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1 8.022 (E&M) – Lecture 3 Topics: Electric potential Energy associated with an electric field Gauss’s law in differential form … and a lot of vector calculus… (yes, again!)

8.022 (E&M) – Lecture 3 Topics: Electric potential

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Last time… What did we learn?  Energy of a system of charges  Electric field  Gauss’s law in integral form:  Derived last time, but not rigorously… G. Sciolla – MIT 8.022 – Lecture 3

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Page 1: 8.022 (E&M) – Lecture 3 Topics:  Electric potential

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8.022 (E&M) – Lecture 3

Topics:

Electric potential

Energy associated with an electric field

Gauss’s law in differential form

… and a lot of vector calculus… (yes, again!)

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Last time…

What did we learn?

Energy of a system of charges

Electric field

Gauss’s law in integral form:

Derived last time, but not rigorously…

G. Sciolla – MIT 8.022 – Lecture 3

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Gauss’s law NB: Gauss’s law only becauseE~1/r2. If E~ anything else,the r2 would not cancel!!!

Consider charge in a generic surface S

Surround charge with spherical surface S1

concentric to charge

Consider cone of solid angle dΩ from charge to surface S through the little sphere

Electric flux through little sphere:

Electric flux through surface S:

G. Sciolla – MIT 8.022 – Lecture 3

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Confirmation of Gauss’s law

Electric field of spherical shell of charges:

Can we verify this experimentally?

o utside the shell

in sid e the shell

• Charge a spherical surface with Van de Graaf generator • Is it charged? (D7 and D8) • Is Electric Field radial?

Does E~1/r2φ~1/r? Neon tube on only when oriented radially(D24)

• (D29?)

G. Sciolla – MIT 8.022 – Lecture 3

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Confirmation of Gauss’s law (2)

Cylindrical shevely charged

Gauus tells us that

Einside = 0

Eoutside > 0

Can we verify this experimentally?

Demo D26

Charge 2 conductve spheres bynducton outside the cylnder: one sphere will be + and the other will be -: it works because Eoutside > 0

Try to do the same inside inside cylinder nothing happens because E=0

(explainnduction on the board)

G. Sciolla – MIT 8.022 – Lecture 3

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Energy stored in E:

Squeezing charges…

Consider a spherical shell of charge of radius r

How much work dW to “squeeze” it to a radius r-dr?

Guess the pressure necessary to squeeze it:

We can now calculate dW:

G. Sciolla – MIT 8.022 – Lecture 3

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Energy stored in the electric field

Work done on the system:

We do work on the system (dW): same sign charges have been squeezed on a smaller surface, closer together and they do not like that…

Where does the energy go?

We created electric field where there was none (between r and r-dr) The electrc field we created must be storng the energy

Energy is conserved dU = dW

is the energy density of the electric field E

Energy is stored in the E field:

NB: integrate over entire space not only where charges are! Example: charged sphere

G. Sciolla – MIT 8.022 – Lecture 3

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Electric potential difference

Work to move q from r1 to r2 :

W12 depends on the test charge q

define a quantity that is independent of q and just describes the properties of the space:

Physical interpretation: φ 12 is work that I must do to move a unit charge from P1 to P2

Units:

cgs: statvolts = erg/esu; SI: Volt = N/C; 1 statvolts = “3” 102 v

Electric potential difference between P1 and P2

G. Sciolla – MIT 8.022 – Lecture 3

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Electric potential

The electric potential difference φ12 is defined as the work to move a unit charge between P1 and P2: we need 2 points!

Can we define similar concept describing the properties of the space?

Yes, just fix one of the points (e.g.: P=infinity):

Application 1: Calculate φ(r) created by a point charge in the origin:

Application 2: Calculate potential difference between points P1 and P2;

Potential difference is really the difference of potentials!

G. Sciolla – MIT 8.022 – Lecture 3

Potential

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Potentials of standard charge distributions

The potential created by a point charge is

Given this + superposition we can calculate anything!

▪ Potential of N point charges:

▪ Potential of charges in a volume V:

▪ Potential of charges on a surface S:

▪ Potential of charges on a line L:

G. Sciolla – MIT 8.022 – Lecture 3

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Some thoughts on potential

Why is potential useful? Isn’t E good enough?

Potential is a scalar function much easier to integrate than electric field or force that are vector functions

When is the potential defined?

Unless you set your reference somehow, the potential has no meaning Usually we choose φ(infinity)=0

This does not work always: e.g.: potential created by a line of charges

Careful: do not confuse potential φ(x,y,z) with potential energy of a system of charges (U)

Potential energy of a system of charges: work done to assemble charge configuration

Potential: work to move test charge from infinity to (x,y,z)

G. Sciolla – MIT 8.022 – Lecture 3

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Energy of electric field revisited

Energy stored in a system of charges:

This can be rewritten as follows:

Where φ(rj) is the potential due to all charges excepted for the q j atthe location of qj(rj) Taking a continuum limit:

NB: this works only when φ(infinity)=0

G. Sciolla – MIT 8.022 – Lecture 3

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Connection between φand E

Consider potential difference between a point at r and r+dr:

The infinitesimal change in potential can be written as:

Useful info because it allows us to find E given φ

Good because is much easier to calculate than E

G. Sciolla – MIT 8.022 – Lecture 3

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Getting familiar with gradients…

1d problem:

The derivative df/dx describes the function’s slope

The gradient describes the change of the function and the direction of the change

2d problem:

The interpretation is the same, but in both directions

The gradient points in the direction where the slope is deepest

G. Sciolla – MIT 8.022 – Lecture 3

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Visualization of gradients

Given the potential φ (x, y)=sin(x)sin(y), calculate its gradient.

The gradient always points uphill E=-gradφ points downhill

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Visualization of gradients:

equipotential surfaces

Same potential φ (x,y)=sin(x)sin(y)

NB: since equipotential lines are perpendicular to the gradient

equipotential lines are always perpendicular to E

G. Sciolla – MIT 8.022 – Lecture 3

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Divergence in E&M (1)

Consider flux of E through surface S:

Cut S into 2 surfaces: S1 and S2 with Snew the surface in between

G. Sciolla – MIT 8.022 – Lecture 3

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Divergence Theorem

Let’s continue splitting into smaller volumes

If we define the divergence of E as

Divergence Theorem(Gauss’s Theorem)

G. Sciolla – MIT 8.022 – Lecture 3

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Gauss’s law in differential form

Simple application of the divergence theorem:

This is valid for any surface V:

Comments:

First Maxwell’s equations

Given E, allows to easily extract charge distribution ρ

G. Sciolla – MIT 8.022 – Lecture 3

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What’s a divergence?

Consider infinitesimal cube centered at P=(x,y,z)

Flux of F through the cube in z direction:

Since ΔzÆ0

Similarly for Φx and Φy

G. Sciolla – MIT 8.022 – Lecture 3

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Divergence in cartesian coordinates

We defined divergence as

But what does this really mean?

This is the usable expression for the divergence: easy to calculate!

G. Sciolla – MIT 8.022 – Lecture 3

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Application of Gauss’s law in differential form

Problem: given the electric field E(r), calculate the charge distribution that created it

Hint: what connects E and ρ ? Gauss’s law.

In cartesian coordinates:

Sphere of radiusR with constant charge density K

G. Sciolla – MIT 8.022 – Lecture 3

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Next time…

Laplace and Poisson equations Curl and its use in Electrostatics Into to conductors (?)

G. Sciolla – MIT 8.022 – Lecture 3