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The equations for transforming between rectangular and spherical coordinates, including the forward and reverse coordinate transformations, unit vectors, and their variations. It also covers the path increment and time derivatives of the unit vectors, as well as the velocity and acceleration of a particle in spherical coordinates.
What you will learn
Typology: Lecture notes
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The forward and reverse coordinate transformations are
r = x
2
2
2
! = arctan x
2
2
, z
& = arctan y , x ( )
x = r sin! cos "
y = r sin! sin "
z = r cos!
where we formally take advantage of the two argument arctan
function to eliminate quadrant confusion.
The unit vectors in the spherical coordinate system are functions of position. It is convenient to express them in terms of
the spherical coordinates and the unit vectors of the rectangular coordinate system which are not themselves functions of
position.
r =
r
r
x
x + y
y + z
z
r
x sin! cos " +
y sin! sin " +
z cos!
z #
r
sin!
x sin " +
y cos "
" # r ˆ = x ˆ cos! cos " + y ˆ cos! sin " $ z ˆ sin!
Using the expressions obtained above it is easy to derive the following handy relationships:
r
! r
r
x cos " cos # +
y cos " sin # $
z sin " =
r
x sin " sin # +
y sin " cos # = $
x sin # +
y cos # ( )
sin " =
! r
x cos " $
y sin " = $
r sin # +
( )
! r
x sin " cos $ #
y sin " sin $ #
z cos " = #
r
x cos " sin $ +
y cos " cos $ =
$ cos "
x
y
z
r
^
!
^
"
^
!
"
r
r
We will have many uses for the path increment d
r expressed in spherical coordinates:
d
r = d r r ˆ ( )
= r ˆ dr + rd r ˆ = r ˆ dr + r
!
r
! r
dr +
!
r
!"
d " +
!
r
!#
d #
rdr +
" rd " +
We will also have many uses for the time derivatives of the unit vectors expressed in spherical coordinates:
r =
r
! r
r ˙ +
r
r
! r
r +
r
! r
r +
r sin " +
" cos "
The velocity and acceleration of a particle may be expressed in spherical coordinates by taking into account the associated
rates of change in the unit vectors:
v =
r =
rr +
r
r
v =
r
r +
! r
" r
" sin!
a =
v =
r r ˙ +
r ˙ r ˙ +
! r
! r ˙
! r
" r
" sin! +
" r ˙
" sin! +
" r
" sin! +
" r
! cos!
" sin!
r +
r
r + #
r
" cos!
r
r
! r
! cos!
r
" sin! +
" r ˙
" sin! +
" r
" sin! +
" r
! cos!
a = r ˆ " r "! r
2
! r
2
sin
2
" r
" + 2 r "
"! r
2
sin " cos "
Any (static) scalar field u may be considered to be a function of the spherical coordinates r , θ, and φ. The value of u
changes by an infinitesimal amount du when the point of observation is changed by d
r. That change may be determined
from the partial derivatives as
du =
! u
! r
dr +
! u
d " +
! u
d #.
But we also define the gradient in such a way as to obtain the result
du =
! u " d
r
Therefore,
! u
! r
dr +
! u
d " +
! u
d # =
$ u % d
r
or, in spherical coordinates,
! u
! r
dr +
! u
d " +
! u
d # =
$ u
r
dr +
$ u
"
rd " +
$ u
r sin " d #
The curl
A is also carried out taking into account that the unit vectors themselves are functions of the coordinates.
Thus, we have
r
r
r sin $
r
r + A
$
%
where the derivatives must be taken before the cross product so that
r
r
r sin $
r "
r
r sin $
r "
r
r +
$
%
r
r
$
%
r
r
r +
$
%
r
r
$
%
r sin $
r
r +
$
%
r
r
$
%
With the help of the partial derivatives previously obtained, we find
r "
r
r +
$
%
r
r
r ˆ +
$
%
r
$
, r ˆ ( )
r sin $
r
r +
$
%
r
sin $
$
cos $
%
r sin $ +
$ cos $
$
%
r
r
r
%
r ˆ +
$
r
r sin $
r
r sin $
$
r ,
%
r
%
cos $
r sin $
r
r
r
%
r sin $
$
%
cos $
r sin $
%
r sin $
r
%
r
$
r
r
$
r
r
r sin #
%
sin #
r sin #
r
& sin #
$ r
rA
%
r
$ r
rA
r
The Laplacian is a scalar operator that can be determined from its definition as
2
u =
! u
( )
r
$
r
#$
%
r sin $
#%
r
$
r
#$
%
r sin $
#%
r "
r
$
r
#$
%
r sin $
#%
$
r
#$
r
$
r
#$
%
r sin $
#%
%
r sin $
#%
r
$
r
#$
%
r sin $
#%
With the help of the partial derivatives previously obtained, we find
2
u =
r "
r
2
u
2
r
2
r
2
u
#%# r
r
2
sin %
r sin %
2
u
#&# r
r
r
2
u
r
r
r
2
u
2
& cos %
r sin
2
r sin %
2
u
r sin %
& sin %
r
2
u
& cos %
r
r
2
u
r sin % +
% cos %
r sin %
r sin %
2
u
2
2
u
2
r
r
2
2
u
2
r
cos %
r
2
sin %
r
2
sin
2
2
u
2
2
u
2
r
r
2
2
u
2
cos %
r
2
sin %
r
2
sin
2
2
u
2
r
2
r
2
r
2
sin %
sin %
r
2
sin
2
2
u
2
Thus, the Laplacian operator can be written as
2
r
2
" r
r
2
" r
r
2
sin )
sin )
r
2
sin
2
2
2