Math Class Didn’t Show Its Work, companion reader · Chapter 28

What Is Happening Right Now?

An average can tell what happened over an interval. It cannot tell what was happening at one moment.

These four demonstrations use the chapter's constructed position model, s = t^2 in meters and seconds. Each one keeps the interval nonzero, computes an honest average rate, and then watches what those rates approach as the interval shrinks.

Every example in these readers is a constructed teaching example taken from or modeled on the book's own worked examples. The numbers are declared inputs chosen to make the mathematics visible. They are not measurements of any real person, product or study.

Demonstration 1 of 4

An average rate needs two times

Between 2 seconds and another time, how fast was the position changing on average?

The two points on the curve fix a secant line, and its slope is the average rate. Everything that happened in between is squeezed into that one number.

\[[f(b) - f(a)]/(b - a)\]

\[\text{slope} = \text{vertical change} / \text{horizontal change}\]

a and b are two input times, here a = 2 seconds. f(b) - f(a) is the change in position in meters and b - a the change in time in seconds, so the quotient is in meters per second.

Predict first. Set the second time to 2 as well. What happens to the average rate?

Choose an example

Figure: An average rate needs two times. The curve s = t squared with a dashed secant line through (2, 4) and (3, 9). Its slope is 5 meters per second.
Second time b (seconds): 3
Constructed example: the chapter's position model with positions 4 meters at 2 seconds and 9 meters at 3 seconds.

Calculated values

Interval
from 2 to 3 seconds
Change in position
9 - 4 = 5 m
Change in time
3 - 2 = 1 s
Average rate
5 meters per second

[s(3) - s(2)]/(3 - 2) = (9 - 4)/1 = 5/1 = 5 meters per second. This one number summarizes the whole interval.

Use the idea

When someone reports an average rate, ask for the two endpoints. A different interval can give a different rate for the same motion.

Where the conclusion applies

The constructed model s = t^2 with fixed units. Reversing both changes keeps the rate; reversing only one flips its sign. Equal endpoints leave a zero denominator and no rate.

Check your understanding: What is the average rate from t = 2 to t = 4?
(16 - 4)/(4 - 2) = 12/2 = 6 meters per second.

Chapter 28 source: section "Average rate uses two inputs". Demonstration C28-D01.

Demonstration 2 of 4

Shrink the interval without making it zero

What do the average rates near t = 2 do as the interval gets shorter from either side?

For every nonzero h the quotient simplifies to 4 + h, so the rates lie on a straight line with a hole at h = 0. From both sides they head toward 4.

\[[s(2 + h) - s(2)]/h\]

\[= h(4 + h)/h\]

\[= 4 + h\]

h is the interval length in seconds and is never 0. Positive h looks later than t = 2; negative h looks earlier. The quotient is the average rate over that interval.

Predict first. Switch h from 0.1 to -0.1. Will the rate land above 4 or below it?

Choose an example

Figure: Shrink the interval without making it zero. A straight line of rates 4 + h for h from -1 to 1, with an open circle at h = 0 where the quotient is never evaluated. The point h = 0.1, rate 4.1, is marked.
Step h (seconds): 0.1
Constructed example: the chapter's values h = 0.5, 0.1 and -0.1, plus h = -0.5.

Calculated values

Second time 2 + h
2 + 0.1 = 2.1 seconds
s(2 + h)
2.1^2 = 4.41
Difference quotient
(4.41 - 4)/0.1 = 4.1
Simplified rule
4 + 0.1 = 4.1
Rate approached as h shrinks
4 meters per second

With h = 0.1: [s(2.1) - s(2)]/0.1 = (4.41 - 4)/0.1 = 0.41/0.1 = 4.1. The simplified rule agrees: 4 + 0.1 = 4.1. The cancellation h(4 + h)/h = 4 + h is allowed because h is not 0.

Use the idea

When a calculation needs a rate at an instant, keep the interval nonzero, simplify, and only then ask what the result approaches.

Where the conclusion applies

The model s = t^2 near t = 2. Cancelling h is legal only because h is not 0; substituting h = 0 into the original quotient gives 0/0, which is not a rate.

Check your understanding: Using 4 + h, what is the average rate from t = 2 to t = 2.01?
h = 0.01, so 4 + 0.01 = 4.01 meters per second. Check: (4.0401 - 4)/0.01 = 4.01.

Chapter 28 source: section "Shrink the interval without making it zero". Demonstration C28-D02.

Demonstration 3 of 4

Nearby secants approach a direction

As the second point slides toward (2, 4), what happens to the secant and to the tangent estimate?

The base point (2, 4) stays fixed while the second point moves in. The dashed secant turns toward the dotted line of slope 4, the limiting direction.

\[s = t^2\]

\[4(0.1) = 0.4\]

The secant joins (2, 4) to (2 + h, (2 + h)^2). Its slope is 4 + h. The tangent estimate of the position change is 4 times h; the discrepancy is how far that estimate is off.

Predict first. Shrink h from 0.1 to 0.01. How big is the discrepancy now?

Choose an example

Figure: Nearby secants approach a direction. The curve s = t squared near (2, 4). A dashed secant joins (2, 4) to (2.1, 4.41) with slope 4.1; a dotted line through (2, 4) has slope 4.
Interval length h (seconds): 0.1
Constructed example: the chapter's table of intervals from 2 to 3, 2.5, 2.1 and 2.01.

Calculated values

Interval length h
0.1 s
Secant slope 4 + h
4 + 0.1 = 4.1 m/s
Exact change
2.1^2 - 4 = 0.41 m
Tangent estimate 4h
4(0.1) = 0.4 m
Discrepancy
0.41 - 0.4 = 0.01 m

Over h = 0.1 s, the exact change is 2.1^2 - 4 = 0.41 m and the tangent estimate is 4(0.1) = 0.4 m, a discrepancy of 0.01 m. The secant slope 4.1 sits 0.1 above 4; shrink h and both the slope gap and the discrepancy shrink.

Use the idea

Near a point where a rate exists, change is roughly the rate times the small step. The word roughly is honest only for small steps.

Where the conclusion applies

The model s = t^2 near t = 2. The local estimate 4h is good over small h, not over every interval: at h = 1 it is off by a whole meter.

Check your understanding: At h = 0.5, what are the exact change, the tangent estimate, and the discrepancy?
2.5^2 - 4 = 6.25 - 4 = 2.25 meters; 4(0.5) = 2 meters; the discrepancy is 0.25 meter.

Chapter 28 source: section "Nearby secants approach a direction". Demonstration C28-D03.

Demonstration 4 of 4

A corner has no single rate

At the corner of |x|, do the slopes from the left and from the right agree?

On the right the graph is the line y = x, on the left the line y = -x. Every right-hand quotient is 1 and every left-hand quotient is -1, however small h gets.

\[[g(h) - g(0)]/h = |h|/h = 1\]

\[|h|/h = -1\]

g(x) = |x| is the distance of x from 0. h is a nonzero step from 0; |h|/h is the slope of the secant from (0, 0) to (h, |h|).

Predict first. Switch h from 0.01 to -0.01. Does the secant slope move a little or flip completely?

Choose an example

Figure: A corner has no single rate. A V-shaped graph of |x| with its corner at the origin. A dashed secant runs from (0, 0) to (0.01, 0.01) with slope 1.
Step h from 0: 0.01
Constructed example: the chapter's absolute value function at 0, with steps chosen for the reader.

Calculated values

Step h
0.01
g(h) - g(0)
|0.01| - 0 = 0.01
Quotient |h|/h
0.01/0.01 = 1
Right-hand quotients
1 for every positive h
Left-hand quotients
-1 for every negative h
g'(0)
undefined (the sides approach 1 and -1)

With h = 0.01: [g(0.01) - g(0)]/0.01 = 0.01/0.01 = 1. Every right-hand quotient gives 1, however small h is. The other side gives -1. The sides disagree, so g'(0) does not exist, even though |x| is continuous at 0.

Use the idea

When a graph has a sharp corner, check both one-sided rates before naming a single rate.

Where the conclusion applies

Only the example g(x) = |x| at 0. The function is continuous there; it is the derivative that fails, because the two sides approach different numbers.

Check your understanding: For g(x) = |x|, what is the quotient [g(h) - g(0)]/h at h = -0.2?
|-0.2|/(-0.2) = 0.2/(-0.2) = -1.

Chapter 28 source: section "Derivatives can fail to exist". Demonstration C28-D04.