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8.012 Physics I: Classical Mechanics MIT OpenCourseWare rms of Use, visit: .
8.012 Physics I: Classical Mechanics MIT OpenCourseWare rms of Use, visit: .

... A cylinder of mass M, length L and radius R is spinning about its long axis with angular velocity on a frictionless horizontal surface. The cylinder is given a sharp, horizontal strike with impulse Δp at a distance r from its center of mass (COM). Assume that constant gravitational acceleration acts ...
Document
Document

... three-quarters circle. A golf ball is pushed into the tube at one end at high speed. The ball rolls through the tube and exits at the opposite end. Describe the path of the golf ball as it exits the tube. The ball will move along a path which is tangent to the spiral at the point where it exits the ...
Derive the mass to velocity relation
Derive the mass to velocity relation

Inertial and Non-Inertial Frames of Reference - K
Inertial and Non-Inertial Frames of Reference - K

... (which is an inertial frame of reference) the ball just continues to move forward at the speed it was already going, and it’s motion is easily explained by the law of inertia. To an observer in the inertial frame of reference (the ground) the bus experiences a net force causing it to decelerate. The ...
Chapter 4-4
Chapter 4-4

... • Weight = Fg • Fg = mass x gravity ...
Chapter 8: Rotational Motion
Chapter 8: Rotational Motion

Newtons` second law is customarily presented to beginning students
Newtons` second law is customarily presented to beginning students

... 1. Introduction. Center of gravity, center of mass, this concept seems very familiar. Indeed, many people including students of science have used the phrase in daily conversation. Yet, “what is the center of mass?”, and of more concern, what are its properties? We explore these ideas in the attempt ...
Chapter 9 Linear Momentum and Collisions
Chapter 9 Linear Momentum and Collisions

... Time of collision is short enough that external forces may be ignored Inelastic collision: momentum is conserved but kinetic energy is not Completely inelastic collision: objects stick ...
10.2 Simple Harmonic Motion and the Reference Circle
10.2 Simple Harmonic Motion and the Reference Circle

14_Lecture_Outline
14_Lecture_Outline

Lecture Outline
Lecture Outline

... The physical pendulum • A physical pendulum is any real pendulum that uses an extended body instead of a point-mass bob. • For small amplitudes, its motion is simple harmonic. (See Figure 14.23 at the right.) • Follow Example 14.9. ...
Chapter 5 Summary
Chapter 5 Summary

5. Systems of Particles
5. Systems of Particles

... But it only changes because the position of the particle changes, not because the potential function itself is changing). 5.1.5 Why the Two Body Problem is Really a One Body Problem Solving the dynamics of N mutually interacting particles is hard. Here “hard” means that no one knows how to do it unl ...
Chapter 2 KINETICS OF PARTICLES: NEWTON`S SECOND LAW
Chapter 2 KINETICS OF PARTICLES: NEWTON`S SECOND LAW

Luis Anchordoqui
Luis Anchordoqui

1 Speed of light is the maximal possible speed 2 Adding velocities
1 Speed of light is the maximal possible speed 2 Adding velocities

... v > c, even worse things happen: 1 − v 2 /c2 becomes less then zero, and then its square root does not exist! (or becomes purely imaginary, if you know what I am talking about). This suggests that perhaps it is not possible for any object to move faster than light. And perhaps it is not possible to ...
Getting mathematical - Teaching Advanced Physics
Getting mathematical - Teaching Advanced Physics

... These graphs can be represented by equations. For displacement: x = A sin 2ft or x = A sin t f is the frequency of the oscillation, and is related to the period T by f = 1/T. The amplitude of the oscillation is A. Velocity: v = 2f A cos 2ft = A cos t Acceleration: a = - (2f)2 A sin 2ft = - ...
Word version of Episode 302
Word version of Episode 302

Newton’s Laws of Motion
Newton’s Laws of Motion

... All objects were classified into categories of earth, water, air, or fire. “Natural motion” occurred when an object sought to return to its “natural place” after being moved from it by some type of “violent motion.” ...
IB Phys Y1
IB Phys Y1

... Define the concepts of distance, position, displacement, speed, velocity and acceleration for the motion of objects. Explain the difference between instantaneous and average values of speed, velocity and acceleration. Outline the conditions under which the equations for uniformly accelerated motion ...
Q8188
Q8188

... performance factors when the system shows a negative stiffness. The floor displacement is maximum for without retrofitted building frame as compared to retrofitted building frame. In building using shear walls, floor displacement is minimum for shear wall placed at corner then at intermediate and co ...
Centripetal acceleration
Centripetal acceleration

... Why does the formula for centripetal acceleration that we just wrote down have the square of the speed in the numerator, and not just the speed? One way to see this is using what is called dimensional analysis. In essence, you check the units on both sides of the equation and the units match if the ...
California Physics Standard 1a Send comments to: layton@physics
California Physics Standard 1a Send comments to: layton@physics

Slide 1
Slide 1

... Two masses are vertically hanging on either side of a small frictionless pulley (this is called an Atwood machine). One of the objects has three kilograms of mass. What is the mass of the other object if it is stationary? What is the mass of the other object if it is moving at a constant speed down ...
AP physics final AP test review Mechanics
AP physics final AP test review Mechanics

... Since speed of object remains constant, kinetic energy remains constant, and work is zero. Friction, tension, normal force, gravity and the magnetic force are common forces that can act centripetally to cause uniform circular motion. 26. Centripetal Force (A-184 #46) A car initially travels north an ...
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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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