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lecture14
lecture14

... point A to each other point in the body, and each squared distance is scaled by the mass of each point Ai 2 i A ...
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Study Guide for Mechanics Lab Final

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... 31. A 200.0 kg astronaut and equipment move with a velocity of 2.00 m/s toward an orbiting spacecraft. How long will the astronaut need to fire a 100.0 N rocket backpack to stop the motion relative to the spacecraft? a. This is an impulse problem where we have to drain away the momentum of the astro ...
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... 26. *A 2 Kg mass and a 3 Kg mass are attached to a massless cord that passes over a frictionless pulley. The masses are free to move. a. Draw the scenario, showing all forces acting on both masses. (in class) b. What direction does the smaller mass move? (up) c. What is the acceleration of the syste ...
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... When a ball enters a curve, even if its speed does not change, it is accelerating because its direction is changing. When a ball goes around a curve, the change in the direction of the velocity is toward the center of the curve. Acceleration toward the center of a curved or circular path is called c ...
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... higher an object goes, the longer it stays in flight. The shell hitting submarine #2 goes less high, therefore it stays in flight for less time than the other shell. Thus, submarine #2 is hit first. ...
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... 2. Hang the 200-g mass at the point by which the meterstick is still in equilibrium. Record this point 3. Find the theoretical value, that is, solve analytically the position of the 200-g mass in order to balance the meterstick using the conditions for static equilibrium. 4. Calculate the percentage ...
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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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