poisson’s and laplace’s equation

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Gandhinagar Institute Of Technology Subject Field Theory (2140909) Branch Electrical Topic – Poisson’s and Laplace’s Equation

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Page 1: Poisson’s and Laplace’s Equation

Gandhinagar Institute

Of Technology

Subject – Field Theory (2140909)

Branch – Electrical

Topic – Poisson’s and Laplace’s Equation

Page 2: Poisson’s and Laplace’s Equation

Name Enrollment No.

Abhishek Chokshi 140120109005

Himal Desai 140120109008

Dheeraj Yadav 140120109010

Guided By – Prof. Supraja Ma’am

Page 3: Poisson’s and Laplace’s Equation

Laplace’s and Poisson’s Equation

We have determined the electric field 𝐸 in a region using

Coulomb’s law or Gauss law when the charge distribution is

specified in the region or using the relation 𝐸 = −𝛻𝑉 when the

potential V is specified throughout the region.

However, in practical cases, neither the charge distribution nor

the potential distribution is specified only at some boundaries.

These type of problems are known as electrostatic boundary

value problems.

For these type of problems, the field and the potential V are

determined by using Poisson’s equation or Laplace’s equation.

Laplace’s equation is the special case of Poisson’s equation.

Page 4: Poisson’s and Laplace’s Equation

For the Linear material Poisson’s and Laplace’s equation can

be easily derived from Gauss’s equation

𝛻 ∙ 𝐷 = 𝜌𝑉But,

𝐷 =∈ 𝐸

Putting the value of 𝐷 in Gauss Law,

𝛻 ∗ (∈ 𝐸) = 𝜌𝑉From homogeneous medium for which ∈ is a constant, we write

𝛻 ∙ 𝐸 =𝜌𝑉∈

Also, 𝐸 = −𝛻𝑉

Then the previous equation becomes,

𝛻 ∙ (−𝛻𝑉) =𝜌𝑉∈

Or,

𝛻 ∙ 𝛻𝑉 = −𝜌𝑉∈

Page 5: Poisson’s and Laplace’s Equation

𝛻2𝑉 = −𝜌𝑉∈

This equation is known as Poisson’s equation which state that

the potential distribution in a region depend on the local

charge distribution.

In many boundary value problems, the charge distribution is

involved on the surface of the conductor for which the free volume charge density is zero, i.e., ƍ=0. In that case, Poisson’s equation reduces to,

𝛻2𝑉 = 0

This equation is known as Laplace’s equation.

Page 6: Poisson’s and Laplace’s Equation

Laplace Equation in Three Coordinate

System

In Cartesian coordinates:

𝛻𝑉 =𝜕𝑉

𝜕𝑥𝑎𝑥 +

𝜕𝑉

𝜕𝑦𝑎𝑦 +

𝜕𝑉

𝜕𝑧𝑎𝑧

and,

𝛻𝐴 =𝜕𝐴𝑥𝜕𝑥

+𝜕𝐴𝑦

𝜕𝑦+𝜕𝐴𝑧𝜕𝑧

Knowing

𝛻2𝑉 = 𝛻 ∙ 𝛻𝑉

Hence, Laplace’s equation is,

𝛻2𝑉 =𝜕2𝑉

𝜕𝑥2+𝜕2𝑉

𝜕𝑦2+𝜕2𝑉

𝜕𝑧2= 0

Page 7: Poisson’s and Laplace’s Equation

In cylindrical coordinates:

𝛻 ∙ 𝑉 =𝜕𝑉

𝜕𝜌𝑎𝜌 +

1

𝜌

𝜕𝑉

𝜕∅𝑎∅ +

𝜕𝑉

𝜕𝑧𝑎𝑧

and,

𝛻 ∙ 𝐴 =1

𝜌

𝜕

𝜕𝜌(𝜌𝐴𝜌) +

1

𝜌

𝜕𝐴∅𝜕∅

+𝜕𝐴𝑧𝜕𝑧

Knowing

𝛻2𝑉 = 𝛻 ∙ 𝛻𝑉

Hence, Laplace’s equation is,

𝛻2𝑉 =1

𝜌

𝜕

𝜕𝜌(𝜌𝜕𝑉

𝜕𝜌) +

1

𝜌2𝜕2𝑉

𝜕∅2+𝜕2𝑉

𝜕𝑧2= 0

Page 8: Poisson’s and Laplace’s Equation

In spherical coordinates:

𝛻 ∙ 𝑉 =𝜕𝑉

𝜕𝑟𝑎𝑟 +

1

𝑟

𝜕𝑉

𝜕𝜃𝑎𝜃 +

1

𝑟 sin 𝜃

𝜕𝑉

𝜕∅𝑎∅

and,

𝛻 ∙ 𝐴 =1

𝑟2𝜕

𝜕𝑟(𝑟2𝐴𝑟) +

1

𝑟 sin 𝜃

𝜕

𝜕𝜃(𝐴𝜃 sin 𝜃) +

1

𝑟 sin 𝜃

𝜕𝐴∅𝜕∅

Knowing

𝛻2𝑉 = 𝛻 ∙ 𝛻𝑉

Hence, Laplace’s equation is,

𝛻2𝑉 =1

𝑟2𝜕

𝜕𝑟(𝑟2𝜕𝑉

𝜕𝑟) +

1

𝑟2 sin 𝜃

𝜕

𝜕𝜃(sin 𝜃

𝜕𝑉

𝜕𝜃) +

1

𝑟2 sin 𝜃

𝜕2𝑉

𝜕∅2= 0

Page 9: Poisson’s and Laplace’s Equation

Application of Laplace’s and Poisson’s

Equation

Using Laplace or Poisson’s equation we can obtain:

1. Potential at any point in between two surface when

potential at two surface are given.

2. We can also obtain capacitance between these two

surface.

Page 10: Poisson’s and Laplace’s Equation

EXAMPLE:

Let 𝑉 = 2𝑥𝑦3𝑧3and ∈=∈0. Given point P(1,3,-1).Find V at

point P. Also Find V satisfies Laplace equation.

SOLUTION:

𝑉 = 2𝑥𝑦3𝑧3

V(1,3,-1) = 2*1*32(−1)3

= -18 volt

Laplace equation in Cartesian system is

𝛻2𝑉 =𝜕2𝑉

𝜕𝑥2+𝜕2𝑉

𝜕𝑦2+𝜕2𝑉

𝜕𝑧2= 0

Differentiating given V,

𝜕𝑉

𝜕𝑥= 2𝑦2𝑧3

𝜕2𝑉

𝜕𝑥2= 0

Page 11: Poisson’s and Laplace’s Equation

𝜕𝑉

𝜕𝑦= 4𝑥𝑦𝑧3

𝜕2𝑉

𝜕𝑦2= 4𝑥𝑧3

𝜕𝑉

𝜕𝑧= 6𝑥𝑦2𝑧2

𝜕2𝑉

𝜕𝑧2= 12𝑥𝑦2𝑧

Adding double differentiating terms,

𝜕2𝑉

𝜕𝑥2+𝜕2𝑉

𝜕𝑦2+𝜕2𝑉

𝜕𝑧2= 0 + 4*𝑧2 + 12*x*𝑦2*z ≠ 0

Thus given V does not satisfy Laplace equation

Page 12: Poisson’s and Laplace’s Equation

EXAMPLE:

Consider two concentric spheres of radii a and b, a<b. The

outer sphere is kept at a potential 𝑉0 and the inner sphere at

zero potential. Solve Laplace equation in spherical

coordinates to find,

1. The potential and electric field in the region between two

spheres.

2. Find the capacitance between them.

SOLUTION:

From the given data it is clear that V is a function of r only.

i.e. 𝜕𝑉

𝜕𝜃and

𝜕𝑉

𝜕𝜙are zero. We know the Laplace's equation in

spherical coordinate system as,

𝛻2𝑉 =1

r2𝜕

𝜕𝑟𝑟2𝜕𝑉

𝜕𝑟+

1

𝑟2 sin 𝜃

𝜕

𝜕𝜃sin 𝜃

𝜕𝑉

𝜕𝜃+

1

𝑟2 sin 𝜃

𝜕2𝑉

𝜕𝜙2= 0

Page 13: Poisson’s and Laplace’s Equation

This equation reduces to,

𝛻2𝑉 =1

r2𝜕

𝜕𝑟𝑟2𝜕𝑉

𝜕𝑟= 0

𝑖. 𝑒.𝜕

𝜕𝑟𝑟2𝜕𝑉

𝜕𝑟= 0

By Integrating we get,

𝑟2𝜕𝑉

𝜕𝑟= 𝐴

Or,𝜕𝑉

𝜕𝑟=𝐴

𝑟2

Integrating again we get,

𝑉 = −𝐴

𝑟+ 𝐵…………………(i)

Page 14: Poisson’s and Laplace’s Equation

The given boundary condition are,

V = V0 at r = b and V = 0 at r = a

Applying these boundary con to equ (i)

V0 = −A

b+ B and 0 = −

A

a+ B…………(ii)

Subtracting equ (i) from equ (ii)

V0 − 0 = −A

b+A

a= A

1

a−1

b

A =+V01a−1b

Putting value of A in equ (ii) we get,

B =+V0b

1a−1b

Page 15: Poisson’s and Laplace’s Equation

Putting these values in equ (i), we get potential V as,

𝑉 =𝑉0

𝑟1𝑎−1𝑏

+𝑉0

𝑏1𝑎−1𝑏

= 𝑉0

1𝑟+1𝑏

1𝑎−1𝑏

We have,

𝐸 = − 𝛻 𝑉 = −𝜕𝑉

𝜕𝜌𝑎𝑟

𝐸 =𝑉0

𝑟21𝑎−1𝑏

𝑎𝑟 ( 𝑉/𝑚)

Page 16: Poisson’s and Laplace’s Equation

(b) To Find capacitance :

The flux density is,

𝐷 = ∈ 𝐸 =∈ 𝑉0

𝑟21𝑎−1𝑏

𝑎𝑟 (𝐶/𝑚2)

The charge density on the inner sphere i.e. at r=a is,

𝜌𝑠 = 𝐷 | 𝑟 = 𝑎 ∙ 𝑎𝑟 =∈ 𝑉0

𝑎21𝑎−1𝑏

(𝐶/𝑚2)

The capacitance is now calculated by,

𝐶 =𝑄

𝑉0=

4 𝜋 𝑎2𝜌𝑠

𝑉0=

4𝜋∈1

𝑎−1

𝑏

(𝐹)…...Ans

Page 17: Poisson’s and Laplace’s Equation

EXAMPLES:

Two parallel conducting disks are separated by a distance

5mm at Z=0 and Z=5 mm. If V=0 at Z=0 and V=100 at

z=5 mm. Find charge densities on the disks.

SOLUTION:

From the given con. It is clear that V is a fun. Of z only.

Laplace’s equation of cylindrical coordinate system, we get

𝛻2𝑉 =𝜕2V

𝜕z2= 0; 𝑖. 𝑒

𝜕2V

𝜕z2= 0

Integrating twice we get,dV

d2= A and V = Az + B …… i

Page 18: Poisson’s and Laplace’s Equation

Where, A and B are constants of integration. To determine

these constants apply the boundary conditions.

V=0 at z=0 and V=100 Volts at z=5 mm

Putting these in equ (i)

0 = 𝐴 0 + 𝐵 𝑎𝑛𝑑 100 = 𝐴 5 × 10−3 + 𝐵

𝐵 = 0 𝑖. 𝑒. 𝐴 =100

5 × 10−3= 20 × 103

Putting these in equ (i), the potential is obtained as,

𝑉 = 20 × 103𝑧

Now, the electric field between the circular disks is obtained

using the relation,

𝐸 = − 𝛻 𝑉 = −𝜕𝑉

𝜕𝜌𝑎𝜌 +

𝜕𝑉

𝜌 𝜕∅𝑎∅ +

𝜕𝑉

𝜕𝑧𝑎𝑧

Page 19: Poisson’s and Laplace’s Equation

E = −𝜕V

𝜕z az = − 20 × 103 az

consider, the medium between the circular disks as free

space, which gives the flux density as,

D = ∈0 E =10−9

36 π× −20 × 103 az

= −0.177 × 10−6 az (C /m2 )

Since D is constant between the phase and normal to the

plates, we say that

ρs = Dn = ±0.177 × 10−6 az (C /m2 )

Page 20: Poisson’s and Laplace’s Equation

Uniqueness Theorem

STATEMENT:

A solution of Poisson’s equation (of which

Laplace’s equation is a special case) that satisfies the given

boundary condition is a unique solution.

PROOF:

Let us assume that we have two solution of Laplace’s

equation, 𝑉1 and 𝑉2, both general function of the coordinate

use. Therefore,

𝛻2𝑉1 = 0

and

𝛻2𝑉2 = 0

Page 21: Poisson’s and Laplace’s Equation

Also assume that both 𝑉1 and 𝑉2 satisfies the same

boundary condition . Let us define a new difference

potential :

𝑉1 − 𝑉2 = 𝑉𝑑Now

𝛻2(𝑉1 − 𝑉2) = 0

i.e

𝛻2𝑉𝑑 = 0

We have the vector identity,

𝛻 ∙ 𝑉𝐷 = 𝑉 𝛻 ∙ 𝐷 + 𝐷 ∙ (𝛻𝑉)

Let V= 𝑉𝑑 and D= 𝛻 𝑉𝑑 , then we have

𝛻 ∙ 𝑉𝑑𝛻 𝑉𝑑 = 𝑉𝑑 𝛻2𝑉𝑑 + 𝛻𝑉𝑑

2

From the above equation, 𝛻2𝑉𝑑 = 0, then we have

𝛻 ∙ 𝑉𝑑𝛻 𝑉𝑑 = 𝛻𝑉𝑑2

Page 22: Poisson’s and Laplace’s Equation

Taking the volume integral over the volume gives,

𝑉

𝛻 ∙ 𝑉𝑑𝛻 𝑉𝑑 𝑑𝑣 = 𝑣

𝛻𝑉𝑑2 𝑑𝑣

Now the divergent theorem is:

𝑠

𝐷𝑑 𝑠 = 𝑣

(𝛻 ∙ 𝐷)𝑑𝑣

The right hand side of above equation can now be written in

term of surface integral as,

𝑠

𝑉𝑑𝛻 𝑉𝑑 ∙ 𝑑 𝑠 = 𝑣

𝛻𝑉𝑑2 𝑑𝑣

The surface integral can be evaluated by considering the

surface of very large sphere with radius R. when R is very

large both 𝑉1 and 𝑉2 can be treated as a point charge,

since size of it will be very small compared to R. Hence

the surface integral on LHS decreases and approaches

zero. Thus we have,

Page 23: Poisson’s and Laplace’s Equation

𝑣

𝛻𝑉𝑑2 𝑑𝑣 = 0

Since 𝛻𝑉𝑑2 is always positive, everywhere above

equation is satisfied only if 𝛻𝑉𝑑=0. If the gradient of 𝑉𝑑 i.e.

𝑉1 − 𝑉2 is everywhere zero, then 𝑉1 − 𝑉2 cannot change

with any coordinates i.e. it has same value at all point on

its boundary surface.

Therefore, 𝑉1 = 𝑉2 gives two identical solutions, i.e. unique

solution

Page 24: Poisson’s and Laplace’s Equation