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Recitation Ch 4-1
Recitation Ch 4-1

... 4-58 An electron (mass = 9.11 x 10-31 kg) leaves one end of a TV picture tube with zero initial speed and travels in a straight line to the accelerating grid, which is 1.80 cm away. It reaches the grid with a speed of 3.00 x 106m/s. If the accelerating force is constant, compute (a) the acceleratio ...
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Chap #3
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... Weight is the force of gravity acting on an object. It is numerically equal to mg, were g is about 10 m/s2 here on the surface of the earth. Example: What is the weight of a football player with a mass of 150 kg? W = mg = 150 kg×10m/s 2 = 1500 N (; 330 lb) Practice: What is the mass of a ballerina w ...
Chapter 8 - RHIG - Wayne State University
Chapter 8 - RHIG - Wayne State University

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Chapter 4 (in pdf)

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An earthquake is the vibration of the Earth that results in a

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... A force F = 100 N presses a brake pad against the edge of a spinning disk. The axis of rotation is perpendicular to the plane of the disk, through its center. The coefficient of friction between the pad and the disk is  = 0.4. The spinning disk has mass of M = 15 kg, a radius of R = 0.5 m, and a mo ...
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4.2.2 Newton`s Laws - Renton School District

... the wings. If an airplane is going to fly, the amount of lift must be greater than the force of gravity, and the amount of thrust produced by the engine must be greater than the drag force created by air resistance. Wing shapes that provide lift and have the proper angle of attack (the angle at whic ...
advanced placement chemistry
advanced placement chemistry

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W3.13 Newton`s Law Quick Hitters 2

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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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