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Subsections
The purpose of this lab is to introduce you to some of the Maple
commands that can be used to plot surfaces in three dimensions.
To assist you, there is a worksheet associated with this lab that
contains examples and even solutions to some of the exercises. You can
copy that worksheet to your home directory with the following command,
which must be run in a terminal window for example, not in Maple.
cp /math/calclab/MA1024/Surf_start.mws My_Documents
You can copy the worksheet now, but you should read through the lab
before you load it into Maple. Once you have read to the exercises,
start up Maple, load
the worksheet Surf_start.mws, and go through it
carefully. Then you can start working on the exercises.
The graph of a function of a single real variable is a set of
points
in the plane. Typically, the graph of such a function
is a curve. For functions of two variables in Cartesian
coordinates, the graph is a set of points
in
three-dimensional space. For this reason, visualizing
functions of two variables is usually more difficult.
One of the most valuable services provided by computer software such
as Maple is that it allows us to produce intricate graphs with a minimum
of effort on our part. This becomes especially apparent when it comes
to functions of two variables, because there are many more computations
required to produce one graph, yet Maple performs all these computations
with only a little guidance from the user.
The simplest way of describing a surface in Cartesian coordinates is
as the graph of a function
over a domain, e.g. a set of
points in the
plane. The domain can have any shape, but a
rectangular one is the easiest to deal with.
Another common, but more difficult way of describing a surface is as
the graph of an equation
, where
is a constant. In
this case, we say the surface is defined implicitly. A third way of
representing a surface
is through the use of level
curves. The idea is that a plane
intersects the
surface in a curve. The projection of this curve on the
plane is
called a level curve. A collection of such curves for different values
of
is a representation of the surface called a contour plot.
Similar to the idea of level curves is to look at cross sections of the surface to see what two-dimensional shape is traced, not only in the
plane by letting
be constant, but also in the
plane by holding
constant and the
plane by holding
constant.
- Generate a surface plot and contour plot for the
following function on the given domain:
- a)
- What does the contour plot look like in the regions where
the surface plot has a steep incline? What does it look like
where the surface plot is almost flat?
- b)
- What can you say about the surface plot in a region where the
contour plot looks like a series of nested circles?
- Determine the shape of the given quadric surface (a sphere, a paraboloid,
an ellipsoid, an hyperboloid, a parabolic saddle, or an hyperbolic saddle) by answering each question below.
- a)
- Plot the intersections of this shape and the two planes perpendicular to the
-axis
and
. What two-dimensional shapes are graphed?
- b)
- Plot the intersections of this shape and the two planes perpendicular to the
-axis
and
. What two-dimensional shapes are graphed?
- c)
- Plot the intersections of this shape and the two planes perpendicular to the
-axis
and
. What two-dimensional shapes are graphed?
- d)
- Describe the three-dimensional shape based on your results. Then supply a plot in three-dimensions to support your answer.
- Consider the following function
which represents the deviation, in inches, of last year's rainfall from the average annual rainfall in a certain area.
- a)
- Graph the surface corresponding to the function
. Use axes that are boxed.
- b)
- What are (approximately using values from the plot) the maximum and minimum values of the rainfall deviation and approximately where do they occur?
- c)
- Use a contour plot and shade in the region on your printout of this domain in which the deviation was between
inches and
inches.
Next: About this document ...
Up: lab_template
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Dina Solitro
2006-03-16