From Points to Regions

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

Number of cars = rho (b - a)

If the traffic density is not constant and is given by a function, rho(x) then simple multiplication is replaced by integration

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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

Rate of decrease of number of cars = k (b - a)

and if the rate at which the density is decreasing is not constant then simple multiplication is replaced by integration.

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Two Dimensions

In R2 we are primarily interested in regions like those described in the section on volume that can be described by

E = { (x, y) : a <= x <= b and f(x) <= y <= g(x)}

or

E = { (x, y) : c <= y <= d and p(y) <= x <= q(y)}

Recall that in R2 a vector field

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

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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

Total population = density * area

and if the population density is given by a funtion then simple multiplication is replaced by integration.

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This is often computed by an iterated integral

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or

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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

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which is often computed by an iterated integral

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or

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Three Dimensions

In R3 we are usually interested in regions that can be described by

E = { (x, y, z) : (x, y) is in D and p(x, y) <= z <= q(x, y) }

where D is a region that can be described by

D = { (x, y) : a <= x <= b and f(x) <= y <= g(x)}

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

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represents migration and is measured in units, for example, of individuals per unit of area per unit of time then

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represents the rate at which the population density at each point is decreasing and is measured in units of individuals per unit of volume per unit of time.

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.

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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 the rate at which the total population is decreasing is obtained by multiple integration and often evaluated by an iterated integral.

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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

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where alpha2 is a positive constant called the thermal diffusivity of the material of which the object is made. Notice that heat is flowing "downhill" from points at which the temperature is high toward points at which it is lower. The rate at which the temperature at a point is decreasing is, as usual, div F and, thus, the rate at which the temperature at a point is increasing is given by

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This last equation is called the Heat Equation and describes the way in which heat "diffuses" through an object whose composition is uniform. It describes other kinds of diffusion as well and is also called the Diffusion Equation. The heat equation can be written in three, two, or one dimensions.

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In one dimension it describes the way heat diffuses through a thin wire and in two dimensions it describes the way in which heat diffuses through a thin plate.



Integration in Cylindrical Coordinates

Missing figure 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

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and the temperature of each point might be described by a function like

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In this situation we are often interested in the integral

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which can be evaluated by the iterated 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

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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.

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  2. Missing equation

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  4. Suppose that the concentration of a particular pollutant in a cylindrical aquifer whose length is 100 meters and whose radius is 10 meters is given by

    Missing equation

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

  5. Suppose that the temperature of a uniform cylindrical bar of metal of length ten centimeters and radius one centimeter is given by

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    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

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

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In this situation we are often interested in the integral

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which can be evaluated by

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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

Missing equation

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.

  1. Missing equation

  2. Missing equation

  3. Missing equation

  4. Suppose that the concentration of a particular pollutant in a spherical aquifer whose radius is 10 meters is given by

    Missing equation

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

  5. Suppose that the temperature of a uniform metal sphere of radius one centimeter is given by

    Missing equation

    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?


Copyright c 1997 by Frank Wattenberg, Department of Mathematics, Montana State University, Bozeman, MT 59717