From: 3blue1brown
Integration is a common mathematical tool used to find the average of a continuous variable [00:00:19]. This application provides an insightful perspective on why integrals and derivatives are inverses of each other [00:00:29].
Finding the Average of a Continuous Function
Consider the graph of sin(x) between 0 and π, which represents half of its period [00:00:33]. A practical question could be, “What is the average height of this graph on that interval?” [00:00:40]. This is relevant for modeling cyclic phenomena, such as the average effectiveness of solar panels based on the number of daylight hours over a year [00:00:46].
The challenge with finding the average of a continuous variable lies in the infinite number of values within a given range. Unlike a finite set of numbers, where you sum them and divide by their count, you cannot sum infinitely many values and divide by infinity [00:01:48].
When faced with the desire to “add together infinitely many values associated with a continuum,” the key is almost always to use an integral [00:02:08].
Approximating the Average with Finite Sums
A helpful first step is to approximate the continuous situation with a finite sum [00:02:17]. Imagine sampling a finite number of points evenly spaced along the range from 0 to π [00:02:20]. The average of this finite sample can be found by summing the heights (sin(x) at each point) and dividing by the number of sampled points [00:02:32]. As more points are sampled, this approximation should get closer to the true average of the continuous variable [00:02:47].
This concept is related to taking an integral, where you also consider a sample of inputs on a continuum [00:03:07]. Instead of just adding heights, an integral adds “little areas,” specifically sin(x) times dx
, where dx
is the spacing between samples [00:03:18]. The integral is the value that this sum approaches as dx
approaches 0 [00:03:31].
Deriving the Average Value Formula
To formally connect the finite average to the integral, reframe the expression for the average (sum of heights / number of sampled points) in terms of dx
, the spacing between samples [00:03:50].
If the interval length is π and the spacing is dx
, the number of samples is approximately π / dx
[00:04:31]. Substituting this into the average formula:
Average ≈ (Sum of sin(x) values) / (π / dx
) [00:04:34]
Rearranging, this becomes:
Average ≈ (Sum of (sin(x) * dx
)) / π [00:04:38]
As the number of samples increases (i.e., dx
approaches 0), the sum in the numerator approaches the integral of sin(x) between 0 and π [00:05:02].
Therefore, the average height of a graph over an interval is:
Average Height = (Integral of f(x) over the interval) / (Width of the interval)
[00:05:11]
This means the average height is the area under the graph divided by its width [00:05:11].
Solving the Example: Average of sin(x)
To compute the integral, an antiderivative of the function (sin(x)) is needed [00:05:31]. The derivative of cos(x) is -sin(x), so the antiderivative of sin(x) is -cos(x) [00:05:45].
To evaluate the integral of sin(x) between 0 and π:
- Evaluate the antiderivative at the upper bound (π): -cos(π) = 1 [00:06:22].
- Evaluate the antiderivative at the lower bound (0): -cos(0) = -1 [00:06:22].
- Subtract the lower bound value from the upper bound value: 1 - (-1) = 2 [00:06:25].
This means the area under the sine graph from 0 to π is 2 [00:06:43].
The average height of sin(x) on the interval [0, π] is then:
Average Height = Area / Width = 2 / π
[00:06:48]
Which is approximately 0.64 [00:07:01].
Integrals and Derivatives as Inverses
This problem illustrates an important aspect of the relationship between integrals and derivatives. The process of finding the average value (2/π) involved:
- Looking at the change in the antiderivative (-cos(x)) over the input range [0, π] [00:07:20].
- Dividing by the length of that range (π) [00:07:24].
This fraction, (Change in Antiderivative) / (Change in x)
, is precisely the rise-over-run slope between the starting and ending points of the antiderivative graph [00:07:30].
Since sin(x) is the derivative of -cos(x), sin(x) gives the slope of the -cos(x) graph at every point [00:07:50]. Therefore, the average value of sin(x) can be thought of as the average slope over all tangent lines of the -cos(x) graph between 0 and π [00:08:03]. It makes intuitive sense that the average slope of a graph over a range should equal the total slope (rise over run) between its start and end points [00:08:08].
Generalization
For any function f(x)
, its average value on an interval [a, b]
is given by:
Average Value = (Integral of f(x) from a to b) / (b - a)
[00:08:33]
This is the signed area under the graph divided by its width [00:08:47].
The connection to finite averages is maintained:
- A finite sample’s average is
(Sum of f(x) values) / (Number of samples)
[00:09:14]. - Number of samples ≈
(b - a) / dx
[00:09:08]. - Substituting yields
(Sum of (f(x) * dx)) / (b - a)
[00:09:18]. - As
dx
approaches 0, the sum becomes the integral [00:09:27].
Evaluating the integral requires finding an antiderivative of f(x)
, often denoted as F(x)
[00:09:42]. The integral’s value is F(b) - F(a)
, which represents the change in height of the antiderivative graph between the bounds [00:09:51].
Thus, the average value is:
Average Value = (F(b) - F(a)) / (b - a)
[00:10:21]
This is the slope of the antiderivative graph between the two endpoints [00:10:31]. Since f(x)
is the derivative of F(x)
by definition, f(x)
gives the slope of the tangent line to F(x)
at each point [00:10:41]. This perspective highlights why antiderivatives are crucial for solving integrals: reframing the question of finding an average as finding the average slope allows the answer to be found by comparing only the endpoints of the antiderivative graph [00:11:01].
When to Think of Integrals
Two key “sensations” should bring integrals to mind:
- If a problem can be approximated by breaking it into small pieces and summing them up [00:11:27].
- If an idea understood in a finite context (like averaging numbers) needs to be generalized to an infinite, continuous range of values [00:11:42]. In such cases, phrasing the problem in terms of an integral is often the solution [00:11:56]. This is particularly common in probability [00:12:02].