 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"...
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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