Tuesday Jan. 27, 2009

In class today a mixture of theoretical type stuff and some examples of instruments that could be used to measure lightning and thunderstorm electric fields (that make use of some of these concepts).


Point 1 is the integral form of Gauss' Law that was derived in class last Thursday.  It is a relatively simple thing to show that if the charge q is located outside the volume V then the surface integral of E is zero.


Here we use the divergence theorem to write the surface integral of E as a volume integral of the divergence of E.  The charge enclosed by a volume of space charge is the volume integral of the space charge density rho.  We can set the two volume integrals equal to each other and obtain the differential form of Gauss' law. 

Homework #1 pt. 1 was handed out at this point.  I would suggest using the differential form of Gauss' Law to answer the first question.  Here also is a handout with the various operators (gradient, divergence, etc) in cartesian, cylindrical, and spherical polar coordinates.

If you write the electric field as the gradient of the electrostatic potential and then substitute that into Gauss' Law you can obtain Poisson's Equation.  Laplace's equation applies in situtations where the volume space charge density is zero.


Next we imagine placing a conductor in an electric field


Free electrons inside the conductor will quickly move around and redistribute themselves in such a way that they will cancel out the field in the conductor (as the electrons move they leave behind positively charged atoms).  Very quickly the field inside the conductor will be zero.  There is also no space charge inside the conductor, all the charge is distributed along the surface on the conductor.  The electric field lines in the vicinity of the conductor will be distorted and will strike the surface of the conductor perpendicular (if there were any tangential component, charges would move and cancel it out).

Next we'll use Gauss' Law to determine a relationship between the surface charge density and the electric field strength at the surface of a conductor.

A cylindrical volume, half inside and half outside the conductor is used.  You must integrate the electric field, E, over the surface of the cylinder. 

1.  The E field is zero inside the conductor.  So you get no contribution to the surface integral from the bottom end of the cylinder.

2.   Along the sides of the cylinder, E is perpendicular to the vector normal to the surface.  So there is no contribution to the surface integral from the sides of the cylinder.

3.   The only contribution comes from the top end of the cylinder.  E and the normal vector are parallel.  So the contribution from the top end is just E A, where A is the area of the top end of the cylinder.   The charge enclosed is just A σ
, where σ is the surface charge density.  The electric field at the surface of the conductor is perpendicular to the conductor and has the value highlighted in yellow.


One way of measuring time varying electric fields (from lightning discharges say) is to use a flat plate antenna (aka flush plate dipole antenna).  It basically consists of a large flat grounded plate that would be positioned on the ground (preferably flush with the surrounding ground).  A smaller circular sensor plate is found inside a center hole as shown below.


Charge induced by a changing electric field moves to and from the sensor plate.  This current is proportional to the time derivative of the electric field.  Integrating the current gives an output signal that is proportional to E.

In the circuit above the antenna is connected to a capacitor (this is a passive integrator).  Some kind of measuring device would be connected across the capacitor.



In some cases the input impedance of the measuring device together with a small capacitance in the passive integrator (a small capacitance would provide higher gain) gives a time decay constant that is too short.  An example is shown above.



A cloud to ground discharge typically last around 0.5 seconds.  You could use a so-called "slow E field antenna" to faithfully record the electric field changes that occur during the totality of the flash.  A slow antenna might have a time decay constant of several seconds.  If you want to study the individual return strokes, say, you can use a "fast E field antenna" which has a much shorter (typically about 1 ms) decay time constant.



When the E field antenna sensor plate is connected to an active integrator circuit like shown above, the input impedance of the measuring equipment won't affect the decay time constant.  The decay time constant is determined by the R and C values in the operational amplifier feedback circuit.


Flat plate antennas can be used to measure time varying electric fields but not static fields.  For static fields, a "field mill" is usually used.