I want to talk a little bit about
direct and inverse variations.
So I'll do direct variation on the left over here.
And I'll do inverse variation, or two variables that
vary inversely, on the right-hand side over here.
So a very simple definition for two variables
that vary directly would be something like this.
y varies directly with x if y is equal to some constant with x.
So we could rewrite this in kind of English
as y varies directly with x.
And if this constant seems strange to you,
just remember this could be literally any constant number.
So let me give you a bunch of particular examples
of y varying directly with x.
You could have y is equal to x.
Because in this situation, the constant is 1.
We didn't even write it.
We could write y is equal to 1x, then k is 1.
We could write y is equal to 2x.
We could write y is equal to 1/2 x.
We could write y is equal to negative 2x.
We are still varying directly.
We could have y is equal to negative 1/2 x.
We could have y is equal to pi times x.
We could have y is equal to negative pi times x.
I don't want to beat a dead horse now.
I think you get the point.
Any constant times x-- we are varying directly.
And to understand this maybe a little bit more tangibly,
let's think about what happens.
And let's pick one of these scenarios.
Well, I'll take a positive version and a negative version,
just because it might not be completely intuitive.
So let's take the version of y is equal to 2x,
and let's explore why we say they vary directly
with each other.
So let's pick a couple of values for x
and see what the resulting y value would have to be.
So if x is equal to 1, then y is 2 times 1, or is 2.
If x is equal to 2, then y is 2 times
2, which is going to be equal to 4.
So when we doubled x, when we went from 1 to 2--
so we doubled x-- the same thing happened to y.
We doubled y.
So that's what it means when something varies directly.
If we scale x up by a certain amount,
we're going to scale up y by the same amount.
If we scale down x by some amount,
we would scale down y by the same amount.
And just to show you it works with all of these,
let's try the situation with y is equal to negative 2x.
I'll do it in magenta.
y is equal to negative-- well, let
me do a new example that I haven't even written here.
Let's try y is equal to negative 3x.
So once again, let me do my x and my y.
When x is equal to 1, y is equal to negative 3 times
1, which is negative 3.
When x is equal to 2, so negative 3 times
2 is negative 6.
So notice, we multiplied.
So if we scaled-- let me do that in that same green color.
If we scale up x by 2-- it's a different green color,
but it serves the purpose-- we're also scaling up y by 2.
To go from 1 to 2, you multiply it by 2.
To go from negative 3 to negative 6,
you're also multiplying by 2.
So we grew by the same scaling factor.
And if you wanted to go the other way-- let's try,
I don't know, let's go to x is 1/3.
If x is 1/3, then y is going to be-- negative 3 times
1/3 is negative 1.
So notice, to go from 1 to 1/3, we divide by 3.
To go from negative 3 to negative 1,
we also divide by 3.
We also scale down by a factor of 3.
So whatever direction you scale x in,
you're going to have the same scaling direction as y.
That's what it means to vary directly.
Now, it's not always so clear.
Sometimes it will be obfuscated.
So let's take this example right over here.
y is equal to negative 3x.
And I'm saving this real estate for inverse variation
in a second.
You could write it like this, or you could algebraically
manipulate it.
You could maybe divide both sides of this equation by x,
and then you would get y/x is equal to negative 3.
Or maybe you divide both sides by x,
and then you divide both sides by y.
So from this, so if you divide both sides by y now,
you could get 1/x is equal to negative 3 times 1/y.
These three statements, these three equations,
are all saying the same thing.
So sometimes the direct variation
isn't quite in your face.
But if you do this, what I did right here with any of these,
you will get the exact same result.
Or you could just try to manipulate it back
to this form over here.
And there's other ways we could do it.
We could divide both sides of this equation by negative 3.
And then you would get negative 1/3 y is equal to x.
And now, this is kind of an interesting case
here because here, this is x varies directly with y.
Or we could say x is equal to some k times y.
And in general, that's true.
If y varies directly with x, then
we can also say that x varies directly with y.
It's not going to be the same constant.
It's going to be essentially the inverse of that constant,
but they're still directly varying.
Now with that said, so much said,
about direct variation, let's explore
inverse variation a little bit.
Inverse variation-- the general form,
if we use the same variables.
And it always doesn't have to be y and x.
It could be an a and a b.
It could be a m and an n.
If I said m varies directly with n,
we would say m is equal to some constant times n.
Now let's do inverse variation.
So if I did it with y's and x's, this
would be y is equal to some constant times 1/x.
So instead of being some constant times x,
it's some constant times 1/x.
So let me draw you a bunch of examples.
It could be y is equal to 1/x.
It could be y is equal to 2 times 1/x, which is clearly
the same thing as 2/x.
It could be y is equal to 1/3 times 1/x, which
is the same thing as 1 over 3x.
it could be y is equal to negative 2 over x.
And let's explore this, the inverse variation, the same way
that we explored the direct variation.
So let's pick-- I don't know/ let's pick y is equal to 2/x.
And let me do that same table over here.
So I have my table.
I have my x values and my y values.
If x is 1, then y is 2.
If x is 2, then 2 divided by 2 is 1.
So if you multiply x by 2, if you scale it
up by a factor of 2, what happens to y?
y gets scaled down by a factor of 2.
You're dividing by 2 now.
Notice the difference.
Here, however we scaled x, we scaled up y by the same amount.
Now, if we scale up x by a factor, when
we have inverse variation, we're scaling down y by that same.
So that's where the inverse is coming from.
And we could go the other way.
If we made x is equal to 1/2.
So if we were to scale down x, we're
going to see that it's going to scale up y.
Because 2 divided by 1/2 is 4.
So here we are scaling up y.
So they're going to do the opposite things.
They vary inversely.
And you could try it with the negative version of it,
as well.
So here we're multiplying by 2.
And once again, it's not always neatly written for you
like this.
It can be rearranged in a bunch of different ways.
But it will still be inverse variation
as long as they're algebraically equivalent.
So you can multiply both sides of this equation right
here by x.
And you would get xy is equal to 2.
This is also inverse variation.
You would get this exact same table over here.
You could divide both sides of this equation by y.
And you could get x is equal to 2/y, which is also
the same thing as 2 times 1/y.
So notice, y varies inversely with x.
And you could just manipulate this algebraically
to show that x varies inversely with y.
So y varies inversely with x.
This is the same thing as saying-- and we just showed it
over here with a particular example--
that x varies inversely with y.
And there's other things.
We could take this and divide both sides by 2.
And you would get y/2 is equal to 1/x.
There's all sorts of crazy things.
And so in general, if you see an expression that
relates to variables, and they say,
do they vary inversely or directly or maybe neither?
You could either try to do a table like this.
If you scale up x by a certain amount
and y gets scaled up by the same amount, then
it's direct variation.
If you scale up x by some-- and you
might want to try a couple different times--
and you scale down y, you do the opposite with y,
then it's probably inverse variation.
A surefire way of knowing what you're dealing with
is to actually algebraically manipulate the equation
so it gets back to either this form, which would tell you
that it's inverse variation, or this form, which would tell you
that it is direct variation.