Double Integrals over General Regions and Polar Coordinates - Prof. Mutai, Lecture notes of Educational Mathematics

An in-depth exploration of double integrals over general regions, focusing on fubini's theorem and its applications. The document also covers double integrals in polar coordinates, with examples and solutions for various problems. It is a valuable resource for students studying advanced calculus, particularly those interested in multivariable calculus and differential geometry.

Typology: Lecture notes

2023/2024

Available from 04/20/2024

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MULTIPLE INTEGRALS
Double integrals
We will start out by assuming that the region in
2
is a rectangle which we will denote
as follows,
dcbaR ,,
This means that the ranges for
x
and
y
are
bxa
and
dyc
.
Also, we will initially assume that
0),( yxf
although this doesn’t really have to be the
case. Let’s start out with the graph of the surface
S
given by graphing
over the
rectangle
R
.
We ask ourselves what the volume of the region under
S
(and above the
xy
-plane of
course) is.
We will approximate the volume much as we approximated the area above. We will first
divide up
bxa
into
n
subintervals and divide up
dyc
into
m
subintervals. This
will divide up
R
into a series of smaller rectangles and from each of these we will choose
a point
),( ** ji yx
. Here is a sketch of this set up.
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pf1d
pf1e
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MULTIPLE INTEGRALS

Double integrals

We will start out by assuming that the region in

2  is a rectangle which we will denote

as follows,

R  a , b   c , d 

This means that the ranges for x and y are axb and c^  yd.

Also, we will initially assume that f ( x , y ) 0 although this doesn’t really have to be the

case. Let’s start out with the graph of the surface (^) S given by graphing f ( x , y ) over the

rectangle R.

We ask ourselves what the volume of the region under S (and above the xy - plane of

course) is.

We will approximate the volume much as we approximated the area above. We will first

divide up (^) axb into n subintervals and divide up cyd into m subintervals. This

will divide up R into a series of smaller rectangles and from each of these we will choose

a point( , )

xi y j. Here is a sketch of this set up.

Now, over each of these smaller rectangles we will construct a box whose height is given

by ( , )

f xi y j. Here is a sketch of that.

Each of the rectangles has a base area of  A and a height of ( , )

f xi y j so the volume of

each of these boxes is f^ (^ xi , yj ) A

. The volume under the surface S is then

approximately,

  

n

i

m

j

V f xi yj A 1 1

( , )

The integral can be worked in steps as follows;

f x ydA f x ydydx f x ydxdy

d

c

b

a

b

a

d

R c

Example

Compute each of the following double integrals over the indicated rectangles.

1. 6 , [ 2 , 4 ] [ 1 , 2 ]

2

 xydA R  

R

2. 2 4 , [ 5 , 4 ] [ 0 , 3 ]

3

 x  ydA R   

R

  1. cos( ) sin( ) , [ 2 , 1 ] [ 0 , 1 ]

2 2

 x y  x  ydA R   

R

4. , [ 0 , 1 ] [ 1 , 2 ]

 dA R

R x y

5.  xe dA , R [ 1 , 2 ][ 0 , 1 ]

R

xy

Solutions

1. 6 , [ 2 , 4 ] [ 1 , 2 ]

2

 xydA R  

R

4

2

2

4

2

4

2

2

1

3

4

2

2

1

2 2      

xydA xydydx xy dx xdx x R

2. 2 4 , [ 5 , 4 ] [ 0 , 3 ]

3

 x  ydA R   

R

4

5

2

4

5

4

5

3 0

4

4

5

3

0

3 3         

   

x ydA x ydydx xy y dx x dx x x R

  1. cos( ) sin( ) , [^2 ,^1 ] [^0 ,^1 ]

2 2     

x y x ydA R R

 

  

   

cos( )

sin( ) 3

sin( ) sin( )

cos( ) sin( ) cos( ) sin( )

1

0

(^13)

0

2

1

2

1

0

(^132)

0

1

2

2 2 2 2

y

y ydy

y

x x y dy

x y x y x ydA x y x ydxdy R

4. , [ 0 , 1 ] [ 1 , 2 ]

 dA R R x y

  1.  xe dA , R [ 1 , 2 ][ 0 , 1 ]

R

xy

As we saw in the previous set of examples we can do the integral in either direction.

However, sometimes one direction of integration is significantly easier than the other so

make sure that you think about which one you should do first before actually doing the

integral.

A double integral can be evaluated easily when the integrand is a product of functions.

Let f ( x , y ) g ( x ) h ( y )where g ( x )is a function of x only and h ( y )is a function of y.

There are two types of regions that we need to look at. Here is a sketch of the regions

These regions are described as;

Case 1: D ( x , y ) axb , g 1 ( x ) yg 2 ( x )

Case 2: D  ( x , y ) h 1 ( x ) xh 2 ( x ), cyd

we are going to use all the points, ( x , y ), in which both of the coordinates satisfy the two

given inequalities. The double integral for both of these cases are defined in terms of

iterated integrals as follows.

Case 1: D ( x , y ) axb , g 1 ( x ) yg 2 ( x )the integral is defined to be;

Case 2: D^ ^ (^ x , y ) h 1 ( x ) xh 2 ( x ), cy ^ d the integral is defined to be;

Some properties of double integrals are:

Examples

Evaluate each of the following integrals over the given region D.

Solutions

In this case we need to determine the two inequalities for x and y that we need to do the

integral. The best way to do this is the graph the two curves. Here is a sketch.

Now, there are two ways to describe this region. If we use functions of x , as shown in

the image we will have to break the region up into two different pieces since the lower

function is different depending upon the value of x. In this case the region would be

given by D 1 (^)  D 2 where,

If we do this, we’ll need to do two separate integrals, one for each of the regions.

To avoid this, we could turn things around and solve the two equations for x to get;

y   2 x  3 , x  y

yx   xy

we notice that the same function is always on the right and the same function is always

on the left and so the region is;

Writing the region in this form means doing a single integral instead of the two integrals.

NB: We can integrate these integrals in either order (i.e. x followed by y or y followed

by x ), although often one order will be easier than the other. In fact, there will be times

when it will not even be possible to do the integral in one order while it will be possible

to do the integral in the other order.

Example

Evaluate the following integrals by first reversing the order of integration.

Solutions:

First, notice that if we try to integrate with respect to y we can’t do the integral because

we would need a

2 y in front of the exponential in order to do the y integration. We are

going to hope that if we reverse the order of integration we will get an integral that we

can do.

Now, when we say that we’re going to reverse the order of integration this means that

we want to integrate with respect to x first and then y. We can’t just interchange the

integrals, keeping the original limits, and be done with it. This would not fix our original

So, as we hoped, we were able to do the integral once we interchanged the order of

integration.

We cannot do this integral by integrating with respect to x first so we’ll hope that by

reversing the order of integration we will get something that we can integrate. Here are

the limits for the variables that we get from this integral.

and the sketch of this region is;

So, if we reverse the order of integration we get the following limits.

The integral is then,

We now look at the volume of the solid that lies below the surface given by zf ( x , y )

and above the region D in the xy - plane. This is given by;

Example

Find the volume of the solid that lies below the surface given by z  16 xy  200 and lies

above the region in the xy - plane bounded by

2 yx and

2 y  8  x.

Solution

By setting the two bounding equations equal we can see that they will intersect at x  2

and (^) x  2. So, the inequalities that will define the region D in the xy - plane are

The volume is then given by;

The region D is really where this solid will sit on the xy - plane and here are the

inequalities that define the region.

The volume of this solid is;

In general,

gives the net volume between the graph of zf ( x , y ) and the region D in the xy - plane.

Regions that are below the xy - plane have a negative volume and regions that are above

the xy - plane have a positive volume.

gives the net area between the curve given by yf ( x ) and the x - axis on the interval

[ a , b ].

The second geometric interpretation of a double integral is

This is easy to see why this is true in general. Let’s suppose that we want to find the area

of the region shown below.

We know that this area can be found by the integral,

Or in terms of a double integral we have,

Double Integrals in Polar Coordinates

We have seen to this point the region D could be easily described in terms of simple

functions in Cartesian coordinates. In this section we want to look at some regions that

are much easier to describe in terms of polar coordinates. For instance, we might have a

region that is a disk, ring, or a portion of a disk or ring. In these cases, using Cartesian

coordinates could be somewhat cumbersome. For instance, let’s suppose we wanted to

do the following integral,

This general region will be defined by inequalities,

Now, to find dA let’s redo the figure above as follows,

As shown, we’ll break up the region into a mesh of radial lines and arcs. Now, if we pull

one of the pieces of the mesh out as shown we have something that is almost, but not

quite a rectangle. The area of this piece is  A. The two sides of this piece both have length

rr 0  ri where r 0 is the radius of the outer arc and ri is the radius of the inner arc. Basic

geometry then tells us that the length of the inner edge is ri  while the length of the out

edge is r 0  where  is the angle between the two radial lines that form the sides of

this piece.

Now, let’s assume that we’ve taken the mesh so small that we can assume that rir 0  r

and with this assumption we can also assume that our piece is close enough to a rectangle

that we can also then assume that,

Also, if we assume that the mesh is small enough then we can also assume that,

With these assumptions we then get,

In order to arrive at this, we had to make the assumption that the mesh was very small.

This is not an unreasonable assumption. Recall that the definition of a double integral is

in terms of two limits and as limits go to infinity the mesh size of the region will get

smaller and smaller. In fact, as the mesh size gets smaller and smaller the formula above

becomes more and more accurate and so we can say that,

Before moving on it is again important to note that dA  drd . The actual formula for dA

has an (^) r in it. It will be easy to forget this (^) r on occasion, but as you’ll see without it some

integrals will not be possible to do.

Now, if we’re going to be converting an integral in Cartesian coordinates into an integral

in polar coordinates we are going to have to make sure that we’ve also converted all the

x ’s and y ’s into polar coordinates as well. To do this we’ll need to remember the

following conversion formulas,

x  r cos , y^  r^ sin,

2 2 2 rxy

We are now able to write down a formula for the double integral in terms of polar

coordinates.

Example

Evaluate the following integrals by converting them into polar coordinates.