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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

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