00:01
Okay, so we have the function, y equals 2x plus 1 to the 1 half power, and on the range from 0 to 1, or the domain from 0 to 1.
00:11
So what we want to do is first estimate the area using its graph and then proceeding to find the exact area by integrating it.
00:21
So in order to estimate this area, we're going to use an estimation technique called the trapezoidal rule, where we have two points a and b.
00:29
And we're going to use those to form a trapezoid that is made underneath the graph.
00:37
So the region under the graph is going to make me look like a trapezoid, and we're going to find the area of that trapezoid that we make, and that's how we can estimate a definite integral.
00:46
So we go ahead and kind of finish drawing out this trapezoid.
00:52
We can see that it's pretty close to what our graph looks like, or what this region looks like underneath the red line here.
00:59
So we're going to use that as estimation technique to approximate this.
01:02
This area.
01:04
And here's the equation.
01:05
So to estimate this integral, we're going to essentially take the area of this trapezoid we just made, where b is the point, is the point one, and its y value, and point a is zero, and its y value.
01:19
We can find its y value by just plugging in to our expression for y and go from there.
01:25
That's what we're going to do.
01:27
So we get this, so equals to b minus a, which is just 1 minus 0.
01:33
Those are the x points.
01:36
And times one half an f of a is just when we plug in zero into our y function that's just one we have to plug in for f of b so we're going to do two times one plus one and take the square root of that so that's going to be the square root of three square root of three there we go and we can simplify that a bit so our estimate for this area using the trapezoid or rule is just one half times one plus root three.
02:24
So there's our estimate.
02:26
It's not going to be exact, but again, it's something we can work with moving into doing the actual integral to get the exact area.
02:36
So there's our approximation using the troposota rule.
02:39
We'll keep going down here...