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1.3 - Rates of Change in Linear and Quadratic Functions

Overview

Average rates of change can tell function types apart. For a linear function, the average rate of change never changes. For a quadratic function, it does change, but at a steady rate. In this topic you'll see why, connect the average rate of change to the slope of a secant line, and use changing rates to decide whether a graph is concave up or concave down.

Average rate of change is the slope of a secant line

A secant line is a line through two points on a graph. The average rate of change of ff over [a,b][a, b] is the slope of the secant line from (a,f(a))(a, f(a)) to (b,f(b))(b, f(b)):
slope of secant line=f(b)−f(a)b−a\text{slope of secant line} = \frac{f(b) - f(a)}{b - a}
So every time you compute an average rate of change, you're finding a slope. For example, here is the secant line for f(x)=x2−4x+5f(x) = x^2 - 4x + 5 over [1,4][1, 4]. Since f(1)=2f(1) = 2 and f(4)=5f(4) = 5:
f(4)−f(1)4−1=5−23=1\frac{f(4) - f(1)}{4 - 1} = \frac{5 - 2}{3} = 1
1.3 - Rates of Change in Linear and Quadratic Functions
The secant line rises 33 units over a run of 33 units, so its slope, which is the average rate of change of ff over [1,4][1, 4], is 11.

Linear functions: A constant rate of change

For a linear function f(x)=mx+bf(x) = mx + b, the average rate of change over any interval, of any length, is the same number mm:
f(x2)−f(x1)x2−x1=(mx2+b)−(mx1+b)x2−x1=m(x2−x1)x2−x1=m\frac{f(x_2) - f(x_1)}{x_2 - x_1} = \frac{(mx_2 + b) - (mx_1 + b)}{x_2 - x_1} = \frac{m(x_2 - x_1)}{x_2 - x_1} = m
For example, look at g(x)=−2x+7g(x) = -2x + 7 at equally spaced inputs:
xx
00
11
22
33
44
g(x)g(x)
77
55
33
11
−1-1
Every output drops by 22, so every average rate of change over these intervals is −2-2. Since the average rates of change over consecutive equal-length intervals are constant, they are changing at a rate of zero. That's the signature of a linear function.

Quadratic functions: Rates that change at a constant rate

For a quadratic function, the average rate of change is not constant. But over consecutive equal-length intervals, the average rates of change follow a linear pattern, so they change by the same amount each step.

Example 1: Average rates of change of a quadratic

Let f(x)=x2−4x+5f(x) = x^2 - 4x + 5. Find the average rates of change over [0,1][0, 1], [1,2][1, 2], [2,3][2, 3], [3,4][3, 4], and [4,5][4, 5].
The outputs are f(0)=5f(0) = 5, f(1)=2f(1) = 2, f(2)=1f(2) = 1, f(3)=2f(3) = 2, f(4)=5f(4) = 5, and f(5)=10f(5) = 10. Each interval has length 11:
Interval
Average rate of change
Change from the previous rate
[0,1][0, 1]
2−51=−3\frac{2 - 5}{1} = -3
[1,2][1, 2]
1−21=−1\frac{1 - 2}{1} = -1
+2+2
[2,3][2, 3]
2−11=1\frac{2 - 1}{1} = 1
+2+2
[3,4][3, 4]
5−21=3\frac{5 - 2}{1} = 3
+2+2
[4,5][4, 5]
10−51=5\frac{10 - 5}{1} = 5
+2+2
Each red segment below is a secant line, labeled with its slope:
1.3 - Rates of Change in Linear and Quadratic Functions
Answer: the average rates of change are −3,−1,1,3,5-3, -1, 1, 3, 5. Each is 22 more than the one before, so the average rates of change are changing at a constant rate of 22 per interval. In fact, the average rate of change over [k,k+1][k, k + 1] is given by the linear function r(k)=2k−3r(k) = 2k - 3.

Why this works for every quadratic

Take any quadratic f(x)=ax2+bx+cf(x) = ax^2 + bx + c and any interval length hh. The average rate of change from xx to x+hx + h is:
f(x+h)−f(x)h=a(x+h)2+b(x+h)+c−(ax2+bx+c)h\frac{f(x + h) - f(x)}{h} = \frac{a(x + h)^2 + b(x + h) + c - (ax^2 + bx + c)}{h}=2axh+ah2+bhh=2ax+ah+b= \frac{2axh + ah^2 + bh}{h} = 2ax + ah + b
With hh fixed, this is a linear function of xx with slope 2a2a. Moving to the next interval adds hh to xx, so each new average rate of change is 2ah2ah more than the last. For f(x)=x2−4x+5f(x) = x^2 - 4x + 5 with h=1h = 1, that's 2(1)(1)=22(1)(1) = 2, which matches the table.

Other functions and sequences

For other function types, neither pattern holds. For f(x)=x3f(x) = x^3 at x=0,1,2,3,4x = 0, 1, 2, 3, 4, the average rates of change over the unit intervals are 1,7,19,371, 7, 19, 37. They aren't constant, and they don't change by a constant amount either: the changes are 6,12,186, 12, 18. In Topic 1.5 you'll see that a cubic needs one more round of differences before the pattern turns constant.
A sequence is also a function: its inputs are the term numbers n=1,2,3,…n = 1, 2, 3, \ldots, so the same ideas apply. The average rate of change from term n1n_1 to term n2n_2 is an2−an1n2−n1\frac{a_{n_2} - a_{n_1}}{n_2 - n_1}.
  • 4,7,10,13,…4, 7, 10, 13, \ldots: each term is 33 more than the last, so the average rate of change is a constant 33 per term. That's a linear pattern (you'll call it an arithmetic sequence in Unit 2).
  • 2,5,10,17,26,…2, 5, 10, 17, 26, \ldots: the changes are 3,5,7,93, 5, 7, 9, which go up by 22 each step. That's a quadratic pattern. (These terms are an=n2+1a_n = n^2 + 1.)

Concavity from average rates of change

Average rates of change over equal-length intervals also reveal concavity:
  • If the average rates of change over equal-length intervals are increasing (for all small intervals), the graph is concave up.
  • If they are decreasing, the graph is concave down.
This matches Topic 1.1: concave up means the rate of change is increasing. In Example 1, the rates −3,−1,1,3,5-3, -1, 1, 3, 5 increase, and the parabola opens up. For any quadratic, the rates change by 2ah2ah each step, so the graph is concave up everywhere when a>0a > 0 and concave down everywhere when a<0a < 0.

Example 2: A growing plant (AP-style)

The height of a plant, h(t)h(t), in centimeters, is measured every 22 weeks. The results are in the table.
tt (weeks)
00
22
44
66
88
h(t)h(t) (centimeters)
1010
1818
2424
2828
3030
(a) Find the average rate of change of hh over each consecutive interval in the table. (b) Is the graph of hh concave up or concave down on 0≤t≤80 \le t \le 8? Give a reason. (c) Is a linear model or a quadratic model more appropriate for these data? Give a reason.
(a) Each interval has length 22, so divide each change in height by 22:
Interval
Average rate of change (cm per week)
[0,2][0, 2]
18−102=4\frac{18 - 10}{2} = 4
[2,4][2, 4]
24−182=3\frac{24 - 18}{2} = 3
[4,6][4, 6]
28−242=2\frac{28 - 24}{2} = 2
[6,8][6, 8]
30−282=1\frac{30 - 28}{2} = 1
(b) The average rates of change over consecutive equal-length intervals, 4,3,2,14, 3, 2, 1 centimeters per week, are decreasing. So the graph of hh is concave down. In context, the plant keeps growing, but more slowly as time goes on.
(c) The average rates of change are not constant, so a linear model doesn't fit. They decrease by exactly 11 from each interval to the next, so they change at a constant rate, which is the pattern of a quadratic function. A quadratic model is more appropriate. (In fact, h(t)=−14t2+92t+10h(t) = -\frac{1}{4}t^2 + \frac{9}{2}t + 10 matches every value in the table.)

Common mistakes

  • Using unequal intervals. The linear and quadratic patterns only show up over equal-length intervals. Check the spacing of the inputs before you compare rates.
  • Confusing the rates with the change in the rates. For a quadratic, the average rates of change are not constant. The change from one rate to the next is.
  • Getting concavity backward with negative rates. Rates of −5,−3,−1-5, -3, -1 are increasing, so the graph is concave up, even though every rate is negative.
  • Forgetting to divide by the interval length. If the inputs go up by 22, divide each change in output by 22.

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