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This is the Lecture Notes of Electricity and Magnetism which includes Vector Potential, Boundary Conditions, Vector Derivative Operator, Vector Calculus, Vector Calculus, Three Co-Ordinate Systems, Two Types of Charge, Coulomb's Law, Electric Field etc. Key important points are: Vector Calculus, Three Co-Ordinate Systems, Cartesian Co-Ordinates, Unit Vector Transformations, Scale Factors, Spherical Polar Cases, Cylindrical Co-Ordinates, Orthogonal Co-Ordinate Systems
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Griffiths: Chapter 1 (Pages 38-54), Also Appendix A of Griffiths
Vector calculus in three co-ordinate systems
We shall be using three orthogonal co-ordinate systems, cartesian, cylindrical and spherical polar that are defined
as follows
~r = (x, y, z) = xˆx + y ˆy + z zˆ (1)
~r = (s, φ, z) = sˆs + z zˆ = scos(φ)ˆx + ssin(φ)ˆy + ˆz (2)
where,
x = scos(φ); y = ssin(φ); x
2
2 = s
2 (3)
~r = (r, θ, φ) = rˆr = rsin(θ)cos(φ)ˆx + rsin(θ)sin(φ)ˆy + rcos(θ)ˆz (4)
where,
x = rsin(θ)cos(φ); y = rsin(θ)sin(φ); z = rcos(θ); x
2
2
2 = r
2 (5)
Unit vector transformations
Relations between unit vectors in the three co-ordinate systems are very useful and can be derived using geometric
reasoning. First consider cylindrical co-ordinates. It is easy to see that,
ˆs = cos(φ)ˆx + sin(φ)ˆy;
φ = −sin(φ)ˆx + cos(φ)ˆy (6)
The first of these equations follows from Eq. (2) and the second is evident on taking projections of
φ onto the x and
y directions. It is also easy to find the transformations from cylindrical to cartesian unit vectors;
xˆ = cos(φ)ˆr − sin(φ)
φ; yˆ = sin(φ)ˆr + cos(φ)
φ (7)
The transformations in the case of polar co-ordinates are,
ˆr = sin(θ)cos(φ)ˆx + sin(θ)sin(φ)ˆy + cos(θ)ˆz; (8)
which follows from Eq. (4),
θ = cos(θ)cos(φ)ˆx + cos(θ)sin(φ)ˆy − sin(θ)ˆz; (9)
and
φ = −sin(φ)ˆx + cos(φ)ˆy (10)
which is the same as the second of Eq. (6). The equations relating unit vectors in spherical polars to those in cartesian
co-ordinates are,
xˆ = sin(θ)cos(φ)ˆr + cos(θ)cos(φ)
θ − sin(φ)
φ; (11)
yˆ = sin(θ)sin(φ)ˆr + cos(θ)sin(φ)
θ + cos(φ)
φ; (12)
and
zˆ = cos(θ)ˆr − sin(θ)
θ (13)
Curvilinear co-ordinates: Scale factors h 1
, h 2
, h 3
In general a set of curvilinear co-ordinates can be orthogonal or non-orthogonal. We focus on the orthogonal case,
which includes cartesian, cylindrical and spherical co-ordinates. We denote the unit vectors as ˆe 1
, ˆe 2
, ˆe 3
, and a position
vector
l is written as,
l = (u 1
, u 2
, u 2
) = u 1
eˆ 1
ˆe 2
ˆe 3
For the Cartesion, Cylindrical, and Spherical Polar cases, we may write (u 1 , u 2 , u 2 ) = (x, y, z), (s, 0 , z), (r, 0 , 0) respec-
tively.
Now imagine displacing the co-ordinates by a small amount du 1 , du 2 , du 3 , this leads to a change in the vector
l by
an amount d
l. In general we can write
d
l = h 1
du 1
eˆ 1
du 2
ˆe 2
du 3
ˆe 3
where h 1 , h 2 , h 3 are the scale factors. They are central to deriving the relations that we need. For the three cases of
interest in this course, we have,
d
l = dxˆx + dy yˆ + dz ˆz; d
l = dssˆ + sdφ
φ + dz zˆ d
l = drrˆ + rdθ
θ + rsin(θ)dφ
φ (16)
leading to: For cartesian co-ordinates, h x
= 1, h y
= 1, h z
= 1; for cylindrical co-orindates, h s
= 1, h φ
= s, h z
= 1; and
for spherical polar co-ordinates, hr = 1, hθ = r, hφ = rsinθ.