
68
INTRODUCTION TO TENSORS
Equation 4.1 describes the current flow through a discrete element.
To
apply Ohm’s
law to a distributed medium, such as a crystalline solid, an alternative form of
this
equation is used:
5
=
UE.
(4.2)
Here
5
is the current density,
E
is the electric field, and
u
is the material’s
conductivity.
In
MKS units,
5
is measured in amperes per meter squared,
E
in
volts per meter, and
u
in inverse ohm-meters.
Equation 4.2 describes
a
very simple physical relationship between the current
density and the electric field, because the conductivity has been expressed as a scalar.
With a scalar conductivity, the amount of current flow is governed solely by the
magnitudes of
(+
and
E,
while the direction of the flow is always parallel to
E.
But in
some materials,
this
is not always the case. Many crystalline solids allow current to
flow more easily in one direction than another. These
nonisotropic
materials must have
different conductivities in different directions.
In
addition, these crystals can even
experience current flow perpendicular to
an
applied electric field. Clearly Equation
4.2, with a scalar conductivity, will not handle these situations.
One solution is to construct an array of conductivity elements and express
Ohm’s
law using matrix notation as
u11 u12 (+13
[
=
[
;::
Uz2
Uz3]
[
.
(4.3)
u32
a33
In Equation 4.3, the current density and electric field vectors are represented by
column matrices and the conductivity
is
now a square matrix.
This
equation can be
written in more compact matrix notation as
or
in subscriptlsummation notation
as
All these expressions produce the desired result. Any linear relationship between
3
and
E
can be described. The 1-component of the current density is related to the
1
-component of the electric field via
u1
1,
while the 2-component of the current density
is related to
the
2-component of the electric field through
u22.
Perpendicular flow is
described by the off-diagonal elements. For example, the
u12
element describes flow
in the 1-direction due to an applied field in the 2-direction.
The matrix representation for nonisotropic conductivity does, however, have a
fundamental problem. The elements of the matrix obviously must depend on our
choice of coordinate system. Just as with the components of a vector, if we reorient
our
coordinate system, the specific values in the matrix array must change. The matrix
array itself, unfortunately, carries no identification of the coordinate system used. The
way we solved
this
problem for vector quantities was
to
incorporate the basis vectors