review vector analysis
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Review of Vector Analysis
Vector analysis is a mathematical tool with whichelectromagnetic (EM) concepts are most conveniently
expressed and best comprehended.
A quantity is called a scalar if it has only magnitude (e.g.,
mass, temperature, electric potential, population).
A quantity is called a vector if it has both magnitude and
direction (e.g., velocity, force, electric field intensity).
The magnitude of a vector is a scalar written as A or
AA
A
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A unit vector along is defined as a vector whose
magnitude is unity (that is,1) and its direction is along
A
A
A
AeA !!
)(A
1!
Thus
Ae
which completely specifies in terms ofA and itsdirection Ae
A
AeAA !
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A vector in Cartesian (or rectangular) coordinates may
be represented as
or
where AX, Ay, and AZ are called the components of in the
x, y, and z directions, respectively; , , and are unitvectors in the x, y and z directions, respectively.
zzyyxx eAeAeA )A,A,A( zyx
A
A
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xe
ze
ye
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Suppose a certain
vector is given by
The magnitude orabsolute value ofthe vector is
(from the Pythagorean theorem)
zyx e4e3e2V !V
385.5432V 222 !!
V
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The Radius Vector
A point P in Cartesian coordinates may be represented by
specifying (x, y, z). The radius vector (or position vector) of
point P is defined as the directed distance from the origin O
to P; that is,
The unit vector in the direction ofr is
zyx ezeyexr !
r
r
zyx
ezeyexe zyxr !
!
222
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Vector Algebra
Two vectors and can be added together to give
another vector ; that is ,
Vectors are added by adding their individual components.
Thus, if and
A B
C
BAC !
zzyyxx eAeAeA zzyyxx eBeBeBB !
zzzyyyxxx e)BA(e)BA(e)BA(C !
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Parallelogram Head torule tail rule
Vector subtraction is similarly carried out as
zzzyyyxxx e)BA(e)BA(e)BA(D
)B(ABAD
!
!!
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The three basic laws of algebra obeyed by any given vector
A, B, and C, are summarized as follows:
Law Addition Multiplication
Commutative
Associative
istributive
where k and l are scalars
ABBA !
C)BA()CB(A !
AA !
A)l()Al(!
BkAk)BA(k !
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When two vectors and are multiplied, the result is
either a scalar or a vector depending on how they are
multiplied. There are two types of vector multiplication:
1. Scalar (or dot) product:
2.Vector (or cross) product:
The dot product of the two vectors and is defined
geometrically as the product of the magnitude of and the
projection of onto (or vice versa):
where is the smaller angle between and
A
ABcosABBA
U!
BA
B
ABU
A
BA v
A B
B
B
A B
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If and then
which is obtained by multiplying and component by
component
),A,A,A(A ZYX! )B,B,B(B ZYX!
ZZYYXX BABABABA !
A B
ABBA !
CABACBA ! )(
A A ! A2
!A2
eX ex ! ey ey ! eZ ez !1
e ey ! ey ez ! e ex ! 0
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The cross product of two vectors and is defined as
where is a unit vector normal to the plane containing
and . The direction of is determined using the right-
hand rule or the right-handed screw rule.
A
A
nABesinABBA U!
B
B
e
ne
BA
irection ofand using(a) right-hand rule,(b) right-handed
screw rule
ne
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If and then
zyx
zyx
zyx
BBBAAA
eee
BA !
),A,A,A(AZYX
! )B,B,B(BZYX
!
zxyyxyzxxzxyzzy e)BABA(e)BABA(e)BABA( !
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Note that the cross product has the following basic
properties:
(i) It is not commutative:
It is anticommutative:
(ii) It is not associative:
(iii) It is distributive:
(iv)
ABB
A v{v
ABBA v!v
)BA()B(A vv{vv
CABACBA vv!v )(
0AA ! )0(sin !U
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Also note that
which are obtained in cyclic permutation and illustrated
below.
yxz
xzy
zyx
eeeeee
eee
!!
!
Cross product using cyclic permutation: (a) moving clockwise leads to positive results;
(b) moving counterclockwise leads to negative results
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Line Integrals
A line integral of a vector field can be calculated whenever a
path has been specified through the field.
The line integral of the field along the path P is defined asV
U!2
1
P
PPdlcosVdlV
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For segment P3,
dl!dxex (the differentiallengthdl pointsto the left)
oo
xx
x
xxo
P
xV-)edx()eV(dlVo
!! !
!03
0
4
! dlVP
field)ive(conservat00xV0xVI ooooP P PP 2 3 41
!!!
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Example. Let the vector field be given by .
Find the line integral of over the semicircular path shown
below
xoeVV !
V
V
Consider the contribution ofthe path segment located atthe angle 5
dl ! dl cos Jex
dl sin Jey
Since J ! U - 90 r
cos J ! cos( U - 90 r) ! sin U
sin J ! sin( U - 90 r) ! cos U
dl ! dl sin Uex
dl cos Uey
! adUdl
{ (sin Uex cos Uey )
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]
o
oo
yxxxo
yxxo
aV
aVdaV
deeeeaV
adeeeVI
2
)0cos180cos(sin
])(cos)([sin
)cos(sin)(
11
180
0
0
180
0 1
180
0
!
r!!
!
!
r
r
r!
!
UU
UUU
UUUU
U
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Surface Integrals
Surface integration amounts to adding up normal
components of a vector field over a given surface S.
We break the surface S into small surface elements and
assign to each element a vector
is equal to the area of the surface element
is the unit vector normal (perpendicular) to the surface
element
nedsds !
ne
ds
The flux ofa vectorfieldAthrough
surface S
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(IfS is a closed surface, is by convention directed
outward)
Then we take the dot product of the vector field at theposition of the surface element with vector . The result is
a differential scalar. The sum of these scalars over all the
surface elements is the surface integral.
is the component of in the direction of (normal
to the surface). Therefore, the surface integral can be
viewed as the flow (or flux) of the vector field through the
surface S
(the net outward flux in the case of a closed surface).
ds
ds
ds
V
UcosV
U! cosdsVdsV
V
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Example. Let be the radius vector
The surface S is defined by
The normal to the surface is directed in the +z direction
Find
V
dyddxd
cz
!
S
dsV
zyx
ezeyexV !
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V is not perpendicular to S, except at one point on the Z axis
Surface S
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5! SS cosdsVdsV
c4d(-d)]-2dc[d
dx)]d(d[cdydxcyx
ccyxdsV
cyx
ccosdxdydscyxV
2
dx
dx
dscos
222
dx
dx
dy
dy
V
222
S
222
222
!!
!
!
!U!!
!
!
U
!
!
!
!
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Introduction to ifferential Operators
An operator acts on a vector field at a point to produce
some function of the vector field. It is like a function of a
function.
If O is an operator acting on a function f(x) of the single
variable X , the result is written O[f(x)]; and means thatfirst f acts on X and then O acts on f.
Example. f(x) = x2 and the operator O is (d/dx+2)
O[f(x)]=d/dx(x2 ) + 2(x2 ) = 2x +2(x2 ) = 2x(1+x)
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An operator acting on a vector field can produce
either a scalar or a vector.
Example. (the length operator),Evaluate at the point x=1, y=2, z=-2
Thus, O is a scalar operator acting on a vector field.
Example. , ,
x=1, y=2, z=-2
Thus, O is a vector operator acting on a vector field.
)]z,y,x(V[O
O(A) ! A A yx ezey3V !)V(O
scalar32.640zy9VV)V(O 22 n!!!!
A2AAA)A(O ! yx ezey3V !
vectore65.16e49.95e4e1240)e2e(6
ez2ey6zy9)ezey3()V(O
yx
yxyx
yx22
yx
n!!
!
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Vector fields are often specified in terms of their rectangular
components:
where , , and are three scalar features functions of
position. Operators can then be specified in terms of ,
, and .
The divergence operator is defined as
zzyyxx e)z,y,x(Ve)x,y,x(Ve)z,y,x(V)z,y,x(V !
xV yV zV
zyx Vz
Vy
Vx
Vx
x
x
x
x
x!
xV
yV zV
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Example . Evaluate at the
point x=1, y=-1, z=2.zyx
2 e)x2(eyexV ! V
0Vz
1Vy
x2Vx
x2VyVxV
zyx
zy
2
x
!x
x!
x
x!
x
x
!!!
31x2V !!
Clearly the divergence operator is a scalar operator.
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1. - gradient, acts on a scalar to produce a vector
2. - divergence, acts on a vector to produce a scalar
3. - curl, acts on a vector to produce a vector
4. -Laplacian, acts on a scalar to produce a scalar
Each of these will be defined in detail in the subsequent
sections.
V
V
Vv
V2
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Cartesian coordinates (x,y,z)
The ranges of the coordinate variables are
A vector in Cartesian coordinates can be written as
The intersection of threeorthogonal infinite places
(x=const, y= const, and z =const)
defines point P.
gg
gg
gg
z
y
x
zzyyxxzyx eAeAeAor)A,A,A(
A
Constant x, y and z surfaces
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zyx edzedyedxdl !
Differential elements in the right handed Cartesian coordinate system
dxdydzd !R
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z
y
x
adxdy
adxdz
adydzdS !
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Cylindrical Coordinates .
- the radial distance from the z axis- the azimuthal angle, measured from the x-axis in the xy plane
- the same as in the Cartesian system.
A vector in cylindrical coordinates can be written as
Cylindrical coordinates amount to a combination of
rectangular coordinates and polar coordinates.
)z,,( JV
gg
TJe gVe
z
200
2/12
z
22
zzz
)AAA(A
eAeAeAor)AA,A(
!
JV
JJVVJV
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Positions in the x-y plane are determined by the values of
Relationship between (x,y,z) and )z,,( JV
JV and
zzx
ytanyx 122 !!J!V
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JV
VJ
JV
!v
!v
!v
eee
eee
eee
z
z
z
0eeeeee
1eeeeee
z
zz
!!!
!!!
VJJJV
JJVV
Point Pand unit vectorsin the cylindricalcoordinate system
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zand,JV
semi-infiniteplane with itsedge alongthe z - axis
Constant surfaces
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Differential elements in cylindrical coordinates
Metric coefficient
zp adzadaddl JVV! J
dzdddv JVV!
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Planar surface( = const)
Cylindricalsurface
( =const)
dS! VdJdzaV dVdzaJ
VdJdVaz
Planar surface( z =const)J
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Spherical coordinates .
- the distance from the origin to the point P
- the angle between the z-axis and the radius
vector of P
- the same as the azimuthal angle incylindrical coordinates
),,r( JU
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0 e r0 e5 T
Colatitude(polarangle)
1 24 34
0 e * 2T
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2/1222
r
rrr
)AAA(A
eAeAeAor)AA,A(
JU
JJUUJU
!
UJ
JU
JU
!v
!v
!v
eee
eee
eee
r
r
r
0eeeeee
1eeeeee
rr
rr
!!!
!!!
JJUU
JJUU
A vector A in spherical coordinates may bewritten as
Point Pand unit vectors in sphericalcoordinates
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U!
JU!
JU!
cosrz
sinsinry
cossinrx
22
11-22
1222
yx
xcos
x
yt n
z
yxt nzyxr
!!J
!U!
rzcos
zt n 11 !V!U
Rel tionships between sp ce v ri bles )z,,(
nd),,,r(),z,y,x( JVJU
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JU nd,,rConst nt surf ces
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Differential elements in the spherical coordinate system
JU JUU! adsinrardadrdl r
JUU! ddrdsinrdv 2
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J
U
J
JU
JUU!
adrdr
adrdsinr
addsinrdS r2
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e e o ecto a ys se e o ecto a ys s
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yy