Physics for Geologists, Second edition
Physics for Geologists, Second edition
Physics for Geologists, Second edition
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78 Electricity and magnetism<br />
Figure 8.2 The field between two electrodes in a homogeneous, isotropic<br />
medium. Lines and surfaces of equal energy, called equipotential<br />
lines/surfaces, are normal to the flow paths. (This is a map of part of<br />
a field, not of a block.)<br />
energy or potential by virtue of the elevation to which water would rise<br />
unassisted in the boreholes (the static water level). A contour map of the<br />
elevation of the water surface in boreholes drilled to the same aquifer is a<br />
map of the energy of the aquifer, as we saw in Figure 3.7. The contours<br />
are lines of equal energy (equipotential lines) and flow lines are normal to<br />
them. The surface contoured is a notional surface called the potentiometric<br />
surface.<br />
Magnetism<br />
Magnetism is one of the fundamental <strong>for</strong>ces of the universe. The mineral<br />
magnetite, FeO . Fe203, commonly with titanium oxide, Ti02, has been<br />
known <strong>for</strong> more than 2500 years <strong>for</strong> its properties of attracting iron and<br />
orientating itself in the Earth's magnetic field. A bar magnet has a magnetic<br />
axis, the ends of which are called poles. The end that seeks the geographical<br />
North when freely suspended is called the North pole or North-seeking pole<br />
(or +); the other is the South or South-seeking pole (or -).<br />
We can magnetize bars of ferromagnetic metals (iron, nickel, cobalt and<br />
some of their alloys) by putting them in a magnetic field; by cooling them<br />
when aligned N-S; by stroking them with another magnet (the new pole at<br />
the beginning of the stroke is the same as the stroking pole); and by hammer-<br />
ing them when oriented in a magnetic field. This last is the reason why steel<br />
ships and boats become magnetized during their construction, particularly<br />
Copyright 2002 by Richard E. Chapman