新概念入门第四册 42 PART B
[audio]http://sound.yywz123.com/tingbbs/xgnrm/xgnrmdsic/42b.mp3[/audio]A simple experiment will help us a little further. Tie a heavy weight at the endof a long piece of string. With the hand held high in the air hold the strings so thatthe weight nearly touches the ground. Now move the hand to and fro and around but not up and down. It will be found that the weight moves but slightly or not at all. (1)_______________________. Imagine an earthquake shock shaking the floor, the paper, you and your hand. In the midst of all this movement the weight and the pen would be still. But as the paper moved from side to side under the pen point its movement would be recorded in ink upon its surface. It was upon this principle that the first instruments were made, but the paper was wrapped round a drum which rotated slowly. As long as all was still the pen drew a straight line, but while the drum was being shaken the line that the pen was drawing wriggled from side to side. The apparatus thus described, however, records only the horizontal component of the wave movement, which is, in fact, much more complicated. (2)_______________________; it would be up and down, to and fro and from side to side. Instruments have been devised and can he so placed that all three elements can be recorded in different graphs. When the instrument is situated at more than 700 miles from the earthquake centre, the graphic record shows three waves arriving one after the other at short intervals. The first records the arrival of longitudinal vibrations. The second marks the arrival of transverse vibrations which travel more slowly and arrive several minutes after the first. These two have travelled through the earth. It was from the study of these that so much was learnt about the interior of the earth. The third, or main wave, is the slowest and has travelled round the earth through the surface rocks.
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