The divergence div F of a vector field F gives us information at each point. In this section we show how the divergence combined with integration can be used to determine what is happening in an entire region. We look at one, two, and three dimensions.
One Dimension
If traffic density in an interval, [a, b], is a constant, rho, then the total number of cars in the interval is determined by simple multiplication
If the traffic density is not constant and is given by a function, rho(x) then simple multiplication is replaced by integration

Similarly, if the rate, div F, at which traffic density is decreasing in an interval, [a, b], is a constant, k, then the rate at which the number of cars in the interval is decreasing is determined by simple multiplication
and if the rate at which the density is decreasing is not constant then simple multiplication is replaced by integration.


measured in units of cars per mile. How many cars are there in the section of the road between the points x = 0 and x = 1?
measured in units of cars per minute. Find the rate at which the number of cars in the section of the road between x = 0 and x = 1 is decreasing? Compute F(0) and F(1). Do you have any comments?
measured in units of cars per minute. Find the rate at which the number of cars in the section of the road between x = 1/2 and x = 1 is decreasing? Compute F(1/2) and F(1). Do you have any comments?
measured in units of cars per minute. Find the rate at which the number of cars in the section of the road between x = 0 and x = 1/2 is decreasing? Compute F(0) and F(1/2). Do you have any comments?
Two Dimensions
In R2 we are primarily interested in regions like those described in the section on volume that can be described by
or
Recall that in R2 a vector field

representing migration is measured in units like individuals per unit of time per unit of length and

which represents the rate at which population density at a point is decreasing is measured in units like individuals per unit of area per unit of time -- that is, individuals per unit of length2 per unit of time.
If the population density in a region is constant then the total population is obtained by simple multiplication
and if the population density is given by a funtion then simple multiplication is replaced by integration.

This is often computed by an iterated integral

or

Similarly, if the rate at which the population density is decreasing is constant then the rate at which the total population is decreasing is obtained by simple multiplication and if the rate at which the population density is decreasing is not constant then simple multplication is replaced by integration

which is often computed by an iterated integral

or



Suppose that the popluation density in this habitat is described by the function
Find the total population in this habitat.
where x and y are measured in kilometers. Suppose that population migration is described by

and is measured in individuals per year per kilometer.
Three Dimensions
In R3 we are usually interested in regions that can be described by
where D is a region that can be described by
We can also work with regions that are made up of several pieces that can be described in this way.
Recall that if a vector field


If population density is contant then the total population in a region is just density multiplied by volume and if population density is not constant then simple multiplication is replaced by multiple integration and often evaluated by an iterated integral.




where x, y, and z are measured in feet.
The population density of fish in the reservoir is described by
measured in fish per cubic foot.
Find the total number of fish in the reservoir.
Heat and Conduction
Heat is often measured in calories -- one calorie is the amount of energy required to raise one gram of water one degree Celsius. The temperature of a body, T(x, y, z), is a measure of the density of heat at that point. If the temperature of a body varies from point to point then heat will flow from hotter areas to cooler areas by a process called conduction. This flow is described by the vector field



is given by
The block is thermally isolated, so that no heat flows into or out of the block. Heat will flow within the block by conduction and the block will approach an equilibrium in which its temperature is uniform. What is its temperature at equilibrium?
is given by
The tetrahedron is thermally isolated, so that no heat flows into or out of it. Heat will flow within the tetrahedron by conduction and it will approach an equilibrium in which its temperature is uniform. What is its temperature at equilibrium?
Integration in Cylindrical Coordinates
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In many situations cylindrical coordinates are easier to use than Cartesian coordinates. For example, the figure at the right shows a cylindrical block
of radius R and height H
that is heated by a red wire running through its center. In this situation
the temperature of a point in the block depends on its distance from the
wire. If we set up our coordinate system so that the wire is running
along the z-axis then the cylinder can be described in cylindrical
coordinates by
![]() and the temperature of each point might be described by a function like ![]() In this situation we are often interested in the integral ![]()
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One of the striking qualities of mathematics and, perhaps, the most important theme of this course is that the exact same mathematics can describe very different or apparently very different physical situations. For example, a function like the function

might describe the temperature at each point in a uniform cylinder. In this case it might be measured in degrees Celsius and is indirectly a measure of the amount of heat energy or calories per unit of volume at each point in the cylinder. It can be thought of as the density of heat energy.
The same function or a similar function might represent the density or concentration of a pollutant in a cylindrical aquifer. The same function or a similar function might represent the density of mosquitos in a cylindrical region around a fluorescent bulb. For each of these three situations describe the units in each element of the three formulas below and describe what the two integrals measure.

What is the total amount of the pollutant in the aquifer? What is the average concentration of pollutant in the aquifer?

Suppose that the bar is thermally isolated so that no heat flows into or out of the bar and that heat flows within the bar by conduction. What will the temperature of the bar be at equilibrium -- that is, when its temperature is uniform?
Integration in Spherical Coordinates
In many situations it is more natural to use spherical coordinates than either Cartesian coordinates of cylindrical coordinates. For example, when a spherical object of the form

is heated by a source at its center, its temperature at each point might be described by a function like

In this situation we are often interested in the integral

which can be evaluated by

One of the striking qualities of mathematics and, perhaps, the most important theme of this course is that the exact same mathematics can describe very different or apparently very different physical situations. For example, a function like the function

might describe the temperature at each point in a uniform sphere. In this case it might be measured in degrees Celsius and is indirectly a measure of the amount of heat energy or calories per unit of volume at each point in the cylinder. It can be thought of as the density of heat energy.
The same function or a similar function might represent the density or concentration of a pollutant in a spherical aquifer. The same function or a similar function might represent the density of mosquitos in a spherical region around an incandescent bulb. For each of these three situations describe the units in each element of the three formulas below and describe what the two integrals measure.

What is the total amount of the pollutant in the aquifer? What is the average concentration of pollutant in the aquifer?

Suppose that the sphere is thermally isolated so that no heat flows into or out of the sphere and that heat flows within the sphere by conduction. What will the temperature of the sphere be at equilibrium -- that is, when its temperature is uniform?