
The situation with forces due to magnetism is more complicated. First, we
find that, despite numerous searches, no evidence of magnetic charges
exist. In other words, there are no particles which create a radial
magnetic field (usually termed
by physicists)
in the way an electric charge creates a radial
field. However,
it turns out that
fields can be created by moving electric charges, i.e. currents produce
fields. The nature of
these fields is somewhat more complicated than the electric charge-electric field case.
We won't go into the form of the
field.
Let's simply say that
you'll see all you ever wanted to know about it when you take Physics
151 or Physics 2. For now, what interests us is the fact that there is
amazing reciprocity in nature. If moving electric charges create
fields, then
fields
must exert forces on moving electric charges,
just as electric charges create and are ``acted upon by''
fields.
The SI unit for magnetic field is the Tesla (abbreviated
as T). Since 1 T is a very large field (the earth's magnetic field is about
) the gauss
(abbreviated as
) is sometimes used.
One gauss is
,
so the earth's magnetic field amounts to about half a gauss.
Again, the nature of the force is different in the magnetic field-electric current case. The force takes on the following characteristic:
where
is the velocity of charge
. The
is called
the cross product.
It is a vector operation.
What it says is simple. If the angle between the vector
and
the vector
is called
, then the magnitude of the
magnetic force is
, and its direction is
perpendicular to both
and
. It's a
screwy system, but nature has its reasons for doing things this way.
Normally, we make life easy for the student by choosing situations to
be set up in such a way that
is perpendicular to
.
In this case, the angle
is
and
.
The force is always perpendicular to both
and
,
so we are forced to use a three-dimensional view for looking at the
situation. This is the case for the mass spectrometer
that you heard about last week. For this device, one sets up electric
fields to accelerate ions, then causes those ions to fly through a region
in which there is a magnetic field directed perpendicular to the flight
path of the ions. This bends them into a curved path whose radius depends
upon the charge and mass of the ion. In this way, the mass spectrometer
separates a compound into a number of identifiable constituents.
See your chemistry lecture notes from last week for a discussion of the
mass spectrometer operation.
The magnetic force is understood to be due to the presence of a magnetic field produced by charges in motion. You can see a 3-D visualization of the production of the field from a wire carrying positive charges (or equivalently and more realistically, a wire carrying negative charges in the opposite direction) in the following video. Note that the scene shows a wire in which the charges are initially at rest. As the camera pans, the charges start to move and the magnetic field expands outward from the wire at the speed of light. The direction of the magnetic field is shown by the white arrows whose rotation depicts the fact that the field is circular around the wire. Enjoy by clicking here or on the image at the beginning of this document.
The aim of this demonstration is to produce plots which illuminate the concept of flux. This is inherently 3-dimensional, so we will make a lot of use of 3-d plots and some animation.
We begin with the concept of describing a flow. We have already introduced the concept of vectors as a way to describe the path of something in motion. We can simulate that by an animation in Maple by using drawing a line in 3-space. The line represents the path of a particle as it moves. How would we draw a line in 3 dimensions? We can make use of the concept of a parametric specification of the line, i.e. instead of writing down an equation for a line, we write down 3 specifications for a line. Each specification is a description of the path of the line along the x, y, or z axis (we call this a parametrization of the line). To parametrize a path along an axis, we simply ask ourselves how the path position changes. For example, let's say we want to draw a path which is parallel to the x-axis. That means that the position of the particle never changes as far the y and z axes are concerned. If the particle started at y=1.5, and z=1.5 (as an example), then, its y and z position will remain (1.5,1.5) no matter what the x position is. In Maple, parametrizations are specified by placing the changes in square brackets: [xp, yp, zp] where xp is the x-parametrization, yp is the y-parametrization, and so on. For a path along the x-axis, we want y and z to stay constant, so let's go to Maple and try plotting:
#
plot3d([x, 1.5, 1.5], x=1..5, y=1..4);
#
#We see a line in space! Set the axes to BOXED to get a good view of
#what we drew. The line is parallel to x and every point on the line
#has a y,z value of (1.5, 1.5). Now let's try to draw lines parallel
#to the y axis and z axis. We draw simulaneous plots.
#
plot3d({[x, 1.5, 1.5], [1.5, y, 1.5], [1.5, 1.5, y]}, x=0..5, y=0..5,
scaling=CONSTRAINED);
#
#Not bad. Note that we couldn't specify z in the last plot since plot3d
#only accepts 2 independent variables. But the variable doesn't matter
#since all we want to do is to represent something that changes linearly.
#Now let's add a little life by animating things. Suppose we want to
#show the path of a particle that starts at the origin and zooms outward
#along the x-axis. We just add a third variable that multiplies the x
#term in our parametric specification. Make it so ...
#
animate3d([x*u, 0.0, 0.0], x=0..5, y=0..5, u=0..1,scaling=CONSTRAINED);
#
#To specify three particles zooming out from the origin along three different
#directions, we say
#
animate3d({[x*u, 0.0, 0.0], [0.0, y*u, 0.0], [0.0, 0.0, y*u]}, x=0..5,
y=0..5, u=0..1,scaling=CONSTRAINED);
#
Alright, enough with setup. What has all this to do with flow? Well, we
can now make it appear as though particles are zooming out from some source
at the origin. For example, maybe we are looking at drops spraying out from
a garden hose sitting at the origin. Let's consider motion along one
dimension for the moment. How would we characterize how much of something
is flowing away from the origin? What we are trying to specify is the
amount of water (the mass) that flows away in a given amount of time.
One way to be quantitative about it is to set up a gate near the source and
have the gate measure how much water flows through it in, say, one second.
The gate can be represented simply as a plane, but how do we position the
plane? Common sense says that to measure all the water leaving, we have
to have the gate closed, i.e. it must be perpendicular to the flow. If the
gate is open, then the water goes past it, but not through it, and hence
is not measured. Let's look at an animated picture of the gate closed and
the gate open... back to Maple
#
animate3d({[x*u, 0.0, 0.0], [2.5, x-2, y-2]}, x=0..5, y=0..5, u=0..1,
title=`Gate_closed_Measure_flow`, labels=[x, y, z], scaling=CONSTRAINED);
#
animate3d({[x*u, 0.0, 0.0], [x, 3.5, y-1]}, x=0..5, y=0..5, u=0..1,
title=`Gate_closed__Flow_is_0`, labels=[x, y, z],scaling=CONSTRAINED);
#
#Notice that the second parametrization is the one specifying the plane.
#Let's make it a little more realistic, by giving the flow a little
#thickness. That is, we stretch it out in y and z a little.
#
animate3d({[x*u, 0.0, 0.0], [x*u, -0.2, 0.0], [x*u, 0.2, 0.0],
[x*u, 0.0, -0.2], [x*u, 0.0, 0.2], [2.5, x-2, y-2]}, x=0..5, y=0..5, u=0..1,
title=`Gate_closed__Measure_flow`, labels=[x, y, z], scaling=CONSTRAINED);
#
animate3d({[x*u, 0.0, 0.0], [x*u, -0.2, 0.0], [x*u, 0.2, 0.0],
[x*u, 0.0, -0.2], [x*u, 0.0, 0.2], [x, 3.5, y-1]}, x=0..5, y=0..5, u=0..1,
title=`Gate_closed__Flow_is_0`, labels=[x, y, z],scaling=CONSTRAINED);
#
What we notice is that to make an accurate measure of the flow, our gate
must be perpendicular to the flow. Thus, the orientation of the gate is
set by the direction of the flow. Now let's extend this reasoning to 3-D.
To explain why everything falls off as
,
we imagine now a source which
emits something equally in all 3 dimensions. How does the flow across
our gate change now? Well, first we have to pick the appropriate gate
for measuring the flow. A single plane won't do, it only covers flow in
only one dimension (the one perpendicular to the plane). The distance
of the gate from the source matters too, since we assume the flow is
spreading out in all directions. Hence, we want a surface which is
perpendicular to the flow outward from the source and equidistant from
the source at every point. This is the description of a sphere with
its origin at the position of the source! So we need to draw the spherical
gate that measures flow a certain distance from the source. We'll make
an animated picture and indicate the flow by lines moving out from
the origin in all directions. How do we parametrize the sphere? It's
easiest to do it by spherical coordinates. To do that, we remember that
the specification or parametrization for a sphere is given by
where
is the radius of the sphere,
varies from 0 to
and
varies from 0 to
.
In these coordinates a straight line along the x-axis can be specified as
where
is the length of the line we want. Now let's combine all this
information by going back to Maple:
#
animate3d({[sin(t)*cos(p), sin(t)*sin(p), cos(t)], [u*sin(p), 0., 0.],
[0., u*sin(p), 0.], [0., 0., u*sin(p)],[u*sin(p), 0, u*sin(p)],
[0, u*sin(p), u*sin(p)]}, p=0..2*Pi, t=0..Pi, u=0..2, labels=[x, y, z],
title=`Source_at_origin`, style=WIREFRAME, scaling=CONSTRAINED, axes=BOXED);
#
Quite a picture isn't it? But it's more than just a picture. If we
imagine anything flowing out from a point, then the measurement of
its flow is the amount that flows past our spherical surface in a given
amount of time. For that same amount of time, if we look at a surface
further away from the source, we see that the amount emitted by the source
is the same, but now the area of our gate is larger. What we see is that
our measurement of the strength of the source or amount of flow from it
seems to go down as 1/(Area of a sphere)! Thus, long before Newton wrote
down the theory of gravity or Coulomb measured the electric force,
Renaissance scholars expected that all forces from a central source must
go down as
#
animate3d({[sin(t)*cos(p), sin(t)*sin(p), cos(t)], [u*sin(p), 0., 0.],
[0., 0., u*sin(p)],[0., u*sin(p), 0.], [u*sin(p), 0, u*sin(p)],
[0, u*sin(p), u*sin(p)], [2*sin(t)*cos(p), 2*sin(t)*sin(p), 2*cos(t)]},
p=0..2*Pi,t=0..Pi, u=0..4, labels=[x, y, z], title=`Source_at_origin`,
style=WIREFRAME, scaling=CONSTRAINED, axes=BOXED);

subsubsection4_1_5_2.html