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Physics for Geologists, Second edition

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66 Electromagnetic radiation<br />

radiation travels, whereas wavelength is not (as we saw when considering<br />

the refraction of light).<br />

Cosmic radiation<br />

Cosmic radiation, which was discovered early in the twentieth century, con-<br />

sists of very high frequency, high energy X-rays together with very high<br />

energy particles. The general level was found to be roughly constant over<br />

24 hours, so clearly the radiation does not come from the Sun. The inten-<br />

sity was found, by apparatus flown in balloons, to increase up to a height<br />

of about 12 km (a height now flown by many aircraft!), then to decrease;<br />

so some cosmic radiation, or its effect, is clearly generated within the<br />

atmosphere. Cosmic radiation is much more intense in the polar regions<br />

than the equatorial, so clearly some of the particles are charged positively,<br />

others negatively. The equatorial regions are protected by the magnetic field's<br />

being approximately tangential to the Earth's surface near the Equator.<br />

Gamma rays<br />

y-rays are high-energy radiation from radioactivity with frequencies greater<br />

than 100 x 1018 Hz (wavelengths shorter than about 10-12 m, or 1 pm), and<br />

their significant property is that they are not affected by magnetic fields so<br />

they are not charged particles. a and 0-particles are affected by magnetic<br />

fields.<br />

y-rays are emitted spontaneously from the nucleus of some unstable isotopes.<br />

They are gradually absorbed when passing through solids, but can<br />

penetrate some millimetres of steel, some centimetres of concrete, and rather<br />

more centimetres of sedimentary rock. The main isotopes yielding y-rays are<br />

of the uranium and thorium families, and 4 0 ~<br />

(potassium-40). 4 0 ~<br />

occurs in<br />

the micas and K-feldspar, and clay minerals by cation-exchange. Mudrocks<br />

or mudstones have a level of y-radiation that is significantly higher than<br />

that of sandstones and most carbonates. The natural y-radiation is, there-<br />

<strong>for</strong>e, a useful borehole-logging parameter. When y-rays are absorbed by<br />

a nucleus, neutrons and a-particles are emitted.<br />

Catalytic activity is enhanced by y-rays. Most clay minerals act as catalysts<br />

in petroleum-chemical reactions, and most emit y-rays spontaneously, and<br />

this may be significant in the generation of petroleum. The catalytic cracking<br />

unit in petroleum refineries used to use natural Fuller's Earth (which contains<br />

montmorillonite and other clay minerals) as the catalyst to improve the yield<br />

of high-octane-number gasoline and reduce the gas yield.<br />

X-rays<br />

X-rays were discovered in 1895 by Wilhelm Rijntgen when he found fluo-<br />

rescence in a cathode tube when electrons were beamed from the cathode<br />

Copyright 2002 by Richard E. Chapman

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