got the complex
solution, you have to take its real part to go back into the
domain you started with, of real numbers,
from the domain of complex numbers.
So, I want the real part is going to be, the real part of
that is, first of all, there's a factor out in front.
That's entirely real. Let's put that out in front,
so doesn't bother us particularly.
And now, I need the product of this complex number and that
complex number. But, I only want the real part
of it. So, I'm not going to multiply
it out and get four terms. I'm just going to look at the
two terms that I do want. I don't want the others.
All right, the real part is cosine omega t,
from the product of this and that.
And, the rest of the real part will be the product of the two i
terms. But, it's i times negative i,
which makes one. And therefore,
it's omega over k times sine omega t.
Now, that's the answer.
And that's the answer, too; they must be equal,
unless there's a contradiction in mathematics.
But, it's extremely important. And that's the other reason why
I'm giving you this, that you learn in this course
to be able to convert quickly and automatically things that
look like this into things that look like that.
And, that's done by means of a basic formula,
which occurs at the end of the notes for reference,
as I optimistically say, although I think for a lot of
you will not be referenced, stuff in the category of,
yeah, I think I've vaguely seen that somewhere.
But, well, we never used it for anything.
Okay, you're going to use it all term.
So, the formula is, the famous trigonometric
identity, which is, so, the problem is to convert
this into the other guy. And, the thing which is going
to do that, enable one to combine the sine and the cosine
terms, is the famous formula that a times the cosine,
I'm going to use theta to make it as neutral as possible,
-- -- so, theta you can think of
as being replaced by omega t in this particular application of
the formula. But, I'll just use a general
angle theta, which doesn't suggest anything in particular.
So, the problem is, you have something which is a
combination with real coefficients of cosine and sine,
and the important thing is that these numbers be the same.
In practice, that means that the omega t,
you're not allowed to have omega one t here,
and some other frequency, omega two t here.
That would correspond to using theta one here,
and theta two here. And, though there is a formula
for combining that, nobody remembers it,
and it's, in general, less universally useful than
the first. If you're going to memorize a
formula, and learn this one, it's best to start with the
ones where the two are equal. That's the basic formula.
The others are variations of it, but there is a sizable
variations. All right, so the answer is
that this is equal to some other constant, real constant,
times the cosine of theta minus phi.
Of course, most people remember this vaguely.
What they don't remember is what the c and the phi are,
how to calculate them. I don't suggest you memorize
the formulas for them. You can if you wish.
Instead, memorize the picture, which is much easier.
Memorize that a and b are the two sides of a right triangle.
Phi is the angle opposite the b side, and c is the length of the
hypotenuse. Okay, that's worth putting up.
I think that's a pink formula. It's even worth two of those,
but I will thrift. Now, let's apply it to this
case to see that it gives the right answer.
So, to use this formula, how I use it?
Well, I should take, I will reproduce the left-hand
side. So that part,
I just copy. And, how about the right?
Well, the amplitude, it's combined into a single
cosine term whose amplitude is, well, the two sides of the
right triangle are one, and omega over k.
The hypotenuse in that case is going to be, well,
why don't we write it here? So, we have one,
and omega over k. And, here's phi.
So, the hypotenuse is going to be the square root of one plus
omega over k squared.
And, that's going to be multiplied by the cosine of
omega t minus this phase lag angle phi.
You can write,
if you wish, phi equals the arc tangent,
but you are not learning a lot by that.
Phi is the arc tangent of omega over k.
That's okay,
but it's true. But, notice there's
cancellation now. This over that is equal to
what? Well, it's equal to this.
And, so when we get in this way, by combining these two
factors, one gets exactly the same formula that we got before.
So, as you can see, in some sense,
there's not, if you can remember this
trigonometric identity, there's not a lot of difference
between the two methods except that this one requires this
extra step. The answer will come out in
this form, and you then, to see what it really looks
like, really have to convert it to this form,
the form in which you can see what the phase lag and the
amplitude is. It's amazing how many people
who should know, this includes working
mathematicians, theoretical mathematicians,
includes even possibly the authors of your textbooks.
I'm not sure, but I've caught them in this,
too, who in this form, everybody remembers that it's
something like that. Unfortunately,
when it occurs as the answer in an answer book,
the numbers are some colossal mess here plus some colossal
mess here. And theta is,
again, a real mess, involving roots and some cube
roots, and whatnot. The only thing is,
these two are the same real mess.
That amounts to just another pure oscillation with the same
frequency as the old guy, and with the amplitude changed,
and with a phase shift, move to the right or left.
So, this is no more general than that.
Notice they both have two parameters in them,
these two coefficients. This one has the two parameters
in an altered form. Okay, well, I wanted,
because of the importance of this formula,
I wanted to take a couple of minutes out for a proof of the
formula, --
-- just to give you chance to stare at it a little more now.
There are three proofs I know. I'm sure there are 27.
The Pythagorean theorem now has several hundred.
But, there are three basic proofs.
There is the one I will not give you, I'll call the high
school proof, which is the only one one
normally finds in books, physics textbooks or other
textbooks. The high school proof takes the
right-hand side, applies the formula for the
cosine of the difference of two angles, which it assumes you had
in trigonometry, and then converts it into this.
It shows you that once you've done that, that a turns out to
be c cosine phi and b, the number b is c sine
phi, and therefore it identifies the
two sides. Now, the thing that's of course
correct and it's the simplest possible argument,
the thing that's no good about it is that the direction at
which it goes is from here to here.
Well, everybody knew that. If I gave you this and told
you, write it out in terms of cosine and sine,
I would assume it dearly hope that practically all of you can
do that. Unfortunately,
when you want to use the formula, it's this way you want
to use it in the opposite direction.
You are starting with this, and want to convert it to that.
Now, the proof, therefore, will not be of much
help. It requires you to go in the
backwards direction, and match up coefficients.
It's much better to go forwards.
Now, there are two proofs that go forwards.
There's the 18.02 proof. Since I didn't teach most of
you 18.02, I can't be sure you had it.
So, I'll spend one minute giving it to you.
What is the 18.02 proof? It is the following picture.
I think this requires deep colored chalk.
This is going to be pretty heavy.
All right, first of all, the a and the b are the given.
So, I'm going to put in that vector.
So, there is the vector whose sides are, whose components are
a and b. I'll write it without the i and
j. I hope you had from Jerison
that form for the vector, if you don't like that,
write ai plus bj, okay?
Now, there's another vector lurking around.
It's the unit vector whose, I'll write it this way,
u because it's a unit vector, and theta to indicate that it's
angle is theta. Now, the reason for doing that
is because you see that the left-hand side is a dot product
of two vectors. The left-hand side of the
identity is the dot product of the vector <a,
b> with the vector whose components are cosine theta and
sine theta.
That's what I'm calling this unit vector.
It's a unit vector because cosine squared plus sine squared
is one.
Now, all this formula is, is saying that scalar product,
the dot product of those two vectors, can be evaluated if you
know their components by the left-hand side of the formula.
And, if you don't know their components, it can be evaluated
in another way, the geometric evaluation,
which goes, what is it? It's a magnitude of one,
times the magnitude of the other, times the cosine of the
included angle. Now, what's the included angle?
Well, theta is this angle from the horizontal to that unit
vector. The angle phi is this angle,
from this picture here. And therefore,
the included angle between (u)theta and my pink vector is
theta minus phi. That's the formula.
It comes from two ways of calculating the scalar product
of the vector whose coefficients are, and the unit vector
whose components are cosine theta and sine theta.
All right, well,
you should, that was 18.02.
There must be an 18.03 proof also. Yes.
What's the 18.03 proof? The 18.03 proof uses complex
numbers. It says, look,
take the left side. Instead of viewing it as the
dot product of two vectors, there's another way.
You can think of it as the part of the products of two complex
numbers. So, the 18.03 argument,
really, the complex number argument says,
look, multiply together a minus bi and the complex
number cosine theta plus i sine theta.
There are different ways of
explaining why I want to put the minus i there instead of i.
But, the simplest is because I want, when I take the real part,
to get the left-hand side. I will.
If I take the real part of this, I'm going to get a cosine
theta plus b sine theta
because of negative i and i make one,
multiplied together. All right, that's the left-hand
side. And now, the right-hand side,
I'm going to use polar representation instead.
What's the polar representation of this guy?
Well, if <a, b> has the angle theta,
then a negative b, a minus bi goes down
below. It has the angle minus phi.
So, this is, has magnitude.
It is polar representation. Its magnitude is a squared plus
b squared, and its angle is negative phi,
not positive phi because this a minus bi goes below
the axis if a and b are positive.
So, it's e to the minus i phi.
That's the first guy. And, how about the second guy?
Well, the second guy is e to the i theta.
So, what's the product? It is a squared plus b squared,
the square root, times e to the i times (theta
minus phi).
And now, what do I want? The real part of this,
and I want the real part of this.
So, let's just say take the real parts of both sides.
If I take the real part of the left-hand side,
I get a cosine theta plus b sine theta.
If I take a real part of this
side, I get square root of a squared plus b squared times e,
times the cosine, that's the real part,
right, of theta minus phi, which is just what it's
supposed to be.
Well, with three different arguments, I'm really pounding
the table on this formula. But, I think there's something
to be learned from at least two of them.
And, you know, I'm still, for awhile,
I will never miss an opportunity to bang complex
numbers into your head because, in some sense,
you have to reproduce the experience of the race.
As I mentioned in the notes, it took mathematicians 300 or
400 years to get used to complex numbers.
So, if it takes you three or four weeks, that's not too bad.
Now, for the rest of the period I'd like to go back to the
linear equations, and try to put into perspective
and summarize, and tell you a couple of things
which I had to leave out, but which are,
in my view, extremely important.
And, up to now, I don't want to leave you with
any misapprehensions. So, I'm going to summarize this
way, whereas last lecture I went from the most general equation
to the most special. I'd like to just write them
down in the reverse order, now.
So, we are talking about basic linear equations.
First order, of course, we haven't moved as
a second order yet. So, the most special one,
and the one we talked about essentially all of the previous
two times, or last Friday, anyway, was the equation where
the k, the coefficient of y, is constant,
and where you also get it on the right-hand side quite
providentially. So, this is the most special
form, and it's the one which governed what I will call the
temperature-concentration model, or if you want to be grown up,
the conduction-diffusion model, conduction-diffusion which
describes the processes, which the equation is modeling,
whereas these simply described the variables of things,
which you usually are trying to calculate when you use the
equation. Now, there are a class of
things where the thing is constant, but where the k does
not appear naturally on the right hand side.
And, you're going to encounter them pretty quickly in physics,
for one place. So, I better not try to sweep
those under the rug. Let's just call that q of t.
And finally, there is the most general case,
where you allow k to be non-constant.
That's the one we began, when we talked about the linear
equation. And you know how to solve it in
general by a definite or an indefinite integral.
Now, there's one other thing, which I want to talk about.
I will do all these in a certain order.
But, from the beginning, you should keep in mind that
there's another between the first two cases.
Between the first two cases, there's another extremely
important distinction, and that is as to whether k is
positive or not. Up to now, we've always had k
positive. So, I'm going to put that here.
So, it's understood when I write these, that k is positive.
I want to talk about that, too.
But, first things first. The first thing I wanted to do
was to show you that this, the first case,
the most special case, does not just apply to this.
It applies to other things, too.
Let me give you a mixing problem.
The typical mixing problem gives another example.
You've already done in recitation, and you did one for
the problem set, the problem of the two rooms
filled with smoke. But, let me do it just using
letters, so that the ideas stand out a little more clearly,
and you are not preoccupied with the numbers,
and calculating with the numbers, and trying to get
numerical examples. So, it's as simple as k sub
mixing. It looks like this.
You have a tank, a room, I don't know,
where everything's getting mixed in.
It has a certain volume, which I will call v.
Something is flowing in, a gas or a liquid.
And, r will be the flow rate, in some units.
Now, since it can't pile up inside this sealed container,
which I'm sure is full, the flow rate out must also be
r. And, what we're interested in
is the amount of salt. So, x, let's suppose these are
fluid flows, and the dissolved substance that I'm talking about
is not carbon monoxide, it's salt, any dissolved
substance, some pollutant or whatever the problem calls for.
Let's use salt. So, it's the amount of salt in
the tank at time t. I'm interested in knowing how
that varies with time. Now, there's nothing to be said
about how it flows out. What flows out,
of course, is what happens to be in the tank.
But, I do have to say what flows in.
Now, the only convenient way to describe the in-flow is in terms
of its concentration. The salt will be dissolved in
the in-flowing water, and so there will be a certain
concentration. And, as you will see,
for a secret reason, I'm going to give that the
subscript e. So, e is the concentration of
the incoming salt, in other words,
in the fluid, how many grams are there per
liter in the incoming fluid. That's the data.
So, this is the data. r is part of the data.
r is the flow rate. v is the volume.
I think I won't bother writing that down, and the problem is to
determine what happens to x of t.
Now, I strongly recommend you not attempt to work directly
with the concentrations unless you feel you have a really good
physical feeling for concentrations.
I strongly recommend you work with a variable that you are
given, namely, the dependent variable,
which is the amount of salt, grams.
Well, because it's something you can physically think about.
It's coming in, it's getting mixed up,
and some of it is going out. So, the basic equation is going
to be that the rate of change of salt in the tank is the rate of
salt inflow, let me write salt inflow, minus the rate of salt
outflow. Okay, at what rate is salt
flowing in? Well, the flow rate is the flow
rate of the liquid. I multiply the flow rate,
1 L per minute times the concentration,
3 g per liter. That means 3 g per minute.
It's going to be, therefore, the product of the
flow rate and the concentration, incoming concentration.
How about the rate of the salt outflow?
Well, again, the rate of the liquid outflow
is r. And, what is the concentration
of salt in the outflow? I must use, when you talk flow
rates, the other factor must be the concentration,
not the amount. So, what is the concentration
in the outflow? Well, it's the amount of salt
in the tank divided by its volume.
So, the analog, the concentration here is x
divided by v. Now, here's a typical messy
equation, dx / dt, let's write it in the standard,
linear form, plus r times x over v equals r
times the given concentration, which is a function of time.
Now, this is going to be some given function,
and there will be no reason whatsoever why you can't solve
it in that form. And, that's normally what you
will do. Nonetheless,
in trying to understand how it fits into this paradigm,
which kind of equation is it? Well, clearly there's an
awkwardness in that on the right-hand side,
we have concentration, and on the left-hand side,
we seem to have amounts. Now, the way to understand the
equation as opposed to the way to solve it, well,
it's a step on the way to solving it.
But, I emphasize, you can and normally will solve
it in exactly that form. But, to understand what's
happening, it's better to express it in terms of
concentration entirely, and that's why it's called the
concentration, or the diffusion,
concentration-diffusion equation.
So, I'm going to convert this to concentrations.
Now, there's no problem here. x over v is the concentration
in the tank. And now, immediately,
you see, hey, it looks like it's going to
come out just in the first form. But, wait a minute.
How about the x? How do I convert that?
Well, what's the relation between x?
So, if the concentration in the tank is equal to x over v,
so the tank concentration, then x is equal to C times the
constant, V, and dx / dt, therefore, will be c times dC /
dt. You see that?
Now, that's not in standard form.
Let's put it in standard form. To put it in standard form,
I see, now, that it's not r that's the critical quantity.
It's r divided by v. So, it's dC / dt,
C prime, plus r divided by v, --
-- I'm going to call that k, k C, no let's not,
r divided by v is equal to r divided by v times Ce.
That's the equation expressed
in a form where the concentration is the dependent
variable, rather than the amount of salt itself.
And, you can see it falls exactly in this category.
That means that I can talk about it.
The natural way to talk about this equation is in terms of,
the same way we talked about the temperature equation.
I said concentration. I mean, that concentration has
nothing to do with this concentration.
This is the diffusion model, where salt solution outside,
cell in the middle, salt diffusing through a
semi-permeable membrane into that, uses Newton's law of
diffusion, except he didn't do a law of diffusion.
But, he is sticky. His name is attached to
everything. So, that's this concentration
model. It's the one entirely analogous
to the temperature. And the physical setup is the
same. This one is entirely different.
Mixing in this form of this problem has really nothing to do
with this model whatsoever. But, nor does that
concentration had anything to do with this concentration,
which refers to the result of the mixing in the tank.
But, what happens is the differential equation is the
same. The language of input and
response that we talked about is also available here.
So, everything is the same. And, the most interesting thing
is that it shows that the analog of the conductivity,
the k, the analog of conductivity and diffusivity is
this quantity. I should not be considering r
and v by themselves. I should be considering as the
basic quantity, the ratio of those two.
Now, why is that, is the basic parameter.
What is this? Well, r is the rate of outflow,
and the rate of inflow, what's r over v?
r over v is the fractional rate of outflow.
In other words, if r over v is one tenth,
it means that 1/10 of the tank will be emptied in a minute,
say. In other words,
we lumped these two constants into a single k,
and at the same time have simplified the units.
What are the units? This is volume per minute.
This is volume. So, it's simply reciprocal
minutes, reciprocal time, which was the same units of
that diffusivity and conductivity had,
reciprocal time. The space variables have
entirely disappeared. So, it that way,
it's simplified. It's simplified conceptually,
and now, you can answer the same type of questions we asked
before about this. I think it would be better for
us to move on, though.
Well, just an example, one really simple thing,
so, suppose since we spent so much time worrying about what
was happening with sinusoid inputs, I mean,
when could Ce be sinusoidal, for example?
Well, roughly sinusoidal if, for example,
some factory were polluting. If this were a lake,
and some factory were polluting it, but in the beginning,
at the beginning of the day, they produced a lot of the
pollutant, and by the end of the day when it wound down,
it might well happen that the concentration of pollutants in
the incoming stream would vary sinusoidally with a 24 hour
cycle. And then, we would be asking,
so, suppose this varies sinusoidally.
In other words, it's like cosine omega t.
I'm asking, how closely does
the concentration in the tank follow C sub e?
Now, what would that depend upon?
Think about it. Well, the answer,
suppose k is large. Closely, let's just analyze one
case, if k is big. Now, what would make k big?
We know that from the temperature thing.
If the conductivity is high, then the inner temperature will
follow the outer temperature closely, and the same thing with
the diffusion model. But we, of course,
therefore, since the equation is the same, we must get the
same result here. Now, what would make k big?
If r is big, if the flow rate is very fast,
we will expect the concentration of the inside of
that tank to match fairly closely the concentration of the
pollutant, of the incoming salt solution, or,
if the tank is very small. For fixed flow rates,
if the tank is very small, well, then it gets emptied
quickly. So, both of these are,
I think, intuitive results. And, of course,
as before, we got them from that, by trying to analyze the
final form of the solution. In other words,
we got them by looking at that form of the solution up there,
and seeing if k is big. As k increases,
what happens to the amplitude, and what happens to the phase
lag? But, that summarizes the two.
So, this means, closely means,
that the phase lag is, big or small?
The lag is small. And, the amplitude is,
well, the amplitude, the biggest the amplitude could
ever be is one because that's the amplitude of this.
So, the amplitude is near one, one because that's the
amplitude of the incoming signal, input,
whatever you want to call it. Okay, now, I'd like to spend
the rest of the time talking about the failures of number
one, and when you have to use number two, and when even number
two is no good. So, let me end first-order
equations by putting my worst foot forward.
Well, I'm just trying to avoid disappointment at
misapprehensions from you. I'll watch you leave this room
and say, well, he said that,
okay. So, the first one you're going
to encounter very shortly where one is not satisfied,
but two is, so on some examples where you need two,
well, it's going to happen right here.
Somebody, sooner or later, it's going to draw on that
loathsome orange chalk, which is unerasable,
something which looks like that.
Remember, you saw it here first.
r, yeah, we had that. Okay, see, I had it in high
school too. That's the capacitance.
This is the resistance. That's the electromotive force:
battery, or a source of alternating current,
something like that. Now, of course,
what you're interested in is how the current flows in the
circuit. Since current across the
capacitance doesn't make sense, you have to talk about the
charge on the capacitance. So, q, it's customary in a
circle this simple to use as the variable not current,
but the charge on the capacitance.
And then Kirchhoff's, you are also supposed to know
that the derivative, that the time derivative of q
is what's called the current in the circuit.
That sort of intuitive. But, i in a physics class,
j in an electrical engineering class, and why,
not the letter Y, but why is that?
That's because of electrical engineers use lots of lots of
complex numbers and therefore, you have to call current j,
I guess. I think they do j in physics,
too, now. No, no they don't.
I don't know. So, i is ambiguous if you are
in that particular subject. And it's customary to use,
I don't know. Now it's completely safe.
Okay, where are we? Well, the law is,
the basic differential equation is Kirchhoff's voltage law,
but the sum of the voltage drops across these three has to
be zero. So, it's R times i,
which is dq / dt. That's Ohm's law.
That's the voltage drop across resistance.
The voltage drop across the capacitance is Coulomb's law,
one form of Coulomb's law. It's q divided by C.
And, that has to be the voltage drop.
And then, there is some sign convention.
So, this is either plus or minus, depending on your sign
conventions, but it's E of t. Now, if I put that in standard
form, in standard form I probably should say q prime plus
q over RC equals, well, I suppose,
E over R. And, this is what would appear
in the equation. But, it's not the natural
thing. The k is one over RC.
And, that's the reciprocal.
The RC constant is what everybody knows is important
when you talk about a little circuit of that form.
On the other hand, the right-hand side,
it's quite unnatural to try to stick in the right-hand side
that same RC. Call this EC over RC.
People don't do that, and therefore,
it doesn't really fall into the paradigm of that first equation.
It's the second equation that really falls into the category.
Another simple example of this is chained to k,
radioactively changed to k. Well, let's say the radioactive
substance, A, decays into,
let's say, one atom of this produces one atom of that for
simplicity. So, it decays into B,
which then still is radioactive and decays further.
Okay, what's the differential equation, which is going to be,
it's going to govern this situation?
What I want to know is how much B there is at any given time.
So, I want a differential equation for the quantity of the
radioactive product at any given time.
Well, what's it going to look like?
Well, it's the amount coming in minus the amount going out,
so to speak. The rate of inflow minus the
rate of outflow, except it's not the same type
of physical flow we had before. How fast is it coming in?
Well, A is decaying at a certain rate,
and so the rate at which A decays is by the basic
radioactive law. It's k1, it's constant,
decay constant, times the amount of A present.
If I used the differential
equation with A here, I'd have to put a negative sign
because it's the rate at which that stuff is leaving A.
But, I'm interested in the rate at which it's coming in to B.
So, it has a positive sign. And then, the rate at which B
is decaying, and therefore the quantity of good B is gone,
-- -- that will have some other
constant, B. So, that will be the equation,
and to avoid having two dependent variables in there,
we know how A is decaying. So, it's k1,
some constant times A, sorry, A will be e to the
negative, you know, the decay law,
so, times the initial amount that was there times e to the
negative k1 t. That's how much A there is at
any given time. It's decaying by the
radioactive decay law, minus k2 B.
Okay, so how does the differential equation look like?
It looks like B prime plus k2 B equals an exponential,
k1 A zero e to the negative k1 t.
But, there's no reason to
expect that that constant really has anything to do with k2.
It's unnatural to put it in that form, which is the correct
one. Now, in the last two minutes,
I wish to alienate half the class by pointing out that if k
is less than zero, none of the terminology of
transient, steady-state input response applies.
The technique of solving the equation is identical.
But, you cannot interpret. So, the technique is the same,
and therefore it's worth learning.
The technique is the same. In other words,
the solution will be still e to the negative kt integral q of t
e to the kt dt plus
a constant times e to the k, oh, this is terrible,
no. dy / dt, let's give an example.
The equation I'm going to look at is something that looks like
this: y equals q of t, let's say, okay,
a constant, but the constant a is positive.
So, the constant here is negative.
Then, when I solve, my k, in other words,
is now properly written as negative a.
And therefore, this formula should now become
not this, but the negative k is a t.
And, here it's negative a t. And, here it is positive a t.
Now, why is it, if this is going to be the
solution, why are all those things totally irrelevant?
This is not a transient any longer because if a is positive,
this goes to infinity. Or, if I go to minus infinity,
then C is negative. So, it's not transient.
It's not going to zero, and it depends heavily on the
initial conditions. That means that of these two
functions, this is the important guy.
This is just fixed, some fixed function.
Everything, in other words, is going to depend upon the
initial conditions, whereas in the other cases we
have been studying, the initial conditions after a
while don't matter anymore. Now, why did I say I would
alienate half of you? Well, because in what subjects
will a be positive? In what subjects will k be
negative? k is typically negative in
biology, economics, Sloan.
In other words, the simple thing is think of it
in biology. What's the simplest equation
for population growth? Well, it is dP / dt equals
some, if the population is growing, a times P,
and a is a positive number. That means P prime minus a P is
zero. So, the thing I want to leave
you with is this. If life is involved,
k is likely to be negative. k is positive when inanimate
things are involved; I won't say dead,
inanimate.