introduction to electromagnetism
TRANSCRIPT
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Electricity Magnetism
Electromagnetism
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Introduction to Electrodynamicsby D. J.Griffith
Engineering Electromagnetic by WilliamH. Hayt & J A Buck
Principles of Electromagneticsby MatthewN. O. Sadiku
Text Books To Be Referred
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James Clerk Maxwell Michael Faraday
Electromagnetic Induction
Electromagnetic Waves
Electromagnetism
Light, microwaves, x-rays, and TV and radio
transm issions are al l kinds of electrom agnet ic waves.
They are al l the same kind of wavy disturbance that
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.
A fundamental interactionbetween the magnetic field
and the presence and motionof an electric charge
Electromagnetism
A Field is any physical quantity which takes on
different values at different points in space.
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Electricity and magnetism are differentaspects ofelectromagnetism
A movingelectric charge
producesmagnetic fields
Changingmagnetic fieldsmove electric
charges
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Charges in motion (an electrical current)
produce a magnetic field
Magnetic field from electricity
A static distribution of charges
produces an electric field
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A changingmagnetic field produces an electric current in a loop surrounding the field
Electricity from changing magnetic
field (Induced Current)
(electromagnetic induction, or Faradays Law)
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The Electricity and Magnetism
A changing magnetic (electric) field produces an
electric (magnetic)field.
Electric (Magnetic)field produces force on charges
An accelerating charge produces electro-magnetic
waves (radiation)
Both electric and magnetic fields can transport energy Electric field energy used in electrical circuits.
Magnetic field carries energy through transformer.
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Waves
A changing electric field can give rise to a changing
magnetic field, and vise versa.
In an electromagnetic wave, the electric and magnetic
fields keep each other going so that it can propagate
through free space.
The energy (E) associated with the em wave is h.Thus
the frequency of oscillation determines the energy that the
wave will carry.
Higher frequency waves such as Gamma rays
carry significantly more energy than smaller
frequency waves like radio waves or visible light.An electromagnetic wave is a transverse wave, with the electric and magnetic fields
oscillating at right angles to each other.
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Electromagnetic
Radiation
Interrelated electric and magnetic fields traveling through space
All electromagnetic radiation travels at speed c = 3108 m/s invacuum. real number is 299792458.0 m/s exactly
Electromagnetic waves travel through empty space!
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An electromagnetic(EM) wave can be
described using
vectors, as it has both
magnitude anddirectional
components
It is a transverse
wave, which means it
vibrates at right
angles to the direction
in which it travels
Properties of Electromagnetic
Waves
This 3D diagram shows a plane
linearly polarized wavepropagating from left to right
with the same wave equations.
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When two or more such waves meet they can
interact in a variety of ways.
If two waves meet, and are of the same
frequency, amplitude and phase, then they willconstructively interfere with each other to
produce a wave with twice the amplitude.
If the two waves met and were out of phase by
180 then they would destructively interfere andtherefore cancel each other out .
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Examples of Electromagnetic Radiation
AM and FM radio waves (including TV signals)
Cell phone communication links
Microwaves
Infrared radiation
Light
X-rays
Gamma rays
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Uses of Electromagnetic Waves
Communication systems
One-way and two-way
Radar
Cooking (with microwaves)
Medical Imaging (X rays)
Night Vision (infrared)Astronomy (radio, wave, IR, visible, UV, gamma)
All that we experience through our eyes is conveyed by
electromagnetic radiation
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The Electromagnetic Spectrum
Relationship between frequency, speed and wavelength = c
Different frequencies of electromagnetic radiation are better suitedto different purposes.
The electromagnetic spectrum is the full range of frequencies orwavelengths at which a wave can oscillate.
The wavelength is the distance a wave will travel during one fullcycle or oscillation. What our eyes detect as visible light areelectromagnetic waves with a wavelength between 750nm and400nm.
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Electrostatics: Charges are at rest(no time-variation)Magnetostatics: Charges are in steady motion(no time-variation)Electrodynamics: Charges are in time-varyingmotion(give rise to waves that propagate and carryenergy and information)
What is Electromagnetic?
ChargeRest Motion
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What is a charge q?
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Three Universal Constants
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Fundamental Relationships
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COORDINATE SYSTEMSRECTANGULARCYLINDRICAL SPHERICAL
Choice is based onsym metry of problem
Examples:Sheets - RECTANGULARWires/Cables - CYLINDRICALSpheres - SPHERICAL
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The coordinate surfaces ofthe Cartesian coordinates(x, y, z). The z-axis isvertical and the x-axis ishighlighted in green.Thus, the red plane showsthe points with x=1, theblue plane shows the pointswith z=1, and the yellowplane shows the points withy=-1. The three surfacesintersect at the point P(shown as a black sphere)with the Cartesiancoordinates (1, -1, 1).
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The coordinate surfaces of the
cylindrical coordinates (r, , z).
The red cylinder shows thepoints with r=2, the blue plane
shows the points with z=1, and
the yellow half-plane shows the
points with =60. The z-axis
is vertical and the x-axis is
highlighted in green. The three
surfaces intersect at the point P
with those coordinates (shown
as a black sphere); the
Cartesian coordinates of P are
roughly (1.0, 1.732, 1.0).
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Illustration of spherical
coordinates. The red sphere
shows the points with r= 2,
the blue cone shows the
points with inclination (or
elevation) = 45, and the
yellow half-plane shows the
points with azimuth = 60. The zenith
direction is vertical, and the
zero-azimuth axis is
highlighted in green. Thespherical coordinates
(2,45,60) determine the
point of space where those
three surfaces intersect,
shown as a black sphere.
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Cartesian CoordinatesP(x, y, z)
Spherical Coordinates
P(r, , )
Cylindrical Coordinates
P(r, , z)
x
y
z
P(x,y,z)
z
rx
y
z
P(r, , z)
r
z
yx
P(r, , )
Orthogon al Coordinate Systems
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x
z
y
UNIT VECTORS
ji
kUnit Vector
Representation
for Rectangular
Coordinate
System
i
The Unit Vectors imply :
j
k
Points in the direction of increasing x
Points in the direction of increasing y
Points in the direction of increasing z
Rectangular Coordinate System
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Cartesian Coo rd inate
System
x y z
x y z
B B i B j B k
A A i A j A k
cos AB x x y y z zA B A B A B A B A B
Scalar Produc t
AB x y z
x y z
i j k
A B A B sin A A A
B B B
Vector Product
2 2 2
2 2 2
x y z
x y z
A A A A
B B B B
Magnitude of vector
x
y
z
AxAy
AzA
B
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x
y
z
Z plane
x plane
i
j
k
x1
y1
z1
AxAy
Az
),,( 111 zyxA
Base vector p ropert ies
. 1
0
i i j j k k
i j j k k i
i j k
j k i
k i j
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The right-handed Cartesian coordinate system indicating the coordinate planes.
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A three dimensional Cartesian coordinate system, with origin O and axis linesX, Yand
Z, oriented as shown by the arrows. The tic marks on the axes are one length unit apart.
The black dot shows the point with coordinatesX= 2, Y= 3, andZ= 4, or (2,3,4).
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METRIC COEFFICIENTS1. Rectangular Coordinates:
When a small distance is moved in x-direction, the displacement is dxSimilarly dx and dy can be generated
Unit is in meters
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Cartesian Coordinates
Differential quantities:
Length:
Area:
Volume:
dzzdyydxxld
dxdyzsd
dxdzysd
dydzxsd
z
y
x
dxdydzdv
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AREA INTEGRALS
integration over 2 delta distances
dx
dy
Example:
x
y
2
6
3 7
AREA = 7
3
6
2
dxdy = 16
Note that: z = con stant
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CYLINDRICALCOORDINATES
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The coordinate surfaces of the
cylindrical coordinates (, , z).
The red cylinder shows thepoints with r=2, the blue plane
shows the points with z=1, and
the yellow half-plane shows the
points with =60. The z-axisis vertical and the x-axis is
highlighted in green. The three
surfaces intersect at the point P
with those coordinates (shown
as a black sphere); the
Cartesian coordinates of P are
roughly (1.0, 1.732, 1.0).
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Cylindrical Coordinate
Surfaces. The three
orthogonal components, r
(green), (red), and z
(blue), each increasing at a
constant rate. The point is
at the intersection between
the three colored surfaces
VECTOR REPRESENTATION: CYLINDRICAL
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VECTOR REPRESENTATION: CYLINDRICAL
COORDINATES
Cylindrical representation uses: r ,f, z
zzrr aAaAaAA
ff
r r z z A B A B A B A B
UNIT VECTORS:
zraaa f
ScalarProduct
1
1
1
r r
z z
a a
a a
a a
is azimuth angleP (r, , z)
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r
f
z
P
x
z
y
VECTOR REPRESENTATION: UNIT VECTORS
Cylindrical Coordinate System
za
fa
ra
The Unit Vectors imply :
za
Points in the direction of increasing r
Points in the direction of increasing
Points in the direction of increasing z
ra
fa
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METRIC COEFFICIENTSCylindrical Coordinates:
Distance = r df
x
y
dfr
Differential Distances: ( dr, rdf, dz )dris infinitesimal displacement alongr,
r d is along and
dz is along zdirection.
y
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Differential quantit ies:
Length element:
Area element:
Volume element:
r r z z
r z
dl a dl a dl a dl
dl a dr a r d a dz
f
f
f
ff
rdrdasd
drdzasd
dzrdasd
zz
rr
dzddrrdv f
Limits of integration ofr, , are 0
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Show that Volume of a Cylinder of radiusR and height H is
HR
dzdrdr
dzddrrdvV
R H
v
2
0
2
0 0
HR2
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Find out the are of curved surface of a rightcircular cylinder of radius 2m, height 5mand phi is 0 to 2pi.
R is constant,
Radial component of area = dAr
2
2
0 0
20
2
m
R H
dzrddA
H
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Physical systems which have cylindrical
often most conveniently treated by usin
coordinates.
1.Cylindrical capacitor
2.Electric field of line charge.
Appl icat ions
I l t lid l k d t
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SPHERICAL COORDINATESIn last slides we looked atcylindrical coordinates -- a
system of coordinates
that is very useful whenthe important things about
a three-dimensionalpoint
are its distance from the
z-axis and its angle from
the positive xy-plane.Now we look at situations
in which the important
things about a point are
its distance from theorigin and, using terms
from geography, its
latitude and longitude. In
this situation we use
spherical coordinates.
The f i rs t of these coordinates -- r--
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The f i rs t of these coordinates r
denotes the point 's d is tance from the
or ig in. The movie below shows the sets
o f po in ts w ith rho = 0.2, 0.3, ... 1.0.
-- -- .Think of yourself as located at the origin with your right hand
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Think of yourself as located at the origin with your right hand
pointing straight upward along the positive z-axis. Then face
the point in question and lower your right hand until it is
pointing at this point. The angle by which your right hand is
lowered is the coordinate phi. Notice if theta = 0 then the point
is on the positive z-axis; if theta = pi / 2 then the point is in the
xy-plane; and if theta = pi then the point is on the negative z-
axis. The movie below shows points with constant values of
theta for theta = 0, pi / 16, 2 pi / 16, ... pi.
The third coord inate --
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The third coord inate
ph i-- is ident ical to the
coordinate theta used
in cyl indr icalcoordinates. It
measures the angle
from the posi t ive xz-
plane to the po int. Themovie below shows
points wi th constant
values o f theta.
This system o f coo rdinates is very sim ilar to the system --long i tude
and lat i tude-- of coord inates used to descr ibe po ints on the earth's
surface.
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SPHERICAL COORDINATES
r
f
P
x
z
y
Spher ical representation uses: r,, fUNI T VECTORS:
f
aaar
ff aAaAaAA rr
is zenith angle( starts from +Z reaches up toZ) ,
is azimuth angle (starts from +X direction and lies in x-y plane )
P (r, , )
Illustration of spherical
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p
coordinates. The red
sphere shows the
points with r = 2, the
blue cone shows thepoints with inclination
(or elevation) = 45,
and the yellow half-
plane shows thepoints with
azimuth = 60. The
zenith direction is
vertical, and the zero-
azimuth axis is
highlighted in green.
The spherical
coordinates
(2,45,60) determine
r
f
UNIT VECTORS
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UNIT VECTORS
Spherical Coordinate System
r
f
P
x
z
y
a
fa
ra
The Unit Vectors imply :
Points in the direction of increasing r
Points in the direction of increasing
Points in the direction of increasing ra
fa
a
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Spherical Coordinates
Limits of integration ofr, , are 0
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Show that Volume of a sphere of radius R is
2
22
0 0 0
3
3
sin
sin
2 23
4
3
v
R
V dv r dr d d
r dr d d
R x x
R
f
f
34
3R
C CO C S
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Representation of differential length (length element) dl in different coordinate systems:
x y zdl dxa dya dza
r zdl dr a r d a dza
sin rdl dr a r d a r d a
rectangular
cylindrical
spherical
METRIC COEFFICIENTS
Spherical Coordinates
dRdl
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Differential quantities:
Length Element:
Area Element:
Volume Element:
dRRddRR
dldldlRld R
sin
dsinRdl
Rddl
dRdlR
ddRdsinRdv
2
RdRd
dldl
sd
dRdsinRdldlsd
ddsinRRdldlRsd
R
R
R
2
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Physical systems which have spherical symmetry are often mostconveniently treated by using spher ical polar coordinates.
1. I f the potential of the physical system to be examined is
spherical ly symmetr ic, then the Schrodinger equation inspherical coordinates can be used to advantage.
2. Electr ic potential of sphere
Applications of Spherical Coordinate
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