I open this thread to discuss the matter of GROUND BALANCE as seen during bench testing and simulations.
Difficult ground is the one that gives a resistive response and also a reactive response.
The resistive response is due to the conductivity of the ground.
The reactive response is due to the magnetic permeability of the ground.
The combination of the 2 responses in a wide variety of proportions, amounts to the generalized HOT GROUND.
We would like to totally eliminate this ground response, so that we can better see the desired targets.
The best material I found so far, for simulating hot ground in the lab, is to use a pile of red bricks under the coil. The red bricks have their color from the iron oxide, generated by the firing at high temperature of the bricks.
The firing also leaves a remanent magnetism by aligning the magnetic particles in the brick to the earth's field. A red brick therefore has a slight magnetic field surrounding it, in the shape of a magnetic dipole. This can easily be verified with a magnetometer.
When we take a few bricks and pile them up, without verifying the pole sign of the dipole, most likely the bricks end up with the poles in all different directions so the various fields partly cancel themselves.
When we subject the bricks to the TX field, some of the magnetic particles align themselves to the TX field. When we remove our TX field, these particles realign with the Earth's field.
So far, we seem to have a fair similarity with HOT GROUND.
Let's look at some signal traces, to see if we can discern changes with the proximity of the Bricks to the coil.
For a start, I propose to take some screen shots with brick ground and without.
I would much appreciate, if somebody would superpose the pictures by GIMP or Photoshop, to make the differences easier to see.
Then I would like to see some suggestions of how to improve on this ground model and how to reproduce the wide variety we find in the field, in a controlled and repeatable manner.
Let's do it!!!!!
Tinkerer
Difficult ground is the one that gives a resistive response and also a reactive response.
The resistive response is due to the conductivity of the ground.
The reactive response is due to the magnetic permeability of the ground.
The combination of the 2 responses in a wide variety of proportions, amounts to the generalized HOT GROUND.
We would like to totally eliminate this ground response, so that we can better see the desired targets.
The best material I found so far, for simulating hot ground in the lab, is to use a pile of red bricks under the coil. The red bricks have their color from the iron oxide, generated by the firing at high temperature of the bricks.
The firing also leaves a remanent magnetism by aligning the magnetic particles in the brick to the earth's field. A red brick therefore has a slight magnetic field surrounding it, in the shape of a magnetic dipole. This can easily be verified with a magnetometer.
When we take a few bricks and pile them up, without verifying the pole sign of the dipole, most likely the bricks end up with the poles in all different directions so the various fields partly cancel themselves.
When we subject the bricks to the TX field, some of the magnetic particles align themselves to the TX field. When we remove our TX field, these particles realign with the Earth's field.
So far, we seem to have a fair similarity with HOT GROUND.
Let's look at some signal traces, to see if we can discern changes with the proximity of the Bricks to the coil.
For a start, I propose to take some screen shots with brick ground and without.
I would much appreciate, if somebody would superpose the pictures by GIMP or Photoshop, to make the differences easier to see.
Then I would like to see some suggestions of how to improve on this ground model and how to reproduce the wide variety we find in the field, in a controlled and repeatable manner.
Let's do it!!!!!
Tinkerer
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