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Fields and Waves Lesson 3.3 ELECTROSTATICS - POTENTIALS Darryl Michael/GE CRD MAXWELL’S SECOND EQUATION Lesson 2.2 looked at Maxwell’s 1st equation:  D      D  ds     dv Today, we will use Maxwell’s 2nd equation:   E  0 or    E  dl  0 Importance of this equation is that it allows the use of Voltage or Electric Potential POTENTIAL ENERGY Work done by a force is given by:  dl  F    F  dl If vectors are parallel, particle gains energy - Kinetic Energy   If,  F  dl  0 Conservative Force Example : GRAVITY  F • going DOWN increases KE, decreases PE • going UP increases PE, decreases KE POTENTIAL ENERGY If dealing with a conservative force, can use concept of POTENTIAL ENERGY For gravity, the potential energy has the form mgz Define the following integral:     F  dl  Potential Energy Change P2 P1 POTENTIAL ENERGY     Since  E  dl  0 and F  q  E We can define: Potential Energy =     q  E  dl P2 P1 Also define: Voltage = Potential Energy/Charge   V ( P2 )  V ( P1 )    E  dl P2 P1 Voltage always needs reference or use voltage difference POTENTIAL ENERGY Example: Use case of point charge at origin and obtain potential everywhere from E-field Spherical Geometry Point charge at (0,0,0)  E q 4 0 r 2 Integration Path r  dl  aˆ r  infinity Reference: V=0 at infinity POTENTIAL ENERGY The integral for computing the potential of the point charge is:   V (r )  V (r  )    E  dl r r  0 r V (r )    E  dr r  r   r  q 4 0 r  dr 2 V (r )  q 4 0 r POTENTIAL ENERGY - problems Do Problem 1a Hint for 1a: R=a R=b R=r Use r=b as the reference Start here and move away or inside r<b region POTENTIAL ENERGY - problems For conservative fields:    E  dl  0 ,which implies that:      E  ds  0 , for any surface    E  0 From vector calculus:   f  0 ,for any field f Define:  E  V Can write:  E  f POTENTIAL SURFACES Potential is a SCALAR quantity Graphs are done as Surface Plots or Contour Plots Example - Parallel Plate Capacitor +V0/2 +V0 +V0 -V0 -V0 0 Potential Surfaces -V0/2 E-Field E-field from Potential Surfaces From:  E  V Gradient points in the direction of largest change Therefore, E-field lines are perpendicular (normal) to constant V surfaces (add E-lines to potential plot) Do problem 2 Numerical Simulation of Potential In previous lesson 2.2, problem 3 and today in problem 1, Given  or Q E-field derive V derive Look for techniques so that , given  or Q V derive Numerical Simulation of Potential For the case of a point charge: q q  V     V (r ) 4 0 r 4 0 r  r  Distance from charge  r , is field point where we are measuring/calculating V  r , is location of charge Numerical Simulation of Potential For smooth charge distribution:   (r )  dv  V (r )     4 0 r  r     (r )  dl  V (r )     4 0 r  r  Volume charge distribution Line charge distribution Numerical Simulation of Potential Problem 3    (r )  dl  V (r )     4 0 r  r  Setup for Problem 3a and 3b Line charge:  r origin   r  r  r Location of measurement of V Line charge distribution Integrate along charge means dl is dz Numerical Simulation of Potential Problem 3 contd... Numerical Approximation Break line charge into 4 segments l  r Charge for each segment   r  r q   l  l Segment length qi V    4 ch arg es 4 0 r  ri Distance to charge Numerical Simulation of Potential Problem 3 contd... For Part e…. Get V(r = 0.1) and V(r = 0.11) Use:  V V E  V   aˆ r   aˆ r r r So..use 2 points to get V and r • V is a SCALAR field and easier to work with • In many cases, easiest way to get E-field is to first find V and then use,  E  V