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Polar Coordinates & Graphs
Polar Coordinates & Graphs
Besides the rectangular coordinates, we may track
the location of a point P in the plane by its polar
coordinates (r, ),
P
x
y
(r, )p
Polar Coordinates & Graphs
Besides the rectangular coordinates, we may track
the location of a point P in the plane by its polar
coordinates (r, ), where r is the signed distance from
the origin (0, 0) to P,
P
x
y
(r, )p
r
Polar Coordinates & Graphs
P
x
y

O
Besides the rectangular coordinates, we may track
the location of a point P in the plane by its polar
coordinates (r, ), where r is the signed distance from
the origin (0, 0) to P, and  is an angle measured from
the positive x–axis which gives the direction to P.
(r, )p
r
Polar Coordinates & Graphs
Conversion Rules
Let (x, y)R and (r, )P be the
rectangular and the polar
coordinates of P,
P
x
y

O
Besides the rectangular coordinates, we may track
the location of a point P in the plane by its polar
coordinates (r, ), where r is the signed distance from
the origin (0, 0) to P, and  is an angle measured from
the positive x–axis which gives the direction to P.
(r, )p = (x, y)R
r
Polar Coordinates & Graphs
Conversion Rules
Let (x, y)R and (r, )P be the
rectangular and the polar
coordinates of P, then
x = r*cos()
P
x
y

O
x = r*cos()
The rectangular and polar conversions
Besides the rectangular coordinates, we may track
the location of a point P in the plane by its polar
coordinates (r, ), where r is the signed distance from
the origin (0, 0) to P, and  is an angle measured from
the positive x–axis which gives the direction to P.
(r, )p = (x, y)R
r
Polar Coordinates & Graphs
Conversion Rules
Let (x, y)R and (r, )P be the
rectangular and the polar
coordinates of P, then
x = r*cos()
y = r*sin()
P
x
y

O
x = r*cos()
y = r*sin()
The rectangular and polar conversions
r
(r, )p = (x, y)R
Besides the rectangular coordinates, we may track
the location of a point P in the plane by its polar
coordinates (r, ), where r is the signed distance from
the origin (0, 0) to P, and  is an angle measured from
the positive x–axis which gives the direction to P.
Polar Coordinates & Graphs
Conversion Rules
Let (x, y)R and (r, )P be the
rectangular and the polar
coordinates of P, then
x = r*cos()
y = r*sin()
r = √x2 + y2
tan() = y/x
P
x
y

O
x = r*cos()
y = r*sin()
The rectangular and polar conversions
r = √x2 + y2
(r, )p = (x, y)R
Besides the rectangular coordinates, we may track
the location of a point P in the plane by its polar
coordinates (r, ), where r is the signed distance from
the origin (0, 0) to P, and  is an angle measured from
the positive x–axis which gives the direction to P.
Polar Coordinates & Graphs
Conversion Rules
Let (x, y)R and (r, )P be the
rectangular and the polar
coordinates of P, then
P
x
y

O
x = r*cos()
y = r*sin()
The rectangular and polar conversions
x = r*cos()
y = r*sin()
r = √x2 + y2
tan() = y/x
r = √x2 + y2
If P is in quadrants I, II or IV
then  may be extracted
by inverse trig functions. But if P is in quadrant III, then
 can’t be calculated directly by inverse trig-functions.
(r, )p = (x, y)R
Besides the rectangular coordinates, we may track
the location of a point P in the plane by its polar
coordinates (r, ), where r is the signed distance from
the origin (0, 0) to P, and  is an angle measured from
the positive x–axis which gives the direction to P.
Polar Equations
Polar Coordinates & Graphs
Polar Equations
A rectangular equation in x and y gives the relation
between the horizontal displacement x and vertical
displacement y of locations.
Polar Coordinates & Graphs
Polar Equations
A rectangular equation in x and y gives the relation
between the horizontal displacement x and vertical
displacement y of locations. A polar equation gives a
relation of the distance r the direction .
Polar Coordinates & Graphs
Polar Equations
A rectangular equation in x and y gives the relation
between the horizontal displacement x and vertical
displacement y of locations. A polar equation gives a
relation of the distance r the direction .
Polar Coordinates & Graphs
The rectangular equation y = x
specifies that the horizontal
displacement x must be the same
as the vertical displacement y for
our points P.
Polar Equations
A rectangular equation in x and y gives the relation
between the horizontal displacement x and vertical
displacement y of locations. A polar equation gives a
relation of the distance r the direction .
Polar Coordinates & Graphs
The rectangular equation y = x
specifies that the horizontal
displacement x must be the same
as the vertical displacement y for
our points P.
y
y
x
x
P(x, y)
The graph of y = x in the
the rectangular system
Polar Equations
A rectangular equation in x and y gives the relation
between the horizontal displacement x and vertical
displacement y of locations. A polar equation gives a
relation of the distance r the direction .
Polar Coordinates & Graphs
The rectangular equation y = x
specifies that the horizontal
displacement x must be the same
as the vertical displacement y for
our points P.
y
y
x
x
P(x, y)
The graph of y = x in the
the rectangular system
The polar equation r =  says that
the distance r must be the same as
the rotational measurement  for P.
Its graph is the Archimedean spiral.
Polar Equations
A rectangular equation in x and y gives the relation
between the horizontal displacement x and vertical
displacement y of locations. A polar equation gives a
relation of the distance r the direction .
Polar Coordinates & Graphs
The rectangular equation y = x
specifies that the horizontal
displacement x must be the same
as the vertical displacement y for
our points P.
y
y
x
x
P(x, y)
x
P(r, )

r
The graph of y = x in the
the rectangular system
Graph of r =  in the
polar system.
The polar equation r =  says that
the distance r must be the same as
the rotational measurement  for P.
Its graph is the Archimedean spiral.
Let’s look at some basic examples of polar graphs.
Polar Coordinates & Graphs
The Constant Equations r = c &  = c
Let’s look at some basic examples of polar graphs.
Polar Coordinates & Graphs
The Constant Equations r = c &  = c
Example A. Graph the following polar
equations.
a. (r = c)
b. ( = c)
Let’s look at some basic examples of polar graphs.
Polar Coordinates & Graphs
The Constant Equations r = c &  = c
Example A. Graph the following polar
equations.
a. (r = c) The constant equation r = c
indicates that “the distance r is c, a
fixed constant” and that  may be of
any value.
b. ( = c)
Let’s look at some basic examples of polar graphs.
Polar Coordinates & Graphs
The Constant Equations r = c &  = c
Example A. Graph the following polar
equations.
a. (r = c) The constant equation r = c
indicates that “the distance r is c, a
fixed constant” and that  may be of
any value. This equation describes the
circle of radius c, centered at (0,0).
b. ( = c)
Let’s look at some basic examples of polar graphs.
Polar Coordinates & Graphs
The Constant Equations r = c &  = c
Example A. Graph the following polar
equations.
a. (r = c) The constant equation r = c
indicates that “the distance r is c, a
fixed constant” and that  may be of
any value. This equation describes the
circle of radius c, centered at (0,0).
x
y
c
The constant
equation r = c
b. ( = c)
Let’s look at some basic examples of polar graphs.
Polar Coordinates & Graphs
The Constant Equations r = c &  = c
Example A. Graph the following polar
equations.
a. (r = c) The constant equation r = c
indicates that “the distance r is c, a
fixed constant” and that  may be of
any value. This equation describes the
circle of radius c, centered at (0,0).
x
y
c
The constant
equation r = c
b. ( = c) The constant equation  = c
requires that “the directional angle  is c,
a fixed constant” and the distance r may
be of any value.
Let’s look at some basic examples of polar graphs.
Polar Coordinates & Graphs
The Constant Equations r = c &  = c
Example A. Graph the following polar
equations.
a. (r = c) The constant equation r = c
indicates that “the distance r is c, a
fixed constant” and that  may be of
any value. This equation describes the
circle of radius c, centered at (0,0).
x
y
c
The constant
equation r = c
b. ( = c) The constant equation  = c
requires that “the directional angle  is c,
a fixed constant” and the distance r may
be of any value. This equation describes
the line with polar angle c.
Let’s look at some basic examples of polar graphs.
Polar Coordinates & Graphs
The Constant Equations r = c &  = c
Example A. Graph the following polar
equations.
a. (r = c) The constant equation r = c
indicates that “the distance r is c, a
fixed constant” and that  may be of
any value. This equation describes the
circle of radius c, centered at (0,0).
x
y
c
The constant
equation r = c
b. ( = c) The constant equation  = c
requires that “the directional angle  is c,
a fixed constant” and the distance r may
be of any value. This equation describes
the line with polar angle c.
x
y
The constant
equation  = c
 = c
Polar Coordinates & Graphs
For the graphs of other polar equations we need to plot
points accordingly.
Polar Coordinates & Graphs
For the graphs of other polar equations we need to plot
points accordingly. For this we will use the polar graph
paper such as the one shown here which is gridded in
terms of the distances and directional angles.
Polar Coordinates & Graphs
For the graphs of other polar equations we need to plot
points accordingly. For this we will use the polar graph
paper such as the one shown here which is gridded in
terms of the distances and directional angles.
Example B. a. Graph r = 3cos().
Polar Coordinates & Graphs
For the graphs of other polar equations we need to plot
points accordingly. For this we will use the polar graph
paper such as the one shown here which is gridded in
terms of the distances and directional angles.
Example B. a. Graph r = 3cos(). r 
3 0o
3(3/2) ≈ 2.6 30o
3(2/2) ≈ 2.1 45o
1.5 60o
0 90o
Let’s plot the
points starting
with  going
from 0 to 90o.
Polar Coordinates & Graphs
For the graphs of other polar equations we need to plot
points accordingly. For this we will use the polar graph
paper such as the one shown here which is gridded in
terms of the distances and directional angles.
Example B. a. Graph r = 3cos(). r 
3 0o
3(3/2) ≈ 2.6 30o
3(2/2) ≈ 2.1 45o
1.5 60o
0 90o
Let’s plot the
points starting
with  going
from 0 to 90o.
Polar Coordinates & Graphs
For the graphs of other polar equations we need to plot
points accordingly. For this we will use the polar graph
paper such as the one shown here which is gridded in
terms of the distances and directional angles.
Example B. a. Graph r = 3cos(). r 
3 0o
3(3/2) ≈ 2.6 30o
3(2/2) ≈ 2.1 45o
1.5 60o
0 90o
Let’s plot the
points starting
with  going
from 0 to 90o.
Polar Coordinates & Graphs
For the graphs of other polar equations we need to plot
points accordingly. For this we will use the polar graph
paper such as the one shown here which is gridded in
terms of the distances and directional angles.
Example B. a. Graph r = 3cos(). r 
3 0o
3(3/2) ≈ 2.6 30o
3(2/2) ≈ 2.1 45o
1.5 60o
0 90o
Let’s plot the
points starting
with  going
from 0 to 90o.
Polar Coordinates & Graphs
For the graphs of other polar equations we need to plot
points accordingly. For this we will use the polar graph
paper such as the one shown here which is gridded in
terms of the distances and directional angles.
Example B. a. Graph r = 3cos(). r 
3 0o
3(3/2) ≈ 2.6 30o
3(2/2) ≈ 2.1 45o
1.5 60o
0 90o
Let’s plot the
points starting
with  going
from 0 to 90o.
Polar Coordinates & Graphs
For the graphs of other polar equations we need to plot
points accordingly. For this we will use the polar graph
paper such as the one shown here which is gridded in
terms of the distances and directional angles.
Example B. a. Graph r = 3cos(). r 
3 0o
3(3/2) ≈ 2.6 30o
3(2/2) ≈ 2.1 45o
1.5 60o
0 90o
Let’s plot the
points starting
with  going
from 0 to 90o. 3
Polar Coordinates & Graphs
For the graphs of other polar equations we need to plot
points accordingly. For this we will use the polar graph
paper such as the one shown here which is gridded in
terms of the distances and directional angles.
Example B. a. Graph r = 3cos(). r 
3 0o
3(3/2) ≈ 2.6 30o
3(2/2) ≈ 2.1 45o
1.5 60o
0 90o
Let’s plot the
points starting
with  going
from 0 to 90o. 3
Polar Coordinates & Graphs
For the graphs of other polar equations we need to plot
points accordingly. For this we will use the polar graph
paper such as the one shown here which is gridded in
terms of the distances and directional angles.
Example B. a. Graph r = 3cos(). r 
3 0o
3(3/2) ≈ 2.6 30o
3(2/2) ≈ 2.1 45o
1.5 60o
0 90o
Let’s plot the
points starting
with  going
from 0 to 90o. 3
Polar Coordinates & Graphs
For the graphs of other polar equations we need to plot
points accordingly. For this we will use the polar graph
paper such as the one shown here which is gridded in
terms of the distances and directional angles.
Example B. a. Graph r = 3cos(). r 
3 0o
3(3/2) ≈ 2.6 30o
3(2/2) ≈ 2.1 45o
1.5 60o
0 90o
Let’s plot the
points starting
with  going
from 0 to 90o. 3
Polar Coordinates & Graphs
For the graphs of other polar equations we need to plot
points accordingly. For this we will use the polar graph
paper such as the one shown here which is gridded in
terms of the distances and directional angles.
Example B. a. Graph r = 3cos(). r 
3 0o
3(3/2) ≈ 2.6 30o
3(2/2) ≈ 2.1 45o
1.5 60o
0 90o
Let’s plot the
points starting
with  going
from 0 to 90o. 3
Polar Coordinates & Graphs
For the graphs of other polar equations we need to plot
points accordingly. For this we will use the polar graph
paper such as the one shown here which is gridded in
terms of the distances and directional angles.
Example B. a. Graph r = 3cos(). r 
3 0o
3(3/2) ≈ 2.6 30o
3(2/2) ≈ 2.1 45o
1.5 60o
0 90o
–1.5 120o
≈ –2.1 135o
≈ –2.6 150o
–3 180o
Let’s plot the
points starting
with  going
from 0 to 90o. 3
Next continue
with  from
90o to 180o as
shown in the table.
Polar Coordinates & Graphs
For the graphs of other polar equations we need to plot
points accordingly. For this we will use the polar graph
paper such as the one shown here which is gridded in
terms of the distances and directional angles.
Example B. a. Graph r = 3cos(). r 
3 0o
3(3/2) ≈ 2.6 30o
3(2/2) ≈ 2.1 45o
1.5 60o
0 90o
–1.5 120o
≈ –2.1 135o
≈ –2.6 150o
–3 180o
Let’s plot the
points starting
with  going
from 0 to 90o. 3
Next continue
with  from
90o to 180o as
shown in the table.
Polar Coordinates & Graphs
For the graphs of other polar equations we need to plot
points accordingly. For this we will use the polar graph
paper such as the one shown here which is gridded in
terms of the distances and directional angles.
Example B. a. Graph r = 3cos(). r 
3 0o
3(3/2) ≈ 2.6 30o
3(2/2) ≈ 2.1 45o
1.5 60o
0 90o
–1.5 120o
≈ –2.1 135o
≈ –2.6 150o
–3 180o
Let’s plot the
points starting
with  going
from 0 to 90o. 3
Next continue
with  from
90o to 180o as
shown in the table.
negative so the points are in the 4th quadrant.
Note the r’s are
Polar Coordinates & Graphs
For the graphs of other polar equations we need to plot
points accordingly. For this we will use the polar graph
paper such as the one shown here which is gridded in
terms of the distances and directional angles.
Example B. a. Graph r = 3cos(). r 
3 0o
3(3/2) ≈ 2.6 30o
3(2/2) ≈ 2.1 45o
1.5 60o
0 90o
–1.5 120o
≈ –2.1 135o
≈ –2.6 150o
–3 180o
Let’s plot the
points starting
with  going
from 0 to 90o. 3
Next continue
with  from
90o to 180o as
shown in the table.
negative so the points are in the 4th quadrant.
Note the r’s are
Polar Coordinates & Graphs
Continuing with  from 180o to 270o, r 
–3 180o
≈ –2.6 210o
≈ –2.1 225o
–1.5 240o
0 270o
1.5 300o
≈ 2.1 315o
≈ 2.6 330o
3 360o
again r’s are
negative, hence
the points are
located in the
1st quadrant.
Polar Coordinates & Graphs
Continuing with  from 180o to 270o, r 
–3 180o
≈ –2.6 210o
≈ –2.1 225o
–1.5 240o
0 270o
1.5 300o
≈ 2.1 315o
≈ 2.6 330o
3 360o
again r’s are
negative, hence
the points are
located in the
1st quadrant.
In fact, they
trace over the
same points as  goes from 0o to 90o
Polar Coordinates & Graphs
Continuing with  from 180o to 270o, r 
–3 180o
≈ –2.6 210o
≈ –2.1 225o
–1.5 240o
0 270o
1.5 300o
≈ 2.1 315o
≈ 2.6 330o
3 360o
again r’s are
negative, hence
the points are
located in the
1st quadrant.
3
In fact, they
trace over the
same points as  goes from 0o to 90o
Polar Coordinates & Graphs
Continuing with  from 180o to 270o, r 
–3 180o
≈ –2.6 210o
≈ –2.1 225o
–1.5 240o
0 270o
1.5 300o
≈ 2.1 315o
≈ 2.6 330o
3 360o
again r’s are
negative, hence
the points are
located in the
1st quadrant.
3
In fact, they
trace over the
Finally as  goes from 270o to 360o we trace over the
same points as  goes from 90o to 180o in the 4th
quadrant.
same points as  goes from 0o to 90o
Polar Coordinates & Graphs
Continuing with  from 180o to 270o, r 
–3 180o
≈ –2.6 210o
≈ –2.1 225o
–1.5 240o
0 270o
1.5 300o
≈ 2.1 315o
≈ 2.6 330o
3 360o
again r’s are
negative, hence
the points are
located in the
1st quadrant.
3
In fact, they
trace over the
Finally as  goes from 270o to 360o we trace over the
same points as  goes from 90o to 180o in the 4th
quadrant. As we will see shortly, these points form a
circle and for every period of 180o the graph of
r = cos() traverses this circle once.
same points as  goes from 0o to 90o
Polar Coordinates & Graphs
b. Convert r = 3cos() to a
rectangular equation. Verify it’s
a circle and find the center and
radius of this circle.
3
Polar Coordinates & Graphs
b. Convert r = 3cos() to a
rectangular equation. Verify it’s
a circle and find the center and
radius of this circle.
Multiply both sides by r so we
have r2 = 3r*cos(). 3
Polar Coordinates & Graphs
b. Convert r = 3cos() to a
rectangular equation. Verify it’s
a circle and find the center and
radius of this circle.
Multiply both sides by r so we
have r2 = 3r*cos().
In terms of x and y, it’s
x2 + y2 = 3x
3
Polar Coordinates & Graphs
b. Convert r = 3cos() to a
rectangular equation. Verify it’s
a circle and find the center and
radius of this circle.
Multiply both sides by r so we
have r2 = 3r*cos().
In terms of x and y, it’s
x2 + y2 = 3x
x2 – 3x + y2 = 0
3
Polar Coordinates & Graphs
b. Convert r = 3cos() to a
rectangular equation. Verify it’s
a circle and find the center and
radius of this circle.
Multiply both sides by r so we
have r2 = 3r*cos().
In terms of x and y, it’s
x2 + y2 = 3x
x2 – 3x + y2 = 0
completing the square,
x2 – 3x + (3/2)2 + y2 = 0 + (3/2)2
3
Polar Coordinates & Graphs
b. Convert r = 3cos() to a
rectangular equation. Verify it’s
a circle and find the center and
radius of this circle.
Multiply both sides by r so we
have r2 = 3r*cos().
In terms of x and y, it’s
x2 + y2 = 3x
x2 – 3x + y2 = 0
completing the square,
x2 – 3x + (3/2)2 + y2 = 0 + (3/2)2
(x – 3/2)2 + y2 = (3/2)2
3
3
Polar Coordinates & Graphs
b. Convert r = 3cos() to a
rectangular equation. Verify it’s
a circle and find the center and
radius of this circle.
Multiply both sides by r so we
have r2 = 3r*cos().
In terms of x and y, it’s
x2 + y2 = 3x
x2 – 3x + y2 = 0
completing the square,
x2 – 3x + (3/2)2 + y2 = 0 + (3/2)2
(x – 3/2)2 + y2 = (3/2)2
so the points form the circle centered at (3/2, 0)
with radius 3/2.
Polar Coordinates & Graphs
In general, the polar
equations of the form
r = ±D*cos()
r = ±D*sin()
are circles with diameter D
and tangent to the x or y axis
at the origin. r = ±a*cos()
r = ±a*sin()
D x
y
Polar Coordinates & Graphs
In general, the polar
equations of the form
r = ±D*cos()
r = ±D*sin()
are circles with diameter D
and tangent to the x or y axis
at the origin. r = ±a*cos()
r = ±a*sin()
D x
y
The points (r, ) and (r, –) are the
vertical mirror images of each other
across the x–axis.
x
(r, )
(r, –)
1
Polar Coordinates & Graphs
In general, the polar
equations of the form
r = ±D*cos()
r = ±D*sin()
are circles with diameter D
and tangent to the x or y axis
at the origin. r = ±a*cos()
r = ±a*sin()
D x
y
The points (r, ) and (r, –) are the
vertical mirror images of each other
across the x–axis. So if r = f() = f(–)
such as r = cos() = cos(–),
then its graph is symmetric with
respect to the x–axis,
x
(r, )
(r, –)
1
Polar Coordinates & Graphs
In general, the polar
equations of the form
r = ±D*cos()
r = ±D*sin()
are circles with diameter D
and tangent to the x or y axis
at the origin. r = ±a*cos()
r = ±a*sin()
D x
y
The points (r, ) and (r, –) are the
vertical mirror images of each other
across the x–axis. So if r = f() = f(–)
such as r = cos() = cos(–),
then its graph is symmetric with
respect to the x–axis,
x
(r, )
(r, –)
r = cos() = cos(–)
1
Polar Coordinates & Graphs
In general, the polar
equations of the form
r = ±D*cos()
r = ±D*sin()
are circles with diameter D
and tangent to the x or y axis
at the origin. r = ±a*cos()
r = ±a*sin()
D x
y
The points (r, ) and (r, –) are the
vertical mirror images of each other
across the x–axis. So if r = f() = f(–)
such as r = cos() = cos(–),
then its graph is symmetric with
respect to the x–axis, so r = ±D*cos()
are the horizontal circles.
x
(r, )
(r, –)
r = cos() = cos(–)
1
Polar Coordinates & Graphs
x
(r, )
(–r, –)
y
The points (r, ) and (–r, –) are the
mirror images of each other across
the y–axis.
Polar Coordinates & Graphs
x
(r, )
r = sin() = –sin(–)
(–r, –)
y
The points (r, ) and (–r, –) are the
mirror images of each other across
the y–axis. So if r = f(–) = –f()
such as r = sin() = –sin(–),
then its graph is symmetric to the
y–axis and so r = ±D*sin()
are the two vertical circles.
Polar Coordinates & Graphs
x
(r, )
r = sin() = –sin(–)
(–r, –)
y
x
y
r = cos()
r = –cos()
r = sin()
r = –sin()
1
1
Here they are with their orientation
starting at  = 0.
The points (r, ) and (–r, –) are the
mirror images of each other across
the y–axis. So if r = f(–) = –f()
such as r = sin() = –sin(–),
then its graph is symmetric to the
y–axis and so r = ±D*sin()
are the two vertical circles.
Polar Coordinates & Graphs
The Cardioids
r = c(1 ± cos())
r = c(1 ± sin())
The graphs of the equations of the form
are called the cardioids, or the heart shaped curves.
Example C. Graph r = 1 – cos().
The graph of r = 1 – cos() is symmetric with respect
to the x–axis because cos() = cos(–). Therefore we
will plot  from 0o to 180o and take its mirrored image
across the x–axis for the complete graph. As  goes
from 0o to 180o, cos() goes from 1 to –1, and the
expression 1 – cos() goes from 0 to 2. The table is
shown below, readers may verify the approximate
values of r’s.
Polar Coordinates & Graphs
The Cardioids
r = c(1 ± cos())
r = c(1 ± sin())
The graphs of the equations of the form
are called the cardioids, or the heart shaped curves.
Example C. Graph r = 1 – cos().
Polar Coordinates & Graphs
The Cardioids
r = c(1 ± cos())
r = c(1 ± sin())
The graphs of the equations of the form
are called the cardioids, or the heart shaped curves.
Example C. Graph r = 1 – cos().
The graph of r = 1 – cos() is symmetric with respect
to the x–axis because cos() = cos(–).
Polar Coordinates & Graphs
The Cardioids
r = c(1 ± cos())
r = c(1 ± sin())
The graphs of the equations of the form
are called the cardioids, or the heart shaped curves.
Example C. Graph r = 1 – cos().
The graph of r = 1 – cos() is symmetric with respect
to the x–axis because cos() = cos(–). Therefore we
will plot  from 0o to 180o and take its mirrored image
across the x–axis for the complete graph.
Polar Coordinates & Graphs
The Cardioids
r = c(1 ± cos())
r = c(1 ± sin())
The graphs of the equations of the form
are called the cardioids, or the heart shaped curves.
Example C. Graph r = 1 – cos().
The graph of r = 1 – cos() is symmetric with respect
to the x–axis because cos() = cos(–). Therefore we
will plot  from 0o to 180o and take its mirrored image
across the x–axis for the complete graph. As  goes
from 0o to 180o, cos() goes from 1 to –1, and the
expression 1 – cos() goes from 0 to 2.
Polar Coordinates & Graphs
The Cardioids
r = c(1 ± cos())
r = c(1 ± sin())
The graphs of the equations of the form
are called the cardioids, or the heart shaped curves.
Example C. Graph r = 1 – cos().
The graph of r = 1 – cos() is symmetric with respect
to the x–axis because cos() = cos(–). Therefore we
will plot  from 0o to 180o and take its mirrored image
across the x–axis for the complete graph. As  goes
from 0o to 180o, cos() goes from 1 to –1, and the
expression 1 – cos() goes from 0 to 2. The table is
shown below, readers may verify the approximate
values of r’s.
r=1–cos() 
0 0o
≈ 0.13 30o
≈ 0.29 45o
0.5 60o
1 90o
1.5 120o
≈ 1.71 135o
≈ 1.87 150o
2 180o
Polar Coordinates & Graphs
x
2
r=1–cos() 
0 0o
≈ 0.13 30o
≈ 0.29 45o
0.5 60o
1 90o
1.5 120o
≈ 1.71 135o
≈ 1.87 150o
2 180o
Polar Coordinates & Graphs
x
2
r=1–cos() 
0 0o
≈ 0.13 30o
≈ 0.29 45o
0.5 60o
1 90o
1.5 120o
≈ 1.71 135o
≈ 1.87 150o
2 180o
Polar Coordinates & Graphs
x
2
Polar Coordinates & Graphs
r=1–cos() 
0 0o
≈ 0.13 30o
≈ 0.29 45o
0.5 60o
1 90o
1.5 120o
≈ 1.71 135o
≈ 1.87 150o
2 180o
x
2
Polar Coordinates & Graphs
r=1–cos() 
0 0o
≈ 0.13 30o
≈ 0.29 45o
0.5 60o
1 90o
1.5 120o
≈ 1.71 135o
≈ 1.87 150o
2 180o
Reflecting across the x–axis, we have the cardioid.
x
2
Polar Coordinates & Graphs
r=1–cos() 
0 0o
≈ 0.13 30o
≈ 0.29 45o
0.5 60o
1 90o
1.5 120o
≈ 1.71 135o
≈ 1.87 150o
2 180o
x
2
Reflecting across the x–axis, we have the cardioid.
Polar Coordinates & Graphs
The cardioid is the
track of a point on
a circle as it
r=1–cos() 
0 0o
≈ 0.13 30o
≈ 0.29 45o
0.5 60o
1 90o
1.5 120o
≈ 1.71 135o
≈ 1.87 150o
2 180o
x
2
Reflecting across the x–axis, we have the cardioid.
revolves around another circle of the same size.
Polar Coordinates & Graphs
The cardioid is the
track of a point on
a circle as it
r=1–cos() 
0 0o
≈ 0.13 30o
≈ 0.29 45o
0.5 60o
1 90o
1.5 120o
≈ 1.71 135o
≈ 1.87 150o
2 180o
x
2
Reflecting across the x–axis, we have the cardioid.
revolves around another circle of the same size.
Polar Coordinates & Graphs
The cardioid is the
track of a point on
a circle as it
r=1–cos() 
0 0o
≈ 0.13 30o
≈ 0.29 45o
0.5 60o
1 90o
1.5 120o
≈ 1.71 135o
≈ 1.87 150o
2 180o
x
2
Reflecting across the x–axis, we have the cardioid.
revolves around another circle of the same size.
Polar Coordinates & Graphs
The cardioid is the
track of a point on
a circle as it
r=1–cos() 
0 0o
≈ 0.13 30o
≈ 0.29 45o
0.5 60o
1 90o
1.5 120o
≈ 1.71 135o
≈ 1.87 150o
2 180o
x
2
Reflecting across the x–axis, we have the cardioid.
revolves around another circle of the same size.
Polar Coordinates & Graphs
The cardioid is the
track of a point on
a circle as it
r=1–cos() 
0 0o
≈ 0.13 30o
≈ 0.29 45o
0.5 60o
1 90o
1.5 120o
≈ 1.71 135o
≈ 1.87 150o
2 180o
x
2
Reflecting across the x–axis, we have the cardioid.
revolves around another circle of the same size.
Polar Coordinates & Graphs
A cardioid is also the outline or the
envelope of a series of circles that
pass through some fixed point o
Polar Coordinates & Graphs
o
A cardioid is also the outline or the
envelope of a series of circles that
pass through some fixed point o
Polar Coordinates & Graphs
o
A cardioid is also the outline or the
envelope of a series of circles that
pass through some fixed point o
whose centers sit on another
circle K that contains o,
Polar Coordinates & Graphs
o
A cardioid is also the outline or the
envelope of a series of circles that
pass through some fixed point o
whose centers sit on another
circle K that contains o,
as shown.
K
Polar Coordinates & Graphs
o
A cardioid is also the outline or the
envelope of a series of circles that
pass through some fixed point o
whose centers sit on another
circle K that contains o,
as shown.
K
Polar Coordinates & Graphs
o
A cardioid is also the outline or the
envelope of a series of circles that
pass through some fixed point o
whose centers sit on another
circle K that contains o,
as shown.
K
Polar Coordinates & Graphs
o
A cardioid is also the outline or the
envelope of a series of circles that
pass through some fixed point o
whose centers sit on another
circle K that contains o,
as shown.
K
Polar Coordinates & Graphs
o
A cardioid is also the outline or the
envelope of a series of circles that
pass through some fixed point o
whose centers sit on another
circle K that contains o,
as shown.
K
Polar Coordinates & Graphs
o
A cardioid is also the outline or the
envelope of a series of circles that
pass through some fixed point o
whose centers sit on another
circle K that contains o,
as shown.
K
Polar Coordinates & Graphs
o
A cardioid is also the outline or the
envelope of a series of circles that
pass through some fixed point o
whose centers sit on another
circle K that contains o,
as shown.
K
Polar Coordinates & Graphs
o
cases of polar equations of the form
r = a ± b*cos() and r = a ± b*sin().
K
A cardioid is also the outline or the
envelope of a series of circles that
pass through some fixed point o
whose centers sit on another
circle K that contains o,
as shown. Cardioids are special
Polar Coordinates & Graphs
o
cases of polar equations of the form
r = a ± b*cos() and r = a ± b*sin().
K
A cardioid is also the outline or the
envelope of a series of circles that
pass through some fixed point o
whose centers sit on another
circle K that contains o,
as shown. Cardioids are special
We summarize the graphs of these equations below.
Polar Coordinates & Graphs
o
cases of polar equations of the form
r = a ± b*cos() and r = a ± b*sin().
K
A cardioid is also the outline or the
envelope of a series of circles that
pass through some fixed point o
whose centers sit on another
circle K that contains o,
as shown. Cardioids are special
We summarize the graphs of these equations below.
The graphs of r = a ± b*sin() are rotations of the
graphs of r = a ± b*cos() = a(1 ± k*cos())
where k is a constant.
Polar Coordinates & Graphs
o
cases of polar equations of the form
r = a ± b*cos() and r = a ± b*sin().
K
A cardioid is also the outline or the
envelope of a series of circles that
pass through some fixed point o
whose centers sit on another
circle K that contains o,
as shown. Cardioids are special
We summarize the graphs of these equations below.
The graphs of r = a ± b*sin() are rotations of the
graphs of r = a ± b*cos() = a(1 ± k*cos())
where k is a constant. Regarding the “a” as a scalar,
we reduce to examining the graphs of the polar
equations of the form r = 1 ± k*cos().
Polar Coordinates & Graphs
The graph of a polar equation of the form
r = 1 ± k*cos() depends on the value of |k|.
Polar Coordinates & Graphs
The graph of a polar equation of the form
r = 1 ± k*cos() depends on the value of |k|.
We may classify the graphs r = 1 – k*cos() where k is
a positive number into three types.
Polar Coordinates & Graphs
The graph of a polar equation of the form
r = 1 ± k*cos() depends on the value of |k|.
We may classify the graphs r = 1 – k*cos() where k is
a positive number into three types.
For k = 1, or r = 1 – cos(),
we get a cardioid.
r = 1 – cos()
k = 1
Polar Coordinates & Graphs
The graph of a polar equation of the form
r = 1 ± k*cos() depends on the value of |k|.
We may classify the graphs r = 1 – k*cos() where k is
a positive number into three types.
For k = 1, or r = 1 – cos(),
we get a cardioid.
For k < 1, e.g. r = 1 – ½ *cos(),
we have r > 0 for all ’s.
r = 1 – cos()
k = 1
Polar Coordinates & Graphs
The graph of a polar equation of the form
r = 1 ± k*cos() depends on the value of |k|.
We may classify the graphs r = 1 – k*cos() where k is
a positive number into three types.
For k = 1, or r = 1 – cos(),
we get a cardioid.
For k < 1, e.g. r = 1 – ½ *cos(),
we have r > 0 for all ’s.
This means the graph does not
pass through the origin.
r = 1 – cos()
k = 1
Polar Coordinates & Graphs
The graph of a polar equation of the form
r = 1 ± k*cos() depends on the value of |k|.
We may classify the graphs r = 1 – k*cos() where k is
a positive number into three types.
For k = 1, or r = 1 – cos(),
we get a cardioid.
r = 1 – k *cos()
0 < k < 1
r = 1 – cos()
k = 1
For k < 1, e.g. r = 1 – ½ *cos(),
we have r > 0 for all ’s.
This means the graph does not
pass through the origin.
Instead, the cusp, i.e. the
pinched point at the origin of the
cardioid is pushed out as shown.
Polar Coordinates & Graphs
For k > 1, e.g. r = 1 – 2cos(),
we have r = –1 < 0 for  = 0.
Polar Coordinates & Graphs
For k > 1, e.g. r = 1 – 2cos(),
we have r = –1 < 0 for  = 0.
In fact, as  goes from 0 to π/3,
r goes from –1 to 0,
Polar Coordinates & Graphs
For k > 1, e.g. r = 1 – 2cos(),
we have r = –1 < 0 for  = 0.
In fact, as  goes from 0 to π/3,
r goes from –1 to 0, and the
corresponding points traverse
from (–1, 0) to (0, π/3) as
shown.
x
r = 1 – 2cos()
(–1, 0) (0, π/3)
Polar Coordinates & Graphs
For k > 1, e.g. r = 1 – 2cos(),
we have r = –1 < 0 for  = 0.
In fact, as  goes from 0 to π/3,
r goes from –1 to 0, and the
corresponding points traverse
from (–1, 0) to (0, π/3) as
shown. As  goes from π/3 to
π/2, r increases from 0 to 1,
so the points traverse from (0, π/3 )
to (1, π/2).
x
r = 1 – 2cos()
(–1, 0) (0, π/3)
Polar Coordinates & Graphs
For k > 1, e.g. r = 1 – 2cos(),
we have r = –1 < 0 for  = 0.
In fact, as  goes from 0 to π/3,
r goes from –1 to 0, and the
corresponding points traverse
from (–1, 0) to (0, π/3) as
shown. As  goes from π/3 to
π/2, r increases from 0 to 1,
x
r = 1 – 2cos()
(0, π/3)
(–1, 0)
(1, π/2)
(3, π)
so the points traverse from (0, π/3 )
to (1, π/2).
Polar Coordinates & Graphs
For k > 1, e.g. r = 1 – 2cos(),
we have r = –1 < 0 for  = 0.
In fact, as  goes from 0 to π/3,
r goes from –1 to 0, and the
corresponding points traverse
from (–1, 0) to (0, π/3) as
shown. As  goes from π/3 to
π/2, r increases from 0 to 1,
r increases from 1 to 3, and the points traverse from
(1, π/2) to (3, π).
x
r = 1 – 2cos()
(0, π/3)
(–1, 0)
(1, π/2)
(3, π)
so the points traverse from (0, π/3 )
to (1, π/2). As  from π/2 to π,
Polar Coordinates & Graphs
For k > 1, e.g. r = 1 – 2cos(),
we have r = –1 < 0 for  = 0.
In fact, as  goes from 0 to π/3,
r goes from –1 to 0, and the
corresponding points traverse
from (–1, 0) to (0, π/3) as
shown. As  goes from π/3 to
π/2, r increases from 0 to 1,
r increases from 1 to 3, and the points traverse from
(1, π/2) to (3, π).
For 1 < k, r = 1 – k*cos()
has an inner loop.
x
r = 1 – 2cos()
(0, π/3)
(–1, 0)
(1, π/2)
(3, π)
so the points traverse from (0, π/3 )
to (1, π/2). As  from π/2 to π,
Polar Coordinates & Graphs
For k > 1, e.g. r = 1 – 2cos(),
we have r = –1 < 0 for  = 0.
In fact, as  goes from 0 to π/3,
r goes from –1 to 0, and the
corresponding points traverse
from (–1, 0) to (0, π/3) as
shown. As  goes from π/3 to
π/2, r increases from 0 to 1,
r increases from 1 to 3, and the points traverse from
(1, π/2) to (3, π). Finally since cos() = cos(–), we
obtain the entire graph by taking its reflection across
the x–axis.
For 1 < k, r = 1 – k*cos()
has an inner loop.
x
r = 1 – 2cos()
(0, π/3)
(–1, 0)
(1, π/2)
(3, π)
so the points traverse from (0, π/3 )
to (1, π/2). As  from π/2 to π,
Polar Coordinates & Graphs
For k > 1, e.g. r = 1 – 2cos(),
we have r = –1 < 0 for  = 0.
In fact, as  goes from 0 to π/3,
r goes from –1 to 0, and the
corresponding points traverse
from (–1, 0) to (0, π/3) as
shown. As  goes from π/3 to
π/2, r increases from 0 to 1,
so the points traverse from (0, π/3 )
to (1, π/2). As  from π/2 to π,
r increases from 1 to 3, and the points traverse from
(1, π/2) to (3, π). Finally since cos() = cos(–), we
obtain the entire graph by taking its reflection across
the x–axis. Note that we have an inner loop if k > 1.
For 1 < k, r = 1 – k*cos()
has an inner loop.
x
r = 1 – 2cos()
(0, π/3)
(–1, 0)
(1, π/2)
(3, π)
Polar Coordinates & Graphs
Here is a sequence of graphs for r = 1 – kcos().
r = 1 – (1/4)cos()
Polar Coordinates & Graphs
Here is a sequence of graphs for r = 1 – kcos().
r = 1 – (1/4)cos() r = 1 – (1/2)cos()
Polar Coordinates & Graphs
Here is a sequence of graphs for r = 1 – kcos().
r = 1 – (1/4)cos() r = 1 – (1/2)cos() r = 1 – 1cos()
Polar Coordinates & Graphs
Here is a sequence of graphs for r = 1 – kcos().
r = 1 – (1/4)cos() r = 1 – (1/2)cos() r = 1 – 1cos() r = 1 – 2cos()
Polar Coordinates & Graphs
Here is a sequence of graphs for r = 1 – kcos().
r = 1 – (1/4)cos() r = 1 – (1/2)cos() r = 1 – 1cos() r = 1 – 2cos() r = 1 – 4cos()
Polar Coordinates & Graphs
Here is a sequence of graphs for r = 1 – kcos().
r = 1 – (1/4)cos() r = 1 – (1/2)cos() r = 1 – 1cos() r = 1 – 2cos() r = 1 – 4cos()
Polar equations of the forms r = sin(n) or r = cos(n),
where n is a positive integer, form floral shape petals
that mathematicians call “roses”.
The Roses
Polar Coordinates & Graphs
Here is a sequence of graphs for r = 1 – kcos().
r = 1 – (1/4)cos() r = 1 – (1/2)cos() r = 1 – 1cos() r = 1 – 2cos() r = 1 – 4cos()
Polar equations of the forms r = sin(n) or r = cos(n),
where n is a positive integer, form floral shape petals
that mathematicians call “roses”.
The Roses
Polar Coordinates & Graphs
Here is a sequence of graphs for r = 1 – kcos().
r = 1 – (1/4)cos() r = 1 – (1/2)cos() r = 1 – 1cos() r = 1 – 2cos() r = 1 – 4cos()
Polar equations of the forms r = sin(n) or r = cos(n),
where n is a positive integer, form floral shape petals
that mathematicians call “roses”.
Recall that for n = 1, r = cos() consists of two
overlapping circles, i.e. the graph traverses the circle
twice as  goes from 0 to 2π.
The Roses
Polar Coordinates & Graphs
Here is a sequence of graphs for r = 1 – kcos().
r = 1 – (1/4)cos() r = 1 – (1/2)cos() r = 1 – 1cos() r = 1 – 2cos() r = 1 – 4cos()
Polar equations of the forms r = sin(n) or r = cos(n),
where n is a positive integer, form floral shape petals
that mathematicians call “roses”.
Recall that for n = 1, r = cos() consists of two
overlapping circles, i.e. the graph traverses the circle
twice as  goes from 0 to 2π. This is different from the
cases when n is even where the graph consists of 2n
petals.
The Roses
Polar Coordinates & Graphs
r = cos(1) r = cos(3)
If n is odd, the graph of r = cos(n) consists of
n petals as  goes from 0 to π,
r = cos(7)
r = cos(5)
Polar Coordinates & Graphs
r = cos(1) r = cos(3)
If n is odd, the graph of r = cos(n) consists of
n petals as  goes from 0 to π, then the graph follows
the same path as  goes from π to 2π.
r = cos(7)
r = cos(5)
Polar Coordinates & Graphs
r = cos(1) r = cos(3)
If n is odd, the graph of r = cos(n) consists of
n petals as  goes from 0 to π, then the graph follows
the same path as  goes from π to 2π.
If n is even, the graph of r = cos(n) traces out
2n petals as  goes from 0 to 2π.
r = cos(7)
r = cos(5)
Polar Coordinates & Graphs
r = cos(1) r = cos(3)
If n is odd, the graph of r = cos(n) consists of
n petals as  goes from 0 to π, then the graph follows
the same path as  goes from π to 2π.
r = cos(2) r = cos(4) r = cos(6) r = cos(8)
If n is even, the graph of r = cos(n) traces out
2n petals as  goes from 0 to 2π.
r = cos(7)
r = cos(5)
Polar Coordinates & Graphs
Following is a brief argument for the differences in the
graphs of r = sin(n) depending on n is even or odd.
Polar Coordinates & Graphs
Following is a brief argument for the differences in the
graphs of r = sin(n) depending on n is even or odd.
Let’s look at the graph of r = | sin(3) |.
Polar Coordinates & Graphs
Following is a brief argument for the differences in the
graphs of r = sin(n) depending on n is even or odd.
Let’s look at the graph of r = | sin(3) |.
For 0 ≤  < 2π, we have that 0 ≤ 3 < 6π.
Polar Coordinates & Graphs
Following is a brief argument for the differences in the
graphs of r = sin(n) depending on n is even or odd.
Let’s look at the graph of r = | sin(3) |.
For 0 ≤  < 2π, we have that 0 ≤ 3 < 6π.
If 3 = 0, π, 2π, 3π, 4π, 5π, then r = sin(3) = 0,
or r = 0 when  = 0, π/3, 2π/3, π, 4π/3, 5π/3
π/3
2π/3
The graph of
r = | sin(3) |
0
Polar Coordinates & Graphs
Following is a brief argument for the differences in the
graphs of r = sin(n) depending on n is even or odd.
Let’s look at the graph of r = | sin(3) |.
For 0 ≤  < 2π, we have that 0 ≤ 3 < 6π.
If 3 = 0, π, 2π, 3π, 4π, 5π, then r = sin(3) = 0,
or r = 0 when  = 0, π/3, 2π/3, π, 4π/3, 5π/3.
Similarly, r = 1 when  = π/6, π/2, 5π/6, 7π/6, 3π/2, 11π/6.
π/3
2π/3
The graph of
r = | sin(3) |
0
Polar Coordinates & Graphs
Following is a brief argument for the differences in the
graphs of r = sin(n) depending on n is even or odd.
As  goes from 0 to π/6 to π/3, r goes
from 0 to 1 back to 0.
Let’s look at the graph of r = | sin(3) |.
For 0 ≤  < 2π, we have that 0 ≤ 3 < 6π.
If 3 = 0, π, 2π, 3π, 4π, 5π, then r = sin(3) = 0,
or r = 0 when  = 0, π/3, 2π/3, π, 4π/3, 5π/3.
Similarly, r = 1 when  = π/6, π/2, 5π/6, 7π/6, 3π/2, 11π/6.
π/3
2π/3
The graph of
r = | sin(3) |
0
Polar Coordinates & Graphs
Following is a brief argument for the differences in the
graphs of r = sin(n) depending on n is even or odd.
(1, π/6)
π/3
The graph of
r = | sin(3) |
0
Let’s look at the graph of r = | sin(3) |.
For 0 ≤  < 2π, we have that 0 ≤ 3 < 6π.
If 3 = 0, π, 2π, 3π, 4π, 5π, then r = sin(3) = 0,
or r = 0 when  = 0, π/3, 2π/3, π, 4π/3, 5π/3.
Similarly, r = 1 when  = π/6, π/2, 5π/6, 7π/6, 3π/2, 11π/6.
2π/3
As  goes from 0 to π/6 to π/3, r goes
from 0 to 1 back to 0. So the graph
starts at the origin and makes a petal
(loop), to a tip of distance 1 from the
origin, back to the origin in a period
of π/3.
Polar Coordinates & Graphs
Following is a brief argument for the differences in the
graphs of r = sin(n) depending on n is even or odd.
(1, π/6)
As  goes from 0 to π/6 to π/3, r goes
from 0 to 1 back to 0. So the graph
starts at the origin and makes a petal
(loop), to a tip of distance 1 from the
origin, back to the origin in a period
of π/3. Repeat this every π/3, we get
6 petals for r = | sin(3) |.
π/3
2π/3
The graph of
r = | sin(3) |
0
Let’s look at the graph of r = | sin(3) |.
For 0 ≤  < 2π, we have that 0 ≤ 3 < 6π.
If 3 = 0, π, 2π, 3π, 4π, 5π, then r = sin(3) = 0,
or r = 0 when  = 0, π/3, 2π/3, π, 4π/3, 5π/3.
Similarly, r = 1 when  = π/6, π/2, 5π/6, 7π/6, 3π/2, 11π/6.
Polar Coordinates & Graphs
Let’s now consider the signs of r = sin(3) as shown.
below.
0
π/3
2π/3
0
π/3
2π/3
+
+
+
–
– –
The signs of
r = sin(3)
The graph of
r = | sin(3) |
(1, π/6)
Polar Coordinates & Graphs
Let’s now consider the signs of r = sin(3) as shown.
below.
0
π/3
2π/3
0
π/3
2π/3
+
+
+
–
– –
The signs of
r = sin(3)
Note the difference in the signs of opposite segments.
The graph of
r = | sin(3) |
(1, π/6)
Polar Coordinates & Graphs
Let’s now consider the signs of r = sin(3) as shown.
below.
0
π/3
2π/3 π/3
2π/3
+
+
+
–
– –
The signs of
r = sin(3)
Note the difference in the signs of opposite segments.
Hence the “negative petals” flip across the origin in the
graph of r = sin(3) as shown.
The graph of
r = | sin(3) |
(1, π/6)
0
Polar Coordinates & Graphs
Let’s now consider the signs of r = sin(3) as shown.
below.
0
π/3
2π/3
0
π/3
2π/3
0
π/3
2π/3
+
+
+
–
– –
The signs of
r = sin(3)
Note the difference in the signs of opposite segments.
Hence the “negative petals” flip across the origin in the
graph of r = sin(3) as shown.
The graph of
r = sin(3)
The graph of
r = | sin(3) |
– –
–
(1, π/6)
(1, π/6) =
(–1, 7π/6)
Polar Coordinates & Graphs
Let’s now consider the signs of r = sin(3) as shown.
below.
0
π/3
2π/3
0
π/3
2π/3
0
π/3
2π/3
+
+
+
–
– –
The signs of
r = sin(3)
Note the difference in the signs of opposite segments.
Hence the “negative petals” flip across the origin in the
graph of r = sin(3) as shown. This is true in general
when n is odd, that the graph of r = sin(n) consists of
n petals because the “negative petals”
fold into the opposite positive ones
The graph of
r = sin(3)
The graph of
r = | sin(3) |
– –
–
(1, π/6)
(1, π/6) =
(–1, 7π/6)
Polar Coordinates & Graphs
Let’s now consider the signs of r = sin(3) as shown.
below.
0
π/3
2π/3
0
π/3
2π/3
0
π/3
2π/3
+
+
+
–
– –
The signs of
r = sin(3)
Note the difference in the signs of opposite segments.
Hence the “negative petals” flip across the origin in the
graph of r = sin(3) as shown. This is true in general
when n is odd, that the graph of r = sin(n) consists of
n petals because the “negative petals” fold into the
opposite positive ones and the graph traverses each
petal twice as  goes from 0 to 2π.
The graph of
r = sin(3)
The graph of
r = | sin(3) |
– –
–
(1, π/6)
(1, π/6) =
(–1, 7π/6)
Example C. Sketch the graph r = sin(5).
Polar Coordinates & Graphs
Example C. Sketch the graph r = sin(5).
The graph r = sin(5) consists
of 5 petals sitting evenly in 10
wedges each having a radial
angle of π/5.
Polar Coordinates & Graphs
Example C. Sketch the graph r = sin(5).
The graph r = sin(5) consists
of 5 petals sitting evenly in 10
wedges each having a radial
angle of π/5.
0
Polar Coordinates & Graphs
2π/5
π/5
r = sin(5)
(1, π/10) =
(–1, 11π/10)
Example C. Sketch the graph r = sin(5).
The graph r = sin(5) consists
of 5 petals sitting evenly in 10
wedges each having a radial
angle of π/5.
0
Polar Coordinates & Graphs
2π/5
π/5
r = sin(5)
The graph r = sin(5) consists
of 5 petals sitting evenly in 10
wedges each having a radial
angle of π/5.
Polar Coordinates & Graphs
(1, π/10) =
(–1, 11π/10)
0
2π/5
π/5
Example C. Sketch the graph r = sin(5).
+
–
+
–
+
+ +
– –
–
r = sin(5)
The graph r = sin(5) consists
of 5 petals sitting evenly in 10
wedges each having a radial
angle of π/5.
Polar Coordinates & Graphs
(1, π/10) =
(–1, 11π/10)
0
2π/5
π/5
Example C. Sketch the graph r = sin(5).
+
–
+
–
+
+ +
– –
–
r = sin(5)
In general if n is odd, r = sin(n)
has n petals from 0 to 2π.
The graph r = sin(5) consists
of 5 petals sitting evenly in 10
wedges each having a radial
angle of π/5.
Polar Coordinates & Graphs
π/4
+
–
+
–
+
–
–
+
(1, π/10) =
(–1, 11π/10)
0
2π/5
π/5
Example C. Sketch the graph r = sin(5).
+
–
+
–
+
+ +
– –
–
r = sin(5)
In general if n is odd, r = sin(n)
has n petals from 0 to 2π.
If n is even, e.g. r = sin(4), then
its signs are distributed as shown,
i.e. two opposite wedges have
the same sign
r = sin(4)
The graph r = sin(5) consists
of 5 petals sitting evenly in 10
wedges each having a radial
angle of π/5.
Polar Coordinates & Graphs
r = sin(4)
π/4
+
–
+
–
+
–
–
+
If n is even, e.g. r = sin(4), then
its signs are distributed as shown,
i.e. two opposite wedges have
the same sign so the graph of
r = sin(4) retains all eight petals.
(1, π/10) =
(–1, 11π/10)
0
2π/5
π/5
Example C. Sketch the graph r = sin(5).
+
–
+
–
+
+ +
– –
–
r = sin(5)
In general if n is odd, r = sin(n)
has n petals from 0 to 2π.
The graph r = sin(5) consists
of 5 petals sitting evenly in 10
wedges each having a radial
angle of π/5.
Polar Coordinates & Graphs
r = sin(4)
π/4
+
–
+
–
+
–
–
+
If n is even, e.g. r = sin(4), then
its signs are distributed as shown,
i.e. two opposite wedges have
the same sign so the graph of
r = sin(4) retains all eight petals.
In general if n is even, r = sin(n)
has 2n petals.
(1, π/10) =
(–1, 11π/10)
0
2π/5
π/5
Example C. Sketch the graph r = sin(5).
+
–
+
–
+
+ +
– –
–
r = sin(5)
In general if n is odd, r = sin(n)
has n petals from 0 to 2π.
Polar Equations
Spirals
A spiral is the graph of r = f() where f() is increasing
or decreasing.
Polar Equations
Spirals
A spiral is the graph of r = f() where f() is increasing
or decreasing.
Example D. a. Graph r =  where  ≥ 0.
Polar Equations
Spirals
A spiral is the graph of r = f() where f() is increasing
or decreasing.
Example D. a. Graph r =  where  ≥ 0.
The polar equation states that the
distance r is the same as .
Polar Equations
x
r = 
Spirals
A spiral is the graph of r = f() where f() is increasing
or decreasing.
Example D. a. Graph r =  where  ≥ 0.
The polar equation states that the
distance r is the same as .
Starting at (0, 0), as  increases,
r increases, so the points are circling
outward from the origin at a steady rate.
Polar Equations
A uniformly banded spiral such as this
one is called an Archimedean spiral.
x
The Archimedean Spiral
r = 
Spirals
A spiral is the graph of r = f() where f() is increasing
or decreasing.
Example D. a. Graph r =  where  ≥ 0.
The polar equation states that the
distance r is the same as .
Starting at (0, 0), as  increases,
r increases, so the points are circling
outward from the origin at a steady rate.
Polar Equations
A uniformly banded spiral such as this
one is called an Archimedean spiral.
x
The Archimedean Spiral
r = 
Spirals
A spiral is the graph of r = f() where f() is increasing
or decreasing.
Example D. a. Graph r =  where  ≥ 0.
The polar equation states that the
distance r is the same as .
Starting at (0, 0), as  increases,
r increases, so the points are circling
outward from the origin at a steady rate.
b. Convert the polar equation r = 
into a rectangular equation by using
the cosine inverse to express .
Polar Equations
We will use the cosine inverse
function to express  in x&y,
x
r = 
x
Polar Equations
We will use the cosine inverse
function to express  in x&y, i.e.
 = cos–1(x/r) = cos–1(x/√x2 + y2 ).
x
r = 
x
Polar Equations
We have the equation that
We will use the cosine inverse
function to express  in x&y, i.e.
 = cos–1(x/r) = cos–1(x/√x2 + y2 ).
cos–1(x/√x2 + y2) = √x2 + y2 ( = r ) x
r = 
x
Polar Equations
We have the equation that
We will use the cosine inverse
function to express  in x&y, i.e.
 = cos–1(x/r) = cos–1(x/√x2 + y2 ).
cos–1(x/√x2 + y2) = √x2 + y2 ( = r ) x
r = 
This rectangular equation only
gives the part of the spiral where
0 < √x2 + y2 ≤ π (why?)
x
Polar Equations
We have the equation that
We will use the cosine inverse
function to express  in x&y, i.e.
 = cos–1(x/r) = cos–1(x/√x2 + y2 ).
cos–1(x/√x2 + y2) = √x2 + y2 ( = r ) x
r = 
This rectangular equation only
gives the part of the spiral where
0 < √x2 + y2 ≤ π (why?)
cos–1(x/√x2 + y2) = √x2 + y2
x
x
The “Lost in Translation”
from the polar to the
rectangular equation
Polar Equations
We have the equation that
We will use the cosine inverse
function to express  in x&y, i.e.
 = cos–1(x/r) = cos–1(x/√x2 + y2 ).
cos–1(x/√x2 + y2) = √x2 + y2 ( = r ) x
r = 
This rectangular equation only
gives the part of the spiral where
0 < √x2 + y2 ≤ π (why?)
For other parts of the spirals,
we add nπ to  with n = 1,2,..
cos–1(x/√x2 + y2) = √x2 + y2
x
x
The “Lost in Translation”
from the polar to the
rectangular equation
Polar Equations
We have the equation that
We will use the cosine inverse
function to express  in x&y, i.e.
 = cos–1(x/r) = cos–1(x/√x2 + y2 ).
cos–1(x/√x2 + y2) = √x2 + y2 ( = r ) x
r = 
This rectangular equation only
gives the part of the spiral where
0 < √x2 + y2 ≤ π (why?)
cos–1(x/√x2 + y2) = √x2 + y2
x
x
The “Lost in Translation”
from the polar to the
rectangular equation
For other parts of the spirals,
we add nπ to  with n = 1,2,.. to
obtain more distant segments, so
cos–1(x/√x2 + y2) + nπ = √x2 + y2.
Polar Equations
We have the equation that
We will use the cosine inverse
function to express  in x&y, i.e.
 = cos–1(x/r) = cos–1(x/√x2 + y2 ).
cos–1(x/√x2 + y2) = √x2 + y2 ( = r ) x
r = 
This rectangular equation only
gives the part of the spiral where
0 < √x2 + y2 ≤ π (why?)
cos–1(x/√x2 + y2) = √x2 + y2
x
x
The “Lost in Translation”
from the polar to the
rectangular equation
This shows the advantages of the
polar system in certain settings.
cos–1(x/√x2 + y2) + nπ = √x2 + y2.
For other parts of the spirals,
we add nπ to  with n = 1,2,.. to
obtain more distant segments, so
Polar Coordinates & Graphs
The Log or Equiangular Spirals
Polar Coordinates & Graphs
The Log or Equiangular Spirals
The spirals r = aeb where a, b are constants are
called logarithmic spirals.
Polar Coordinates & Graphs
The Log or Equiangular Spirals
The spirals r = aeb where a, b are constants are
called logarithmic spirals.
The log–spirals, named after the log–form  = β*ln(r)
of the equation r = eα, are also known as the
equiangular spirals.
Polar Coordinates & Graphs
The Log or Equiangular Spirals
The spirals r = aeb where a, b are constants are
called logarithmic spirals.
r = e0.15 r = e0.75
r = e0.35
The log–spirals, named after the log–form  = β*ln(r)
of the equation r = eα, are also known as the
equiangular spirals.
Here are some examples of log–spirals.
Polar Coordinates & Graphs
The Log or Equiangular Spirals
The spirals r = aeb where a, b are constants are
called logarithmic spirals.
r = e0.15 r = e0.75
r = e0.35
The log–spirals, named after the log–form  = β*ln(r)
of the equation r = eα, are also known as the
equiangular spirals.
Here are some examples of log–spirals.
Log–spirals are also called equiangular spirals
because of its geometric characteristic.
Polar Coordinates & Graphs
The geometric significance of an equiangular spiral
is that the angle between the tangent line and
the radial line at any point on the spiral is a fixed
constant.
Polar Coordinates & Graphs
k
The geometric significance of an equiangular spiral
is that the angle between the tangent line and
the radial line at any point on the spiral is a fixed
constant.
Equiangular spirals
Polar Coordinates & Graphs
k
k
The geometric significance of an equiangular spiral
is that the angle between the tangent line and
the radial line at any point on the spiral is a fixed
constant.
Equiangular spirals
Polar Coordinates & Graphs
k
k
q
The geometric significance of an equiangular spiral
is that the angle between the tangent line and
the radial line at any point on the spiral is a fixed
constant.
Equiangular spirals
Polar Coordinates & Graphs
q
k
k
q
The geometric significance of an equiangular spiral
is that the angle between the tangent line and
the radial line at any point on the spiral is a fixed
constant.
Equiangular spirals
Polar Coordinates & Graphs
q
k
k
q
Equiangular spirals
The geometric significance of an equiangular spiral
is that the angle between the tangent line and
the radial line at any point on the spiral is a fixed
constant.
If the curve spirals outward, the tangential angle must
be more than π/2
Polar Coordinates & Graphs
q
k
k
q
Equiangular spirals
The geometric significance of an equiangular spiral
is that the angle between the tangent line and
the radial line at any point on the spiral is a fixed
constant.
If the curve spirals outward, the tangential angle must
be more than π/2. If the tangential angle is π/2,
the spiral contracts into a circle.
Polar Coordinates & Graphs
q
k
k
q
Equiangular spirals
The geometric significance of an equiangular spiral
is that the angle between the tangent line and
the radial line at any point on the spiral is a fixed
constant.
If the curve spirals outward, the tangential angle must
be more than π/2. If the tangential angle is π/2,
the spiral contracts into a circle. If the tangential angle
is less than π/2, then it’s spiraling inward toward (0,0).
Polar Coordinates & Graphs
Equiangular spirals occur in nature frequently.
http://en.wikipedia.
org/wiki/Logarithmi
c_spiral
Polar Coordinates & Graphs
Equiangular spirals occur in nature frequently.
In many biological growth processes,
the new growth is extruded at a fixed angle from the
existing structure,
http://en.wikipedia.
org/wiki/Logarithmi
c_spiral
Polar Coordinates & Graphs
Equiangular spirals occur in nature frequently.
In many biological growth processes,
the new growth is extruded at a fixed angle from the
existing structure, e.g. the growth of new sea shell
along the edge of the old shell, or the growth of plants.
http://en.wikipedia.
org/wiki/Logarithmi
c_spiral
Polar Coordinates & Graphs
Equiangular spirals occur in nature frequently.
In many biological growth processes,
the new growth is extruded at a fixed angle from the
existing structure, e.g. the growth of new sea shell
along the edge of the old shell, or the growth of plants.
Over time the equiangular–spiral growth lines emerge.
http://en.wikipedia.
org/wiki/Logarithmi
c_spiral
Polar Coordinates & Graphs
Rotations of Polar Graphs
Polar Coordinates & Graphs
Let r1 = cos() = f() and
r2 = cos( – π/4) = g() so that
r2 = g( + π/4) = f() = r1.
Rotations of Polar Graphs
Polar Coordinates & Graphs
Let r1 = cos() = f() and
r2 = cos( – π/4) = g() so that
r2 = g( + π/4) = f() = r1. Therefore,
the point (r2,  + π/4) on the graph of g
is the point (r1, ) on the graph of f
rotated by the angle π/4 as shown.
x
y
r = cos()
Rotations of Polar Graphs
Polar Coordinates & Graphs
Let r1 = cos() = f() and
r2 = cos( – π/4) = g() so that
r2 = g( + π/4) = f() = r1. Therefore,
the point (r2,  + π/4) on the graph of g
is the point (r1, ) on the graph of f
rotated by the angle π/4 as shown.
x
y
r = cos()
r = cos( – π/4)
π/4
Rotations of Polar Graphs
Polar Coordinates & Graphs
Let r1 = cos() = f() and
r2 = cos( – π/4) = g() so that
r2 = g( + π/4) = f() = r1. Therefore,
the point (r2,  + π/4) on the graph of g
is the point (r1, ) on the graph of f
rotated by the angle π/4 as shown.
x
y
r = cos()
r = cos( – π/4)
π/4
Rotations of Polar Graphs
In general, given r1 = f(), let r2 = g() = f( – α)
so that g( + α) = f(), then the point (r2,  + α)
is the point (r1, ) on the graph of f, rotated by α.
Polar Coordinates & Graphs
Let r1 = cos() = f() and
r2 = cos( – π/4) = g() so that
r2 = g( + π/4) = f() = r1. Therefore,
the point (r2,  + π/4) on the graph of g
is the point (r1, ) on the graph of f
rotated by the angle π/4 as shown.
x
y
r = cos()
r = cos( – π/4)
π/4
Rotations of Polar Graphs
In general, given r1 = f(), let r2 = g() = f( – α)
so that g( + α) = f(), then the point (r2,  + α)
is the point (r1, ) on the graph of f, rotated by α.
If α is positive, then the graph of r2 = f( – α) is the
counter clockwise rotation of r1 = f() by the angle α,
Polar Coordinates & Graphs
Let r1 = cos() = f() and
r2 = cos( – π/4) = g() so that
r2 = g( + π/4) = f() = r1. Therefore,
the point (r2,  + π/4) on the graph of g
is the point (r1, ) on the graph of f
rotated by the angle π/4 as shown.
x
y
r = cos()
r = cos( – π/4)
π/4
Rotations of Polar Graphs
In general, given r1 = f(), let r2 = g() = f( – α)
so that g( + α) = f(), then the point (r2,  + α)
is the point (r1, ) on the graph of f, rotated by α.
If α is positive, then the graph of r2 = f( – α) is the
counter clockwise rotation of r1 = f() by the angle α,
and the graph of r2 = f( + α) is the clockwise rotation
of r1 = f() by the angle α.
Polar Coordinates & Graphs
Radial Extensions/Contractions
of Polar Graphs
Polar Coordinates & Graphs
The point (2r, ) is the radial extension of
the point (r, ) as shown.
Radial Extensions/Contractions
of Polar Graphs

O
(r, )p
r
Polar Coordinates & Graphs
The point (2r, ) is the radial extension of
the point (r, ) as shown.
Radial Extensions/Contractions
of Polar Graphs

O
(r, )p
r
(2r, )p
Polar Coordinates & Graphs
The point (2r, ) is the radial extension of
the point (r, ) as shown.
Radial Extensions/Contractions
of Polar Graphs

O
(r, )p
r
In general, the graph of r = kf()
when k is a constant,
is the radial stretch/compression
of the graph r = f().
(2r, )p
Polar Coordinates & Graphs
The point (2r, ) is the radial extension of
the point (r, ) as shown.
Radial Extensions/Contractions
of Polar Graphs

O
(r, )p
r
x
y
r = cos( – π/4)
r = 2cos( – π/4)
radial stretch/compression k >0
In general, the graph of r = kf()
when k is a constant,
is the radial stretch/compression
of the graph r = f().
The graphs of
r1 = cos ( – π/4),
(2r, )p
Polar Coordinates & Graphs
The point (2r, ) is the radial extension of
the point (r, ) as shown.
Radial Extensions/Contractions
of Polar Graphs

O
(r, )p
r
x
y
r = cos( – π/4)
r = 2cos( – π/4)
radial stretch/compression k >0
In general, the graph of r = kf()
when k is a constant,
is the radial stretch/compression
of the graph r = f().
The graphs of
r1 = cos ( – π/4),
r2 = 2cos ( – π/4)
(2r, )p
Polar Coordinates & Graphs
The point (2r, ) is the radial extension of
the point (r, ) as shown.
Radial Extensions/Contractions
of Polar Graphs

O
(r, )p
r
x
y
r = cos( – π/4)
r = 2cos( – π/4)
radial stretch/compression k >0
r = ½ cos( – π/4)
In general, the graph of r = kf()
when k is a constant,
is the radial stretch/compression
of the graph r = f().
The graphs of
r1 = cos ( – π/4),
r2 = 2cos ( – π/4) and
r3 = ½ * cos ( – π/4)
are shown here as examples.
(2r, )p
Polar Coordinates & Graphs
If k < 0, then the graph of r = kf() is the
diagonal reflection across the origin
of r = |k| f().
Polar Coordinates & Graphs
If k < 0, then the graph of r = kf() is the
diagonal reflection across the origin
of r = |k| f(). Here are the graphs
of r = –2cos ( – π/4)
and r = 2cos ( – π/4).
x
r = 2cos( – π/4)
r = –2cos( – π/4)
r = cos( – π/4)
Diagonal
Reflection
with k < 0

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20 polar equations and graphs

  • 2. Polar Coordinates & Graphs Besides the rectangular coordinates, we may track the location of a point P in the plane by its polar coordinates (r, ), P x y (r, )p
  • 3. Polar Coordinates & Graphs Besides the rectangular coordinates, we may track the location of a point P in the plane by its polar coordinates (r, ), where r is the signed distance from the origin (0, 0) to P, P x y (r, )p r
  • 4. Polar Coordinates & Graphs P x y  O Besides the rectangular coordinates, we may track the location of a point P in the plane by its polar coordinates (r, ), where r is the signed distance from the origin (0, 0) to P, and  is an angle measured from the positive x–axis which gives the direction to P. (r, )p r
  • 5. Polar Coordinates & Graphs Conversion Rules Let (x, y)R and (r, )P be the rectangular and the polar coordinates of P, P x y  O Besides the rectangular coordinates, we may track the location of a point P in the plane by its polar coordinates (r, ), where r is the signed distance from the origin (0, 0) to P, and  is an angle measured from the positive x–axis which gives the direction to P. (r, )p = (x, y)R r
  • 6. Polar Coordinates & Graphs Conversion Rules Let (x, y)R and (r, )P be the rectangular and the polar coordinates of P, then x = r*cos() P x y  O x = r*cos() The rectangular and polar conversions Besides the rectangular coordinates, we may track the location of a point P in the plane by its polar coordinates (r, ), where r is the signed distance from the origin (0, 0) to P, and  is an angle measured from the positive x–axis which gives the direction to P. (r, )p = (x, y)R r
  • 7. Polar Coordinates & Graphs Conversion Rules Let (x, y)R and (r, )P be the rectangular and the polar coordinates of P, then x = r*cos() y = r*sin() P x y  O x = r*cos() y = r*sin() The rectangular and polar conversions r (r, )p = (x, y)R Besides the rectangular coordinates, we may track the location of a point P in the plane by its polar coordinates (r, ), where r is the signed distance from the origin (0, 0) to P, and  is an angle measured from the positive x–axis which gives the direction to P.
  • 8. Polar Coordinates & Graphs Conversion Rules Let (x, y)R and (r, )P be the rectangular and the polar coordinates of P, then x = r*cos() y = r*sin() r = √x2 + y2 tan() = y/x P x y  O x = r*cos() y = r*sin() The rectangular and polar conversions r = √x2 + y2 (r, )p = (x, y)R Besides the rectangular coordinates, we may track the location of a point P in the plane by its polar coordinates (r, ), where r is the signed distance from the origin (0, 0) to P, and  is an angle measured from the positive x–axis which gives the direction to P.
  • 9. Polar Coordinates & Graphs Conversion Rules Let (x, y)R and (r, )P be the rectangular and the polar coordinates of P, then P x y  O x = r*cos() y = r*sin() The rectangular and polar conversions x = r*cos() y = r*sin() r = √x2 + y2 tan() = y/x r = √x2 + y2 If P is in quadrants I, II or IV then  may be extracted by inverse trig functions. But if P is in quadrant III, then  can’t be calculated directly by inverse trig-functions. (r, )p = (x, y)R Besides the rectangular coordinates, we may track the location of a point P in the plane by its polar coordinates (r, ), where r is the signed distance from the origin (0, 0) to P, and  is an angle measured from the positive x–axis which gives the direction to P.
  • 11. Polar Equations A rectangular equation in x and y gives the relation between the horizontal displacement x and vertical displacement y of locations. Polar Coordinates & Graphs
  • 12. Polar Equations A rectangular equation in x and y gives the relation between the horizontal displacement x and vertical displacement y of locations. A polar equation gives a relation of the distance r the direction . Polar Coordinates & Graphs
  • 13. Polar Equations A rectangular equation in x and y gives the relation between the horizontal displacement x and vertical displacement y of locations. A polar equation gives a relation of the distance r the direction . Polar Coordinates & Graphs The rectangular equation y = x specifies that the horizontal displacement x must be the same as the vertical displacement y for our points P.
  • 14. Polar Equations A rectangular equation in x and y gives the relation between the horizontal displacement x and vertical displacement y of locations. A polar equation gives a relation of the distance r the direction . Polar Coordinates & Graphs The rectangular equation y = x specifies that the horizontal displacement x must be the same as the vertical displacement y for our points P. y y x x P(x, y) The graph of y = x in the the rectangular system
  • 15. Polar Equations A rectangular equation in x and y gives the relation between the horizontal displacement x and vertical displacement y of locations. A polar equation gives a relation of the distance r the direction . Polar Coordinates & Graphs The rectangular equation y = x specifies that the horizontal displacement x must be the same as the vertical displacement y for our points P. y y x x P(x, y) The graph of y = x in the the rectangular system The polar equation r =  says that the distance r must be the same as the rotational measurement  for P. Its graph is the Archimedean spiral.
  • 16. Polar Equations A rectangular equation in x and y gives the relation between the horizontal displacement x and vertical displacement y of locations. A polar equation gives a relation of the distance r the direction . Polar Coordinates & Graphs The rectangular equation y = x specifies that the horizontal displacement x must be the same as the vertical displacement y for our points P. y y x x P(x, y) x P(r, )  r The graph of y = x in the the rectangular system Graph of r =  in the polar system. The polar equation r =  says that the distance r must be the same as the rotational measurement  for P. Its graph is the Archimedean spiral.
  • 17. Let’s look at some basic examples of polar graphs. Polar Coordinates & Graphs The Constant Equations r = c &  = c
  • 18. Let’s look at some basic examples of polar graphs. Polar Coordinates & Graphs The Constant Equations r = c &  = c Example A. Graph the following polar equations. a. (r = c) b. ( = c)
  • 19. Let’s look at some basic examples of polar graphs. Polar Coordinates & Graphs The Constant Equations r = c &  = c Example A. Graph the following polar equations. a. (r = c) The constant equation r = c indicates that “the distance r is c, a fixed constant” and that  may be of any value. b. ( = c)
  • 20. Let’s look at some basic examples of polar graphs. Polar Coordinates & Graphs The Constant Equations r = c &  = c Example A. Graph the following polar equations. a. (r = c) The constant equation r = c indicates that “the distance r is c, a fixed constant” and that  may be of any value. This equation describes the circle of radius c, centered at (0,0). b. ( = c)
  • 21. Let’s look at some basic examples of polar graphs. Polar Coordinates & Graphs The Constant Equations r = c &  = c Example A. Graph the following polar equations. a. (r = c) The constant equation r = c indicates that “the distance r is c, a fixed constant” and that  may be of any value. This equation describes the circle of radius c, centered at (0,0). x y c The constant equation r = c b. ( = c)
  • 22. Let’s look at some basic examples of polar graphs. Polar Coordinates & Graphs The Constant Equations r = c &  = c Example A. Graph the following polar equations. a. (r = c) The constant equation r = c indicates that “the distance r is c, a fixed constant” and that  may be of any value. This equation describes the circle of radius c, centered at (0,0). x y c The constant equation r = c b. ( = c) The constant equation  = c requires that “the directional angle  is c, a fixed constant” and the distance r may be of any value.
  • 23. Let’s look at some basic examples of polar graphs. Polar Coordinates & Graphs The Constant Equations r = c &  = c Example A. Graph the following polar equations. a. (r = c) The constant equation r = c indicates that “the distance r is c, a fixed constant” and that  may be of any value. This equation describes the circle of radius c, centered at (0,0). x y c The constant equation r = c b. ( = c) The constant equation  = c requires that “the directional angle  is c, a fixed constant” and the distance r may be of any value. This equation describes the line with polar angle c.
  • 24. Let’s look at some basic examples of polar graphs. Polar Coordinates & Graphs The Constant Equations r = c &  = c Example A. Graph the following polar equations. a. (r = c) The constant equation r = c indicates that “the distance r is c, a fixed constant” and that  may be of any value. This equation describes the circle of radius c, centered at (0,0). x y c The constant equation r = c b. ( = c) The constant equation  = c requires that “the directional angle  is c, a fixed constant” and the distance r may be of any value. This equation describes the line with polar angle c. x y The constant equation  = c  = c
  • 25. Polar Coordinates & Graphs For the graphs of other polar equations we need to plot points accordingly.
  • 26. Polar Coordinates & Graphs For the graphs of other polar equations we need to plot points accordingly. For this we will use the polar graph paper such as the one shown here which is gridded in terms of the distances and directional angles.
  • 27. Polar Coordinates & Graphs For the graphs of other polar equations we need to plot points accordingly. For this we will use the polar graph paper such as the one shown here which is gridded in terms of the distances and directional angles. Example B. a. Graph r = 3cos().
  • 28. Polar Coordinates & Graphs For the graphs of other polar equations we need to plot points accordingly. For this we will use the polar graph paper such as the one shown here which is gridded in terms of the distances and directional angles. Example B. a. Graph r = 3cos(). r  3 0o 3(3/2) ≈ 2.6 30o 3(2/2) ≈ 2.1 45o 1.5 60o 0 90o Let’s plot the points starting with  going from 0 to 90o.
  • 29. Polar Coordinates & Graphs For the graphs of other polar equations we need to plot points accordingly. For this we will use the polar graph paper such as the one shown here which is gridded in terms of the distances and directional angles. Example B. a. Graph r = 3cos(). r  3 0o 3(3/2) ≈ 2.6 30o 3(2/2) ≈ 2.1 45o 1.5 60o 0 90o Let’s plot the points starting with  going from 0 to 90o.
  • 30. Polar Coordinates & Graphs For the graphs of other polar equations we need to plot points accordingly. For this we will use the polar graph paper such as the one shown here which is gridded in terms of the distances and directional angles. Example B. a. Graph r = 3cos(). r  3 0o 3(3/2) ≈ 2.6 30o 3(2/2) ≈ 2.1 45o 1.5 60o 0 90o Let’s plot the points starting with  going from 0 to 90o.
  • 31. Polar Coordinates & Graphs For the graphs of other polar equations we need to plot points accordingly. For this we will use the polar graph paper such as the one shown here which is gridded in terms of the distances and directional angles. Example B. a. Graph r = 3cos(). r  3 0o 3(3/2) ≈ 2.6 30o 3(2/2) ≈ 2.1 45o 1.5 60o 0 90o Let’s plot the points starting with  going from 0 to 90o.
  • 32. Polar Coordinates & Graphs For the graphs of other polar equations we need to plot points accordingly. For this we will use the polar graph paper such as the one shown here which is gridded in terms of the distances and directional angles. Example B. a. Graph r = 3cos(). r  3 0o 3(3/2) ≈ 2.6 30o 3(2/2) ≈ 2.1 45o 1.5 60o 0 90o Let’s plot the points starting with  going from 0 to 90o.
  • 33. Polar Coordinates & Graphs For the graphs of other polar equations we need to plot points accordingly. For this we will use the polar graph paper such as the one shown here which is gridded in terms of the distances and directional angles. Example B. a. Graph r = 3cos(). r  3 0o 3(3/2) ≈ 2.6 30o 3(2/2) ≈ 2.1 45o 1.5 60o 0 90o Let’s plot the points starting with  going from 0 to 90o. 3
  • 34. Polar Coordinates & Graphs For the graphs of other polar equations we need to plot points accordingly. For this we will use the polar graph paper such as the one shown here which is gridded in terms of the distances and directional angles. Example B. a. Graph r = 3cos(). r  3 0o 3(3/2) ≈ 2.6 30o 3(2/2) ≈ 2.1 45o 1.5 60o 0 90o Let’s plot the points starting with  going from 0 to 90o. 3
  • 35. Polar Coordinates & Graphs For the graphs of other polar equations we need to plot points accordingly. For this we will use the polar graph paper such as the one shown here which is gridded in terms of the distances and directional angles. Example B. a. Graph r = 3cos(). r  3 0o 3(3/2) ≈ 2.6 30o 3(2/2) ≈ 2.1 45o 1.5 60o 0 90o Let’s plot the points starting with  going from 0 to 90o. 3
  • 36. Polar Coordinates & Graphs For the graphs of other polar equations we need to plot points accordingly. For this we will use the polar graph paper such as the one shown here which is gridded in terms of the distances and directional angles. Example B. a. Graph r = 3cos(). r  3 0o 3(3/2) ≈ 2.6 30o 3(2/2) ≈ 2.1 45o 1.5 60o 0 90o Let’s plot the points starting with  going from 0 to 90o. 3
  • 37. Polar Coordinates & Graphs For the graphs of other polar equations we need to plot points accordingly. For this we will use the polar graph paper such as the one shown here which is gridded in terms of the distances and directional angles. Example B. a. Graph r = 3cos(). r  3 0o 3(3/2) ≈ 2.6 30o 3(2/2) ≈ 2.1 45o 1.5 60o 0 90o Let’s plot the points starting with  going from 0 to 90o. 3
  • 38. Polar Coordinates & Graphs For the graphs of other polar equations we need to plot points accordingly. For this we will use the polar graph paper such as the one shown here which is gridded in terms of the distances and directional angles. Example B. a. Graph r = 3cos(). r  3 0o 3(3/2) ≈ 2.6 30o 3(2/2) ≈ 2.1 45o 1.5 60o 0 90o –1.5 120o ≈ –2.1 135o ≈ –2.6 150o –3 180o Let’s plot the points starting with  going from 0 to 90o. 3 Next continue with  from 90o to 180o as shown in the table.
  • 39. Polar Coordinates & Graphs For the graphs of other polar equations we need to plot points accordingly. For this we will use the polar graph paper such as the one shown here which is gridded in terms of the distances and directional angles. Example B. a. Graph r = 3cos(). r  3 0o 3(3/2) ≈ 2.6 30o 3(2/2) ≈ 2.1 45o 1.5 60o 0 90o –1.5 120o ≈ –2.1 135o ≈ –2.6 150o –3 180o Let’s plot the points starting with  going from 0 to 90o. 3 Next continue with  from 90o to 180o as shown in the table.
  • 40. Polar Coordinates & Graphs For the graphs of other polar equations we need to plot points accordingly. For this we will use the polar graph paper such as the one shown here which is gridded in terms of the distances and directional angles. Example B. a. Graph r = 3cos(). r  3 0o 3(3/2) ≈ 2.6 30o 3(2/2) ≈ 2.1 45o 1.5 60o 0 90o –1.5 120o ≈ –2.1 135o ≈ –2.6 150o –3 180o Let’s plot the points starting with  going from 0 to 90o. 3 Next continue with  from 90o to 180o as shown in the table. negative so the points are in the 4th quadrant. Note the r’s are
  • 41. Polar Coordinates & Graphs For the graphs of other polar equations we need to plot points accordingly. For this we will use the polar graph paper such as the one shown here which is gridded in terms of the distances and directional angles. Example B. a. Graph r = 3cos(). r  3 0o 3(3/2) ≈ 2.6 30o 3(2/2) ≈ 2.1 45o 1.5 60o 0 90o –1.5 120o ≈ –2.1 135o ≈ –2.6 150o –3 180o Let’s plot the points starting with  going from 0 to 90o. 3 Next continue with  from 90o to 180o as shown in the table. negative so the points are in the 4th quadrant. Note the r’s are
  • 42. Polar Coordinates & Graphs Continuing with  from 180o to 270o, r  –3 180o ≈ –2.6 210o ≈ –2.1 225o –1.5 240o 0 270o 1.5 300o ≈ 2.1 315o ≈ 2.6 330o 3 360o again r’s are negative, hence the points are located in the 1st quadrant.
  • 43. Polar Coordinates & Graphs Continuing with  from 180o to 270o, r  –3 180o ≈ –2.6 210o ≈ –2.1 225o –1.5 240o 0 270o 1.5 300o ≈ 2.1 315o ≈ 2.6 330o 3 360o again r’s are negative, hence the points are located in the 1st quadrant. In fact, they trace over the same points as  goes from 0o to 90o
  • 44. Polar Coordinates & Graphs Continuing with  from 180o to 270o, r  –3 180o ≈ –2.6 210o ≈ –2.1 225o –1.5 240o 0 270o 1.5 300o ≈ 2.1 315o ≈ 2.6 330o 3 360o again r’s are negative, hence the points are located in the 1st quadrant. 3 In fact, they trace over the same points as  goes from 0o to 90o
  • 45. Polar Coordinates & Graphs Continuing with  from 180o to 270o, r  –3 180o ≈ –2.6 210o ≈ –2.1 225o –1.5 240o 0 270o 1.5 300o ≈ 2.1 315o ≈ 2.6 330o 3 360o again r’s are negative, hence the points are located in the 1st quadrant. 3 In fact, they trace over the Finally as  goes from 270o to 360o we trace over the same points as  goes from 90o to 180o in the 4th quadrant. same points as  goes from 0o to 90o
  • 46. Polar Coordinates & Graphs Continuing with  from 180o to 270o, r  –3 180o ≈ –2.6 210o ≈ –2.1 225o –1.5 240o 0 270o 1.5 300o ≈ 2.1 315o ≈ 2.6 330o 3 360o again r’s are negative, hence the points are located in the 1st quadrant. 3 In fact, they trace over the Finally as  goes from 270o to 360o we trace over the same points as  goes from 90o to 180o in the 4th quadrant. As we will see shortly, these points form a circle and for every period of 180o the graph of r = cos() traverses this circle once. same points as  goes from 0o to 90o
  • 47. Polar Coordinates & Graphs b. Convert r = 3cos() to a rectangular equation. Verify it’s a circle and find the center and radius of this circle. 3
  • 48. Polar Coordinates & Graphs b. Convert r = 3cos() to a rectangular equation. Verify it’s a circle and find the center and radius of this circle. Multiply both sides by r so we have r2 = 3r*cos(). 3
  • 49. Polar Coordinates & Graphs b. Convert r = 3cos() to a rectangular equation. Verify it’s a circle and find the center and radius of this circle. Multiply both sides by r so we have r2 = 3r*cos(). In terms of x and y, it’s x2 + y2 = 3x 3
  • 50. Polar Coordinates & Graphs b. Convert r = 3cos() to a rectangular equation. Verify it’s a circle and find the center and radius of this circle. Multiply both sides by r so we have r2 = 3r*cos(). In terms of x and y, it’s x2 + y2 = 3x x2 – 3x + y2 = 0 3
  • 51. Polar Coordinates & Graphs b. Convert r = 3cos() to a rectangular equation. Verify it’s a circle and find the center and radius of this circle. Multiply both sides by r so we have r2 = 3r*cos(). In terms of x and y, it’s x2 + y2 = 3x x2 – 3x + y2 = 0 completing the square, x2 – 3x + (3/2)2 + y2 = 0 + (3/2)2 3
  • 52. Polar Coordinates & Graphs b. Convert r = 3cos() to a rectangular equation. Verify it’s a circle and find the center and radius of this circle. Multiply both sides by r so we have r2 = 3r*cos(). In terms of x and y, it’s x2 + y2 = 3x x2 – 3x + y2 = 0 completing the square, x2 – 3x + (3/2)2 + y2 = 0 + (3/2)2 (x – 3/2)2 + y2 = (3/2)2 3
  • 53. 3 Polar Coordinates & Graphs b. Convert r = 3cos() to a rectangular equation. Verify it’s a circle and find the center and radius of this circle. Multiply both sides by r so we have r2 = 3r*cos(). In terms of x and y, it’s x2 + y2 = 3x x2 – 3x + y2 = 0 completing the square, x2 – 3x + (3/2)2 + y2 = 0 + (3/2)2 (x – 3/2)2 + y2 = (3/2)2 so the points form the circle centered at (3/2, 0) with radius 3/2.
  • 54. Polar Coordinates & Graphs In general, the polar equations of the form r = ±D*cos() r = ±D*sin() are circles with diameter D and tangent to the x or y axis at the origin. r = ±a*cos() r = ±a*sin() D x y
  • 55. Polar Coordinates & Graphs In general, the polar equations of the form r = ±D*cos() r = ±D*sin() are circles with diameter D and tangent to the x or y axis at the origin. r = ±a*cos() r = ±a*sin() D x y The points (r, ) and (r, –) are the vertical mirror images of each other across the x–axis. x (r, ) (r, –) 1
  • 56. Polar Coordinates & Graphs In general, the polar equations of the form r = ±D*cos() r = ±D*sin() are circles with diameter D and tangent to the x or y axis at the origin. r = ±a*cos() r = ±a*sin() D x y The points (r, ) and (r, –) are the vertical mirror images of each other across the x–axis. So if r = f() = f(–) such as r = cos() = cos(–), then its graph is symmetric with respect to the x–axis, x (r, ) (r, –) 1
  • 57. Polar Coordinates & Graphs In general, the polar equations of the form r = ±D*cos() r = ±D*sin() are circles with diameter D and tangent to the x or y axis at the origin. r = ±a*cos() r = ±a*sin() D x y The points (r, ) and (r, –) are the vertical mirror images of each other across the x–axis. So if r = f() = f(–) such as r = cos() = cos(–), then its graph is symmetric with respect to the x–axis, x (r, ) (r, –) r = cos() = cos(–) 1
  • 58. Polar Coordinates & Graphs In general, the polar equations of the form r = ±D*cos() r = ±D*sin() are circles with diameter D and tangent to the x or y axis at the origin. r = ±a*cos() r = ±a*sin() D x y The points (r, ) and (r, –) are the vertical mirror images of each other across the x–axis. So if r = f() = f(–) such as r = cos() = cos(–), then its graph is symmetric with respect to the x–axis, so r = ±D*cos() are the horizontal circles. x (r, ) (r, –) r = cos() = cos(–) 1
  • 59. Polar Coordinates & Graphs x (r, ) (–r, –) y The points (r, ) and (–r, –) are the mirror images of each other across the y–axis.
  • 60. Polar Coordinates & Graphs x (r, ) r = sin() = –sin(–) (–r, –) y The points (r, ) and (–r, –) are the mirror images of each other across the y–axis. So if r = f(–) = –f() such as r = sin() = –sin(–), then its graph is symmetric to the y–axis and so r = ±D*sin() are the two vertical circles.
  • 61. Polar Coordinates & Graphs x (r, ) r = sin() = –sin(–) (–r, –) y x y r = cos() r = –cos() r = sin() r = –sin() 1 1 Here they are with their orientation starting at  = 0. The points (r, ) and (–r, –) are the mirror images of each other across the y–axis. So if r = f(–) = –f() such as r = sin() = –sin(–), then its graph is symmetric to the y–axis and so r = ±D*sin() are the two vertical circles.
  • 62. Polar Coordinates & Graphs The Cardioids r = c(1 ± cos()) r = c(1 ± sin()) The graphs of the equations of the form are called the cardioids, or the heart shaped curves. Example C. Graph r = 1 – cos(). The graph of r = 1 – cos() is symmetric with respect to the x–axis because cos() = cos(–). Therefore we will plot  from 0o to 180o and take its mirrored image across the x–axis for the complete graph. As  goes from 0o to 180o, cos() goes from 1 to –1, and the expression 1 – cos() goes from 0 to 2. The table is shown below, readers may verify the approximate values of r’s.
  • 63. Polar Coordinates & Graphs The Cardioids r = c(1 ± cos()) r = c(1 ± sin()) The graphs of the equations of the form are called the cardioids, or the heart shaped curves. Example C. Graph r = 1 – cos().
  • 64. Polar Coordinates & Graphs The Cardioids r = c(1 ± cos()) r = c(1 ± sin()) The graphs of the equations of the form are called the cardioids, or the heart shaped curves. Example C. Graph r = 1 – cos(). The graph of r = 1 – cos() is symmetric with respect to the x–axis because cos() = cos(–).
  • 65. Polar Coordinates & Graphs The Cardioids r = c(1 ± cos()) r = c(1 ± sin()) The graphs of the equations of the form are called the cardioids, or the heart shaped curves. Example C. Graph r = 1 – cos(). The graph of r = 1 – cos() is symmetric with respect to the x–axis because cos() = cos(–). Therefore we will plot  from 0o to 180o and take its mirrored image across the x–axis for the complete graph.
  • 66. Polar Coordinates & Graphs The Cardioids r = c(1 ± cos()) r = c(1 ± sin()) The graphs of the equations of the form are called the cardioids, or the heart shaped curves. Example C. Graph r = 1 – cos(). The graph of r = 1 – cos() is symmetric with respect to the x–axis because cos() = cos(–). Therefore we will plot  from 0o to 180o and take its mirrored image across the x–axis for the complete graph. As  goes from 0o to 180o, cos() goes from 1 to –1, and the expression 1 – cos() goes from 0 to 2.
  • 67. Polar Coordinates & Graphs The Cardioids r = c(1 ± cos()) r = c(1 ± sin()) The graphs of the equations of the form are called the cardioids, or the heart shaped curves. Example C. Graph r = 1 – cos(). The graph of r = 1 – cos() is symmetric with respect to the x–axis because cos() = cos(–). Therefore we will plot  from 0o to 180o and take its mirrored image across the x–axis for the complete graph. As  goes from 0o to 180o, cos() goes from 1 to –1, and the expression 1 – cos() goes from 0 to 2. The table is shown below, readers may verify the approximate values of r’s.
  • 68. r=1–cos()  0 0o ≈ 0.13 30o ≈ 0.29 45o 0.5 60o 1 90o 1.5 120o ≈ 1.71 135o ≈ 1.87 150o 2 180o Polar Coordinates & Graphs x 2
  • 69. r=1–cos()  0 0o ≈ 0.13 30o ≈ 0.29 45o 0.5 60o 1 90o 1.5 120o ≈ 1.71 135o ≈ 1.87 150o 2 180o Polar Coordinates & Graphs x 2
  • 70. r=1–cos()  0 0o ≈ 0.13 30o ≈ 0.29 45o 0.5 60o 1 90o 1.5 120o ≈ 1.71 135o ≈ 1.87 150o 2 180o Polar Coordinates & Graphs x 2
  • 71. Polar Coordinates & Graphs r=1–cos()  0 0o ≈ 0.13 30o ≈ 0.29 45o 0.5 60o 1 90o 1.5 120o ≈ 1.71 135o ≈ 1.87 150o 2 180o x 2
  • 72. Polar Coordinates & Graphs r=1–cos()  0 0o ≈ 0.13 30o ≈ 0.29 45o 0.5 60o 1 90o 1.5 120o ≈ 1.71 135o ≈ 1.87 150o 2 180o Reflecting across the x–axis, we have the cardioid. x 2
  • 73. Polar Coordinates & Graphs r=1–cos()  0 0o ≈ 0.13 30o ≈ 0.29 45o 0.5 60o 1 90o 1.5 120o ≈ 1.71 135o ≈ 1.87 150o 2 180o x 2 Reflecting across the x–axis, we have the cardioid.
  • 74. Polar Coordinates & Graphs The cardioid is the track of a point on a circle as it r=1–cos()  0 0o ≈ 0.13 30o ≈ 0.29 45o 0.5 60o 1 90o 1.5 120o ≈ 1.71 135o ≈ 1.87 150o 2 180o x 2 Reflecting across the x–axis, we have the cardioid. revolves around another circle of the same size.
  • 75. Polar Coordinates & Graphs The cardioid is the track of a point on a circle as it r=1–cos()  0 0o ≈ 0.13 30o ≈ 0.29 45o 0.5 60o 1 90o 1.5 120o ≈ 1.71 135o ≈ 1.87 150o 2 180o x 2 Reflecting across the x–axis, we have the cardioid. revolves around another circle of the same size.
  • 76. Polar Coordinates & Graphs The cardioid is the track of a point on a circle as it r=1–cos()  0 0o ≈ 0.13 30o ≈ 0.29 45o 0.5 60o 1 90o 1.5 120o ≈ 1.71 135o ≈ 1.87 150o 2 180o x 2 Reflecting across the x–axis, we have the cardioid. revolves around another circle of the same size.
  • 77. Polar Coordinates & Graphs The cardioid is the track of a point on a circle as it r=1–cos()  0 0o ≈ 0.13 30o ≈ 0.29 45o 0.5 60o 1 90o 1.5 120o ≈ 1.71 135o ≈ 1.87 150o 2 180o x 2 Reflecting across the x–axis, we have the cardioid. revolves around another circle of the same size.
  • 78. Polar Coordinates & Graphs The cardioid is the track of a point on a circle as it r=1–cos()  0 0o ≈ 0.13 30o ≈ 0.29 45o 0.5 60o 1 90o 1.5 120o ≈ 1.71 135o ≈ 1.87 150o 2 180o x 2 Reflecting across the x–axis, we have the cardioid. revolves around another circle of the same size.
  • 79. Polar Coordinates & Graphs A cardioid is also the outline or the envelope of a series of circles that pass through some fixed point o
  • 80. Polar Coordinates & Graphs o A cardioid is also the outline or the envelope of a series of circles that pass through some fixed point o
  • 81. Polar Coordinates & Graphs o A cardioid is also the outline or the envelope of a series of circles that pass through some fixed point o whose centers sit on another circle K that contains o,
  • 82. Polar Coordinates & Graphs o A cardioid is also the outline or the envelope of a series of circles that pass through some fixed point o whose centers sit on another circle K that contains o, as shown. K
  • 83. Polar Coordinates & Graphs o A cardioid is also the outline or the envelope of a series of circles that pass through some fixed point o whose centers sit on another circle K that contains o, as shown. K
  • 84. Polar Coordinates & Graphs o A cardioid is also the outline or the envelope of a series of circles that pass through some fixed point o whose centers sit on another circle K that contains o, as shown. K
  • 85. Polar Coordinates & Graphs o A cardioid is also the outline or the envelope of a series of circles that pass through some fixed point o whose centers sit on another circle K that contains o, as shown. K
  • 86. Polar Coordinates & Graphs o A cardioid is also the outline or the envelope of a series of circles that pass through some fixed point o whose centers sit on another circle K that contains o, as shown. K
  • 87. Polar Coordinates & Graphs o A cardioid is also the outline or the envelope of a series of circles that pass through some fixed point o whose centers sit on another circle K that contains o, as shown. K
  • 88. Polar Coordinates & Graphs o A cardioid is also the outline or the envelope of a series of circles that pass through some fixed point o whose centers sit on another circle K that contains o, as shown. K
  • 89. Polar Coordinates & Graphs o cases of polar equations of the form r = a ± b*cos() and r = a ± b*sin(). K A cardioid is also the outline or the envelope of a series of circles that pass through some fixed point o whose centers sit on another circle K that contains o, as shown. Cardioids are special
  • 90. Polar Coordinates & Graphs o cases of polar equations of the form r = a ± b*cos() and r = a ± b*sin(). K A cardioid is also the outline or the envelope of a series of circles that pass through some fixed point o whose centers sit on another circle K that contains o, as shown. Cardioids are special We summarize the graphs of these equations below.
  • 91. Polar Coordinates & Graphs o cases of polar equations of the form r = a ± b*cos() and r = a ± b*sin(). K A cardioid is also the outline or the envelope of a series of circles that pass through some fixed point o whose centers sit on another circle K that contains o, as shown. Cardioids are special We summarize the graphs of these equations below. The graphs of r = a ± b*sin() are rotations of the graphs of r = a ± b*cos() = a(1 ± k*cos()) where k is a constant.
  • 92. Polar Coordinates & Graphs o cases of polar equations of the form r = a ± b*cos() and r = a ± b*sin(). K A cardioid is also the outline or the envelope of a series of circles that pass through some fixed point o whose centers sit on another circle K that contains o, as shown. Cardioids are special We summarize the graphs of these equations below. The graphs of r = a ± b*sin() are rotations of the graphs of r = a ± b*cos() = a(1 ± k*cos()) where k is a constant. Regarding the “a” as a scalar, we reduce to examining the graphs of the polar equations of the form r = 1 ± k*cos().
  • 93. Polar Coordinates & Graphs The graph of a polar equation of the form r = 1 ± k*cos() depends on the value of |k|.
  • 94. Polar Coordinates & Graphs The graph of a polar equation of the form r = 1 ± k*cos() depends on the value of |k|. We may classify the graphs r = 1 – k*cos() where k is a positive number into three types.
  • 95. Polar Coordinates & Graphs The graph of a polar equation of the form r = 1 ± k*cos() depends on the value of |k|. We may classify the graphs r = 1 – k*cos() where k is a positive number into three types. For k = 1, or r = 1 – cos(), we get a cardioid. r = 1 – cos() k = 1
  • 96. Polar Coordinates & Graphs The graph of a polar equation of the form r = 1 ± k*cos() depends on the value of |k|. We may classify the graphs r = 1 – k*cos() where k is a positive number into three types. For k = 1, or r = 1 – cos(), we get a cardioid. For k < 1, e.g. r = 1 – ½ *cos(), we have r > 0 for all ’s. r = 1 – cos() k = 1
  • 97. Polar Coordinates & Graphs The graph of a polar equation of the form r = 1 ± k*cos() depends on the value of |k|. We may classify the graphs r = 1 – k*cos() where k is a positive number into three types. For k = 1, or r = 1 – cos(), we get a cardioid. For k < 1, e.g. r = 1 – ½ *cos(), we have r > 0 for all ’s. This means the graph does not pass through the origin. r = 1 – cos() k = 1
  • 98. Polar Coordinates & Graphs The graph of a polar equation of the form r = 1 ± k*cos() depends on the value of |k|. We may classify the graphs r = 1 – k*cos() where k is a positive number into three types. For k = 1, or r = 1 – cos(), we get a cardioid. r = 1 – k *cos() 0 < k < 1 r = 1 – cos() k = 1 For k < 1, e.g. r = 1 – ½ *cos(), we have r > 0 for all ’s. This means the graph does not pass through the origin. Instead, the cusp, i.e. the pinched point at the origin of the cardioid is pushed out as shown.
  • 99. Polar Coordinates & Graphs For k > 1, e.g. r = 1 – 2cos(), we have r = –1 < 0 for  = 0.
  • 100. Polar Coordinates & Graphs For k > 1, e.g. r = 1 – 2cos(), we have r = –1 < 0 for  = 0. In fact, as  goes from 0 to π/3, r goes from –1 to 0,
  • 101. Polar Coordinates & Graphs For k > 1, e.g. r = 1 – 2cos(), we have r = –1 < 0 for  = 0. In fact, as  goes from 0 to π/3, r goes from –1 to 0, and the corresponding points traverse from (–1, 0) to (0, π/3) as shown. x r = 1 – 2cos() (–1, 0) (0, π/3)
  • 102. Polar Coordinates & Graphs For k > 1, e.g. r = 1 – 2cos(), we have r = –1 < 0 for  = 0. In fact, as  goes from 0 to π/3, r goes from –1 to 0, and the corresponding points traverse from (–1, 0) to (0, π/3) as shown. As  goes from π/3 to π/2, r increases from 0 to 1, so the points traverse from (0, π/3 ) to (1, π/2). x r = 1 – 2cos() (–1, 0) (0, π/3)
  • 103. Polar Coordinates & Graphs For k > 1, e.g. r = 1 – 2cos(), we have r = –1 < 0 for  = 0. In fact, as  goes from 0 to π/3, r goes from –1 to 0, and the corresponding points traverse from (–1, 0) to (0, π/3) as shown. As  goes from π/3 to π/2, r increases from 0 to 1, x r = 1 – 2cos() (0, π/3) (–1, 0) (1, π/2) (3, π) so the points traverse from (0, π/3 ) to (1, π/2).
  • 104. Polar Coordinates & Graphs For k > 1, e.g. r = 1 – 2cos(), we have r = –1 < 0 for  = 0. In fact, as  goes from 0 to π/3, r goes from –1 to 0, and the corresponding points traverse from (–1, 0) to (0, π/3) as shown. As  goes from π/3 to π/2, r increases from 0 to 1, r increases from 1 to 3, and the points traverse from (1, π/2) to (3, π). x r = 1 – 2cos() (0, π/3) (–1, 0) (1, π/2) (3, π) so the points traverse from (0, π/3 ) to (1, π/2). As  from π/2 to π,
  • 105. Polar Coordinates & Graphs For k > 1, e.g. r = 1 – 2cos(), we have r = –1 < 0 for  = 0. In fact, as  goes from 0 to π/3, r goes from –1 to 0, and the corresponding points traverse from (–1, 0) to (0, π/3) as shown. As  goes from π/3 to π/2, r increases from 0 to 1, r increases from 1 to 3, and the points traverse from (1, π/2) to (3, π). For 1 < k, r = 1 – k*cos() has an inner loop. x r = 1 – 2cos() (0, π/3) (–1, 0) (1, π/2) (3, π) so the points traverse from (0, π/3 ) to (1, π/2). As  from π/2 to π,
  • 106. Polar Coordinates & Graphs For k > 1, e.g. r = 1 – 2cos(), we have r = –1 < 0 for  = 0. In fact, as  goes from 0 to π/3, r goes from –1 to 0, and the corresponding points traverse from (–1, 0) to (0, π/3) as shown. As  goes from π/3 to π/2, r increases from 0 to 1, r increases from 1 to 3, and the points traverse from (1, π/2) to (3, π). Finally since cos() = cos(–), we obtain the entire graph by taking its reflection across the x–axis. For 1 < k, r = 1 – k*cos() has an inner loop. x r = 1 – 2cos() (0, π/3) (–1, 0) (1, π/2) (3, π) so the points traverse from (0, π/3 ) to (1, π/2). As  from π/2 to π,
  • 107. Polar Coordinates & Graphs For k > 1, e.g. r = 1 – 2cos(), we have r = –1 < 0 for  = 0. In fact, as  goes from 0 to π/3, r goes from –1 to 0, and the corresponding points traverse from (–1, 0) to (0, π/3) as shown. As  goes from π/3 to π/2, r increases from 0 to 1, so the points traverse from (0, π/3 ) to (1, π/2). As  from π/2 to π, r increases from 1 to 3, and the points traverse from (1, π/2) to (3, π). Finally since cos() = cos(–), we obtain the entire graph by taking its reflection across the x–axis. Note that we have an inner loop if k > 1. For 1 < k, r = 1 – k*cos() has an inner loop. x r = 1 – 2cos() (0, π/3) (–1, 0) (1, π/2) (3, π)
  • 108. Polar Coordinates & Graphs Here is a sequence of graphs for r = 1 – kcos(). r = 1 – (1/4)cos()
  • 109. Polar Coordinates & Graphs Here is a sequence of graphs for r = 1 – kcos(). r = 1 – (1/4)cos() r = 1 – (1/2)cos()
  • 110. Polar Coordinates & Graphs Here is a sequence of graphs for r = 1 – kcos(). r = 1 – (1/4)cos() r = 1 – (1/2)cos() r = 1 – 1cos()
  • 111. Polar Coordinates & Graphs Here is a sequence of graphs for r = 1 – kcos(). r = 1 – (1/4)cos() r = 1 – (1/2)cos() r = 1 – 1cos() r = 1 – 2cos()
  • 112. Polar Coordinates & Graphs Here is a sequence of graphs for r = 1 – kcos(). r = 1 – (1/4)cos() r = 1 – (1/2)cos() r = 1 – 1cos() r = 1 – 2cos() r = 1 – 4cos()
  • 113. Polar Coordinates & Graphs Here is a sequence of graphs for r = 1 – kcos(). r = 1 – (1/4)cos() r = 1 – (1/2)cos() r = 1 – 1cos() r = 1 – 2cos() r = 1 – 4cos() Polar equations of the forms r = sin(n) or r = cos(n), where n is a positive integer, form floral shape petals that mathematicians call “roses”. The Roses
  • 114. Polar Coordinates & Graphs Here is a sequence of graphs for r = 1 – kcos(). r = 1 – (1/4)cos() r = 1 – (1/2)cos() r = 1 – 1cos() r = 1 – 2cos() r = 1 – 4cos() Polar equations of the forms r = sin(n) or r = cos(n), where n is a positive integer, form floral shape petals that mathematicians call “roses”. The Roses
  • 115. Polar Coordinates & Graphs Here is a sequence of graphs for r = 1 – kcos(). r = 1 – (1/4)cos() r = 1 – (1/2)cos() r = 1 – 1cos() r = 1 – 2cos() r = 1 – 4cos() Polar equations of the forms r = sin(n) or r = cos(n), where n is a positive integer, form floral shape petals that mathematicians call “roses”. Recall that for n = 1, r = cos() consists of two overlapping circles, i.e. the graph traverses the circle twice as  goes from 0 to 2π. The Roses
  • 116. Polar Coordinates & Graphs Here is a sequence of graphs for r = 1 – kcos(). r = 1 – (1/4)cos() r = 1 – (1/2)cos() r = 1 – 1cos() r = 1 – 2cos() r = 1 – 4cos() Polar equations of the forms r = sin(n) or r = cos(n), where n is a positive integer, form floral shape petals that mathematicians call “roses”. Recall that for n = 1, r = cos() consists of two overlapping circles, i.e. the graph traverses the circle twice as  goes from 0 to 2π. This is different from the cases when n is even where the graph consists of 2n petals. The Roses
  • 117. Polar Coordinates & Graphs r = cos(1) r = cos(3) If n is odd, the graph of r = cos(n) consists of n petals as  goes from 0 to π, r = cos(7) r = cos(5)
  • 118. Polar Coordinates & Graphs r = cos(1) r = cos(3) If n is odd, the graph of r = cos(n) consists of n petals as  goes from 0 to π, then the graph follows the same path as  goes from π to 2π. r = cos(7) r = cos(5)
  • 119. Polar Coordinates & Graphs r = cos(1) r = cos(3) If n is odd, the graph of r = cos(n) consists of n petals as  goes from 0 to π, then the graph follows the same path as  goes from π to 2π. If n is even, the graph of r = cos(n) traces out 2n petals as  goes from 0 to 2π. r = cos(7) r = cos(5)
  • 120. Polar Coordinates & Graphs r = cos(1) r = cos(3) If n is odd, the graph of r = cos(n) consists of n petals as  goes from 0 to π, then the graph follows the same path as  goes from π to 2π. r = cos(2) r = cos(4) r = cos(6) r = cos(8) If n is even, the graph of r = cos(n) traces out 2n petals as  goes from 0 to 2π. r = cos(7) r = cos(5)
  • 121. Polar Coordinates & Graphs Following is a brief argument for the differences in the graphs of r = sin(n) depending on n is even or odd.
  • 122. Polar Coordinates & Graphs Following is a brief argument for the differences in the graphs of r = sin(n) depending on n is even or odd. Let’s look at the graph of r = | sin(3) |.
  • 123. Polar Coordinates & Graphs Following is a brief argument for the differences in the graphs of r = sin(n) depending on n is even or odd. Let’s look at the graph of r = | sin(3) |. For 0 ≤  < 2π, we have that 0 ≤ 3 < 6π.
  • 124. Polar Coordinates & Graphs Following is a brief argument for the differences in the graphs of r = sin(n) depending on n is even or odd. Let’s look at the graph of r = | sin(3) |. For 0 ≤  < 2π, we have that 0 ≤ 3 < 6π. If 3 = 0, π, 2π, 3π, 4π, 5π, then r = sin(3) = 0, or r = 0 when  = 0, π/3, 2π/3, π, 4π/3, 5π/3 π/3 2π/3 The graph of r = | sin(3) | 0
  • 125. Polar Coordinates & Graphs Following is a brief argument for the differences in the graphs of r = sin(n) depending on n is even or odd. Let’s look at the graph of r = | sin(3) |. For 0 ≤  < 2π, we have that 0 ≤ 3 < 6π. If 3 = 0, π, 2π, 3π, 4π, 5π, then r = sin(3) = 0, or r = 0 when  = 0, π/3, 2π/3, π, 4π/3, 5π/3. Similarly, r = 1 when  = π/6, π/2, 5π/6, 7π/6, 3π/2, 11π/6. π/3 2π/3 The graph of r = | sin(3) | 0
  • 126. Polar Coordinates & Graphs Following is a brief argument for the differences in the graphs of r = sin(n) depending on n is even or odd. As  goes from 0 to π/6 to π/3, r goes from 0 to 1 back to 0. Let’s look at the graph of r = | sin(3) |. For 0 ≤  < 2π, we have that 0 ≤ 3 < 6π. If 3 = 0, π, 2π, 3π, 4π, 5π, then r = sin(3) = 0, or r = 0 when  = 0, π/3, 2π/3, π, 4π/3, 5π/3. Similarly, r = 1 when  = π/6, π/2, 5π/6, 7π/6, 3π/2, 11π/6. π/3 2π/3 The graph of r = | sin(3) | 0
  • 127. Polar Coordinates & Graphs Following is a brief argument for the differences in the graphs of r = sin(n) depending on n is even or odd. (1, π/6) π/3 The graph of r = | sin(3) | 0 Let’s look at the graph of r = | sin(3) |. For 0 ≤  < 2π, we have that 0 ≤ 3 < 6π. If 3 = 0, π, 2π, 3π, 4π, 5π, then r = sin(3) = 0, or r = 0 when  = 0, π/3, 2π/3, π, 4π/3, 5π/3. Similarly, r = 1 when  = π/6, π/2, 5π/6, 7π/6, 3π/2, 11π/6. 2π/3 As  goes from 0 to π/6 to π/3, r goes from 0 to 1 back to 0. So the graph starts at the origin and makes a petal (loop), to a tip of distance 1 from the origin, back to the origin in a period of π/3.
  • 128. Polar Coordinates & Graphs Following is a brief argument for the differences in the graphs of r = sin(n) depending on n is even or odd. (1, π/6) As  goes from 0 to π/6 to π/3, r goes from 0 to 1 back to 0. So the graph starts at the origin and makes a petal (loop), to a tip of distance 1 from the origin, back to the origin in a period of π/3. Repeat this every π/3, we get 6 petals for r = | sin(3) |. π/3 2π/3 The graph of r = | sin(3) | 0 Let’s look at the graph of r = | sin(3) |. For 0 ≤  < 2π, we have that 0 ≤ 3 < 6π. If 3 = 0, π, 2π, 3π, 4π, 5π, then r = sin(3) = 0, or r = 0 when  = 0, π/3, 2π/3, π, 4π/3, 5π/3. Similarly, r = 1 when  = π/6, π/2, 5π/6, 7π/6, 3π/2, 11π/6.
  • 129. Polar Coordinates & Graphs Let’s now consider the signs of r = sin(3) as shown. below. 0 π/3 2π/3 0 π/3 2π/3 + + + – – – The signs of r = sin(3) The graph of r = | sin(3) | (1, π/6)
  • 130. Polar Coordinates & Graphs Let’s now consider the signs of r = sin(3) as shown. below. 0 π/3 2π/3 0 π/3 2π/3 + + + – – – The signs of r = sin(3) Note the difference in the signs of opposite segments. The graph of r = | sin(3) | (1, π/6)
  • 131. Polar Coordinates & Graphs Let’s now consider the signs of r = sin(3) as shown. below. 0 π/3 2π/3 π/3 2π/3 + + + – – – The signs of r = sin(3) Note the difference in the signs of opposite segments. Hence the “negative petals” flip across the origin in the graph of r = sin(3) as shown. The graph of r = | sin(3) | (1, π/6) 0
  • 132. Polar Coordinates & Graphs Let’s now consider the signs of r = sin(3) as shown. below. 0 π/3 2π/3 0 π/3 2π/3 0 π/3 2π/3 + + + – – – The signs of r = sin(3) Note the difference in the signs of opposite segments. Hence the “negative petals” flip across the origin in the graph of r = sin(3) as shown. The graph of r = sin(3) The graph of r = | sin(3) | – – – (1, π/6) (1, π/6) = (–1, 7π/6)
  • 133. Polar Coordinates & Graphs Let’s now consider the signs of r = sin(3) as shown. below. 0 π/3 2π/3 0 π/3 2π/3 0 π/3 2π/3 + + + – – – The signs of r = sin(3) Note the difference in the signs of opposite segments. Hence the “negative petals” flip across the origin in the graph of r = sin(3) as shown. This is true in general when n is odd, that the graph of r = sin(n) consists of n petals because the “negative petals” fold into the opposite positive ones The graph of r = sin(3) The graph of r = | sin(3) | – – – (1, π/6) (1, π/6) = (–1, 7π/6)
  • 134. Polar Coordinates & Graphs Let’s now consider the signs of r = sin(3) as shown. below. 0 π/3 2π/3 0 π/3 2π/3 0 π/3 2π/3 + + + – – – The signs of r = sin(3) Note the difference in the signs of opposite segments. Hence the “negative petals” flip across the origin in the graph of r = sin(3) as shown. This is true in general when n is odd, that the graph of r = sin(n) consists of n petals because the “negative petals” fold into the opposite positive ones and the graph traverses each petal twice as  goes from 0 to 2π. The graph of r = sin(3) The graph of r = | sin(3) | – – – (1, π/6) (1, π/6) = (–1, 7π/6)
  • 135. Example C. Sketch the graph r = sin(5). Polar Coordinates & Graphs
  • 136. Example C. Sketch the graph r = sin(5). The graph r = sin(5) consists of 5 petals sitting evenly in 10 wedges each having a radial angle of π/5. Polar Coordinates & Graphs
  • 137. Example C. Sketch the graph r = sin(5). The graph r = sin(5) consists of 5 petals sitting evenly in 10 wedges each having a radial angle of π/5. 0 Polar Coordinates & Graphs 2π/5 π/5 r = sin(5)
  • 138. (1, π/10) = (–1, 11π/10) Example C. Sketch the graph r = sin(5). The graph r = sin(5) consists of 5 petals sitting evenly in 10 wedges each having a radial angle of π/5. 0 Polar Coordinates & Graphs 2π/5 π/5 r = sin(5)
  • 139. The graph r = sin(5) consists of 5 petals sitting evenly in 10 wedges each having a radial angle of π/5. Polar Coordinates & Graphs (1, π/10) = (–1, 11π/10) 0 2π/5 π/5 Example C. Sketch the graph r = sin(5). + – + – + + + – – – r = sin(5)
  • 140. The graph r = sin(5) consists of 5 petals sitting evenly in 10 wedges each having a radial angle of π/5. Polar Coordinates & Graphs (1, π/10) = (–1, 11π/10) 0 2π/5 π/5 Example C. Sketch the graph r = sin(5). + – + – + + + – – – r = sin(5) In general if n is odd, r = sin(n) has n petals from 0 to 2π.
  • 141. The graph r = sin(5) consists of 5 petals sitting evenly in 10 wedges each having a radial angle of π/5. Polar Coordinates & Graphs π/4 + – + – + – – + (1, π/10) = (–1, 11π/10) 0 2π/5 π/5 Example C. Sketch the graph r = sin(5). + – + – + + + – – – r = sin(5) In general if n is odd, r = sin(n) has n petals from 0 to 2π. If n is even, e.g. r = sin(4), then its signs are distributed as shown, i.e. two opposite wedges have the same sign r = sin(4)
  • 142. The graph r = sin(5) consists of 5 petals sitting evenly in 10 wedges each having a radial angle of π/5. Polar Coordinates & Graphs r = sin(4) π/4 + – + – + – – + If n is even, e.g. r = sin(4), then its signs are distributed as shown, i.e. two opposite wedges have the same sign so the graph of r = sin(4) retains all eight petals. (1, π/10) = (–1, 11π/10) 0 2π/5 π/5 Example C. Sketch the graph r = sin(5). + – + – + + + – – – r = sin(5) In general if n is odd, r = sin(n) has n petals from 0 to 2π.
  • 143. The graph r = sin(5) consists of 5 petals sitting evenly in 10 wedges each having a radial angle of π/5. Polar Coordinates & Graphs r = sin(4) π/4 + – + – + – – + If n is even, e.g. r = sin(4), then its signs are distributed as shown, i.e. two opposite wedges have the same sign so the graph of r = sin(4) retains all eight petals. In general if n is even, r = sin(n) has 2n petals. (1, π/10) = (–1, 11π/10) 0 2π/5 π/5 Example C. Sketch the graph r = sin(5). + – + – + + + – – – r = sin(5) In general if n is odd, r = sin(n) has n petals from 0 to 2π.
  • 144. Polar Equations Spirals A spiral is the graph of r = f() where f() is increasing or decreasing.
  • 145. Polar Equations Spirals A spiral is the graph of r = f() where f() is increasing or decreasing. Example D. a. Graph r =  where  ≥ 0.
  • 146. Polar Equations Spirals A spiral is the graph of r = f() where f() is increasing or decreasing. Example D. a. Graph r =  where  ≥ 0. The polar equation states that the distance r is the same as .
  • 147. Polar Equations x r =  Spirals A spiral is the graph of r = f() where f() is increasing or decreasing. Example D. a. Graph r =  where  ≥ 0. The polar equation states that the distance r is the same as . Starting at (0, 0), as  increases, r increases, so the points are circling outward from the origin at a steady rate.
  • 148. Polar Equations A uniformly banded spiral such as this one is called an Archimedean spiral. x The Archimedean Spiral r =  Spirals A spiral is the graph of r = f() where f() is increasing or decreasing. Example D. a. Graph r =  where  ≥ 0. The polar equation states that the distance r is the same as . Starting at (0, 0), as  increases, r increases, so the points are circling outward from the origin at a steady rate.
  • 149. Polar Equations A uniformly banded spiral such as this one is called an Archimedean spiral. x The Archimedean Spiral r =  Spirals A spiral is the graph of r = f() where f() is increasing or decreasing. Example D. a. Graph r =  where  ≥ 0. The polar equation states that the distance r is the same as . Starting at (0, 0), as  increases, r increases, so the points are circling outward from the origin at a steady rate. b. Convert the polar equation r =  into a rectangular equation by using the cosine inverse to express .
  • 150. Polar Equations We will use the cosine inverse function to express  in x&y, x r =  x
  • 151. Polar Equations We will use the cosine inverse function to express  in x&y, i.e.  = cos–1(x/r) = cos–1(x/√x2 + y2 ). x r =  x
  • 152. Polar Equations We have the equation that We will use the cosine inverse function to express  in x&y, i.e.  = cos–1(x/r) = cos–1(x/√x2 + y2 ). cos–1(x/√x2 + y2) = √x2 + y2 ( = r ) x r =  x
  • 153. Polar Equations We have the equation that We will use the cosine inverse function to express  in x&y, i.e.  = cos–1(x/r) = cos–1(x/√x2 + y2 ). cos–1(x/√x2 + y2) = √x2 + y2 ( = r ) x r =  This rectangular equation only gives the part of the spiral where 0 < √x2 + y2 ≤ π (why?) x
  • 154. Polar Equations We have the equation that We will use the cosine inverse function to express  in x&y, i.e.  = cos–1(x/r) = cos–1(x/√x2 + y2 ). cos–1(x/√x2 + y2) = √x2 + y2 ( = r ) x r =  This rectangular equation only gives the part of the spiral where 0 < √x2 + y2 ≤ π (why?) cos–1(x/√x2 + y2) = √x2 + y2 x x The “Lost in Translation” from the polar to the rectangular equation
  • 155. Polar Equations We have the equation that We will use the cosine inverse function to express  in x&y, i.e.  = cos–1(x/r) = cos–1(x/√x2 + y2 ). cos–1(x/√x2 + y2) = √x2 + y2 ( = r ) x r =  This rectangular equation only gives the part of the spiral where 0 < √x2 + y2 ≤ π (why?) For other parts of the spirals, we add nπ to  with n = 1,2,.. cos–1(x/√x2 + y2) = √x2 + y2 x x The “Lost in Translation” from the polar to the rectangular equation
  • 156. Polar Equations We have the equation that We will use the cosine inverse function to express  in x&y, i.e.  = cos–1(x/r) = cos–1(x/√x2 + y2 ). cos–1(x/√x2 + y2) = √x2 + y2 ( = r ) x r =  This rectangular equation only gives the part of the spiral where 0 < √x2 + y2 ≤ π (why?) cos–1(x/√x2 + y2) = √x2 + y2 x x The “Lost in Translation” from the polar to the rectangular equation For other parts of the spirals, we add nπ to  with n = 1,2,.. to obtain more distant segments, so cos–1(x/√x2 + y2) + nπ = √x2 + y2.
  • 157. Polar Equations We have the equation that We will use the cosine inverse function to express  in x&y, i.e.  = cos–1(x/r) = cos–1(x/√x2 + y2 ). cos–1(x/√x2 + y2) = √x2 + y2 ( = r ) x r =  This rectangular equation only gives the part of the spiral where 0 < √x2 + y2 ≤ π (why?) cos–1(x/√x2 + y2) = √x2 + y2 x x The “Lost in Translation” from the polar to the rectangular equation This shows the advantages of the polar system in certain settings. cos–1(x/√x2 + y2) + nπ = √x2 + y2. For other parts of the spirals, we add nπ to  with n = 1,2,.. to obtain more distant segments, so
  • 158. Polar Coordinates & Graphs The Log or Equiangular Spirals
  • 159. Polar Coordinates & Graphs The Log or Equiangular Spirals The spirals r = aeb where a, b are constants are called logarithmic spirals.
  • 160. Polar Coordinates & Graphs The Log or Equiangular Spirals The spirals r = aeb where a, b are constants are called logarithmic spirals. The log–spirals, named after the log–form  = β*ln(r) of the equation r = eα, are also known as the equiangular spirals.
  • 161. Polar Coordinates & Graphs The Log or Equiangular Spirals The spirals r = aeb where a, b are constants are called logarithmic spirals. r = e0.15 r = e0.75 r = e0.35 The log–spirals, named after the log–form  = β*ln(r) of the equation r = eα, are also known as the equiangular spirals. Here are some examples of log–spirals.
  • 162. Polar Coordinates & Graphs The Log or Equiangular Spirals The spirals r = aeb where a, b are constants are called logarithmic spirals. r = e0.15 r = e0.75 r = e0.35 The log–spirals, named after the log–form  = β*ln(r) of the equation r = eα, are also known as the equiangular spirals. Here are some examples of log–spirals. Log–spirals are also called equiangular spirals because of its geometric characteristic.
  • 163. Polar Coordinates & Graphs The geometric significance of an equiangular spiral is that the angle between the tangent line and the radial line at any point on the spiral is a fixed constant.
  • 164. Polar Coordinates & Graphs k The geometric significance of an equiangular spiral is that the angle between the tangent line and the radial line at any point on the spiral is a fixed constant. Equiangular spirals
  • 165. Polar Coordinates & Graphs k k The geometric significance of an equiangular spiral is that the angle between the tangent line and the radial line at any point on the spiral is a fixed constant. Equiangular spirals
  • 166. Polar Coordinates & Graphs k k q The geometric significance of an equiangular spiral is that the angle between the tangent line and the radial line at any point on the spiral is a fixed constant. Equiangular spirals
  • 167. Polar Coordinates & Graphs q k k q The geometric significance of an equiangular spiral is that the angle between the tangent line and the radial line at any point on the spiral is a fixed constant. Equiangular spirals
  • 168. Polar Coordinates & Graphs q k k q Equiangular spirals The geometric significance of an equiangular spiral is that the angle between the tangent line and the radial line at any point on the spiral is a fixed constant. If the curve spirals outward, the tangential angle must be more than π/2
  • 169. Polar Coordinates & Graphs q k k q Equiangular spirals The geometric significance of an equiangular spiral is that the angle between the tangent line and the radial line at any point on the spiral is a fixed constant. If the curve spirals outward, the tangential angle must be more than π/2. If the tangential angle is π/2, the spiral contracts into a circle.
  • 170. Polar Coordinates & Graphs q k k q Equiangular spirals The geometric significance of an equiangular spiral is that the angle between the tangent line and the radial line at any point on the spiral is a fixed constant. If the curve spirals outward, the tangential angle must be more than π/2. If the tangential angle is π/2, the spiral contracts into a circle. If the tangential angle is less than π/2, then it’s spiraling inward toward (0,0).
  • 171. Polar Coordinates & Graphs Equiangular spirals occur in nature frequently. http://en.wikipedia. org/wiki/Logarithmi c_spiral
  • 172. Polar Coordinates & Graphs Equiangular spirals occur in nature frequently. In many biological growth processes, the new growth is extruded at a fixed angle from the existing structure, http://en.wikipedia. org/wiki/Logarithmi c_spiral
  • 173. Polar Coordinates & Graphs Equiangular spirals occur in nature frequently. In many biological growth processes, the new growth is extruded at a fixed angle from the existing structure, e.g. the growth of new sea shell along the edge of the old shell, or the growth of plants. http://en.wikipedia. org/wiki/Logarithmi c_spiral
  • 174. Polar Coordinates & Graphs Equiangular spirals occur in nature frequently. In many biological growth processes, the new growth is extruded at a fixed angle from the existing structure, e.g. the growth of new sea shell along the edge of the old shell, or the growth of plants. Over time the equiangular–spiral growth lines emerge. http://en.wikipedia. org/wiki/Logarithmi c_spiral
  • 175. Polar Coordinates & Graphs Rotations of Polar Graphs
  • 176. Polar Coordinates & Graphs Let r1 = cos() = f() and r2 = cos( – π/4) = g() so that r2 = g( + π/4) = f() = r1. Rotations of Polar Graphs
  • 177. Polar Coordinates & Graphs Let r1 = cos() = f() and r2 = cos( – π/4) = g() so that r2 = g( + π/4) = f() = r1. Therefore, the point (r2,  + π/4) on the graph of g is the point (r1, ) on the graph of f rotated by the angle π/4 as shown. x y r = cos() Rotations of Polar Graphs
  • 178. Polar Coordinates & Graphs Let r1 = cos() = f() and r2 = cos( – π/4) = g() so that r2 = g( + π/4) = f() = r1. Therefore, the point (r2,  + π/4) on the graph of g is the point (r1, ) on the graph of f rotated by the angle π/4 as shown. x y r = cos() r = cos( – π/4) π/4 Rotations of Polar Graphs
  • 179. Polar Coordinates & Graphs Let r1 = cos() = f() and r2 = cos( – π/4) = g() so that r2 = g( + π/4) = f() = r1. Therefore, the point (r2,  + π/4) on the graph of g is the point (r1, ) on the graph of f rotated by the angle π/4 as shown. x y r = cos() r = cos( – π/4) π/4 Rotations of Polar Graphs In general, given r1 = f(), let r2 = g() = f( – α) so that g( + α) = f(), then the point (r2,  + α) is the point (r1, ) on the graph of f, rotated by α.
  • 180. Polar Coordinates & Graphs Let r1 = cos() = f() and r2 = cos( – π/4) = g() so that r2 = g( + π/4) = f() = r1. Therefore, the point (r2,  + π/4) on the graph of g is the point (r1, ) on the graph of f rotated by the angle π/4 as shown. x y r = cos() r = cos( – π/4) π/4 Rotations of Polar Graphs In general, given r1 = f(), let r2 = g() = f( – α) so that g( + α) = f(), then the point (r2,  + α) is the point (r1, ) on the graph of f, rotated by α. If α is positive, then the graph of r2 = f( – α) is the counter clockwise rotation of r1 = f() by the angle α,
  • 181. Polar Coordinates & Graphs Let r1 = cos() = f() and r2 = cos( – π/4) = g() so that r2 = g( + π/4) = f() = r1. Therefore, the point (r2,  + π/4) on the graph of g is the point (r1, ) on the graph of f rotated by the angle π/4 as shown. x y r = cos() r = cos( – π/4) π/4 Rotations of Polar Graphs In general, given r1 = f(), let r2 = g() = f( – α) so that g( + α) = f(), then the point (r2,  + α) is the point (r1, ) on the graph of f, rotated by α. If α is positive, then the graph of r2 = f( – α) is the counter clockwise rotation of r1 = f() by the angle α, and the graph of r2 = f( + α) is the clockwise rotation of r1 = f() by the angle α.
  • 182. Polar Coordinates & Graphs Radial Extensions/Contractions of Polar Graphs
  • 183. Polar Coordinates & Graphs The point (2r, ) is the radial extension of the point (r, ) as shown. Radial Extensions/Contractions of Polar Graphs  O (r, )p r
  • 184. Polar Coordinates & Graphs The point (2r, ) is the radial extension of the point (r, ) as shown. Radial Extensions/Contractions of Polar Graphs  O (r, )p r (2r, )p
  • 185. Polar Coordinates & Graphs The point (2r, ) is the radial extension of the point (r, ) as shown. Radial Extensions/Contractions of Polar Graphs  O (r, )p r In general, the graph of r = kf() when k is a constant, is the radial stretch/compression of the graph r = f(). (2r, )p
  • 186. Polar Coordinates & Graphs The point (2r, ) is the radial extension of the point (r, ) as shown. Radial Extensions/Contractions of Polar Graphs  O (r, )p r x y r = cos( – π/4) r = 2cos( – π/4) radial stretch/compression k >0 In general, the graph of r = kf() when k is a constant, is the radial stretch/compression of the graph r = f(). The graphs of r1 = cos ( – π/4), (2r, )p
  • 187. Polar Coordinates & Graphs The point (2r, ) is the radial extension of the point (r, ) as shown. Radial Extensions/Contractions of Polar Graphs  O (r, )p r x y r = cos( – π/4) r = 2cos( – π/4) radial stretch/compression k >0 In general, the graph of r = kf() when k is a constant, is the radial stretch/compression of the graph r = f(). The graphs of r1 = cos ( – π/4), r2 = 2cos ( – π/4) (2r, )p
  • 188. Polar Coordinates & Graphs The point (2r, ) is the radial extension of the point (r, ) as shown. Radial Extensions/Contractions of Polar Graphs  O (r, )p r x y r = cos( – π/4) r = 2cos( – π/4) radial stretch/compression k >0 r = ½ cos( – π/4) In general, the graph of r = kf() when k is a constant, is the radial stretch/compression of the graph r = f(). The graphs of r1 = cos ( – π/4), r2 = 2cos ( – π/4) and r3 = ½ * cos ( – π/4) are shown here as examples. (2r, )p
  • 189. Polar Coordinates & Graphs If k < 0, then the graph of r = kf() is the diagonal reflection across the origin of r = |k| f().
  • 190. Polar Coordinates & Graphs If k < 0, then the graph of r = kf() is the diagonal reflection across the origin of r = |k| f(). Here are the graphs of r = –2cos ( – π/4) and r = 2cos ( – π/4). x r = 2cos( – π/4) r = –2cos( – π/4) r = cos( – π/4) Diagonal Reflection with k < 0