 
 
 
 
 
   
We will start by considering a very special case of flux and then slowly
generalize until we have the flux integral. For now we will be considering
flowing water. We wish to find the rate at which water is flowing through
the surface S, when the velocity of the water is  .
.
 , and has been
oriented with a direction of positive flow
, and has been
oriented with a direction of positive flow  . If water is flowing
through the surface in the direction of
. If water is flowing
through the surface in the direction of  with a constant speed
 with a constant speed  , what is the rate at which water is flowing
through S? The rate will be the total volume of water which flows past S
in a time
, what is the rate at which water is flowing
through S? The rate will be the total volume of water which flows past S
in a time  divided by
 divided by  . First compute the total volume
that flows past S. The water flowing through S forms a cylinder with a
height of
. First compute the total volume
that flows past S. The water flowing through S forms a cylinder with a
height of  and a base with area
 and a base with area  . The total volume of water will be
. The total volume of water will be 



 is the same as
 is the same as  . Now we have a skewed cylinder with base S and height
. Now we have a skewed cylinder with base S and height  , where
, where  is the
angle between
 is the
angle between  and
 and  .
.(illus of skewed cylinder)
The total volume is

 be a unit vector (I'll start using
 be a unit vector (I'll start using  ),
then we can write the volume as
),
then we can write the volume as 



|  | (1) | 
 is constant. In this case we divide the
surface S into many small patches, each of which is nearly flat. Now we
can assume
 is constant. In this case we divide the
surface S into many small patches, each of which is nearly flat. Now we
can assume  is nearly constant on each little
patch and use case 2. To get the total flux we add up the flux over all of
the small patches. Divide S into k patches
 is nearly constant on each little
patch and use case 2. To get the total flux we add up the flux over all of
the small patches. Divide S into k patches  each of which has area
each of which has area  and
normal vector
 and
normal vector  . Take the
velocity at the center of the jth patch (or anywhere on the patch) to
be
. Take the
velocity at the center of the jth patch (or anywhere on the patch) to
be  . Using
. Using  the flux through the jth patch is given by
the flux through the jth patch is given by 


 and
 and  the
sum is replaced with an integral and we write
 the
sum is replaced with an integral and we write 
 
|  | (2) | 
 by
 by 


 is defined to be the area vector
 is defined to be the area vector  and (
 and (![[*]](http://www.math.arizona.edu/~doc/latex2html/gifs/cross_ref_motif.gif) ) will be written as
) will be written as 



Examples:
 through the triangle with
vertices (0,0,0), (0,2,4), and (0,0,4) and oriented in the +x direction.
This triangle lies in the yz-plane (since x is zero for all of the
points) so the normal vector is
 through the triangle with
vertices (0,0,0), (0,2,4), and (0,0,4) and oriented in the +x direction.
This triangle lies in the yz-plane (since x is zero for all of the
points) so the normal vector is  .
.
 
The problem says that the surface is oriented in the positive x direction
so we will use  . An infinitesimal piece of area in the 
yz-plane looks like dS=dydz (because the surface is flat). Therefore
. An infinitesimal piece of area in the 
yz-plane looks like dS=dydz (because the surface is flat). Therefore  . The flux through the triangle is
. The flux through the triangle is 
![\begin{displaymath}
\int_{S}\vec{F}\cdot d\vec{A} =\int_{S}\left[ 4z\hat{\imath}...
 ...\sin \left( x^{2}z\right) \hat{k}\right] \cdot \hat{\imath}dydz\end{displaymath}](img42.gif)

 through the triangle is
 through the triangle is  .
. through the sphere x2+y2+z2=R2. First we notice that the
normal vector must point radially inward or outward. By convention, the
normal vector of a closed surface is taken to be outward. So
 through the sphere x2+y2+z2=R2. First we notice that the
normal vector must point radially inward or outward. By convention, the
normal vector of a closed surface is taken to be outward. So  , and
, and  since
 since  everywhere on the sphere. The flux integral is thus
everywhere on the sphere. The flux integral is thus 


 
 
 
 
