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Conservation of impulse and momentum
Conservation of impulse and momentum

... For a system of particles, we can define a “fictitious” center of mass of an aggregate particle of mass mtot, where mtot is the sum ( mi) of all the particles. This system of particles then has an aggregate velocity of vG = ( mivi) / mtot. The motion of this fictitious mass is based on motion of t ...
V K M I + =
V K M I + =

Relationships between linear and angular motion Examples
Relationships between linear and angular motion Examples

Rotational Motion
Rotational Motion

... changes with time determines the angular velocity ω. The direction of angular velocity is either clockwise or counterclockwise. How quickly the angular velocity changes determines the angular acceleration α. The linear velocity v and linear acceleration also v depend on the radius of rotation, which ...
ExamView - Newton`s Laws Review.tst
ExamView - Newton`s Laws Review.tst

Forces
Forces

khammoe_literature-review
khammoe_literature-review

Slide 1 - Mother Seton
Slide 1 - Mother Seton

force-problems-with-acceleration-2-step
force-problems-with-acceleration-2-step

... second ball rolled with the same force accelerates 4 m/sec2. What are the masses of the two balls? ...
Background Experiment 1: Open-Mic and Oscillating Air Molecules
Background Experiment 1: Open-Mic and Oscillating Air Molecules

... Figure 1: It’s open-mic time in 102. Image credit: metromusicmakers.com. For this part of the experiment, you will use a sound recording software package called Audacity. Download a free copy from: http://web.audacityteam.org/download/. It is a wonderful, easy to use piece of software that is essent ...
S Waves
S Waves

... Earthquakes occur due to movements that take place within the Earth. Large pressures build up between huge plates of land both above and below the sea. The release of these pressures is accompanied by huge releases of energy as one land mass slides against another. ...
Chapter 3 Summary
Chapter 3 Summary

... • The weight on the surface of the Earth would be 98.0 N • Fgrav = m g • The mass on the Moon would be 10.0 kg • The weight on the Moon would be ~ 16.3 N • gMoon ~ 1/6 gEarth ...
AP 1 Midterm Review
AP 1 Midterm Review

ROTATIONAL MOTION
ROTATIONAL MOTION

5 pt 1 pt
5 pt 1 pt

... Moh’s scale for Talc ...
5.1 The First Law: The Law of Inertia
5.1 The First Law: The Law of Inertia

Forces in 1D Phet Lab
Forces in 1D Phet Lab

... Newton’s Laws describe motion and forces in the world around us. Object have inertia, undergo acceleration and experience forces. Forces are measured in Newtons (N)… Newton’s First Law states: __________________________________________________________________________ Newton’s Second Law states: ____ ...
force - Typepad
force - Typepad

... • Friction is the "evil monster" of all motion. Regardless of which direction something moves in, friction pulls it the other way. – Move something left, friction pulls right. Move something up, friction pulls down. • It appears as if nature has given us friction to stop us from moving anything.  ...
Thermohaline Fine Structure in an Oceanographic Front from
Thermohaline Fine Structure in an Oceanographic Front from

... temperature (SST) measurements acquired during seismic profiling show the front between the Labrador Current (LC) and the NAC and show that seismic reflectance differs between these water masses. The impedance contrasts responsible for the observed reflections are caused by small changes in sound sp ...
Chapter 12 Notes
Chapter 12 Notes

... When you combine forces by adding or subtracting, you are finding the Net Force. The net force is the overall force acting on an object after all forces have been combined. ...
Moment of Inertia - Ryerson Department of Physics
Moment of Inertia - Ryerson Department of Physics

... A heavy flywheel is set in rotation by a mass attached to a string wrapped around the axle of the flywheel. The force exerted by the falling mass is related to the torque, Γ, and the rate of change of angular velocity of the wheel, that is, the angular acceleration, α. The moment of inertia, I, is t ...
Worked solutions Chapter 2: Collisions and
Worked solutions Chapter 2: Collisions and

... v p = v g – v w = 500 km h–1 north – 100 km h–1 west = 500 km h–1 north + 100 km h–1 east Using vectors and trigonometry, this gives v p = 510 km h–1 at 11 T so D is correct. Using the formula x = ut + 0.5at2, then 2.0 = 0 + 0.5 × 9.8t2 and t = 0.64 s for both For ball X: horizontal velocity = 5.0 ...
Newton`s Laws Problem Solving Worksheet Name: Use g = 10.0 m
Newton`s Laws Problem Solving Worksheet Name: Use g = 10.0 m

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File

PowerPoints
PowerPoints

... – Example: if the acceleration is along the direction of motion, the speed grows by the same amount in each time interval (e.g., second) – if the speed changes by 1 meter per second each second, the acceleration is (1 meter per second) per second, or 1 m/s2. if v = 15 m/s at time t = 0, and a = 1 m/ ...
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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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