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Lab 7 Ballistic Pendulum! !
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... Calculate the initial speed from this data. Include the uncertainty. Analysis Here is a case where two measurements of the same value are done two different ways without an expected value. How do we know if the two experiments agree? We now have two pdf’s, one for each experiment. One question we wa ...
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... Fnet (t )  m 2 x(t ) Since both m and  are constants, notice that the Net Force, Fnet, is proportional to the position, x, of point P. The negative sign signifies that the direction of the Net Force is opposite the direction of the position. In other words, the Net Force, Fnet, is a restoring fo ...
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... given initial angle. If Eq B3 holds, and the higher terms are negligible, the plot should be close to linear. Perform a linear least squares fit of the data to T()/T* vs.  (and find A from this fit). Compare your slope with the theoretical value of 1/16. It is not necessary to find the uncertaint ...
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Seismometer

Seismometers are instruments that measure motion of the ground, including those of seismic waves generated by earthquakes, volcanic eruptions, and other seismic sources. Records of seismic waves allow seismologists to map the interior of the Earth, and locate and measure the size of these different sources.The word derives from the Greek σεισμός, seismós, a shaking or quake, from the verb σείω, seíō, to shake; and μέτρον, métron, measure and was coined by David Milne-Home in 1841, to describe an instrument designed by Scottish physicist James David Forbes.Seismograph is another Greek term from seismós and γράφω, gráphō, to draw. It is often used to mean seismometer, though it is more applicable to the older instruments in which the measuring and recording of ground motion were combined than to modern systems, in which these functions are separated.Both types provide a continuous record of ground motion; this distinguishes them from seismoscopes, which merely indicate that motion has occurred, perhaps with some simple measure of how large it was.The concerning technical discipline is called seismometry, a branch of seismology.
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