Part 1: Change of Variable into Polar Coordinates
We can also apply the change of variable formula to the polar
coordinate transformation
x = rcos( q) , y = rsin( q) |
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However, due to the importance of polar coordinates, we derive its change of
variable formula more rigorously.
To begin with, the Jacobian determinant is
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¶( x,y)
¶( r,q)
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= |
ê ê
ê
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ê ê
ê
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= rcos2( q) +rsin2( q) = r |
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As a result, the area differential for polar coordinates is
dA = |
ê ê
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¶( x,y)
¶( r,q)
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ê ê
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drdq = r dr dq |
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Let us consider now the polar region S defined by
q = a,q = b,r = g( q) ,r = f( q) |
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where f( q) and g( q) are contained
in [ p,q] for all q in [ a,b] .
If q0,¼,qm is an h-fine partition of [a,b] and r0,¼,rn is an h-fine partition
of [ p,q] , then the image of [ a,b]×[ p,q] is a partition of the image of the region with
near parallelograms whose areas are denoted by DAjk:
Since the area differential is dA = rdrdq, the area of the "near parallelogram" is approximately
so that if xjk = rjcos( qk) and yjk = rjsin( qk) , then
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lim
h® 0
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n å
j = 1
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m å
k = 1
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f(xjk,yjk) DAjk = |
lim
h®0
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n å
j = 1
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m å
k = 1
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f( rjcos( qk) ,rjsin( qk) ) rjDrjDqj |
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Writing each of these limits as double integrals results in the formula for
change of variable in polar coordinates:
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f( x,y) dA = |
ó õ
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b
a
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ó õ
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f( q)
g(q)
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f( rcos(q), rsin(q) ) rdrdq |
| (1) |
To aid in the use of (1), let us notice that if p is
constant, then r = p is a circle of radius p centered at the origin in the
xy-plane, while if a is constant, then q = a is a ray
at angle a beginning at the origin of the xy-plane.
Polar coordinates for the origin are r = 0 for every value of q.
EXAMPLE 1 Use (1) to evaluate
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1
0
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Ö |
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2-x2 |
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( x2+y2) dydx |
x |
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Solution: To do so, we transform the iterated integral into a
double integral
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1
0
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Ö |
 |
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2-x2 |
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( x2+y2)dydx = |
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( x2+y2) dA |
x |
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where R is a sector of a circle with radius Ö2. In polar
coordinates, R is the region between r = 0 and r = Ö2 for q
in [ p/4,p/2] :
Since r2 = x2+y2, the double integral thus becomes
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( x2+y2) dA = |
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p/2
p/4
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Ö2
0
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r2 rdrdq = |
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p/2
p/4
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Ö2
0
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r3 drdq |
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and the resulting iterated integral is then easily evaluated:
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( x2+y2) dA = |
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p/2
p/4
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r4
4
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ê ê
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Ö2
0
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dq = |
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p/2
p/4
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dq = |
p
4
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Check your Reading: What does y = x, x > 0 correspond to in
polar coordinates?