Physics 121 - Electricity and Magnetism Lecture 05 -Electric Potential Y&F Chapter 23 Sect. 1-5 • • • • • • • • • Electric Potential Energy versus Electric Potential Calculating the Potential from the Field Potential due to a Point Charge Equipotential Surfaces Calculating the Field from the Potential Potentials on, within, and near Conductors Potential due to a Group of Point Charges Potential due to a Continuous Charge Distribution Summary 1 Copyright R. Janow Fall 2015 Electrostatics: Two spheres, different radii, one with charge Initially Connect wire between spheres, then disconnect it Q10= 10 C r1= 10 cm wire Q1f= ?? Q2f= ?? •Are final charges equal? •What determines how charge redistributes itself? Q20= 0 C r2= 20 cm Mechanical analogy: Water pressure Open valve, water flows What determines final water levels? gy = PE/unit mass P2 = rgy2 P1 = rgy1 X Copyright R. Janow Fall 2015 ELECTRIC POTENTIAL V(r ) Define: Electrostatic Potential … equals … Potential Energy per unit (test) charge Related to Electrostatic Potential Energy……but…… • DPE: ~ work done ( = force x displacement = charge x field x displacement ) • DV: ~ work done/unit charge ( = field x displacement ) Potential: • summarizes effect of charge at some point in space without specifying a test charge there (like E field, unlike PE) • is a scalar field easier to use than E (vector). E = Gradient (Potential) Both DPE and DV: • imply a reference level • are conservative forces/fields, like gravity • can determine motion of charged particles using: Second Law, F = qE or PE, Work-KE theorem &/or mechanical energy conservation Units, Dimensions: • Potential Energy U: Joules • Potential V: [U]/[q] Joules/C. = VOLTS • Units of field are [V]/[d] = Volts / meter – same as N/C. Copyright R. Janow Fall 2015 Reminder: Work Done by a Constant Force 5-1: In the four examples shown in the sketch, a force F an object and does work. In all four cases, the force has same magnitude and the displacement of the object is to right and has the same magnitude. Rank the cases in order of the work done by the force on object, from most positive to the most negative. acts on the the the Ds A. B. C. D. E. I, IV, III, II II, I, IV, III III, II, IV, I I, IV, II, III III, IV, I, II F I III F F II F IV Copyright R. Janow Fall 2015 Work Done by a Constant Force (a reminder) DW F Ds = FDs cos The work DW done by a constant external force on it is the product of: • the magnitude F of the force • the magnitude Δs of the displacement of the point of application of the force • and cos(θ), where θ is the angle between force and displacement vectors: Dr F F Dr Dr II I WII = FDr WI = 0 F F Dr Dr III In general, force may vary in direction and magnitude along the path: DW F ds WIII = FDr IV WIV = FDr cos f i Result of “Path Integration” may depend on path taken Copyright R. Janow Fall 2015 Definitions: Electrostatic Potential Energy versus Potential E field is “conservative”, like gravity • Work done BY THE FIELD on a test charge moving from i to f does not depend on the path taken. • Work done around any closed path equals zero. dU = dW = Fe ds Fe = q0E (work done by field dV dU / q0 POTENTIAL ENERGY DIFFERENCE: Charge q0 moves from i to f along ANY path POTENTIAL DIFFERENCE: Potential is potential energy per unit charge f Uf Ui DU DW Fe ds = q0 E ds f i Path Integral i DU DW DV = = E Ds q0 q0 (from basic definition) Vf Vi DV DW / q0 = E ds f i ( Evaluate integrals on ANY path from i to f ) Copyright R. Janow Fall 2015 Some distinctions and details D U = q0 D V • • • • • The field is created by a charge distribution elsewhere). A test charge q0 moved between i and f gains or loses potential energy DU. DU and DV do not depend on path. DU also does not depend on |q0| (test charge). Use Work-KE theorem to link potential differences to motion Only differences in electric potential and PE are meaningful: – Relative reference: Choose arbitrary zero reference level for ΔU or ΔV. – Absolute reference: Set Ui = 0 with all charges infinitely far apart – Volt (V) = SI Unit of electric potential • 1 volt = 1 joule per coulomb = 1 J/C • 1 J = 1 VC and 1 J = 1 N m • Electric field units – new name: – 1 N/C = (1 N/C)(1 VC/1 Nm) = 1 V/m • “Electron volt” is an energy unit: – 1 eV = work done moving charge e through a 1 volt potential difference = (1.60×10-19 C)(1 J/C) = 1.60×10-19 J Copyright R. Janow Fall 2015 Work and PE : Who/what does positive or negative work? 5-2: In the figure, suppose we exert a force and move the proton from point i to point f in a uniform electric field directed as shown. Which statement of the following is true? A. B. C. D. E. f i E Electric field does positive work on the proton. Electric potential energy of the proton increases. Electric field does negative work on the proton. Electric potential energy of the proton decreases. Our force does positive work on the proton. Electric potential energy of the proton increases. Our force does positive work on the proton. Electric potential energy of the proton decreases. The changes cannot be determined. •Hint: which directions pertain to displacement and force? Copyright R. Janow Fall 2015 EXAMPLE: Find change in potential as test charge +q0 moves from point i to f in a uniform field i E f o Dx DV or DU depend only on the endpoints ANY PATH from i to f gives same results uniform field To convert potential to/from PE just multiply/divide by q0 DVfi = E ds path Fe = q0E DUfi DWfi = F ds path DVfi DUfi / q0 DUfi = q0DVfi EXAMPLE: CHOOSE A SIMPLE PATH THROUGH POINT “O” DVf ,i = DVo,i DVf ,o DVo,i = 0 Displacement i o is normal to field (path along equipotential) DVf ,i = DVf ,o = - E Dx = E | Dx | • External agent must do positive work on positive test charge to move it from o f • E field does negative work • units of E can be volts/meter What are signs of DU and DV if test charge isCopyright negative? R. Janow Fall 2015 Potential Function for a Point Charge • • • • Infinitely far away choose V(R = infinity) = 0 (reference level) DU = work done on a test charge as it moves to final location DU = q0DV Field is conservative choose most convenient path = radial Find potential V(R) a distance R from a point charge q : V(R) V VR = E ds along radial path from r = R to ds = r̂dr R q dr 1 q E(r ) = k 2 r̂ E ds = V(R) = kq 2 = kq = k r rR R r q V(R ) = k R R R (23.14) • Positive for q > 0, Negative for q<0 • Inversely proportional to r1 NOT r2 Similarly, for potential ENERGY: (use same method but integrate force) U(r ) QV (R ) = k q.Q R (23.9) • Shared PE between q and Q • Overall sign depends on both signs Copyright R. Janow Fall 2015 Visualizing the potential function V(r) for a positive point charge (2 D) For q negative V is negative (funnel) V(r) 1/r r r Copyright R. Janow Fall 2015 On Equi-potential Surfaces: Voltage and potential energy are constant; i.e. DV=0, DU=0 Equipotentials are perpendicular to the electric field lines DV = 0 Vi > Vf DV = 0 Vfi E is the gradient of V DV E Ds DV = 0 • Zero work is done moving charges along an equi-potential DV = - E Ds cos() = 0 for Ds along surface equi - potential and DU = DW = Fe Ds = 0 CONDUCTORS ARE ALWAYS EQUIPOTENTIALS - Charge on conductors moves to make Einside = 0 - Esurf is perpendicular to surface so DV = 0 along any path on or in a conductor Copyright R. Janow Fall 2015 Examples of equipotential surfaces Uniform Field Point charge or outside sphere of charge Dipole Field Equipotentials are planes (evenly spaced) Equipotentials are spheres (not evenly spaced) Equipotentials are not simple shapes Copyright R. Janow Fall 2015 The field E(r) is the gradient of the potential dV E ds = - E ds cos() •Component of ds on E produces potential change •Component of ds normal to E produces no change •Field is normal to equipotential surfaces •For path along equipotential, DV = 0 ds • Gradient = spatial rate of change dV V V V E=- = i ĵ k̂ - V ds is to equipotential ds x y z f (x, y, z ) Math note : is a " partial" derivative x EXAMPLE: UNIFORM FIELD E – 1 dimension DV E Ds = E Ds Ds E DU = q0 DV = q0EDs = FDs Copyright R. Janow Fall 2015 Potential difference between oppositely charged conductors (parallel plate capacitor) + - • Assume Dx << L (infinite sheets) • Equal and opposite surface charges • All charge resides on inner surfaces (opposite charges attract) = E= 0 constant L Dx DV Vf Vi = E Dx Vf E=0 Example: Find the potential difference DV across the capacitor, assuming: • = 1 nanoCoulomb/m2 • Dx = 1 cm & points from negative to positive plate • Uniform field E 1 10-9 DV = E Dx = E Dx = 10-2 0 Vi DV = 1.13 volts A positive test charge +q gains potential energy DU = qDV as it moves from - plate to + plate along any path (including external circuit) Copyright R. Janow Fall 2015 Conductors are always equipotentials Example: Two spheres, different radii, one charged to 90,000 V. Connect wire between spheres – charge moves Conductors come to same potential Charge redistributes to make it so V1f = V2 f r1= 10 cm V10= 90,000 V. wire Q1f Q2f = Q10 r2= 20 cm Initially: V10 kQ10 = 9 104 Volts = Q10 = 1.0 C. r1 V20= 0 V. Q20= 0 V. Find the final charges: V1f = k[Q 10 Q1f ] kQ1f = V2 f = r1 r2 Find the final potential(s): kQ1f V1f = = r1 r2 -1 Q1f = Q10 (1 ) = 0.33 C. r1 Q2f = Q10 Q1f = 0.67 C. 9 109 0.33 x10 6 = 30,000 Volts = V2f Copyright R. Janow 0.1 Fall 2015 Potential inside a hollow conducting shell Vc = Vb (shell is an equipotential) = 18,000 Volts on surface R = 10 cm Shell can be any closed surface (sphere or not) d c a R Find potential Va at point “a” insidea shell b Definition: DVab Va Vb = E ds b Apply Gauss’ Law: choose GS just inside shell: qenc = 0 E = 0 everywhere inside DVab = 0 Va = Vsurface = Vb = Vc = Vd = 18,000 Volts Potential is continuous across surface – field is not E= E(r) dV dr Eoutside= kq / r2 Einside=0 R r V(r) Vinside=Vsurf Voutside= kq / r r R R. Janow Fall 2015 Copyright Potential due to a group of point charges • Use superposition for n point charges • Potential is a scaler… so … • The sum is an algebraic sum, not a vector sum. V(r ) = n 1 V = i 4 0 i =1 n r i =1 r r2 r r1 r qi ri r1 r2 • Comparison: For the electric field, by superposition, for n point charges E(r ) = Ei n i =1 1 4 0 n i=1 qi 2 r̂i r ri • E may be zero where V does not equal to zero. • V may be zero where E does not equal to zero. Copyright R. Janow Fall 2015 Use Superposition Examples: potential due to point charges Note: E may be zero where V does not = 0 V may be zero where E does not = 0 TWO EQUAL CHARGES – Point P at the midpoint between them EP = 0 d +q +q P VP = by symmetry kq kq kq =4 d/2 d/2 d obviously not zero F and E are zero at P but work would have to be done to move a test charge to P from infinity. DIPOLE – Otherwise positioned as above EP 0 d +q -q P but VP = obviously EP = 2 kq kq =0 d/2 d/2 kq d2 /4 = 8 kq d2 Copyright R. Janow Fall 2015 Examples: potential due to point charges - continued Another example: square with charges on corners a q -q d a P a d -q a q Find E & V at center point P d= a 2/2 EP = 0 by symmetry kq k k VP = i = qi = [q q q q] d i d i ri VP = 0 Another example: same as above with all charges positive EP = 0 VP = by symmetry, again kqi k 4kq 8kq = q = = i r d i i a 2 / 2 a 2 i Copyright R. Janow Fall 2015 Electric Field and Electric Potential 5-3: Which of the following figures have V=0 and E=0 at the red point? q -q q q A B q q q q q -q C -q q D q -q E Copyright R. Janow Fall 2015 Method for finding potential function V at a point P due to a continuous charge distribution 1. Assume V = 0 infinitely far away from charge distribution (finite size) 2. Find an expression for dq, the charge in a “small” chunk of the distribution, in terms of l, , or r ldl for a linear distributi on dq = d2 A for a surface distributi on rd3 V for a volume distributi on Typical challenge: express above in terms of chosen coordinates 3. At point P, dV is the differential contribution to the potential due to a pointlike charge dq located in the distribution. Use symmetry. dq dV = scalar, r = distance from dq to P 4 0r 4. Use “superposition”. Add up (integrate) the contributions over the whole charge distribution, varying the displacement r as needed. Scalar VP. 1 dq VP = dVP = (line, surface, or volume integral) 4 0 r dist dist 5. Field E can be gotten from potential by taking the “gradient”: V Rate of potential change E = V dV E ds perpendicular to equipotential s Copyright R. Janow Fall 2015 Example 23.11: Potential along Z-axis of a ring of charge z Q = charge on the ring l = uniform linear charge density = Q/2a r = [a2 + z2]1/2 = distance from dq to “P” ds = arc length = adf P dq = lds = ladf dq dV = k r 2 kal kQ V = dV = d f = r 0 r ring r z f y a dq x FIND ELECTRIC FIELD USING GRADIENT (along z by symmetry) As Before V= All scalars - no need to worry about direction Looks like a point charge formula, but r is on the ring kQ [ z 2 a 2 ]1 / 2 • As z 0, V kQ/a • As a 0 or z inf, V point charge V kQ (z 2 ) kQz Ez = k̂ = 3 k̂ = 2 k̂ 2 3/2 z 2r z [z a ] • E 0 as z 0 (for “a” finite) • E point charge formula forR. Janow z >> Fall a 2015 Copyright Example: Potential Due to a Charged Rod • A rod of length L located parallel to the x axis has a uniform linear charge density . Find the electric potential at a point P located on the y axis a distance d from the origin. • Start with r [x 2 d2 ]1 / 2 dq = ldx 1 dq 1 ldx dV = = 4 0 r 4 0 (x 2 d2 )1 / 2 • Integrate over the charge distribution on interval 0 < x < L L l dx l = ln x ( x 2 d2 )1 / 2 2 2 1 / 2 4 0 (x d ) 4 0 0 V = dV = = • l ln L (L2 d2 )1 / 2 ln(d) 4 0 L0 Check by differentiating d log(x r ) dx for r = [x 2 d2 ]1 / 2 d 1 d(x r ) 1 dr 1 x 1 rx 1 log(x r ) = = (1 )= (1 ) = ( )= dx x r dx xr dx xr r xr r r • Result L (L2 d2 )1 / 2 l V= ln 4 0 d Copyright R. Janow Fall 2015 Example 23.10: Potential near an infinitely long charged line or a charged conducting cylinder E= 2kl r Near line or outside cylinder r > R E is radial. Choose radial integration path if DVfi = Vf - Vi = i f f dr E d r = 2kl i r DVfi = 2kl ln[ri / rf ] Above is negative for rf > ri with l positive E=0 Inside conducting cylinder r < R E is radial. Choose radial integration path if DVinside = i f E dr = 0 Potential inside is constant and equals surface value Copyright R. Janow Fall 2015 Example 23.12: Potential at a symmetry point near a finite line of charge l = Q/2a Uniform linear charge density dq = ldy Charge in length dy dq Potential of point charge dV = k r a a dy VP = dV = kl -a - a (x 2 y2 )1/ 2 Standard integral from tables: (x 2 dy = y2 )1/ 2 ln [ y r ] = ln [ y (x 2 y2 )1/ 2 ] VP = VP a (x 2 a2 )1/ 2 kl ln 2 2 1/ 2 a (x a ) (x 2 a2 )1/ 2 a kQ = ln 2 2 1/ 2 2a (x a ) a Limiting cases: • Point charge formula for x >> 2a • Example 23.10 formula for near field limit x << 2a Copyright R. Janow Fall 2015 Example: Potential on the symmetry axis of a charged disk P • Q = charge on disk whose radius = R. • Uniform surface charge density = Q/4R2 • Disc is a set of rings, each of them da wide in radius • For one of the rings: dq dA = a da df VP,z 1 = 4 0 R 2 0 0 dVP ,z a da d [a2 z2 ]1/ 2 r z R dA = adfda cos() = z/r r 2 = a2 z2 dA=adfda k dq = r f a Double integral x • Integrate twice: first on azimuthal angle f from 0 to 2 which yields a factor of 2 then on ring radius a from 0 to R (note: (1 x)1/ 2 1 21 x 21 41 x2..... for x2 1 ) 2 a da 4 0 0 [ a 2 z 2 ]1/ 2 R VP,z = “Far field” (z>>R): disc looks like point charge a d 2 Use Anti= [ a z 2 ]1/ 2 2 2 1/ 2 derivative: [ a z ] da Vdisk = 2 0 z 2 R2 1/2 z Vdisk 2 0 1 R2 1 Q z = z 2 z 4 0 z “Near field” (z<<R): disc looks like infinite non-conducting sheet of charge Vdisk R 20 z 1 R E dV = dz 2 0 Copyright R. Janow Fall 2015