 he
sophisticated solver of this puzzle knows that
the resistance of a conductor depends on the "resistivity" of the material
out of which it is made and is furthermore directly proportional to the
length of the conductor and inversely proportional to its crossectional
area.
Now, a conventional conductor, like a wire, has a constant
crossectional area, so the resistance varies with its length. The earth
forms what is called a "sheet resistor"...
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Assuming a rather constant conducting depth, the space between
any two points on the surface offers countless pathways via which current
can flow, an effective crossectional area proportional to the surface area,
which is in turn proportional to the distance between the two points. The
effect of widening tends to cancel out the effect of lengthening, giving
a nearly constant resistance.
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The engineering unit for sheet resistance is "ohms per
square." Hey, ohms per square what?
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