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11.5 Graphs of Polar Equations

In this section, we discuss how to graph equations in polar coordinates on the rectangular coordinate plane. Since any given point in the plane has infinitely many different representations in polar coordinates, our `Fundamental Graphing Principle' in this section is not as clean as it was for graphs of rectangular equations on page. We state it below for completeness.

The Fundamental Graphing Principle for Polar Equations

The graph of an equation in polar coordinates is the set of points which satisfy the equation. That is, a point P ( r , θ ) is on the graph of an equation if and only if there is a representation of P , say ( r , θ ) , such that r and θ satisfy the equation.

Our first example focuses on some of the more structurally simple polar equations.

Hopefully, our experience in Example Example 1 makes the following result clear.

Suppose we wish to graph r = 6 cos ( θ ) . A reasonable way to start is to treat θ as the independent variable, r as the dependent variable, evaluate r = f ( θ ) at some `friendly' values of θ and plot the resulting points.2 We generate the table below.

θ r = 6 cos ( θ ) ( r , θ ) 0 6 ( 6 , 0 ) π 4 3 2 ( 3 2 , π 4 ) π 2 0 ( 0 , π 2 ) 3 π 4 3 2 ( 3 2 , 3 π 4 ) π 6 ( 6 , π ) 5 π 4 3 2 ( 3 2 , 5 π 4 ) 3 π 2 0 ( 0 , 3 π 2 ) 7 π 4 3 2 ( 3 2 , 7 π 4 ) 2 π 6 ( 6 , 2 π )

Coordinate-plane figure.
Figure 11.117

Despite having nine ordered pairs, we get only four distinct points on the graph. For this reason, we employ a slightly different strategy. We graph one cycle of r = 6 cos ( θ ) on the θ r -plane3 and use it to help graph the equation on the x y -plane. We see that as θ ranges from 0 to π 2 , r ranges from 6 to 0 . In the x y -plane, this means that the curve starts 6 units from the origin on the positive x -axis ( θ = 0 ) and gradually returns to the origin by the time the curve reaches the y -axis ( θ = π 2 ). The arrows drawn in the figure below are meant to help you visualize this process. In the θ r -plane, the arrows are drawn from the θ -axis to the curve r = 6 cos ( θ ) . In the x y -plane, each of these arrows starts at the origin and is rotated through the corresponding angle θ , in accordance with how we plot polar coordinates. It is a less-precise way to generate the graph than computing the actual function values, but it is markedly faster.

Coordinate-plane figure.
Figure 11.118
Coordinate-plane figure.
Figure 11.119

Next, we repeat the process as θ ranges from π 2 to π . Here, the r values are all negative. This means that in the x y -plane, instead of graphing in Quadrant II, we graph in Quadrant IV, with all of the angle rotations starting from the negative x -axis.

Coordinate-plane figure.
Figure 11.120
Coordinate-plane figure.
Figure 11.121

As θ ranges from π to 3 π 2 , the r values are still negative, which means the graph is traced out in Quadrant I instead of Quadrant III. Since the | r | for these values of θ match the r values for θ in [ 0 , π 2 ] , we have that the curve begins to retrace itself at this point. Proceeding further, we find that when 3 π 2 θ 2 π , we retrace the portion of the curve in Quadrant IV that we first traced out as π 2 θ π . The reader is invited to verify that plotting any range of θ outside the interval [ 0 , π ] results in retracting some portion of the curve.4 We present the final graph below.

Coordinate-plane figure.
Figure 11.122
Coordinate-plane figure.
Figure 11.123

r = 6 cos ( θ ) in the θ r -plane

r = 6 cos ( θ ) in the x y -plane

A few remarks are in order. First, there is no relation, in general, between the period of the function f ( θ ) and the length of the interval required to sketch the complete graph of r = f ( θ ) in the x y -plane. As we saw on page, despite the fact that the period of f ( θ ) = 6 cos ( θ ) is 2 π , we sketched the complete graph of r = 6 cos ( θ ) in the x y -plane just using the values of θ as θ ranged from 0 to π . In Example Example 2, number, the period of f ( θ ) = 5 sin ( 2 θ ) is π , but in order to obtain the complete graph of r = 5 sin ( 2 θ ) , we needed to run θ from 0 to 2 π . While many of the `common' polar graphs can be grouped into families,9 the authors truly feel that taking the time to work through each graph in the manner presented here is the best way to not only understand the polar coordinate system, but also prepare you for what is needed in Calculus. Second, the symmetry seen in the examples is also a common occurrence when graphing polar equations. In addition to the usual kinds of symmetry discussed up to this point in the text (symmetry about each axis and the origin), it is possible to talk about rotational symmetry. We leave the discussion of symmetry to the Exercises. In our next example, we are given the task of finding the intersection points of polar curves. According to the Fundamental Graphing Principle for Polar Equations on page, in order for a point P to be on the graph of a polar equation, it must have a representation P ( r , θ ) which satisfies the equation. What complicates matters in polar coordinates is that any given point has infinitely many representations. As a result, if a point P is on the graph of two different polar equations, it is entirely possible that the representation P ( r , θ ) which satisfies one of the equations does not satisfy the other equation. Here, more than ever, we need to rely on the Geometry as much as the Algebra to find our solutions.

Our work in Example Example 3 justifies the following.

Guidelines for Finding Points of Intersection of Graphs of Polar Equations

To find the points of intersection of the graphs of two polar equations E 1 and E 2 :

Our last example ties together graphing and points of intersection to describe regions in the plane.

Exercises

In Exercises -, plot the graph of the polar equation by hand. Carefully label your graphs.

  1. Circle: r = 6 sin ( θ )
  2. Circle: r = 2 cos ( θ )
  3. Rose: r = 2 sin ( 2 θ )
  4. Rose: r = 4 cos ( 2 θ )
  5. Rose: r = 5 sin ( 3 θ )
  6. Rose: r = cos ( 5 θ )
  7. Rose: r = sin ( 4 θ )
  8. Rose: r = 3 cos ( 4 θ )
  9. Cardioid: r = 3 3 cos ( θ )
  10. Cardioid: r = 5 + 5 sin ( θ )
  11. Cardioid: r = 2 + 2 cos ( θ )
  12. Cardioid: r = 1 sin ( θ )
  13. Limaçon: r = 1 2 cos ( θ )
  14. Limaçon: r = 1 2 sin ( θ )
  15. Limaçon: r = 2 3 + 4 cos ( θ )
  16. Limaçon: r = 3 5 cos ( θ )
  17. Limaçon: r = 3 5 sin ( θ )
  18. Limaçon: r = 2 + 7 sin ( θ )
  19. Lemniscate: r 2 = sin ( 2 θ )
  20. Lemniscate: r 2 = 4 cos ( 2 θ )
  21. r = 3 cos ( θ ) and r = 1 + cos ( θ )
  22. r = 1 + sin ( θ ) and r = 1 cos ( θ )
  23. r = 1 2 sin ( θ ) and r = 2
  24. r = 1 2 cos ( θ ) and r = 1
  25. r = 2 cos ( θ ) and r = 2 3 sin ( θ )
  26. r = 3 cos ( θ ) and r = sin ( θ )
  27. r 2 = 4 cos ( 2 θ ) and r = 2
  28. r 2 = 2 sin ( 2 θ ) and r = 1
  29. r = 4 cos ( 2 θ ) and r = 2
  30. r = 2 sin ( 2 θ ) and r = 1
  31. { ( r , θ ) |  0 r 3 ,  0 θ 2 π }
  32. { ( r , θ ) |  0 r 4 sin ( θ ) ,  0 θ π }
  33. { ( r , θ ) |  0 r 3 cos ( θ ) , π 2 θ π 2 }
  34. { ( r , θ ) |  0 r 2 sin ( 2 θ ) ,  0 θ π 2 }
  35. { ( r , θ ) |  0 r 4 cos ( 2 θ ) , π 4 θ π 4 }
  36. { ( r , θ ) |  1 r 1 2 cos ( θ ) , π 2 θ 3 π 2 }
  37. { ( r , θ ) |  1 + cos ( θ ) r 3 cos ( θ ) , π 3 θ π 3 }
  38. { ( r , θ ) |  1 r 2 sin ( 2 θ ) , 13 π 12 θ 17 π 12 }
  39. { ( r , θ ) |  0 r 2 3 sin ( θ ) ,  0 θ π 6 } { ( r , θ ) |  0 r 2 cos ( θ ) , π 6 θ π 2 }
  40. { ( r , θ ) |  0 r 2 sin ( 2 θ ) ,  0 θ π 12 } { ( r , θ ) |  0 r 1 , π 12 θ π 4 }
  41. The region inside the circle r = 5 .
  42. The region inside the circle r = 5 which lies in Quadrant III.
  43. The region inside the left half of the circle r = 6 sin ( θ ) .
  44. The region inside the circle r = 4 cos ( θ ) which lies in Quadrant IV.
  45. The region inside the top half of the cardioid r = 3 3 cos ( θ )
  46. The region inside the cardioid r = 2 2 sin ( θ ) which lies in Quadrants I and IV.
  47. The inside of the petal of the rose r = 3 cos ( 4 θ ) which lies on the positive x -axis
  48. The region inside the circle r = 5 but outside the circle r = 3 .
  49. The region which lies inside of the circle r = 3 cos ( θ ) but outside of the circle r = sin ( θ )
  50. The region in Quadrant I which lies inside both the circle r = 3 as well as the rose r = 6 sin ( 2 θ )

In Exercises -, find the exact polar coordinates of the points of intersection of graphs of the polar equations. Remember to check for intersection at the pole (origin).

In Exercises -, sketch the region in the x y -plane described by the given set.

In Exercises -, use set-builder notation to describe the polar region. Assume that the region contains its bounding curves.

While the authors truly believe that graphing polar curves by hand is fundamental to your understanding of the polar coordinate system, we would be derelict in our duties if we totally ignored the graphing calculator. Indeed, there are some important polar curves which are simply too difficult to graph by hand and that makes the calculator an important tool for your further studies in Mathematics, Science and Engineering. We now give a brief demonstration of how to use the graphing calculator to plot polar curves. The first thing you must do is switch the MODE of your calculator to POL, which stands for “polar”.

Image: Polar01
Figure 11.176
Image: Polar02
Figure 11.177
Image: Polar03
Figure 11.178

This changes the “Y=” menu as seen above in the middle. Let's plot the polar rose given by r = 3 cos ( 4 θ ) from Exercise above. We type the function into the “r=” menu as seen above on the right. We need to set the viewing window so that the curve displays properly, but when we look at the WINDOW menu, we find three extra lines.

Image: Polar04
Figure 11.179
Image: Polar05
Figure 11.180

In order for the calculator to be able to plot r = 3 cos ( 4 θ ) in the x y -plane, we need to tell it not only the dimensions which x and y will assume, but we also what values of θ to use. From our previous work, we know that we need 0 θ 2 π , so we enter the data you see above. (I'll say more about the θ -step in just a moment.) Hitting GRAPH yields the curve below on the left which doesn't look quite right. The issue here is that the calculator screen is 96 pixels wide but only 64 pixels tall. To get a true geometric perspective, we need to hit ZOOM SQUARE (seen below in the middle) to produce a more accurate graph which we present below on the right.

Image: Polar06
Figure 11.181
Image: Polar07
Figure 11.182
Image: Polar08
Figure 11.183

In function mode, the calculator automatically divided the interval [Xmin, Xmax] into 96 equal subintervals. In polar mode, however, we must specify how to split up the interval [ θ min, θ max] using the θ step. For most graphs, a θ step of 0.1 is fine. If you make it too small then the calculator takes a long time to graph. It you make it too big, you get chunky garbage like this.

Image: Polar09
Figure 11.184

You will need to experiment with the settings in order to get a nice graph. Exercises - give you some curves to graph using your calculator. Notice that some of them have explicit bounds on θ and others do not.

  1. r = θ ,  0 θ 12 π
  2. r = ln ( θ ) ,  1 θ 12 π
  3. r = e .1 θ ,  0 θ 12 π
  4. r = θ 3 θ , 1.2 θ 1.2
  5. r = sin ( 5 θ ) 3 cos ( θ )
  6. r = sin 3 ( θ 2 ) + cos 2 ( θ 3 )
  7. r = arctan ( θ ) , π θ π
  8. r = 1 1 cos ( θ )
  9. r = 1 2 cos ( θ )
  10. r = 1 2 3 cos ( θ )
  11. How many petals does the polar rose r = sin ( 2 θ ) have? What about r = sin ( 3 θ ) , r = sin ( 4 θ ) and r = sin ( 5 θ ) ? With the help of your classmates, make a conjecture as to how many petals the polar rose r = sin ( n θ ) has for any natural number n . Replace sine with cosine and repeat the investigation. How many petals does r = cos ( n θ ) have for each natural number n ?
  12. Show that if f is even17 then the graph of r = f ( θ ) is symmetric about the x -axis.

    1. Show that f ( θ ) = 2 + 4 cos ( θ ) is even and verify that the graph of r = 2 + 4 cos ( θ ) is indeed symmetric about the x -axis. (See Example Example 2 number.)
    2. Show that f ( θ ) = 3 sin ( θ 2 ) is not even, yet the graph of r = 3 sin ( θ 2 ) is symmetric about the x -axis. (See Example Example 3 number.)
  13. Show that if f is odd18 then the graph of r = f ( θ ) is symmetric about the origin.

    1. Show that f ( θ ) = 5 sin ( 2 θ ) is odd and verify that the graph of r = 5 sin ( 2 θ ) is indeed symmetric about the origin. (See Example Example 2 number.)
    2. Show that f ( θ ) = 3 cos ( θ 2 ) is not odd, yet the graph of r = 3 cos ( θ 2 ) is symmetric about the origin. (See Example Example 3 number.)
  14. Show that if f ( π θ ) = f ( θ ) for all θ in the domain of f then the graph of r = f ( θ ) is symmetric about the y -axis.

    1. For f ( θ ) = 4 2 sin ( θ ) , show that f ( π θ ) = f ( θ ) and the graph of r = 4 2 sin ( θ ) is symmetric about the y -axis, as required. (See Example Example 2 number.)
    2. For f ( θ ) = 5 sin ( 2 θ ) , show that f ( π π 4 ) f ( π 4 ) , yet the graph of r = 5 sin ( 2 θ ) is symmetric about the y -axis. (See Example Example 2 number.)
  15. For Exercises and below, let f ( θ ) = cos ( θ ) and g ( θ ) = 2 sin ( θ ) .

    1. Using your graphing calculator, compare the graph of r = f ( θ ) to each of the graphs of r = f ( θ + π 4 ) , r = f ( θ + 3 π 4 ) , r = f ( θ π 4 ) and r = f ( θ 3 π 4 ) . Repeat this process for g ( θ ) . In general, how do you think the graph of r = f ( θ + α ) compares with the graph of r = f ( θ ) ?
    2. Using your graphing calculator, compare the graph of r = f ( θ ) to each of the graphs of r = 2 f ( θ ) , r = 1 2 f ( θ ) , r = f ( θ ) and r = 3 f ( θ ) . Repeat this process for g ( θ ) . In general, how do you think the graph of r = k f ( θ ) compares with the graph of r = f ( θ ) ? (Does it matter if k > 0 or k < 0 ?)
  16. In light of Exercises -, how would the graph of r = f ( θ ) compare with the graph of r = f ( θ ) for a generic function f ? What about the graphs of r = f ( θ ) and r = f ( θ ) ? What about r = f ( θ ) and r = f ( π θ ) ? Test out your conjectures using a variety of polar functions found in this section with the help of a graphing utility.
  17. With the help of your classmates, research cardioid microphones.
  18. Back in Section, in the paragraph before Exercise, we gave you this link to a fascinating list of curves. Some of these curves have polar representations which we invite you and your classmates to research.

Looking back through the graphs in the section, it's clear that many polar curves enjoy various forms of symmetry. However, classifying symmetry for polar curves is not as straight-forward as it was for equations back on page. In Exercises -, we have you and your classmates explore some of the more basic forms of symmetry seen in common polar curves.

In Section, we discussed transformations of graphs. In Exercise we have you and your classmates explore transformations of polar graphs.

Answers

  1. Circle: r = 6 sin ( θ )

    Coordinate-plane figure.
    Figure 11.185
  2. Circle: r = 2 cos ( θ )

    Coordinate-plane figure.
    Figure 11.186
  3. Rose: r = 2 sin ( 2 θ )

    Coordinate-plane figure.
    Figure 11.187
  4. Rose: r = 4 cos ( 2 θ )

    Coordinate-plane figure.
    Figure 11.188
  5. Rose: r = 5 sin ( 3 θ )

    Coordinate-plane figure.
    Figure 11.189
  6. Rose: r = cos ( 5 θ )

    Coordinate-plane figure.
    Figure 11.190
  7. Rose: r = sin ( 4 θ )

    Coordinate-plane figure.
    Figure 11.191
  8. Rose: r = 3 cos ( 4 θ )

    Coordinate-plane figure.
    Figure 11.192
  9. Cardioid: r = 3 3 cos ( θ )

    Coordinate-plane figure.
    Figure 11.193
  10. Cardioid: r = 5 + 5 sin ( θ )

    Coordinate-plane figure.
    Figure 11.194
  11. Cardioid: r = 2 + 2 cos ( θ )

    Coordinate-plane figure.
    Figure 11.195
  12. Cardioid: r = 1 sin ( θ )

    Coordinate-plane figure.
    Figure 11.196
  13. Limaçon: r = 1 2 cos ( θ )

    Coordinate-plane figure.
    Figure 11.197
  14. Limaçon: r = 1 2 sin ( θ )

    Coordinate-plane figure.
    Figure 11.198
  15. Limaçon: r = 2 3 + 4 cos ( θ )

    Coordinate-plane figure.
    Figure 11.199
  16. Limaçon: r = 3 5 cos ( θ )

    Coordinate-plane figure.
    Figure 11.200
  17. Limaçon: r = 3 5 sin ( θ )

    Coordinate-plane figure.
    Figure 11.201
  18. Limaçon: r = 2 + 7 sin ( θ )

    Coordinate-plane figure.
    Figure 11.202
  19. Lemniscate: r 2 = sin ( 2 θ )

    Coordinate-plane figure.
    Figure 11.203
  20. Lemniscate: r 2 = 4 cos ( 2 θ )

    Coordinate-plane figure.
    Figure 11.204
  21. r = 3 cos ( θ ) and r = 1 + cos ( θ )

    Coordinate-plane figure.
    Figure 11.205

    ( 3 2 , π 3 ) , ( 3 2 , 5 π 3 ) , pole

  22. r = 1 + sin ( θ ) and r = 1 cos ( θ )

    Coordinate-plane figure.
    Figure 11.206

    ( 2 + 2 2 , 3 π 4 ) , ( 2 2 2 , 7 π 4 ) , pole

  23. r = 1 2 sin ( θ ) and r = 2

    Coordinate-plane figure.
    Figure 11.207

    ( 2 , 7 π 6 ) , ( 2 , 11 π 6 )

  24. r = 1 2 cos ( θ ) and r = 1

    Coordinate-plane figure.
    Figure 11.208

    ( 1 , π 2 ) , ( 1 , 3 π 2 ) , ( 1 , 0 )

  25. r = 2 cos ( θ ) and r = 2 3 sin ( θ )

    Coordinate-plane figure.
    Figure 11.209

    ( 3 , π 6 ) , pole

  26. r = 3 cos ( θ ) and r = sin ( θ )

    Coordinate-plane figure.
    Figure 11.210

    ( 3 10 10 , arctan ( 3 ) ) , pole

  27. r 2 = 4 cos ( 2 θ ) and r = 2

    Coordinate-plane figure.
    Figure 11.211

    ( 2 , π 6 ) , ( 2 , 5 π 6 ) , ( 2 , 7 π 6 ) , ( 2 , 11 π 6 )

  28. r 2 = 2 sin ( 2 θ ) and r = 1

    Coordinate-plane figure.
    Figure 11.212

    ( 1 , π 12 ) , ( 1 , 5 π 12 ) , ( 1 , 13 π 12 ) , ( 1 , 17 π 12 )

  29. r = 4 cos ( 2 θ ) and r = 2

    Coordinate-plane figure.
    Figure 11.213

    ( 2 , π 6 ) , ( 2 , 5 π 6 ) , ( 2 , 7 π 6 ) ,

    ( 2 , 11 π 6 ) , ( 2 , π 3 ) , ( 2 , 2 π 3 ) ,

    ( 2 , 4 π 3 ) , ( 2 , 5 π 3 )

  30. r = 2 sin ( 2 θ ) and r = 1

    Coordinate-plane figure.
    Figure 11.214

    ( 1 , π 12 ) , ( 1 , 5 π 12 ) , ( 1 , 13 π 12 ) ,

    ( 1 , 17 π 12 ) , ( 1 , 7 π 12 ) , ( 1 , 11 π 12 ) ,

    ( 1 , 19 π 12 ) , ( 1 , 23 π 12 )

  31. { ( r , θ ) |  0 r 3 ,  0 θ 2 π }

    Coordinate-plane figure.
    Figure 11.215
  32. { ( r , θ ) |  0 r 4 sin ( θ ) ,  0 θ π }

    Coordinate-plane figure.
    Figure 11.216
  33. { ( r , θ ) |  0 r 3 cos ( θ ) , π 2 θ π 2 }

    Coordinate-plane figure.
    Figure 11.217
  34. { ( r , θ ) |  0 r 2 sin ( 2 θ ) ,  0 θ π 2 }

    Coordinate-plane figure.
    Figure 11.218
  35. { ( r , θ ) |  0 r 4 cos ( 2 θ ) , π 4 θ π 4 }

    Coordinate-plane figure.
    Figure 11.219
  36. { ( r , θ ) |  1 r 1 2 cos ( θ ) , π 2 θ 3 π 2 }

    Coordinate-plane figure.
    Figure 11.220
  37. { ( r , θ ) |  1 + cos ( θ ) r 3 cos ( θ ) , π 3 θ π 3 }

    Coordinate-plane figure.
    Figure 11.221
  38. { ( r , θ ) |  1 r 2 sin ( 2 θ ) , 13 π 12 θ 17 π 12 }

    Coordinate-plane figure.
    Figure 11.222
  39. { ( r , θ ) |  0 r 2 3 sin ( θ ) ,  0 θ π 6 } { ( r , θ ) |  0 r 2 cos ( θ ) , π 6 θ π 2 }

    Coordinate-plane figure.
    Figure 11.223
  40. { ( r , θ ) |  0 r 2 sin ( 2 θ ) ,  0 θ π 12 } { ( r , θ ) |  0 r 1 , π 12 θ π 4 }

    Coordinate-plane figure.
    Figure 11.224
  41. { ( r , θ ) |  0 r 5 ,  0 θ 2 π }
  42. { ( r , θ ) |  0 r 5 , π θ 3 π 2 }
  43. { ( r , θ ) |  0 r 6 sin ( θ ) , π 2 θ π }
  44. { ( r , θ ) |  4 cos ( θ ) r 0 , π 2 θ π }
  45. { ( r , θ ) |  0 r 3 3 cos ( θ ) ,  0 θ π }
  46. { ( r , θ ) |  0 r 2 2 sin ( θ ) ,  0 θ π 2 } { ( r , θ ) |  0 r 2 2 sin ( θ ) , 3 π 2 θ 2 π }

    or { ( r , θ ) |  0 r 2 2 sin ( θ ) , 3 π 2 θ 5 π 2 }

  47. { ( r , θ ) |  0 r 3 cos ( 4 θ ) ,  0 θ π 8 } { ( r , θ ) |  0 r 3 cos ( 4 θ ) , 15 π 8 θ 2 π }

    or { ( r , θ ) |  0 r 3 cos ( 4 θ ) , π 8 θ π 8 }

  48. { ( r , θ ) |  3 r 5 ,  0 θ 2 π }
  49. { ( r , θ ) |  0 r 3 cos ( θ ) , π 2 θ 0 } { ( r , θ ) | sin ( θ ) r 3 cos ( θ ) ,  0 θ arctan ( 3 ) }
  50. { ( r , θ ) |  0 r 6 sin ( 2 θ ) ,  0 θ π 12 } { ( r , θ ) |  0 r 3 , π 12 θ 5 π 12 } { ( r , θ ) |  0 r 6 sin ( 2 θ ) , 5 π 12 θ π 2 }

Adapted from Precalculus, 3rd corrected edition, by Carl Stitz and Jeff Zeager (stitz-zeager.com), licensed under CC BY-NC-SA 3.0. Changes were made: reformatted as an accessible XYZ web edition. License: CC-BY-NC-SA-3.0.