Equipotential Lines = Contours of constant V E field points downhill Downhill is always...

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Equipotential Lines = Contours of constant V E field points downhill Downhill is always perpendicula r to level Conductors at rest are equipotentia l

Transcript of Equipotential Lines = Contours of constant V E field points downhill Downhill is always...

Page 1: Equipotential Lines = Contours of constant V E field points downhill Downhill is always perpendicular to level Conductors at rest are equipotential.

Equipotential Lines = Contours of constant V

E fieldpoints downhill

Downhill is always perpendicular to level

Conductors at rest are equipotential

Page 2: Equipotential Lines = Contours of constant V E field points downhill Downhill is always perpendicular to level Conductors at rest are equipotential.

Electric potential is a scalar. Electric fields are vectors.

BOTH follow principle of superposition… with multiple sources you can add the (field, potential) from each source.

Page 3: Equipotential Lines = Contours of constant V E field points downhill Downhill is always perpendicular to level Conductors at rest are equipotential.

Rank the magnitudes (smallest to largest) of the electric field at point P in the three arrangements shown.

A] all are the same

B] I, II, III

C] III, II, I

D] II, I, III

Rank the electric potentials at point P (smallest to largest).

Page 4: Equipotential Lines = Contours of constant V E field points downhill Downhill is always perpendicular to level Conductors at rest are equipotential.

Where is on the x axis is the potential = 0? (other than at infinity)Take V = 0 at infinity.

Or choose E: potential is zero nowhere except infinity.

Ans. E

Page 5: Equipotential Lines = Contours of constant V E field points downhill Downhill is always perpendicular to level Conductors at rest are equipotential.

Where is on the x axis is the E field = 0? (other than at infinity)

Or choose E: field is zero nowhere except infinity.

Ans. C ratio of distances = 2:1

Page 6: Equipotential Lines = Contours of constant V E field points downhill Downhill is always perpendicular to level Conductors at rest are equipotential.

Where is on the x axis is the potential = 0? (other than at infinity)Take V = 0 at infinity.

Or choose E: at more than one point shown.

Ans. E (both A & B have V=0)

Page 7: Equipotential Lines = Contours of constant V E field points downhill Downhill is always perpendicular to level Conductors at rest are equipotential.

Where is on the x axis is the E field = 0? (other than at infinity)

Or choose E: off the left edge of the slide

Ans E. 15 units to the left of the -1 charge, the ratio ofdistances is 2:1

Page 8: Equipotential Lines = Contours of constant V E field points downhill Downhill is always perpendicular to level Conductors at rest are equipotential.

Potential from an infinite plane

Potential from an infinite line

(From infinite sources, we can’t take V=0 at infinity.But we are only ever interested in potential differences, so it doesn’t really matter.)

Page 9: Equipotential Lines = Contours of constant V E field points downhill Downhill is always perpendicular to level Conductors at rest are equipotential.

Which graph shows the potential from an infinite line of negative charge density, where x = distance from line?

E (none)

Page 10: Equipotential Lines = Contours of constant V E field points downhill Downhill is always perpendicular to level Conductors at rest are equipotential.

What if you have two sources, say an infinite line and a point charge?

In that case, there is no “zero convention”… no preferred place where we can all agree to make V=0. So it no longer makes any sense to speak of THE potential at a point. We can still find the potential difference between two points, however.

Page 11: Equipotential Lines = Contours of constant V E field points downhill Downhill is always perpendicular to level Conductors at rest are equipotential.

What is the potential difference between a point a distance r to the left of the point charge, and a point immediately below the point charge on the plane? Recall that the field from an infinite plane is E=

Page 12: Equipotential Lines = Contours of constant V E field points downhill Downhill is always perpendicular to level Conductors at rest are equipotential.

finding E from V

If V = -4x + 4y2 (x,y in meters, V in volts) , what is the E field at the origin?

A] 0

B] 4 V/m in the +y direction

C] 4 V/m in the -y direction

D] 4 V/m in the +x direction

E] 4 V/m in the -x direction

Page 13: Equipotential Lines = Contours of constant V E field points downhill Downhill is always perpendicular to level Conductors at rest are equipotential.

If V = -4x + 4y2 (x,y in meters, V in volts) , where is the E field = 0?

A] at the origin

B] at x=1, y=1

C] at x=1, y=-1

D] at both B and C

E] nowhere.

Page 14: Equipotential Lines = Contours of constant V E field points downhill Downhill is always perpendicular to level Conductors at rest are equipotential.

Two conductors in proximity form a “capacitor”: they have a capacity to hold a charge Q (+Q on one and -Q on the other)

with a voltage difference V.

C=Q/V

Note: Capacitance C is italicized. Coulomb C is not.

Capacitance is a property of the geometry of the conductors (and depends on whether there is vacuum or material

between them, as we will see later.)

This is because of linearity (superposition.) If I double the source charges, I will double the field, and double the

potential.

Page 15: Equipotential Lines = Contours of constant V E field points downhill Downhill is always perpendicular to level Conductors at rest are equipotential.

“Reservoir” analogy

The charge on a capacitor (±Q) is like the water

The potential is like the depth of the water

The capacitance is like the area of the lake

So Q=CV

Page 16: Equipotential Lines = Contours of constant V E field points downhill Downhill is always perpendicular to level Conductors at rest are equipotential.

If I put ±2 microcoulombs of charge on the sphere and plate, there is a potential difference of 2 V.

What is the capacitance?

A] 0

B] Cannot determine, since not symmetric

C] 1 microfarad = 10-6 C/V

D] 106 farads

Page 17: Equipotential Lines = Contours of constant V E field points downhill Downhill is always perpendicular to level Conductors at rest are equipotential.

If I put ±2 microcoulombs of charge on the sphere and plate, there is a potential difference of 2 V.

If I put ±4 microcoulombs of charge on the sphere and plate, what will be the potential difference?

A] 0

B] 2 V

C] 4 V

D] 8 V

Page 18: Equipotential Lines = Contours of constant V E field points downhill Downhill is always perpendicular to level Conductors at rest are equipotential.

To calculate the capacitance of a pair of conductors, put+Q on one and -Q on the other, and calculate the potential difference.

(Sometimes we refer to the capacitance of an isolated conductor. In that case, we put charge Q on the conductor and ask what is the potential (compared to infinity.)

Let’s do a cylindrical capacitor example.

Page 19: Equipotential Lines = Contours of constant V E field points downhill Downhill is always perpendicular to level Conductors at rest are equipotential.

Parallel plate capacitor

Two infinite parallel sheets carry charge densities ± What is the electric field at point 1?

Page 20: Equipotential Lines = Contours of constant V E field points downhill Downhill is always perpendicular to level Conductors at rest are equipotential.

Two infinite parallel sheets carry charge densities ± What is the electric field at point 2?

The potential difference between the plates is d

Page 21: Equipotential Lines = Contours of constant V E field points downhill Downhill is always perpendicular to level Conductors at rest are equipotential.

Capacitors “in parallel” (= same potential across them.)

Ceq = C1 + C2

Capacitors “in series” (= same charge on each)

1/Ceq = 1/C1 + 1/C2

Page 22: Equipotential Lines = Contours of constant V E field points downhill Downhill is always perpendicular to level Conductors at rest are equipotential.

What happens to the potential difference if I keep the sameCharge on the plates, but increase separation?A] V increasesB] V decreasesC] V is unchanged

Page 23: Equipotential Lines = Contours of constant V E field points downhill Downhill is always perpendicular to level Conductors at rest are equipotential.

V increases. Where does this energy come from?Answer: it takes work to move the plates apart.

Page 24: Equipotential Lines = Contours of constant V E field points downhill Downhill is always perpendicular to level Conductors at rest are equipotential.

Where is this energy stored??It is stored in the field between the plates. The field is the same, but the volume of space is bigger. The “energy density” is the same, but there is more energy.How much energy?

Page 25: Equipotential Lines = Contours of constant V E field points downhill Downhill is always perpendicular to level Conductors at rest are equipotential.

It is proposed to store solar energy by filling a water tank during the day, raising the water from ground level. (At night, the water drains turning a generator.)

A tank is 20 m high and has vertical sides. When half full, it stores 1 million Joules. How much energy will it store when full?

A] 1 million Joules

B] 2 million Joules

C] 4 million Joules

D] 20 million Joules

Page 26: Equipotential Lines = Contours of constant V E field points downhill Downhill is always perpendicular to level Conductors at rest are equipotential.

“Dielectric” = a fancy word for a real insulator.In real insulators, charges can move, but only very smalldistances… the electrons can shift a bit with respect to the nucleii, but they can’t hop from one nucleus to the next.

What happens to the electric field in a capacitor if we add a dielectric material?

Let’s sketch on the board, and then I’ll quiz you.

Page 27: Equipotential Lines = Contours of constant V E field points downhill Downhill is always perpendicular to level Conductors at rest are equipotential.

By superposition, the field in the dielectric is the sum of the original capacitor field, plus the field from the polarization surface charge.

The total field is therefore

A] bigger than the original capacitor field

B] smaller than the original capacitor field

C] the same as the original capacitor field

Page 28: Equipotential Lines = Contours of constant V E field points downhill Downhill is always perpendicular to level Conductors at rest are equipotential.

Answer: smaller than the original field.

We can write that the new field is the original field, divided by K, the “dielectric constant”

• What is the new potential across the capacitor?

A] same as the old potential, without the dielectric

B] bigger than the old potential, by a factor of K

C] smaller than the old potential, by a factor of K

Page 29: Equipotential Lines = Contours of constant V E field points downhill Downhill is always perpendicular to level Conductors at rest are equipotential.

If I put a charge ±Q on a parallel plate capacitor and insert a dielectric, what happens to V?

A] it increases

B] it decreases

C] it stays the same

Page 30: Equipotential Lines = Contours of constant V E field points downhill Downhill is always perpendicular to level Conductors at rest are equipotential.

If I put a charge ±Q on a parallel plate capacitor and insert a dielectric, what happens to V?

The field in the dielectric is reduced by a factor of K. So the potential goes down.

What happens to the potential energy?

A] it goes up by a factor of K

B] it goes up by a factor of K2

C] it goes down by a factor of K

D] it goes down by a factor of K2

E] it stays the same.

Page 31: Equipotential Lines = Contours of constant V E field points downhill Downhill is always perpendicular to level Conductors at rest are equipotential.

If I put a charge ±Q on a parallel plate capacitor and insert a dielectric, what happens to V?

What happens to the potential energy?It may be counterintuitive, but the potential energy goes down by a factor

of K (not K2).

U=Q2/(2C); the capacitance goes up by a factor of K. (or U = CV2/2 … the voltage drops by K, the capacitance increases by K)

Note: the energy density for a given E field in a dielectric is

The field goes down by a factor of K, but epsilon adds a factor of K.

u = 12 εE

2

Page 32: Equipotential Lines = Contours of constant V E field points downhill Downhill is always perpendicular to level Conductors at rest are equipotential.

If the potential energy goes down, where does the energy go?

• The field pulls the dielectric into the capacitor, giving it kinetic energy. (Very small, here.)

• Application: Optical tweezers

Page 33: Equipotential Lines = Contours of constant V E field points downhill Downhill is always perpendicular to level Conductors at rest are equipotential.

With a fixed charge on the plates, the dielectric is pulled into the capacitor. The field and field energy go down.

What happens if, instead, the capacitor is held at a fixed potential?

The energy goes up! U = CV2/2, and the capacitance goes up.But we cannot conclude that you must push the dielectric in (in fact, you don’t have to) … the extra energy comes from the battery.