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Dynamics: Inverted pendulum on a cart
Dynamics: Inverted pendulum on a cart

Physics
Physics

question 2 - Larbert High School
question 2 - Larbert High School

Upper mantle anisotropic structure of the Eastern Alps E. Qorbani, G
Upper mantle anisotropic structure of the Eastern Alps E. Qorbani, G

ppt document
ppt document

... similar tool for rotations? We already have: p = mv and SF = dp/dt. If we multiply both sides of Newton’s Second law by the radius we have (with v = r): St = r SF = r  dp/dt = d(r  p)/dt = dL/dt (where we have used the fact that dr/dt  p = v  mv = 0) ...
Earthquake magnitude Richter magnitude (Local Magnitude ML
Earthquake magnitude Richter magnitude (Local Magnitude ML

Physics 231 Topic 7: Oscillations Wade Fisher October 5-10 2012
Physics 231 Topic 7: Oscillations Wade Fisher October 5-10 2012

... We can also express this in terms of an angular frequency: The angular frequency  =  /  t = 2 π / T  = the speed at which the angle is changing ...
SC81 Physics Curriculum Map 2010/2011 Revised 7/29/2010
SC81 Physics Curriculum Map 2010/2011 Revised 7/29/2010

... centripetal force and centripetal acceleration for an object in circular motion. 2. Calculate the magnitude of centripetal force and centripetal acceleration for an object in circular motion. S5 C2 PO 11 1. Predict how the force will change between two masses when the distance between them increases ...
04_lecture_outline
04_lecture_outline

Earthquake slip on oceanic transform faults
Earthquake slip on oceanic transform faults

... (solid lines, 20 samples per second), are corrected for the instrument response and ®ltered between 1 and 150 s. The dashed lines are the synthetics. The stations are chosen to allow comparison between earthquakes on each transform and between transforms. The dates, depths and magnitudes are given. ...
File
File

... 2. A car is stopped at a traffic light. If then travels along straight road so that its distance from the light is given by x(t )  bt 2  ct 3 , where b=2.40 m/s2 and c=0.120 m/s3. a) Calculate the average velocity of the car for the time interval t=0 to t=10 s. b) Calculate the instantaneous veloc ...
STP 111 THEOR - Unesco
STP 111 THEOR - Unesco

... Cohesion is the force of attraction between molecules of the same kind e.g the molecules of water Adhesion is the force of attraction between molecules of water and glass Cohesion and adhesion explain the different action of water and mercury when spilled on a clean glass surface. Because of the adh ...
AP Physics Chapter 1
AP Physics Chapter 1

Physics Experiments in Mechanics
Physics Experiments in Mechanics

... Physical quantities, length, mass, time, etc., are constantly being measured in the laboratory. All experimentally determined quantities contain some degree of error or uncertainty. It is important that the experimentalist knows how to record the data and results so that it’s clear just how precise ...
Lecture14-10
Lecture14-10

PHYSICS 111 HOMEWORK SOLUTION #10 April 8, 2013
PHYSICS 111 HOMEWORK SOLUTION #10 April 8, 2013

1 Simple harmonic motion related to circular motion
1 Simple harmonic motion related to circular motion

PPT
PPT

... displacements. The first has a magnitude of 150 cm and makes a angle of 1200 with the positive x-axis. The resultant displacement has a magnitude of 140 cm and is directed at an angle of 35.00 to the positive x axis. Find the magnitude and direction of the second displacement. ...
SPH3U Exam Solutions Lisa Di Lorenzo - ped4126-2010
SPH3U Exam Solutions Lisa Di Lorenzo - ped4126-2010

Chapter 4 Notes
Chapter 4 Notes

... • An elephant and a mouse would both have zero weight in gravity-free space. If they were moving toward you with the same speed would they bump into you with the same force? • No, the elephant is harder to stop, more inertia. ...
Coriolis Force - Atmosphere Physics
Coriolis Force - Atmosphere Physics

Chapter 5-6
Chapter 5-6

... accelerated from rest to 35 m/s over a distance of 0.70 m. Find the magnitude for the average force exerted by the racket on the ball during the serve. 61.3 N [Answer] Newton’s second law: F = m a To find F, we need to find a: For constant acceleration motion: s = (vf2 – vi2 ) /(2*a) Rearrange the e ...
PHYSICS 149: Lecture 3 - Purdue Physics
PHYSICS 149: Lecture 3 - Purdue Physics

Ball 1 of mass m moving right with speed v bounces off ball 2 with
Ball 1 of mass m moving right with speed v bounces off ball 2 with

... Answer: This one is tricky. The hoop goes faster at the top. Both hoop and puck have the same KEtrans = (1/2)mv2, but , in addition, the hoop has some KErot. In going up the hill, both hoop and puck lose the same amount of KE (KE = –mgh). But for the puck, all of its lost KE was translational KE. W ...
SHM Part 1 - Ask Physics
SHM Part 1 - Ask Physics

... after a regular intervals of time is called periodic motion. Therefore, revolution of the Earth around the Sun is a periodic motion. The time period of this periodic motion is roughly 365 days. Therefore, T ≈ 365 days = 365 X 24 X 60 X 60 s = 31536000 s. Hence, frequency: ...
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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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