Gauss’ Law EE 311 - Lecture 20 • The first fundamental law of electrostatics in integral form is Gauss’ Law: Z I ρV Qtot dV E · dS = = (1) ǫ ǫ0 0 V S • This equation tells us that the “electric field flux” out of any closed surface is proportional to the total charge enclosed by the surface 1. Gauss’ law 2. Divergence 3. Using Gauss’ law to calculate fields 4. Examples • The total charge can be expressed as a volume integral of the volume charge density • The surface considered here doesn’t necessarily physically exist; any closed surface that we can imagine will do • Essentially this is telling us that charges are “sources” or “sinks” for fields; if there are no charges in a volume, there cannot be fields created or terminated in that volume 1 2 Divergence Using Gauss’ Law • Although Gauss’ Law is a fundamental law of electrostatics, it is only of limited use for finding fields produced by sources • This is because in integral form it describes an integration of fields; after a function is integrated, a lot of information is lost! • Example: Suppose the electric field flux out of a surface is zero - is the field on that surface then necessarily zero? • It is only possible to use the integral form of Gauss’ Law for finding fields produced by particular sources if the sources have a very high degree of symmetry • Consider Gauss’ Law where the surface used is a tiny cube, aligned with the xyz coordinates in a Cartesian system • There are 6 faces of the cube to keep track of: three sets of 2 parallel planes. The dimensions are small enough that we can neglect field variations in the cube in most cases. • Notice for each pair of parallel planes, the normals are pointing in opposite directions; also, the two planes are displaced by a distance 2∆ • Take the faces centered at x = +∆ and x = −∆ for example, each with area (2∆)2 : Face 1 flux : x̂ · E(∆, y, z)(2∆)2 • We can also try to find a “differential form” of Gauss’ Law: one that applies at a point instead of over some integrated region of space Face 2 flux : −x̂ · E(−∆, y, z)(2∆)2 dsz = z^ dx dy • To do this, simply shrink the surface S to be infinitesimally small - leads to the definition of “divergence” dy dx ^ dx dz dsy = y dz d = dx dy dz ^ dy dz dsx = x 3 dy 4 Divergence Continued • The total for these two faces is then (2∆)2 (Ex (∆, y, z) − Ex (−∆, y, z)) Gauss’ Law : differential form • If we shrink the surface considered to zero size in Gauss’ Law, then we obtain: ∇ · E = ρV /ǫ0 which starts to look like a derivative • We get a similar result for the other two pairs of faces, except they involve the y and z components of the fields • Adding up these three, we find the flux out of the tiny cube is Ψ = (2∆)2 (Ex (∆, y, z) − Ex (−∆, y, z) + Ey (x, ∆, z) − Ey (x, −∆, z) +Ez (x, y, ∆) − Ez (x, y, −∆)) • The divergence is defined as this result divided by the volume of the cube as the cube shrinks to zero size: ∂Ey ∂Ez ∂Ex + + divE = Ψ/(2∆)3 = ∂x ∂y ∂z • This is often notated as ∇ · E; the divergence is a “derivative” that operates on a vector function to produce a scalar 5 • The ρV appears on the right hand side because we divide by the volume in defining the divergence • The above is the “differential form” of Gauss’ Law; it applies at every point in space • The divergence essentially measures how much a field is flowing “into” or “out of” a point in space; it will be zero unless charges are located at this point • The “divergence theorem” allows us to connect the differential and integral forms directly; this is a general mathematical relationship: I Z E · dS = S dV ∇ · E (2) V 6 Using Gauss’ law to find fields • We can use the integral form of Gauss’ law to find the fields produced by a specific set of charges if the charges possess a high degree of symmetry • Based on the symmetry, we can find “Gaussian surfaces” over which the field has only a normal component, and on which that component is constant • If this is true, the total flux is just the field component times the surface area; setting this equal to the charge enclosed determines the amplitude of the field component • Types of sources for which this will work: – infinite line charge (cylindrical coords) – infinite cylinder surface/volume charges (cylindrical coords) – spherical surface/volume charges (spherical coords) – surface charges on an infinite plane (Cartesian coords) • In all these cases, the line, volume, or surface charge densities have to be constant 7 Example Use Gauss’ Law to find the electric field produced by an infinitely long line charge on the z axis; the line charge density ρl is constant on the line. • Line charge: use cylindrical coordinates and a cylindrical Gaussian surface • Think about symmetry with respect to each cylindrical coordinate: – Because the source is infinitely long, there can be no z dependence in the resulting fields. – Because the source is rotationally symmetric, there can be no φ dependence in the resulting fields – Fields will depend on r because this involves distance from the line 8 Example • Now think about symmetry with respect to field direction: – Imagine the line charge as made up of many small positive charges. At a given observation point, we add up all the radially outward pointing contributions from each charge – Because the line charge is infinite, there are always an equal number of charges above and below a given observation point. Thus, all z components of fields cancel out – Because the source is rotationally symmetric, there can be no φ components of the field – A r component makes sense, and will not cancel out. • Resulting form for field is then E(r, φ, z) = r̂Er (r) • This will be constant over the surface area of a cylinder with radius r, and is normal to the cylinder body. Total flux is then 2πrLEr (r) for a cylinder of radius r and length L Finish Example • According to Gauss’ law in integral form, the total flux out of this cylinder equals to the charge enclosed divided by ǫ0 • The cylinder of length L encloses a total charge of ρl L, since the line charge holds ρl coulombs per meter. • Setting these two equal, we find Er (r) = ρl 2πǫ0 r • For this highly symmetric problem, Gauss’ law made it simple to find the field produced by a charge distribution • Notice the field of the line charge falls off as one over the distance, instead of one over distance squared for a point charge. • The infinite size of the line charge makes this slower fall-off possible 9 10 Electric potential • Because electric fields can exert forces on charged objects, they have the ability to do work; i.e. to transfer energy EE 311 - Lecture 21 • Just like moving an object to a higher point in a gravitational field increases its “potential energy”, moving a charged object in an electric field modifies its “electric potential” • Consider a test charge qtest that is moved through an electric field (presumably created by other charges somewhere) 1. Electric potential 2. Path independence: KVL • The work obtained in doing this is Z Z F · dl = qtest E · dl W = 3. Examples C C where C is the path that qtest is moved through • We obtain work here because the field is exerting the force. R The work required by us is −qtest C E · dl 11 12 Electric potential cont’d • An electric potential difference between points P1 and P2 is defined as the work per unit charge required to move a test charge from P1 to P2 in the presence of the electric field E that exists between P1 and P2 • Mathematically this is: V (P2 ) − V (P1 ) = − Z P2 E · dl P1 with V representing the electric potential; note qtest vanished due to “work per unit charge” • The units of V are Newton-meters/Coulomb or Joules per coulomb. This unit is defined to be the Volt • Notice V is a scalar that results from the underlying vector electric field; in many cases it can be much easier to work with V than E • This electric potential is exactly the voltage of circuit theory, but now we have a connection to the underlying fields 13 Path independence • Notice we originally talked about a path C connecting points P1 and P2 when defining the potential, but finally we just used integration starting and stopping points at P1 and P2 • It turns out the particular path chosen doesn’t matter because line integrals of electric fields are path independent • Recall our second fundamental law of electrostatics: I E · dl = 0 (3) C • This looks like the computation of an electric potential, but the path is a closed loop (i.e. starts and stops at the same point) • Consider two alternate paths from P1 to P2 . By reversing the direction of one of these paths, we can create a closed loop path by combining the two. Because the integral over the closed loop is zero, we find the integral over either path from P1 to P2 must be the same • Thus the potential difference between two points is unique 14 Absolute potential KVL • The path-independent property in defining the electric scalar potential also results in “Kirchhoff’s voltage law” (KVL) • If we break a closed loop path into pieces, the line integral of E over each piece will produce a potential difference. • However all of these will have to add to zero; thus the sum of the voltage rises equals the sum of the voltage drops • KVL is one of the fundamental circuit equations, but again we now have a connection to the fields that underly this circuit statement • Remember we’re considering static fields here; this means there are no time variations in the sources producing the fields. KVL will need to be modified when we have time varying sources in EE 312 15 • Notice so far we’ve only defined a potential difference between two points, but not the potential at a particular point • We can get an “absolute potential” by choosing the point P1 to be a reference point (i.e. “ground”), and defining the potential at all other points in terms of this point. • In many cases, the point at distance infinity is taken to be zero absolute potential. • The absolute potential difference at another point then becomes: Z P2 E · dl V (P2 ) = − ∞ This is the work per unit charge required to move a test charge from ∞ to P2 • This is not always the reference point chosen though so it is important to keep track of the “zero volts” reference point in all problems 16 Absolute potential of a point charge • Absolute potential of a point charge at the origin is: Z R q R̂ V (R) = − · dl 4πǫ0 R2 ∞ • Take our path as radially outward from the point charge to infinity; the integral can be performed to get Z ∞ q (R̂ · R̂dR) V (R) = 4πǫ0 R2 R q V (R) = 4πǫ0 R • We can evaluate the amount of work needed to move a test charge qtest in this field simply by taking qtest (V (R2 ) − V (R1 )) ′ • For a point charge at position R , the result is q ¯ ¯ V (R) = ′¯ ¯ 4πǫ0 ¯R − R ¯ • The law of superposition still applies; simply add these for multiple charges or integrate for charge distributions Finding fields from V • We’ve defined the electric potential in terms of a line integral of the electric field • Notice if we take a very small path, the differential voltage obtained is: dV = −E · dl • However, for a scalar function we can also use the gradient to find dV = ∇V · dl • Comparing these two, E = −∇V i.e. the electric field is the gradient of the potential • Using our gradient properties, this tells us that the electric field points in the direction of maximum decrease of the potential • Also, the electric field is everywhere normal to surfaces of constant potential. These surfaces are called “equipotentials” 18 17 An example • Consider a capacitor connected to a battery; the battery supplies positive charges to the top plate of the cap and negative charges to the bottom plate Another example • Consider equipotentials in the x-y plane as shown. What is the electric field? • This results in a downward pointing electric field • The potential difference from the point P2 to P1 is Z P2 E · dl V (P2 ) − V (P1 ) = − y V= 2 Volts P1 • Notice E · dl will be negative here; this means the potential difference is positive, and P2 is at a higher potential than P1 • Electric potentials generally increase as we move closer to positive charges; they decrease as we move closer to negative charges P + + + + y =2m V= 1 Volt y= 0m V= 0 Volts 2 y=−2 m + V− dl E − − − − P V=−1 Volts 1 19 20 x Curl EE 311 - Lecture 22 • We have seen that the computation of V from E is path independent, due to our second law of electrostatics: I E · dl = 0 (4) C • Just as we derived the divergence operator by thinking about Gauss’ law evaluated for a small box, we can derive the “curl” operator by thinking about the above equation on a small path. H • Consider C E · dl for a small square path in the xy plane: 1. Curl 2. Types of media 3. Conductors y 4. Examples 2∆ x 2∆ 21 22 Curl continued Curl properties • If we add up the four contributions from the sides of this path we will get: 2∆(Ey (∆, y) − Ey (−∆, y) + Ex (x, ∆) − Ex (x, ∆)) • If we divide this by the area bounded by the path, it becomes ∂Ex ∂Ey − ∂x ∂y • We could also choose similar paths in the yz or xz planes; separate these as different components of a vector. To do so, multiply each result by a unit vector normal to the area • These are open surfaces: choose direction of normal based on right hand rule with dl • Sum of all three components is the curl; measures the tendency of a vector function for rotation about a point in space • The curl of a vector field produces a vector! 23 • Performing the mathematical analysis shows that the curl operator in Cartesian coordinates is: ¯ ¯ ¯ x̂ ŷ ẑ ¯¯ ¯ ¯ ¯ ∂ ∂ ∂ ¯ curl A = ¯¯ ∂x ∂y ∂z ¯ ¯ ¯ ¯ Ax Ay Az ¯ • The curl of A is also written as ∇ × A • Electrostatic fields have ∇ × E = 0 due to path independence; differential form of second fundamental law • As the divergence theorem connects the divergence operator to a flux integral, Stokes’ Theorem connects the curl operator to a line integral: I Z ¢ ¡ A · dl ∇ × A · dS = C S Here the contour C bounds the area S; dl and dS satsify a r-h-rule relationship 24 Perfect conductors Types of media • So far we’ve been talking about electric fields in free space, i.e. nothing around but vacuum. Things change when fields exist in the presence of other objects or media • We can classify material media into two basic types: – Conductors: contain some loosely held electrons that are free to move (metals) – Insulators: electrons are tightly held, cannot move easily • The conductivity of a material σ in S/m is a measure of this property: high conductivity = good conductor, low conductivity = good insulator • We will focus on either “perfect electric conductors” (PEC) with σ = ∞ or “perfect insulators” with σ = 0 in many cases • A perfect conductor with σ = ∞ is capable of relocating an arbitrary amount of charge from within the conductor • This is not really possible, but a reasonable approximation for most metals • Assume we have a PEC material, and put a charge inside; the inside charge produces an electric field, so that the “free” charges in the PEC start moving around • These “free” charges create their own electric fields as they move around; they keep moving around until all the electric fields cancel out • The end result is that the field is zero inside the PEC; a surface charge density can be left on the surface PEC Material + 111111111111111111 000000000000000000 000000000000000000 111111111111111111 000000000000000000 111111111111111111 000000000000000000 111111111111111111 000000000000000000 111111111111111111 + 000000000000000000 111111111111111111 000000000000000000 111111111111111111 000000000000000000 111111111111111111 000000000000000000 111111111111111111 000000000000000000 111111111111111111 000000000000000000 111111111111111111 000000000000000000 111111111111111111 + PEC Material + + + + + Point charge inside PEC 25 26 Perfect conductor “boundary conditions” Potentials and PEC materials • We can now start to talk about problems involving both free space and PEC regions • We know that there is no volume charge density inside a PEC, that there is no E field inside a PEC, and that there can be surface charge densities ρS on the surface of a PEC • The presence of the surface charges means that there cannot be any tangential E field on the surface of a PEC; if there were, the surface charges would move around to cancel it out • However, there can be a normal E field on the surface of a PEC, because the surface charges can’t move off the PEC • Using Gauss’ law with a small box on the PEC gives us a relationship between the normal component of E on the PEC surface and the “induced” surface charge density ρS • The final “boundary conditions” on a PEC surface are: Etan = 0 Enorm = ρS /ǫ0 27 + + 1111111111111111111 0000000000000000000 + + 0000000000000000000 1111111111111111111 + 0000000000000000000 1111111111111111111 + 0000000000000000000 1111111111111111111 − − + 0000000000000000000 1111111111111111111 + − + − 0000000000000000000 1111111111111111111 0000000000000000000 1111111111111111111 − + − + 0000000000000000000 1111111111111111111 0000000000000000000 1111111111111111111 + + 0000000000000000000 1111111111111111111 0000000000000000000 1111111111111111111 + + 0000000000000000000 1111111111111111111 + + + + + + + Volume charge density=0 everywhere inside PEC; surface charge density can exist on surface; fields inside are zero • The fact that Etan = 0 on the surface of a PEC means that the surface of a PEC is an equipotential surface; i.e. a conductor is everywhere at the same potential in electrostatics • The above statement disagrees with the v(z, t) we studied in transmission line theory; however those were dynamic fields, not static as we are covering here R • PEC’s are equipotentials because evaluating E · dl along the surface of the PEC will always produce zero • We already know that E is normal to equipotential surfaces; our PEC boundary conditions confirm this fact • Also the fact that E vanishes in a PEC means that a solid PEC material has the same potential even everywhere inside the PEC • Placing a PEC in a static field causes surface charges to be induced on the conductor so that Etan vanishes 28 An example Solution • Gauss’ law can still be used to find E fields produced with charges in the presence of PEC materials; just remember properties of PEC’s! • The high degree of spherical symmetry allows Gauss’ Law to be used to find fields here. Fields are of the form E = R̂ER (R) Problem: A point charge is located inside a (non-charged) hollowed PEC sphere. Sphere inner radius is Ri , outer radius is R0 . Find E 000000000000000000000000000 everywhere111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 Point charge q 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 R 000000000000000000000000000 111111111111111111111111111 i 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 R 000000000000000000000000000 111111111111111111111111111 o 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 • For R < Ri , only the point charge is enclosed and the resulting field is ER (R) = 4πǫq0 R2 • For Ri < R < Ro , we are inside the PEC material, where the field must vanish: ER (R) = 0. This is consistent with Gauss’ law because a surface charge density of total charge −q is induced on the inner PEC surface to cancel the total charge enclose; ρS on inner surface is −q/(4πRi2 ) • For R > Ro what happens? We said the PEC material is uncharged; this means the induced charge on the inner surface had to come from somewhere. • Thus a surface charge density of total charge +q is left on the outer sphere surface; field is then ER (R) = 4πǫq0 R2 for R > Ro 29 30 Another example: Method of Images Method of Images • The method of images is a trick that is useful for understanding fields produced by charges in the presence of an infinite PEC plane (i.e “ground plane”) • Consider a point charge above an infinite PEC plane; surface charge density will be induced on plane to cancel tangential electric field • The total field above the PEC is then determined both by the point charge and the surface charge distribution on the PEC surface; complicated! Fields ignoring ground plane Effect of ground plane charges q Infinite PEC "ground plane" q Method of Images q − − − − − − − − Infinite PEC "ground plane" −q 31 • The method of images says that the total fields above the PEC are the same as those in an “image” problem • In the image problem, we get rid of the PEC plane so that only free space is left • In the image problem, we consider the original source above the PEC plane, plus an “image” of the source. The image is the “reflection”of the original source through the PEC plane • The image source has opposite charge to the original, and is the same normal distance away from the PEC plane • It is much easier to find the fields in the “image” problem: just a sum of two point charges. The case with the PEC is much harder due to the distribution of charges on the PEC surface • The “image” sources in this particular case are known as an “electric dipole”: equal but opposite charges separated by a distance 32 Dielectrics • A perfect dielectric material is a perfect insulator; i.e. σ = 0 • There are no “free” charges in a perfect dielectric, so you might think that these materials produce no electric effects • However, the “bound” charges in the atoms of a dielectric still cause electric effects. These electrons are not free to move among atoms, but an electric field still exerts a force on them EE 311 - Lecture 23 • The effect of this is to distort the orbit on the electrons; result is effectively an induced bound-charge dipole, which does produce electric effects 1. Dielectrics 2. Dielectric boundary conditions Distorted electron orbit 3. Examples Negative electron orbits Model of distorted orbit effects − − Positive nucleus + E Positive nucleus + E E + dipole − 33 34 Electric Flux Density Other Dielectric Properties • Notice that the fields of the induced dipoles oppose those of the applied field; total field inside is smaller • We have to account for the effect of these induced dipoles if we want to describe fields in dielectrics. To handle this, we introduce a new field, known as D, the “electric flux density” • The effect of the induced dipoles is then included by modifying Gauss’ Law to: I Z D · dS = dV ρV = Qtot (5) S V It is clear from this equation that the units of D are C/m2 • This is pretty similar to the old Gauss’ law, but the connection between D and E is now important; this connection models how the dipoles in a medium respond to an applied electric field • It turns out in most cases that the induced dipoles are in the same direction as the applied field, with an amplitude directly proportional to the applied field 35 • The end result of this is that D and E are related through a constant ǫ, the “permittivity” of the medium: D = ǫE In free space, D = ǫ0 E and the new and old forms of Gauss’ law are identical • We used the permittivities of media in our study of transmission lines, but hopefully now the meaning is clearer • The induced dipoles don’t remain “bound” charges forever if we keep increasing the applied field; eventually these charges are “ripped” from the atoms to become free charges • This effect is called “dielectric breakdown”; produces sparks in air (at 3 MV/m) • The “dielectric strength” of a material is the maximum E amplitude the material can tolerate before breakdown occurs • Limits the power handling capabilities of devices; table in book 36 Dielectric boundary conditions • We talked about how fields behave at an interface between free space and a PEC; now consider an interface of dielectrics • Consider fields E 1 , D1 above an interface and E 2 , D2 below; apply laws of electrostatics on small regions at the interface R • The law C E · dl = 0 provides information about tangential electric fields E1t and E2t on the interface. We can show that E1t = E2t , i.e. tangential electric fields are continuous H • The law S D · dS = Q provides information about normal flux densities D1n and D2n . We can show that D1n − D2n = ρS . Typically ρS will exist only on a PEC surface D1n ^2 n Medium 1 ε1 E1 E1n } ∆h2 } ∆h2 E1t E2n E2t E2 a ∆s c d b ∆h 2 ∆h 2 ∆l Medium 2 ε2 { { ρs ^ D2n n1 Boundary conditions • Note that normal D will be discontinuous if there is a surface charge density present • Knowledge of normal D can tangential E allows us to determine the total fields D and E both above and below the interface • Remember that these boundary conditions apply only at the interface! Fields away from the interface in the two regions are not necessarily related in any way • A few examples: Are BC’s satisfied? (region 1 is z > 0, region 2 is z < 0): – Region 1 free space, Region 2 PEC: E 1 = x̂2 V/m, E 2 = 0 – Region 1 free space, Region 2 ǫ = 2ǫ0 : E 1 = ŷ3 V/m, E 2 = ŷ(z + 3) – Region 1 ǫ = 3ǫ0 , Region 2 ǫ = 2ǫ0 : E 1 = (x̂2 + ŷ3 + ẑ) V/m, E 2 = (x̂2 + ŷ3 + 1.5ẑ) V/m 37 38 Example: Gauss’ Law with dielectrics Solution • It is easy to use the new Gauss’ Law with dielectrics, just replace previous E with D and forget ǫ0 factors Problem: A point charge q is located at the center of a hollowed dielectric sphere (inner radius Ri , outer radius Ro , permittivity ǫ). Find the electric field everywhere. 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 Permittivity ε 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 Permittivity ε 000000000000000000000000000 111111111111111111111111111 0 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 Point charge q 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 R 000000000000000000000000000 111111111111111111111111111 i 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 R 000000000000000000000000000 111111111111111111111111111 o 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 000000000000000000000000000 111111111111111111111111111 39 • The high degree of spherical symmetry allows Gauss’ Law to be used to find fields here. Fields are of the form D = R̂DR (R) • For R < Ri , only the point charge is enclosed and the resulting q field is DR (R) = 4πR 2 • For Ri < R < Ro , we are inside the dielectric material. However using D automatically takes care of this for us. There are no more charges enclosed so DR is the same as for R < Ri • For R > Ro , no new charges again, so DR stays the same • However, the electric field E is varying in the three regions due to the changing permittivities. • The final E field satisfies the bc’s, and has E = R̂ER (R): q for R < Ri ER = 4πǫ0 R2 q for Ri < R < Ro ER = 4πǫR2 q for Ro < R ER = 4πǫ0 R2 40 Capacitance • Consider two PEC objects of arbitrary shape. Place a total charge of +Q on one of them and −Q on the other; this charge is distributed over the surface of the conductors in a complicated way EE 311 - Lecture 24 • These charges result in an electric field between the two conductors (from + conductor to − conductor). Relationship between charges and E is complicated • If we know E, we can find the potential difference V between the two conductors by line integrating the electric field. The + conductor will be at high potential. 1. Capacitance 2. Calculating capacitance 3. Examples Surface S + + + + Q + Conductor 1 + + + + V + - + + ρs E - - -Q Conductor 2 - - - 41 Capacitors • This structure is called a capacitor. The capacitance of the capacitor is C = |Q|/|V | and has units of Coulombs/V olt or Farads (F) • Because the voltage V that results between the two conductors is directly proportional to the applied charge Q, the capacitance is independent of the amount of charge applied • Capacitance does depend on the geometry of the conductors and the materials surrounding them • We can find the capacitance of a capacitor if we know the electric field everywhere. Normal D boundary condition on PEC surfaces allows ρS , then total charge Q to be determined. Line integral of E determine V . Ratio is capacitance 43 42 Calculating capacitance The following steps are useful for computing the capacitance of highly symmetric caps: 1. Choose an appropriate coordinate system based on symmetry properties of conductors 2. Assume total charges +Q and −Q on the two conductors; for highly symmetric caps, these also determine ρS 3. Find E from Q using Gauss’ law 4. Find the potential difference between the conductors using R1 V = − 2 E · dl, where points 1 and 2 are on the + and − conductors respectively. Choose dl to be as simple as possible 5. The capacitance is then C = Q/V 44 Example: Parallel plate capacitor Example: Follow steps • A parallel plate capacitor (as in our parallel plate T-line) is made from two PEC plates of area A separated by distance d • Cartesian coordinates are best for this structure, due to planar symmetry • Because the plates are of finite size, there are not many symmetry properties of this device, and our procedure doesn’t work. However for “large” plates, we can approximate that the E field for finite plate area is the same as if the plates were infinite. • Assume +Q on top plate, −Q on bottom. ρS = ±Q/A on top/bottom plates • This is called the “no fringing” approximation, because “fringing” fields at the edge of the finite plates are neglected Conducting plate z Area A ρs z=d + V - z=0 +Q + + + + + + + + + + + ds E E E - - - - - - - - - - - -ρs + + + E E - + - + - + Fringing field lines Dielectric ε Conducting plate • Symmetry properties of fields: no x or y variations, only a ẑ component for infinite plates. Thus D = ẑDz (z). Choose a rectangular box for the Gaussian surface, top of box inside upper PEC plate, bottom of box above bottom plate. • The box encloses charge Q on the top plate, flux out of bottom is −Dz (z)A. Gauss’ Law gives Dz (z) = −Q/A = −ρS . Then E = −ẑρS /ǫ • Note this field has constant amplitude and does not decay with distance from the charges; due to assumed infinite size of plane. Also note that PEC boundary condition is satisfied R z=d • Line integral of electric field is V = − z=0 E · ẑdz = Qd/(ǫA) • Capacitance is then C = Q/V = Q/(Qd)ǫA = ǫA/d as expected 45 46 Example: Coaxial capacitor Example: Follow steps • A coaxial capacitor (as in our coaxial T-line) is made from two coaxial cylinders Q on • Assume −Q on inner cylinder, +Q on outer. ρS = − 2πal Q inner cylinder, 2πbl on outer • Because the line is of finite length, there are not many symmetry properties of this device. However for “large” lengths, we can approximate that the E field for finite length is the same as if the line were infinitely long. • Symmetry properties of fields: no φ or z variations, only a r̂ component for infinite length. Thus D = r̂Dr (r). Choose a cylinder for the Gaussian surface, with the cylinder radius between a and b. • This is called the “no fringing” approximation, because “fringing” fields at the ends of the line are neglected • The box encloses charge −Q on the inner cylinder, flux out of cylinder is 2πrDr (r)l. Gauss’ Law gives Dr (r) = −Q/(2πrl). Then E = −r̂Q/(2πrlǫ) • Cylindrical coordinates are best for this structure l + V - b a + + + + + + + + + + + + + E E E - - - - - - - - - - - - - - - - - - - - - - - - ε E E E + + + + + + + + + + + + + ρl -ρl Inner conductor Dielectric material Outer conductor 47 • Line integral of electric field is Z r=b Z r=b Q Q ln(b/a) 1/r = E · r̂dr = V =− 2πlǫ 2πlǫ r=a r=a • Capacitance is then C = Q/V = Q/(Q ln(b/a))2πlǫ = 2πǫl/ ln(b/a) • We previously used this result for our coaxial transmission lines! 48 Capacitor properties • Because a capacitor can hold separated positive and negative charges, it can store electric potential energy; we could get a lot of work out of these charges by letting them move toward each other under their own force • We know from circuit theory the energy stored in a capacitor is 1 2 2 CV ; this is an electrostatic potential energy • Notice both cap types had capacitance directly proportional to ǫ. Larger ǫ values result in a smaller voltage for a fixed amount of charge. This is due to the opposition effect of induced dipole moments in a dielectric • Geometry of conductors matters too: larger individual conductor areas increase capacitance; C increases as conductors brought closer together • Dielectric breakdown limits the maximum voltage that can be applied. Occurs first on inner conductor in coaxial cap 49 Other capacitor properties • Multiple capacitors connected in parallel share the same voltage but combine charges; effective capacitance is sum of individual capacitances • Multiple capacitors in series produce a total voltage that is the sum of the voltage across each. Effective capacitance is “parallel” combination of individual capacitances • We have been able to compute capacitances of a few highly symmetric caps here through the use of Gauss’ law • However procedure is much more difficult for non-symmetric capacitors; need computers to handle this case • Most familiar capacitors: coaxial, “chip” capacitors on PCB’s ( parallel plate) • Any object capable of holding electric charge has a capacitance; second conductor may be the Earth surface 50 Imperfect conductors EE 311 - Lecture 25 1. Imperfect conductors • We’ve now considered both perfect conductors (σ = ∞) and perfect insulators σ = 0; a capacitor combined these two materials. No currents flow in either of these material types • However real materials lie somewhere between these two. In this case, it is possible for currents to flow inside the medium • Current is a measure of the number of coulombs per unit time flowing through a specified area. Total current flowing through a surface is then a scalar quantity, measured in Amps (C/sec) 2. Resistance 3. Example • The current ∆I flowing through a small piece of area dS in a given amount of time can be written as 4. Charge conservation ∆I = J · dS where J is the “current density”, and is a vector having units of A/m2 51 52 Current density Point form of Ohm’s Law • J is a vector point function of space, and captures currents flowing in any possible direction • Example: A volume charge density ρV moving with velocity u produces a current density J = ρV u • While J essentially is a current spread over and flowing through an area, is also possible to have a surface current density J S spread over and flowing through a line. Units of J S are A/m • For example, J S can exist on the surface of a PEC if the surface charges on PEC move along the surface Volume Current density Surface current density J Js l S • Given our definition of J, the total current flowing out of a closed surface S is then I I= J · dS S • An imperfect conductor contains free charges that can move in response to an applied field • In many media, the current density that results is in the same direction as the applied field, and directly proportional to the applied field magnitude: J = σE • In these materials, the parameter σ characterizes the current density induced by applied fields; the units of σ are Amps/V olts/m or Siemens/m • The above equation is the “point form of Ohm’s Law” • Note we can have currents flowing in a medium even if ρV = 0 everywhere in the medium; the currents must be “steady” so that equal amounts of charge move in and out together 53 54 Resistance • In an ohmic medium, an applied electric field results in a current flowing through the medium; the electric field also produces a potential difference in the medium • The ratio of the voltage to the current between two points in the medium is the resistance: R = V /I • We can write this ratio mathematically as: R1 R1 − E · dl − E · dl = R2 R= R 2 J · dS σ S E · dS S Simple Resistance Example • Consider our parallel plate capacitor again, but in this case the dielectric medium inside has conductivity σ • For steady currents, there are no charges in this problem that we didn’t include before when analyzing the capacitor. Thus, fields are identical to the previous solution: E = −ẑQ/(Aǫ) • However a current density now results between the plates: J = σE = −ẑσQ/(Aǫ) • Recall we found C = Q/V or 1/C = V /Q. Write this as R1 R1 − 2 E · dl − 2 E · dl 1/C = R = R D · dS ǫ S E · dS S The denominator uses a Gaussian surface enclosing one of the conductors. • Combine them: RC = ǫ/σ; i.e. it is easy to find R or C from knowing the other. We used this in our T-lines study as well 55 Conducting plate z Area A ρs + z=d V z=0 +Q + + + + + + + + + + ds E E E - - - - - - - - - -ρs + - + + + E E - - + - + - + Fringing field lines Dielectric ε Conducting plate 56 Continue Example • The voltage between the plates is Qd/(Aǫ); to find the total R current flowing between the plates, use I = S J · dS • Choose S to be the same size as the plates, but located in between the two plates. Resulting I is σQ/(ǫ) • The resistance is then R = V /I = Qd/(Aǫ)ǫ/(σQ) = d/(σA) • The resistance between two conductors typically increases with the distance between the two conductors, decreases as σ increases, and decreases as the area through which the currents flow increases • Our answer satisfies RC = d/(σA)ǫA/d = ǫ/σ. • In our T-line studies, this R modeled the current flow between conductors. We represented this as a conductance G which for the parallel plate line is σA/d 57 Equation of charge conservation • One of the fundamental properties of electrostatics is that charge is conserved; it can be moved around, but can neither be created or destroyed • Since moving charges are represented by currents, we should be able to write an equation relating the total current flowing out of a volume to the rate of change of the total charge enclosed • The integral form of the equation of charge conservation is: I Z ∂Qenc ∂ dV ρV = − J · dS = − ∂t V ∂t • This equation is saying that current flowing out of a closed surface results in a decrease of the amount of charge in the volume enclosed by the surface 58 Power dissipation Steady currents and KCL • Using the divergence theorem, we can convert the left hand side to a volume integral. Canceling the volume integrals then yields a differential form: ∇·J =− ∂ρV ∂t • For steady currents, the rate of change of the volume charge density is zero, so the net current flux through any closed surface is zero • This is “Kirchhoff’s current law” for circuits: the sum of the currents out of any closed surface is zero; at circuit junctions the sum of the incoming currents must equal the sum of the outgoing currents • Now that we’ve got both voltages and currents, we can talk about power dissipation • Circuit theory tells us that dc power = VI. How is this related to fields? • Consider a current density that results from moving charges, i.e. J = ρV u • If these charges are moving through an electric field, the electric force on the charges results in the performance of work • Power=work per unit time: P = F · charge = qE · u for a point • Here we’ve got a volume charge density, so the power density in W atts/m3 is ∆P = E · (ρV u) = E · J • The total power dissipated in a volume is then Z Pdiss = E·J V This is “Joule’s Law” in point form 59 dl dt 60