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Let
,
,
be a set of standard right-handed Cartesian coordinates. Furthermore, let
,
,
be three independent functions of these coordinates which are
such that each unique triplet of
,
,
values is associated with a unique triplet of
,
,
values. It follows that
,
,
can be used as an alternative set of coordinates to
distinguish different points in space. Since the surfaces of constant
,
, and
are not
generally parallel planes, but rather curved surfaces, this type of coordinate system is termed curvilinear.
Let
,
, and
. It follows that
,
, and
are
a set of unit basis vectors which are normal to surfaces of constant
,
, and
, respectively, at all points
in space. Note, however, that the direction of these basis vectors is generally a function of position. Suppose that
the
, where
runs from 1 to 3, are mutually orthogonal at all points in space: i.e.,
 |
(1595) |
In this case,
,
,
are said to constitute an orthogonal coordinate system.
Suppose, further, that
 |
(1596) |
at all points in space, so that
,
,
also constitute a right-handed
coordinate system. It follows that
 |
(1597) |
Finally, a general vector
, associated with a particular point in space, can be written
 |
(1598) |
where the
are the local basis vectors of the
,
,
system, and
is termed the
th component of
in this system.
Consider two neighboring points in space whose coordinates in the
,
,
system are
,
,
and
,
,
.
It is easily shown that the vector directed from the first to the second of these points takes the form
 |
(1599) |
Hence, from (1595), an element of length (squared) in the
,
,
coordinate system is written
 |
(1600) |
Here, the
, which are generally functions of position, are known as the scale factors of the system.
Elements of area that are normal to
,
, and
, at a given point in space, take the form
,
, and
, respectively. Finally, an element of
volume, at a given point in space, is written
, where
 |
(1601) |
Note that [see Equation (1481)]
 |
(1602) |
and
 |
(1603) |
The latter result follows from Equations (1480) and (1481) because
,
etc. Finally, it is easily demonstrated from (1595) and (1597) that
Consider a scalar field
. It follows from the chain rule, and the relation
,
that
 |
(1606) |
Hence, the components of
in the
,
,
coordinate system are
 |
(1607) |
Consider a vector field
. We can write
where use has been made of Equations (1479), (1603), and (1604). Thus, the
divergence of
in the
,
,
coordinate system takes the form
 |
(1609) |
We can write
where use has been made of Equations (1483), (1602), and (1606).
It follows from (1605) that
 |
(1611) |
Hence, the components of
in the
,
,
coordinate system are
 |
(1612) |
Now,
[see (1477)], so Equations (1606) and (1609)
yield the following expression for
in the
,
,
coordinate system:
 |
(1613) |
The vector identities (1476) and (1484) can be combined to give the
following expression for
that is valid in a general coordinate system:
Making use of Equations (1607), (1609), and (1612), as well
as the easily demonstrated results
and the tensor identity (1500), Equation (1614) reduces (after a great deal of tedious algebra) to the
following expression for the components of
in the
,
,
coordinate system:
![\begin{displaymath}[({\bf A}\cdot\nabla)\,{\bf B}]_i= \sum_j\left(\frac{A_j}{h_j...
...A_i\,B_j}{h_i\,h_j}\,\frac{\partial h_i}{\partial u_j}\right).
\end{displaymath}](img4403.png) |
(1617) |
Note, incidentally, that the commonly quoted result
is only valid in Cartesian coordinate systems (for which
).
Let us define the gradient
of a vector field
as the tensor whose components in a Cartesian coordinate
system take the form
 |
(1618) |
In an orthogonal curvilinear coordinate system, the above
expression generalizes to
![\begin{displaymath}
(\nabla{\bf A})_{ij} = [({\bf e}_j\cdot\nabla)\,{\bf A}]_i.
\end{displaymath}](img4408.png) |
(1619) |
It thus follows from (1617), and the relation
, that
 |
(1620) |
The vector identity (1482) yields the
following expression for
that is valid in a general coordinate system:
 |
(1621) |
Making use of Equations (1609), (1612), and (1613), as well
as (1615) and (1616), and the tensor identity (1500), the above equation reduces (after a great deal of
tedious algebra) to the following expression for the components of
in the
,
,
coordinate system:
Note, again, that the commonly quoted result
is only valid in Cartesian coordinate systems (for which
).
Next: Cylindrical Coordinates
Up: Non-Cartesian Coordinates
Previous: Introduction
Richard Fitzpatrick
2012-04-27