Vector Calculus - Electricity and Magnetism - Lecture Notes, Study notes of Electromagnetism and Electromagnetic Fields Theory

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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PHY481 - Lecture 3: Vector calculus
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
1. Cartesian co-ordinates
~r = (x, y, z) = xˆx+yˆy+zˆz(1)
2. Cylindrical co-ordinates
~r = (s, φ, z) = sˆs+zˆz=scos(φx+ssin(φ) ˆy+ ˆz(2)
where,
x=scos(φ); y=ssin(φ); x2+y2=s2(3)
3. Spherical polar co-ordinates
~r = (r, θ, φ) = rˆr=rsin(θ)cos(φ) ˆx+rsin(θ)sin(φy+rcos(θz(4)
where,
x=rsin(θ)cos(φ); y=rsin(θ)sin(φ); z=rcos(θ); x2+y2+z2=r2(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(φy;ˆ
φ=sin(φx+cos(φ) ˆy(6)
The first of these equations follows from Eq. (2) and the second is evident on taking projections of ˆ
φonto the x and
y directions. It is also easy to find the transformations from cylindrical to cartesian unit vectors;
ˆx=cos(φrsin(φ)ˆ
φ; ˆy=sin(φr+cos(φ)ˆ
φ(7)
The transformations in the case of polar co-ordinates are,
ˆr=sin(θ)cos(φ)ˆx+sin(θ)sin(φy+cos(θ)ˆz; (8)
which follows from Eq. (4),
ˆ
θ=cos(θ)cos(φx+cos(θ)sin(φ) ˆysin(θz; (9)
and
ˆ
φ=sin(φx+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,
ˆx=sin(θ)cos(φr+cos(θ)cos(φ)ˆ
θsin(φ)ˆ
φ; (11)
ˆy=sin(θ)sin(φr+cos(θ)sin(φ)ˆ
θ+cos(φ)ˆ
φ; (12)
and
ˆz=cos(θrsin(θ)ˆ
θ(13)
pf2

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PHY481 - Lecture 3: Vector calculus

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

  1. Cartesian co-ordinates

~r = (x, y, z) = xˆx + y ˆy + z zˆ (1)

  1. Cylindrical co-ordinates

~r = (s, φ, z) = sˆs + z zˆ = scos(φ)ˆx + ssin(φ)ˆy + ˆz (2)

where,

x = scos(φ); y = ssin(φ); x

2

  • y

2 = s

2 (3)

  1. Spherical polar co-ordinates

~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

  • y

2

  • z

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

  • u 2

ˆe 2

  • u 3

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

  • h 2

du 2

ˆe 2

  • h 3

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.