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Slide 1
Slide 1

... on horizontal air tract. It is attached to an object of mass m2 by a massless string. The pulley has radius R and moment of inertia I about it axis of rotation. When released, the hanging object accelerates downward, the glider accelerates to the right, and the string turns the pulley without slippi ...
Phys_21_N7_WORK_and_ENERGY
Phys_21_N7_WORK_and_ENERGY

... and slowly stretch the spring about 50 cm over several seconds. Hold the sensor still until data collection stops. Do not get any closer than 40 cm to the Motion Detector 16. Examine the graphs. Identify when you started to pulling the spring and when you stopped. 17. Examine the force vs. distance ...
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Principle of Equivalence
Principle of Equivalence

... resulting seismic P-wave propagates such that all the points of constant phase lie on a hemisphere centered at O. The surface of all points of the same phase is called a wave front although the inferred meaning is that the phase in question is associated with some identifiable first arrival of the w ...
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Land Wind Racer Design - Wyoming Scholars Repository

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Uniform circular motion

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PHYSICS 111 HOMEWORK SOLUTION #5 March 3, 2013
PHYSICS 111 HOMEWORK SOLUTION #5 March 3, 2013

ConcepTest 4.6 Force and Two Masses
ConcepTest 4.6 Force and Two Masses

... ConcepTest 4.6 Force and Two Masses A force F acts on mass m1 giving acceleration a1. The same force acts on a different mass m2 giving acceleration a2 = 2a1. If m1 and m2 are glued together and the same force F acts on this combination, what is the resulting acceleration? F ...
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A state-of-the-art multi-component seismic survey

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RP 1P1 Force and Motion - NC Science Wiki

... descriptions of the pattern of motion, such as vibrations and waves. Vibration involves parts of a system moving back and forth in much the same place, so the motion can be summarized by how frequently it is repeated and by how far a particle is displaced during a cycle. Another summary characterist ...
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Newton`s 2nd Law

... is inversely proportional to the mass. That is, By inversely we mean that the two values change in opposite directions. As the denominator increases, the whole quantity decreases. For example, the quantity is less than . ...
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tc mani̇sa celal bayar university physics i laboratory manuals 2016

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FORCES AND NEWTON`S LAWS OF MOTION

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Earthquakes - Perry Local Schools

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... curved path, you are passing through some angle if you take the center of the path as the center of circle. Circular motion and rotational motion might seem like the same thing - and they are very similar. A familiar example will help distinguish them in your mind. The Earth moves in (roughly) unifo ...
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Oscillatory Motion

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... 2. A crane carries a load of 400kg. It raises it from ground level to a height 30m, the crane then lowers it on to a platform 12m above the ground. Find the change in potential energy in each stage. ...
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Rotational Inertia

... weight to a string attached to a step pulley at the center of the disk. See Fig. 1. Using your results, you will determine the moment of inertia of the disk. ...
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... The device in Fig.8-7 is called torsion pendulum. The element of elasticity is associated with the twisting of a suspension wire. If we rotate the desk by some angular displacement  from its rest position (where the reference line is at   0 ) and release it, it will oscillate about that position ...
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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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