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Prof. David R. JacksonECE Dept.
Fall 2014
Notes 6
ECE 2317 Applied Electricity and Magnetism
Notes prepared by the EM Group University of Houston
1
Review of Coordinate Systems
An understanding of coordinate systems is important for doing EM calculations.
2
x
y
z
P (x, y, z)
Kinds of Integrals That Often Occur
20
ˆ
4
C
AB
C
C
v
V
Q d
V E dr
RE d
R
Q dV
(scalar integral,
scalar result)
(vector integral,
scalar result)
(vector integral,
vector result)
(scalar integral,
scalar re
Line
integrals :
Volume
integrals :2
0
ˆ
4v
V
RE dV
R
sult)
(vector integral,
vector result)
20
ˆ
ˆ
4
s
S
S
s
S
Q dS
I J n dS
RE dS
R
(scalar integral,
scalar result)
(vector integral,
scalar result)
(vector integral,
vector result)
Surface
integrals :
We wish to be able to perform all of these in various coordinates.
3
Rectangular Coordinates
ˆ ˆ ˆr xx yy zz
Short hand notation:
, ,r x y z
Note: Different notations are used for vectors in the books.4
Position vector:
zz
yyxx
x
y
z
r
P (x,y,z)
Note: A unit vector direction is defined by increasing one coordinate variable while keeping the other two fixed.
Note: We have the “tip to tail” rule when adding vectors.
Rectangular Coordinates
dV dx dy dz
5
We increment (x, y, z) starting from an initial
point (blue dot).
dxdy
dz
dS = dxdy
dS = dxdz
dS = dydzx
y
z
Rectangular (cont.)
ˆ ˆ ˆdr x dx y dy z dz
Path Integral (we need dr)
Note on notation: The symbol dl is often used instead of dr .
ˆ ˆ ˆr xx yy zz
6
x
y
z
A
BC
dr
r r+dr
Cylindrical Coordinates
2 2
1
cos
sin
tan /
x
y
z z
x y
y x
z z
x
y
z
.z
P (, , z)
7
x
y
Cylindrical (cont.)
Unit Vectors
Note: and depend on (x, y)
x
y
x
y
z
.
z
This is why we often prefer to express them in terms of
ˆ ˆx yand
Note: A unit vector direction is defined by increasing one coordinate variable
while keeping the other two fixed.
8
1 2
1
1
ˆ ˆ ˆ ˆ ˆ ˆ
ˆ ˆ
ˆ ˆ cos
cos
x A x x A y x
A x
x
A
2 ˆ ˆ
cos2
sin
A y
Hence, we have ˆ ˆ ˆcos sinx y
x
y
1 2
ˆ ˆ ˆA x A y Assume
Similarly,Then we have:
Cylindrical (cont.)
so
Expressions for unit vectors (illustrated for )
9
ˆ ˆ ˆcos sin
ˆ ˆ ˆsin cos
ˆ ˆ
ˆˆˆ cos sin
ˆˆˆ sin cos
ˆ ˆ
x y
x y
z z
x
y
z z
Summary of Results
Cylindrical (cont.)
10
Cylindrical (cont.)
11
2 2
ˆ ˆˆ ˆ ˆcos sin cos sin cos sin
ˆ ˆcos sin
ˆ ˆ
r zz
zz
zz
ˆ ˆ ˆr xx yy zz
x
y
z
.
z
r
Substituting from the previous tables of unit vector transformations and coordinate transformations, we have
Example: Express the r vector in cylindrical coordinates.
Cylindrical (cont.)
12
x
y
z
.
z
r
ˆ ˆr zz
zz
ˆˆ ˆr zz Note:
dV d d dz
Note: dS may be in three different forms.
Cylindrical (cont.)
13
We increment (, , z) starting from an initial
point (blue dot).
Differentials
x
y
z
dS = d d
dS = d dzdS = d dz d d
dz
x
y
d
x
y
z
dz
ˆdr d ˆdr d ˆdr z dz
Path Integrals
First, consider differential changes along any of the three coordinate directions.
y
x
d
d
Cylindrical (cont.)
14
In general:
ˆˆ ˆdr d d z dz
Cylindrical (cont.)
2 2 2d dr d d dz
15
Note: A change is z is not shown, but is possible.
If we ever need to find the length along a contour:
x
y
dr
ˆ d
d
C
Spherical Coordinates
x
Note: = r sin
y
z
.z
P (r, , )
r
16
Note: 0
x
y
z
.
P (r, , )
r z
Spherical (cont.)
2 2 2
1
1
sin cos
sin sin
cos
cos /
tan /
x r
y r
z r
r x y z
z r
y x
Note: = r sin
17
y
z
.z
P (r, , )
r
x
Spherical (cont.)
Note: , and depend on (x, y, z). r
Unit Vectors
18
x
y
z
r
Note: A unit vector direction is defined by increasing one coordinate variable
while keeping the other two fixed.
Spherical (cont.)
ˆ ˆ ˆ ˆsin cos sin sin cos
ˆ ˆ ˆcos cos cos sin sin
ˆ ˆ ˆsin cos
ˆˆ ˆ sin cos cos cos sin
ˆˆ ˆ sin sin cos sin cos
ˆˆ cos sin
r x y z
x y z
x y
x r
y r
z r
Transformation of Unit Vectors
19
x
y
z
r
Spherical (cont.)
20
ˆˆ sin cos cos cos sin sin cos
ˆˆ sin sin cos sin cos sin sin
ˆ cos sin cos
r r r
r r
r r
ˆ ˆ ˆr xx yy zz
x
y
z
r
r
Example: Express the r vector in spherical coordinates.
Substituting from the previous tables of unit vector transformations and coordinate transformations, we have
Spherical (cont.)
21
ˆr rr
After simplifying:
ˆ ˆˆr rr Note:
x
y
z
r
r
Spherical (cont.)Differentials
dS = r2 sin d d
2 sindV r dr d d
Note: dS may be in three different forms (only one is shown). The other two are:
dS = r dr ddS = r sin dr d
22
x
y
z d = r sin d
drr d
d
d
We increment (r, , ) starting from an initial point (blue dot).
Spherical (cont.)
ˆdr r dr
x
y
z drr
x
y
z
d
dr
ˆdr r d ˆ sindr r d
ˆ ˆˆ sindr r dr rd r d
Path Integrals
23
x
y
z
drd
r
sind r d
Note that the formula for the dr vector never changes, no matter which direction we go along a path (we never add a minus sign!).
Note on dr Vector
24
ˆˆ ˆdr d d z dz
Example: integrating along a radial path in cylindrical coordinates.
ˆdr d
B
AB
A
V E dr
x
y
A
B
dr
0d
C
x
y A
B
dr
0d
C
B
A
ABV E d
This form does not change, regardless of which limit is larger.
Example
Given:
Find the current I crossing a hemisphere (z > 0) of radius a, in the outward direction.
25
2ˆ [A/m ]J x x
x
y
z
ˆ ˆn r
J
Example (Cont.)
26
2 2
ˆ
ˆ
ˆ ˆ
sin cos
sin cos
sin cos sin cos
sin cos
S
S
x
S
x
S
S
S
S
I J n dS
J r dS
x J r dS
J dS
x dS
a dS
a dS
ˆ ˆ ˆ ˆsin cos sin sin cos
ˆ ˆ ˆcos cos cos sin sin
ˆ ˆ ˆsin cos
ˆˆ ˆ sin cos cos cos sin
ˆˆ ˆ sin sin cos sin cos
ˆˆ cos sin
r x y z
x y z
x y
x r
y r
z r
sin cos
sin sin
cos
x r
y r
z r
Example (Cont.)
27
2 2
2 /22 2 2
0 0
2 /23 2 2
0 0
/23 2
0
/23 3
0
3
sin cos
sin cos sin
sin cos sin
sin sin
sin
2
3
S
I a dS
a a d d
a d d
a d
a d
a
2
2
0
1cos 2
2d
Note :
/23
0
2sin
3d
Note :
32[A]
3I a
Appendix
28
Here we work out some more examples.
ExampleP1 (4, 60 , 1)
P2 (3, 180 , -1)
d = 6.403 [m]
2 2 2
1 2 1 2 1 2d x x y y z z
cos
sin
x
y
z z
1
1
1
4cos 60 2
4sin 60 3.4641
1
x
y
z
2
2
2
3cos 180 3
3sin 180 0
1
x
y
z
Find d = distance between points
Given: Cylindrical coordinates (, , z)with distances in meters
29
This formula only works in rectangular
coordinates!
Example
Given: v = -310-8 (cos2 / r4) [C/m3] , 2 < r < 5 [m]
Solution:
2
2
0 0
28 2
20 0
28 2
20 0
, sin
13 10 cos sin
13 10 cos sin
v
V
b
v
a
b
a
b
a
Q dV
r r drd d
drd dr
d dr dr
x
y
z
b
a
a = 2 [m], b = 5 [m]
Find Q
“A sphere with a hole in it”
30
Note: The integrand is separable and the limits are fixed.
Example (cont.)
2 22
0 0
2
0
2
00
1 cos 2cos
2
1 sin 2
2 4
1 1
1 13/10
sin cos 2
bb
aa
d d
drr r
a b
d
Q = -5.65510-8 [C]
31
Note: The average value of cos2 is 1/2.
22
0
1cos 2
2d
Example
Derive ˆˆ cos sinz r
1 2 3
ˆˆz r A A A
1 ˆˆA z r
2 ˆA z
3ˆˆA z
Let
32
Then
Dot multiply both sides with ˆˆ, ,r
Example (cont.)
1
1
ˆˆ
ˆˆ cos
cos
A z r
z r
A
2
2
ˆ
ˆ cos2
sin
A z
z
A
3
3
ˆˆ
ˆ 0
0
A z
z
A
ˆˆ cos sinz r Result:
x
y
z
rz
z
x
y
z
x
y
z
z
33
1 2 3
ˆˆz r A A A
Example
Derive ˆ ˆ ˆ ˆsin cos sin sin cosr x y z
1
2
3
ˆ ˆ ˆ
ˆ ˆ ˆ
ˆ ˆˆ
A r x x r
A r y y r
A r z z r
component of
component of
component of
Let 1 2 3ˆ ˆ ˆ ˆr x A y A z A
An illustration of finding the x component of r
34
Dot multiply both sides with ˆ ˆ ˆ, ,x y z
x
y
z
r
L
Example (cont.)
ˆ ˆ cos sin cosr x L
ˆ ˆ ˆ ˆsin cos sin sin cosr x y z Result:
ˆ ˆ sin sin sinr y L
Hence
cos sin2
L
Similarly,
ˆ ˆ cosr z
Also,
35
x
y
z
x
L
r
( / 2) -
Example (Part 1)
Find VAB using path C shown below.
2ˆ ˆ ˆ3 2 1E x xy y xy z z
2
02
1
3
1
3 1 1
B B
AB x y z
A A
B
A
AB
V E dr E dx E dy E dz
xy dx xy dy
y x dy dx
V x x x x dx
x
y
1
11y x
x
y
z
C
(0,1,0)
(1,0,0)
.E (x,y,z)
B
A
Top view
36
(This is not an electrostatic field.)
Example (cont.)
02
1
02 2 3
1
12 2 3
0
13 2
0
3 1 1
3 3 2
3 3 2
2
1 1 1 3 4 12 52
4 3 2 12 12
ABV x x x x dx
x x x x x dx
x x x x x dx
x x x dx
Completing the calculus:
VAB = -5/12 [V]
37
Example (cont.)Alternative calculation (we parameterize differently):
38
0 1
2
1 0
3
B B
AB x y z
A A
V E dr E dx E dy E dz
xy dx xy dy
0 12
1 0
0 12 2 3
1 0
3 1 1
3 3
3 1 11
2 3 4
ABV x x dx y y dy
x x dx y y dy
1y x
VAB = -5/12 [V]
Example (Part 2)
Find VAB using path C shown below.
2ˆ ˆ ˆ3 2 1E x xy y xy z z
2
02 2
0
0 1
1 0
3
3 3
0 0
0
B B
x y z
A A
B
A
B
A
E dr E dx E dy E dz
xy dx xy dy
xy dx xy dy xy dx xy dy
dx dy
(same field as in Part 1)
VAB = 0 [V]39
x
y
z
C
(0,1,0)
(1,0,0)
E (x,y,z)
B
A
Example
VAB = -7/6 [V]
Find VAB using an arbitrary path C in the xy plane.
2ˆ ˆ ˆ3 2E x x y y z z
2
0 12
1 0
1 12
0 0
3
3
3
1 13
2 3
7 / 6
B B
x y z
A A
B
A
AB
E dr E dx E dy E dz
x dx y dy
x dx y dy
V x dx y dy
Note: The path does not have to be parameterized: Hence, only the endpoints
are important.
The integral is path independent!
(This is a valid electrostatic field.)
40
x
y
z
C
(0,1,0)
(1,0,0)
E (x,y,z)
B
A
Example ˆ ˆ 2E x x y y
ˆˆ ˆ
ˆ 3
cos 3cos
sin 3sin
ˆˆˆ cos sin
ˆˆˆ sin cos
B
AB
A
V E dr
dr d d zdz
d
x
y
x
y
Ax
C
3 [m]
B
y
Find VAB using path C shown below.
41
Example (cont.)
VAB = 9/2 [V]
ˆ ˆˆ ˆcos sin 3cos sin cos 2 3sinE ˆ 3dr d
Note: The angle must change continuously along the path. If we take the angle to be / 2 at point B, then the
angle must be - at point A.
42
/2
/2
/2
9sin cos
9sin 2
2
cos 29
2 2
9 1 1 9
2 2 2 2
ABV d
d
9 18 sin cos 9sin cosE dr d d
ˆ ˆ 2E x x y y
Example (cont.)
ˆ ˆ 2E x x y y
Ax
C
3 [m]
B
y
Question: Is this integral path independent?
B
AB
A
V E dr
43
Let’s examine this same electric field once again:
Note: The answer is yes because the curl of the electric field is zero, but we do not know this yet.
Example (cont.) ˆ ˆ 2E x x y y
Ax
C
3 [m]
B
y
Let’s find out:B
AB
A
V E dr
0 3
3 0
2
2
99
2
9 / 2
B B
x y z
A A
B
A
E dr E dx E dy E dz
x dx y dy
x dx y dy
Yes, it is path independent!
VAB = 9/2 [V]
44