Electrostatic Boundary value problems Sandra Cruz-Pol, Ph. D. INEL 4151 ch6 Electromagnetics I ECE UPRM Mayagüez, PR Last Chapters: we knew either V or charge distribution, to find E,D. NOW: Only know values of V or Q at some places (boundaries). Some applications Microstrip lines capacitance Microstrip disk for microwave equipment To find E, we will use: Poisson’s equation: Laplace’s equation: (if charge-free) v V 2 V 0 They can be derived from Gauss’s Law 2 D E v E V Depending on the geometry: v V 2 We use appropriate coordinates: cartesian: 2V 2V 2V v x cylindrical: spherical: 2 y 2 z 1 V 2 1 2V 2V v 2 2 2 z v 1 2 V 1 V 1 2V r 2 sin 2 2 2 2 r r r r sin r sin Procedure for solving eqs. 1. 2. 3. 4. 5. 6. Choose Laplace (if no charge) or Poisson Solve by Integration if one variable or by Separation of variables if many variables Apply B.C. Find V, then E=-DV, D=E, J=sE Also, if necessary: Q S dS Dn S I J dS S P.E. 6.1 In a 1-dimensional device, the charge density is given by v o x / a If E=0 at x=0 and V=0 at x=a, find V and E. v 2V 2 x o x3 V Ax B 6a v o x / a Evaluating B.C. v o x 2 V E aˆ x A aˆ x x 2a A0 o a 2 B 6 2V o x3 3 3 V a x 6a o x 2 aˆ x E 2a P.E. 6.3 two conducting plates of size 1x5m are inclined at 45o to each other with a gap of width 4mm separating them as shown below. Find approximate charge per plate if plates are kept at 50V potential difference and medium between them has permittivity of 1.5 Applying B.C. V(0)=0, Vo V(o=45)=Vo=50 V 2 1 V 2 V 2 0 2 45o 1m 2V 0 2 V A B o Vo 1 V aˆ ˆ E a o Vo D E s D n ( 0) Q s dS o Vo o L b z 0 a 1 dzd Vo o L ln( b / a) P.E. 6.3 two conducting plates of size 1x5m are inclined at 45o to each other with a gap of width 4mm separating them as shown below. permittivity of 1.5 Applying B.C. V(0)=0, Q Vo L ln( b / a ) o V(o=45)=Vo=50 C C Vo Vo L ln( b / a) o L ln( b / a) o 1.5 o 1000mm C (5m) ln Vo / 4 5.226mm Q 45o b a 4mm / 2 a 5.226mm o sin 45 / 2 Q Q 444 10 12 F Q CVo 444 pF (50V ) 22nC detail 45o a 4mm / 2 a 5.226mm o sin 45 / 2 45o opuesto brecha / 2 sin a 2 hipotenusa b P.E. 6.5 Determine the potential function for the region inside the rectangular trough of infinite length whose cross section is shown. a) b) The potential V depends on x and y. Vo=100V, b=2a=2m, find V and E at: (x, y)=(a, a/2) (x, y)=(3a/2, a/4) V V 2 0 2 x y 2 2 y V=Vo a V=0 V=0 V=0 b V ( x 0,0 y a ) 0 V ( x b,0 y a ) 0 V ( 0 x b, y 0) 0 V (0 x b, y a ) Vo x P.E. 6.5 (cont.) Since it’s 2 variables, use Separation of Variables V ( x, y ) X ( x)Y ( y ) y V=Vo a X "Y XY " 0 V=0 V=0 X " Y" b V=0 X Y V (0, y ) X (0)Y ( y ) 0 X (0) 0 X "X 0 V (b, y) X (b)Y ( y) 0 X (b) 0 Y "Y 0 V ( x,0) X ( x)Y (0) 0 Y (0) 0 x V ( x, a ) X ( x)Y (a ) Vo inseparabl e Let’s examine 3 Possible Cases A. B. C. =0 <0 >0 Case A: If =o X "X 0 Y "Y 0 X Ax B B.C. X ( 0) 0 X (b) 0 B0 A0 X ( x) 0 V X ( x)Y ( y ) 0 y V=Vo a V=0 V=0 V=0 b This is a trivial solution, therefore cannot be equal to zero. x Case B: <o 2 X " X 0 2 general solution is : X A1ex A2 e x or B.C. X (0) 0 X (b) 0 X B1 cosh x B2 sinh x This is another trivial solution, therefore cannot be equal to zero. B1 0 B2 sinh b 0 B2 0 Case C: >o 2 X " X 0 2 general solution is : B.C. X Co e jx C1e jx X ( 0) 0 X (b) 0 or X g o cos x g1 sin x A series of solutions : nx X n ( x) g n sin b n b 2 2 go 0 g1 sin b 0 sin b 0 n b n 1,2,3,4 Case C: >o 2 Y " Y 0 with general solution is : Y ho cosh y h1 sinh y Yn ( y) h1 sinh x B.C. Y ( 0) 0 n b n 1,2,3,4 ho 0 nx ny Vn ( x, y ) X n ( x)Yn ( y ) g n hn sin sinh b b By superposition, the combination is also a solution: Vn ( x, y ) n 1 nx ny cn sin sinh b b Cont. B.C. at y=a nx na cn sin sinh b b Vn ( x, a ) Vo n 1 If we multiply by sin factor and integrate on x: b 0 mx na mx nx Vo sin dx cn sinh sin sin dx b b 0 b b n 1 b Orthogonality property of sine and cosine: b 0 0 mn 0 sin nx sin mx dx / 2 m n nx na 2 mx Vo sin dx cn sinh sin dx b b 0 b b b nx na 1 Vo cos cn sinh n b 0 b 2 0 b b 2nx 1 cos dx b b nx na 1 2nx Vo cos cn sinh 1 cos dx n b 0 b 20 b b b Vob 1 cos n cn sinh na b n b 2 4Vo na cn n sinh b 0 V ( x, y ) 4Vo n 1, 3, 5 n odd n even nx ny sin sinh b b na n sinh b V=Vo V=0 Equipotential lines Flux lines V=0 Find V(a,a/2) where Vo=100V, b=2a=2m 4V a V ( a, ) o 2 V n 1, 3, 5 400 n 1, 3, 5 44.51V sin na na sinh b 2b na n sinh b V=Vo nx ny sin sinh 2 2 n 1 n sinh 2 V=0 Equipotential lines Flux lines V=0 Find E at (a,a/2) V V E V aˆ x aˆ y x y 4Vo E ( x, y ) b 1 nx ny nx ny cos sinh aˆ x sin cosh aˆ y na b b b b n odd sinh b 400 1 na / 2 na E 0aˆ x sin cosh aˆ y b n odd sinh na b b b (115.12 19.127 3.9411 .8192 0.1703 0.035 0.0074 ...)aˆ y 99.25aˆ y V/m Resistance and Capacitance Resistance If the cross section of a conductor is not uniform we need to integrate: E dl V R l I sE dS S Solve Laplace eq. to find V Then find E from its differential And substitute in the above equation P.E. 6.8 find Resistance of disk of radius b and central hole of radius a. 1 V 1 2V 2V 2 2 0 2 z V A ln B dV E V ˆ d 1 V V ( a) 0 BC : V ( b) Vo V Vo ˆ ln b / a Vo Vo I sE dS S ln( b / a ) 2 ots Vo ln ln b / a a dS dz d ˆ 2tVos I sE dS ln( b / a) S R 0 b a t Capacitance E dS Q C S V E dl l Farads Is defined as the ratio of the charge on one of the plates to the potential difference between the plates: Assume Q and find V (Gauss or Coulomb) Assume V and find Q (Laplace) And substitute E in the equation. Capacitance 1. 2. 3. Parallel plate Coaxial Spherical Parallel plate Capacitor Charge Q and –Q Q s S Plate area, S Dn s aˆ x s E aˆ x or Dielectric, Q E dS E x S 0 Q Qd V E dl dx S S d d 0 Q S C V d Plate area, S - Coaxial Capacitor V Charge +Q & -Q Q E dS E 2L a V E dl b Q - - - Dielectric, d +d + E+ dS + 0 + 0 c - Q b ˆ dˆ ln 2L 2L a Q 2L C b V ln a Q Qd S S Spherical Capacitor Charge +Q & -Q Q E dS Er 4r 2 a Q Q 1 1 V E dl rˆ dr rˆ 2 4r 4 a b b Q 4 C V 1 1 a b What is the Earth's charge? The Earth is electrically charged and acts as a spherical capacitor. The Earth has a net negative charge of about a million coulombs, while an equal and positive charge resides in the atmosphere. The electrical resistivity of the atmosphere decreases with height to an altitude of about 48 kilometres (km), where the resistivity becomes more-or-less constant. This region is known as the electrosphere. There is about a 300 000 volt (V) potential difference between the Earth's surface and the electrosphere, which gives an average electric field strength of about 6 V/metre (m) throughout the atmosphere. Near the surface, the fine-weather electric field strength is about 100 V/m. Capacitors connection Series Parallel 1 1 1 C C1 C2 C C1 C2 Resistance Recall that: E dl V R I sE dS S E dS Q S C V E dl Multiplying, we obtain the Relaxation Time: Solving for R, we obtain it in terms of C: RC s R sC So In summary we obtained: Capacitor Parallel Plate Coaxial C R=/sC S d sd S 2L ln Spherical b a 4 1 1 a b b a 2sL ln 1 1 a b 4s P.E. 6.9 s1 s2 A coaxial cable contains an insulating material of s1 in its upper half and another material with s2 in its lower half. Radius of central wire is a and of the sheath is b. Find the leakage resistance of length L. b ln a R1 s1 L b ln a R2 s2 L They are connected in parallel R R1 || R2 b ln R a L 1 s 1 s 2 R1 R2 R1 R2 P.E. 6.10a 1 2 Two concentric spherical capacitors with 1r=2.5 in its outer half and another material with 2r=3.5 in its inner half. The inner radius is a=1mm, b=3mm and c=2mm . Find their C. We have two capacitors in series: c C1 4r1 o 1 1 a b C2 C 0.53 pF 4r 2 o 1 1 a b C C1C2 C1 C2 P.E. 6.10b 1 Two spherical capacitors with 1r=2.5 in its upper half and another material with 2r=3.5 in its lower half. Inner radius is a=1mm and b=3mm. Find their C. We have two capacitors in parallel: C C1 || C2 C1 C2 2 Q E dS Er 2 sin dd Q 2Er 2 a Q Q 1 1 ˆ ˆ V E dl r dr r 2 2r 2 a b b 2r1 o C1 Q / Vo 1 1 a b 2 1 2 C 0.5 pF 1 1 a b Method of Images Whenever the is a charge in the presence of a conductor. The conductor serves as a mirror. Substitute the conductor for a plane at V=0 and the image. The solution will be valid only for the region above the conductor. Line charge above ground plane E E E L L ˆ1 ˆ 2 2o 1 2o 2 1 ( x, y, z ) (0, y, h) ( x,0, z h) 2 ( x, y, z ) (0, y,h) ( x,0, z h) E L 2o xxˆ ( z h) zˆ xxˆ ( z h) zˆ x 2 ( z h) 2 x 2 ( z h) 2 L 1 L L ˆ 2 V V V 2 ˆ1 2 dl 2 ln o 2 o 1 o 2 L x 2 ( z h) 2 ln 2 2o x ( z h) 2