Draw a graph on a sheet of rubber and pull the sheet up and down, away from the -axis. The curve gets taller, yet every point on the -axis stays where it was. Multiplying the outputs of a function by a constant does exactly this. Multiplying the inputs pulls or squeezes the sheet sideways instead, and there the effect runs opposite to the number in the formula.
Key terms
Vertical stretch and compression
Definition Let be a function and let be a constant. The function has the same domain as , and a point lies on the graph of exactly when lies on the graph of . If the graph of is a vertical stretch of the graph of by the factor . If it is a vertical compression by the factor . Every distance from the -axis is multiplied by , so points on the -axis stay fixed, the zeros of are the zeros of , and the range of consists of the numbers with in the range of .
In plain words Each point moves straight up or down until it is times as far from the -axis as before. The inputs do not change, only the outputs.
Example Let , with zeros and and lowest point . Compare it with and .
The zeros stay at . The lowest point moves down to under the stretch and up to under the compression, and the range becomes and .
Horizontal compression and stretch
Definition Let be a function and let be a constant. The function is defined at exactly when is in the domain of . Since
a point lies on the graph of exactly when lies on the graph of . If the graph of is a horizontal compression of the graph of toward the -axis by the factor . If it is a horizontal stretch away from the -axis by the factor . Points on the -axis stay fixed, and the range does not change.
In plain words The new function gives the output at the input instead of at . For every input is halved, so the graph is squeezed to half its width.
Example Let , with zeros and and lowest point . Then
with zeros and and lowest point . Every first coordinate is halved and every height stays the same. The point moves to , while on the -axis does not move. Squeezing also makes the graph steeper. The secant line of through and has slope , and the matching secant line of through and has slope . This doubling of slopes is why the derivative of carries a factor in the chain rule.
Multiplier
Definition In the formula with nonzero constants and , the number is the outside multiplier and is the inside multiplier. The outside multiplier multiplies each output after has acted. The inside multiplier multiplies each input before acts. When the input of also contains a constant, as in , the inside multiplier is still the coefficient of . Factoring the input as shows that this multiplies the whole of , which matters once stretches and shifts are combined.
In plain words Outside, a multiplier does what it says to the heights. Inside, it does the opposite to the widths, because a bigger multiplier on the input makes reach each value closer to the -axis.
Example Take and the multiplier in both places. At the outside version gives and the inside version gives . The point on the graph of goes to on the graph of and to on the graph of . For this particular the identity shows that the inside multiplier has the same effect as the outside multiplier . That does not happen in general. For every graph with has zeros and , while has zeros and , so no outside multiplier can match it.
Scale factor
Definition A scale factor is the positive number by which a stretch or compression multiplies distances in one direction. For with the vertical scale factor is , with distances measured from the -axis. For with the horizontal scale factor is , with distances measured from the -axis. A scale factor greater than gives a stretch and one between and gives a compression. A negative multiplier adds a reflection, across the -axis when and across the -axis when . In every case a point on the graph of corresponds to a point on the graph of by the rule
In plain words The scale factor says how much bigger or smaller the graph gets in one direction. Read it straight from an outside multiplier, and take the reciprocal of an inside one. The sign only decides whether the graph also flips.
Example Suppose has domain and its graph passes through , and let . The inside multiplier gives the horizontal scale factor , a stretch. The outside multiplier gives the vertical scale factor together with a reflection across the -axis. The point goes to , and indeed . The domain of is , since needs to lie in .
Dilation
Definition For a constant , the dilation of the plane centered at the origin with scale factor sends each point to . The vertical dilation with factor sends to and keeps the -axis fixed, and the horizontal dilation with factor sends to and keeps the -axis fixed. These three maps carry the graph of onto the graphs of
respectively. The word dilation covers both stretches, with , and compressions, with .
In plain words A dilation centered at the origin is a zoom. It changes the size of the picture but not its shape. A dilation in one direction pulls the picture one way only, which in general does change the shape.
Example Zoom the parabola by the factor about the origin. The first rule gives
The point goes to , and indeed . In the same way the zoom with factor carries onto for any , so all these parabolas have the same shape and differ only in size. Parabolas are special in this way, because the vertical dilation of is also a zoom of it. A semicircle stretched vertically, by contrast, becomes half of an ellipse and really changes shape.
Stretches combined with shifts
Definition For constants , , and , consider
For each point on the graph of the point lies on the graph of , because
So the first coordinate is scaled by and then shifted by , and the second is scaled by and then shifted by . With and equal to or this is the rule for shifts and reflections, since then . When the input is written as , factor out first,
so the horizontal shift is and not .
In plain words Rewrite the inside until it reads . Then move each point by scaling first and shifting second, in both directions.
Example Start from and take . Factoring gives , so , , and , and each point goes to .
| Point on | Point on |
|---|---|
As a check, . The domain of is , from . Reading as a shift by would put the starting point at , but , which is not .
Check yourself
- The graph of passes through , and . Find the corresponding points on the graph of .
Show the answer
Each point goes to , which gives , and . As a check, .
- Compress the graph of horizontally by the factor , then stretch it vertically by the factor . Write the new function and find its value at .
Show the answer
The horizontal compression by uses the inside multiplier and the vertical stretch uses the outside multiplier , so and . Since for , the same graph is also .
- Explain how the graph of comes from the graph of .
Show the answer
Factor the inside as . Compress horizontally toward the -axis by the factor , then shift left by . The vertex goes to , and the point goes to . Indeed and .