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Newton 2nd law1
Newton 2nd law1

... – 0, as evident by the non-changing velocity ...
Physics Laboratory #1: Simple Harmonic Motion
Physics Laboratory #1: Simple Harmonic Motion

... the total impulse acting on the object during a given time interval. If the net force is constant, the total impulse is equal to the product of the net force and the time interval over which the net force acts: Fnett  m(v f  vi ) If the net force varies over the time that the net force acts on the ...
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... Zookeepers lift a stretcher that holds a sedated lion. The total mass of the lion and stretcher is 175 kg, and the upward acceleration of the lion and stretcher is 0.657 m/s2. What force is needed to produce this acceleration of the lion and the stretcher? 1. List the given and unknown values. ...
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... along a line that makes an angle of 400 to the right of the original path. The second object moves at an angle of 100o to the left of the path of the first object after the collision. A) Determine the momentum of each object after the collision. B) Calculate the speed of each object after the collis ...
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... Surface waves cause most of the destruction resulting from earthquakes. Surface waves move rock particles in a backward, rolling motion and a side-to-side, swaying motion, as shown in Figure 8. Many buildings are unable to withstand intense shaking because they are made with stiff materials. The bui ...
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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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