Hey, thanks for an unexpected and most informative reply.
The atmosphere is an extremely high impedance, low current voltage source,
Very well put.
with a vertical electric field of typically 100 V/m
This has always fascinated me, though the numbers I’ve seen vary.
and current density in the range of 1 to 10 picoamperes/square meter.
Now that’s VERY new, to me at least - food for much further thought.
http://www.feynmanlectures.caltech.edu/II_09.html
The Master Himself, eh? Will certainly take a look.
How do you plan to measure the voltage due to the charge accumulated on the plate
My first thought was simply to prove that ions were being emitted. As it turns out, very simple. Take a piece of blank PCB 1" x 2", cut the copper across the middle to give two 1"" squares, bridge them with a neon bulb and a capacitor (10 - 100n @ >100V), grasp one end and hold the other near the emitters in a darkened room, and you’ll see the neon flash as accumulated ions charge the cap and ignite the bulb.
and of what use is the measurement?
The first ‘roughy’ I built didn’t flash the bulb - calculated at maybe 2kV max. The second calculated at 5 - 7kV gave 2 - 3 flashes per second. I’m still hoping to find the time to get a string of 1kV resistors as V divider input to a hi-Z voltmeter to get a reasonably accurate number, but so many other things …
the current into or out of the Earth ground would be informative.
Yep, that’s why this post; though NOT Earth GND, but current from the emitters direct to the collector plate (the “connection to the atmosphere”) is what I was wanting.
Much appreciated.