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Lab 3. Centripetal Force
Lab 3. Centripetal Force

SESSION 2: NEWTON`S LAWS Key Concepts X
SESSION 2: NEWTON`S LAWS Key Concepts X

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Recitation 1

... Plugging our A and ω into our x(t) yields the equation of motion we set out to find. (b) To find the maximum speed, we could either take the derivative of x(t) (like we did in 12.2), or realize that the derivative will have another factor of ω in it’s amplitude and jump to the answer vmax = Aω = 6π ...
Gravity - Planet Holloway
Gravity - Planet Holloway

Clicker Question
Clicker Question

... Summary of Newton’s Three Laws • An object tends to remain at rest, or, if moving, to continue moving at constant speed in a straight line (1st Law). Objects tend to resist changes in motion (inertia) – mass measures this. • (2nd Law) When there is a net force on an object, it will accelerate: a = ...
EXAMPLES ON MODELLING OF MECHANICAL AND ELECTRICAL
EXAMPLES ON MODELLING OF MECHANICAL AND ELECTRICAL

Unit I: Concept Enhancer
Unit I: Concept Enhancer

... and acceleration in order to develop Newton’s 2nd Law. In these activities you discovered the variables that affected acceleration. We call acceleration the dependent variable because it depends on the value of other variables such as force and mass. Force and mass are independent variables because ...
Part IV
Part IV

... Example: Accelerometer A small mass m hangs from a thin string & can swing like a pendulum. You attach it above the window of your car as shown. What angle does the string make a. When the car accelerates at a constant a = 1.20 m/s2? b. When the car moves at constant velocity, v = 90 km/h? ...
Achievement - Waimea Physics
Achievement - Waimea Physics

Investigation 1: Gathering Evidence and Modeling
Investigation 1: Gathering Evidence and Modeling

...  Some of the lines will go through the Earth without hitting the inner circle.  Some of the lines, however, will hit the inner circle. This is a boundary between zones with different wave speeds – remember from the last part what happens when waves go through QuickTime™ and a boundaries. TIFF (Unc ...
Lecture 16 - Circular Motion
Lecture 16 - Circular Motion

Force and it laws (Basics)
Force and it laws (Basics)

Force and Motion
Force and Motion

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Newton`s laws Prez - Ms. Gamm

... location • Weight is measured in: Newtons (N) or pounds (lbs) ...
Space For Refection
Space For Refection

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COEFFICIENT OF FRICTION

Physics Section 3 Newton`s Laws of Motion 3.6 Second Law of
Physics Section 3 Newton`s Laws of Motion 3.6 Second Law of

Monday, February 25, 2013
Monday, February 25, 2013

Centripetal force - mrhsluniewskiscience
Centripetal force - mrhsluniewskiscience

... Reminder: AP test and solutions manual giancoli physics principles with applications 6th edition solution manual 3rd site in google gives a pdf Physics – Comcast.net ...
Circular Motion
Circular Motion

... 1. If the central force is continually increased, the body will spiral in. this gives a displacement in the direction of the force, work is done and the body speeds up. 2. If the central force is increased and then held constant, a smaller faster circular path results 3. If the force is held constan ...
Circular Motion
Circular Motion

CFA #2 Study Guide Name: Class: ______ Kinetmatics Review 1. A
CFA #2 Study Guide Name: Class: ______ Kinetmatics Review 1. A

... d) slightly more than 2 N, leftward ...
MASSACHUSETTS INSTITUTE OF TECHNOLOGY
MASSACHUSETTS INSTITUTE OF TECHNOLOGY

Here - UCSB HEP
Here - UCSB HEP

... > m1g Net force on the two blocks is F = m2g. But F=(m1+m2)a Æ a = m2g/(m1+m2). Consider the mass m1: it has the acceleration given above, and the net force on it is the tension of the string. Thus T = m1a = m1m2g/(m1+m2). Then, since m1/(m1+m2) < 1, it follows that T< m2g Æ Correct answer is B (We ...
MOTION RELATIVE TO ROTATING AXES
MOTION RELATIVE TO ROTATING AXES

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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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