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Chapter 4-6 - OPFI Conceptual Physics
Chapter 4-6 - OPFI Conceptual Physics

Vectors & Scalars - The Grange School Blogs
Vectors & Scalars - The Grange School Blogs

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... motion of the body may be viewed within the reference plane, all the forces (and couple moments) acting on the body can then be projected onto the plane. An example of an arbitrary body of this type is shown in the figure below. Here the inertial frame of reference x, y, z has its origin coincident ...
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EXPERIMENT 1- Measurements and Accuracy

... The initial velocity Vo of the projectile can also be determined by using the ballistic pendulum (Fig 2). It consists of a spring gun that fires a metallic ball of mass m which is caught by a catcher at the end of a pendulum of mass M. The collision between the ball and pendulum is perfectly inelast ...
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... represent, mathematically, a system with some input, x(t ) , and output, y(t ) . Figure 1 illustrates typical notation for a linear system, L , where the function x (t ) is input into the system, shown as a box, and the system returns the output signal y (t ) . The arrows indicate whether the functi ...
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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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