AP Precalculus · Unit 1: Polynomial and Rational Functions · Lesson 1.3

Deep Dive: Rates of Change in Linear and Quadratic Functions

🔬 Deep Dive
This is your textbook for this topic. Take your time. Read it more than once.
1.3.A1.3.A.1Concept

Linear Functions: One Rate Everywhere

For a linear function, the average rate of change over any length input-value interval is constant. To see why, take f(x) = mx + b and any interval [p, q]. The output changes by (mq + b) − (mp + b) = m(q − p), and the input changes by q − p, so the ratio is exactly m. Short interval, long interval, left side, right side: always m.

f(x) = mx + b → average rate of change = m on every interval

Build a linear function f(x) = mx + b, then pick any interval you like. Short or long, left or right, the average rate of change comes out the same.

slope m2.0
intercept b1
interval start-1
interval end3
-4-2024-10-50510xf(x)
f(x) = 2.0x + 1change in output: f(3) − f(-1) = 7.00 − (-1.00) = 8.00change in input: 3 − (-1) = 4average rate of change = 2.00 (the slope m)
other intervallengthaverage rate of change
[-4, -3]12.00
[0, 1]12.00
[-3, 4]72.00
[2, 5]32.00
🔑“Constant” does not mean “zero.” The rate of a linear function is the same number everywhere (the slope m), and it is zero only when m = 0. This is the single most useful fact about linear functions: one rate, no matter which interval you pick.
1.3.A1.3.A.2Math

Quadratic Functions: Rates That Follow a Line

A quadratic function f(x) = ax² + bx + c does not have one rate. The average rate of change depends on where the interval sits. But there is a pattern. For consecutive equal-length input-value intervals, the average rates of change can be given by a linear function. If each interval has length h, then

[f(x+h) − f(x)] / h = 2a · (x + h/2) + b

The right side is a linear function of the interval's midpoint x + h/2, with slope 2a. Slide a and b and watch the points on the right-hand graph: they always fall on a straight line.

f(x) = ax² + bx. The five intervals below all have the same length h and sit side by side, starting at x = 0. The graph on the left shows the chords. The graph on the right plots each interval's average rate of change at the interval's midpoint.

a1.0
b0
0123450510152025xf(x)0123450246810midpoint of intervalaverage rate
intervalaverage rate of changechange from the previous
[0.0, 1.0]1.00—
[1.0, 2.0]3.00+2.00
[2.0, 3.0]5.00+2.00
[3.0, 4.0]7.00+2.00
[4.0, 5.0]9.00+2.00
average rate on [x, x + h] = 2a · (midpoint) + b = 2.0 · (midpoint) + 0The points on the right all lie on a straight line with slope 2a = 2.0.change per interval = 2ah = 2 · 1.0 · 1 = 2.00
⚠️The pattern needs equal-length, consecutive intervals. If the intervals have different lengths, or skip around, the rates will not line up on a straight line.
1.3.A1.3.A.3Concept

Average Rate of Change Is a Secant Slope

The average rate of change of a function f over the closed interval [a, b] is the slope of the secant line from the point (a, f(a)) to the point (b, f(b)). Rise over run on that line is the change in output over the change in input.

slope of secant = rise / run = [f(b) − f(a)] / (b − a)

Drag the two endpoints. The dashed line through the two points on the curve is the secant line. Its slope, rise over run, is exactly the average rate of change.

input a2.0
input b5.0
-101234505101520xf(x)
run = 5.00 − (2.00) = 3.00rise = f(5.00) − f(2.00) = 20.00 − (2.00) = 18.00slope of the secant = rise ÷ run = 6.00 = average rate of changeUphill secant: positive average rate.
💡Try f(x) = x² − x with a = 0 and b = 1. The secant is horizontal, so the average rate is 0, yet f is not constant. For the linear function, every secant is the line itself, which is why the rate never changes.
1.3.B1.3.B.11.3.B.2Concept

How Fast Are the Rates Changing?

Now ask a second question: if you list the average rates over consecutive equal-length intervals, how are those rates changing?

For a linear function the rates are all the same constant, so they are changing at a rate of zero. For a quadratic function the rates fit a linear function, so they are changing at a constant rate. In fact, when the intervals have length h, each rate is 2ah larger than the one before it.

linear: rates change by 0
quadratic: rates change by 2ah

Pick a function and an interval length h. The table finds the average rate of change on each consecutive interval of length h, and then asks the new question: how are those rates changing?

x012345
f(x)0.001.004.009.0016.0025.00
average rate on the interval ending here—1.003.005.007.009.00
change in the rate——+2.00+2.00+2.00+2.00
The rates are not the same, but they change by +2.00 every time.So the rates are changing at a constant rate, and they follow a linear function. (1.3.B.2: quadratic)Check: 2ah = 2 · 1.0 · 1 = 2.00
⚠️Two different ideas: a linear function has a constant rate (the same AROC everywhere). A quadratic function has a rate that changes at a constant rate (the AROC moves by the same amount each step). Try the cubic: its rates change by different amounts, so it is neither.
1.3.B1.3.B.3Concept

Concave Up and Concave Down

When the average rate of change over equal-length intervals is increasing for all small-length intervals, the graph is concave up. When it is decreasing for all small-length intervals, the graph is concave down. Concavity reads the trend of the rates, so it works for any function, not only quadratics.

Each chord below is colored by what the average rates are doing: green where the rates are increasing from one interval to the next, coral where they are decreasing. All intervals have the same length.

0123456010203040xf(x)
intervalaverage ratecompared with the previous
[0.0, 1.0]1.00—
[1.0, 2.0]3.00▲ increasing
[2.0, 3.0]5.00▲ increasing
[3.0, 4.0]7.00▲ increasing
[4.0, 5.0]9.00▲ increasing
[5.0, 6.0]11.00▲ increasing
Verdict from the rates: concave up.Increasing rates mean a graph that bends upward (concave up). Decreasing rates mean a graph that bends downward (concave down).
⚠️Concavity is about the rates increasing or decreasing, not about the function itself. A decreasing function can be concave up: rates of −6, −5, −4, −3 are all negative, but each one is larger than the last, so the graph is concave up. Try x³ − 3x too: its rates fall and then rise, so it switches from concave down to concave up.
1.3.A1.3.BMath

Linear, Quadratic, or Neither?

Given a table with equally spaced inputs, you can tell what kind of function it could come from. Find the average rate on each interval. If the rates are all equal, the data is linear. If the rates are not equal but they change by the same amount each step, the data is quadratic. If neither happens, it is something else.

Function typeRates over consecutive equal-length intervalsHow the rates change
LinearThe same constantAt a rate of 0
QuadraticGiven by a linear functionAt a constant rate, 2ah (concave up if a > 0, down if a < 0)
Other typesNeither of theseNot at a constant rate; may be concave up, down, or both

Each table has equally spaced inputs. Work out the average rates and the changes in the rates, then decide what kind of function could be behind the data.

seconds01234
height (ft)04864480
average rate—48.0016.00-16.00-48.00
change in the rate——-32.00-32.00-32.00
Rates change by -32.00 (feet per second, each second) every step.Quadratic. The rates are decreasing, so the graph is concave down.The rate starts positive and ends negative: the height rises and then falls.
🔑In context, name the units twice. The ball's average rate is in feet per second, and how fast that rate changes is in feet per second, each second. A change of −32 means the ball's rate drops by 32 feet per second every second.
← Back to Lesson 1.3Try Guided Practice →Ready for 1.4? Polynomial Functions and Rates of Change takes these ideas to higher degrees.