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full paper - Asia Pacific Journal of Education, Arts and Sciences
full paper - Asia Pacific Journal of Education, Arts and Sciences

... In the Western world prior to the Sixteenth Century, it was generally assumed that the acceleration of a falling body would be proportional to its mass - that is, a 10 kg object was expected to accelerate ten times faster than a 1 kg object. It was an immensely popular work among academicians and ov ...
1443-501 Spring 2002 Lecture #3
1443-501 Spring 2002 Lecture #3

... A uniform rod of length L and mass M is attached at one end to a frictionless pivot and is free to rotate about the pivot in the vertical plane. The rod is released from rest in the horizontal position what is the initial angular acceleration of the rod and the initial linear acceleration of its rig ...
Relative Motion in Two Dimensions
Relative Motion in Two Dimensions

... Relative Motion in Two Dimensions • The method for adding relative velocities also applies to motion in two dimensions. • As with one-dimensional motion, you first draw a vector diagram to describe the motion and then you solve the problem mathematically by resolving vectors into x and y components ...
lab #4 - Physics Department, Princeton University
lab #4 - Physics Department, Princeton University

... For the upward moving points, make plots of x vs. t and y vs. t, and then make quartic polynomial fits to these. If the cubic or quartic terms are large compared to their uncertainties (as reported by WPTools), consider realigning your camera and/or launching the cart on a path more nearly parallel ...
lab #4: rolling friction - Physics
lab #4: rolling friction - Physics

... For the upward moving points, make plots of x vs. t and y vs. t, and then make quartic polynomial fits to these. If the cubic or quartic terms are large compared to their uncertainties (as reported by WPTools), consider realigning your camera and/or launching the cart on a path more nearly parallel ...
PROBLEMS ON MECHANICS
PROBLEMS ON MECHANICS

Chapter 13 - apel slice
Chapter 13 - apel slice

... friction. When highly magnified, surfaces appear quite uneven and rough, making it difficult for them to slide over each other ...
BLACKBOARD COURSE PHYSICS 1.2. PHYS 1433
BLACKBOARD COURSE PHYSICS 1.2. PHYS 1433

PRELAB: FORCES AND MOTION
PRELAB: FORCES AND MOTION

... Standard length of rubber band = _________ cm 3. Attach one end of each of two identical rubber bands to some thing that can’t move and stretch them together side-by-side to the standard length. Q1-1: How does the combined pull of two rubber bands compare to what you felt when only one rubber band w ...
Gravity and freefall - Hertfordshire Grid for Learning
Gravity and freefall - Hertfordshire Grid for Learning

chapter-6-with-changes-thursday-jan-9
chapter-6-with-changes-thursday-jan-9

... Trajectories Depend upon the Viewer So far, air resistance has been ignored in the analysis of projectile motion. While the effects of air resistance are very small for some projectiles, for others, the effects are large and complex. For example, dimples on a golf ball reduce air resistance and maxi ...
PS2_fa15_4 - Instructional Physics Lab
PS2_fa15_4 - Instructional Physics Lab

First 5 chapters
First 5 chapters

Physics - Rotational Motion and Astrophysics: Numerical Examples
Physics - Rotational Motion and Astrophysics: Numerical Examples

Rotational Motion and Astrophysics_tcm4-726390
Rotational Motion and Astrophysics_tcm4-726390

... A flywheel, with a moment of inertia of 1.5 kg m 2 , is driven by an electric motor which provides a driving torque of 7.7 N m. The flywheel rotates with a constant angular velocity of 52 rad s –1 . (a) (b) ...
5.0
5.0

... Note that the force curve is characterized by two parameters (height and width): the maximum force Fmax and the interaction time ∆t. The force Fmax occurs when the carts are closest to each other with their magnets repelling most strongly. As always, ∆t is the time interval during which one cart fee ...
22. Stratigraphy and Tectonic Interpretations of Multichannel
22. Stratigraphy and Tectonic Interpretations of Multichannel

... 12-dB steps up to 84 dB, depending on each input level, and then digitized by a 15-bit A/D converter. Record length and sampling interval are 4000 ms and 4 ms, respectively. Data Processing ...
circular motion
circular motion

deep crustal structure and estimation of moho in the lhasa terrane of
deep crustal structure and estimation of moho in the lhasa terrane of

Kinematics
Kinematics

... What we have actually done is learned all the tools necessary to study what would appear to be a very complicated situation, where an object is moving both horizontally (which we studied in Kinematics) and vertically (which we studied in Free-fall) at the same time. This can be very challenging to w ...
ch. 5-2 forces powerpoint
ch. 5-2 forces powerpoint

... Preview ...
Friction Intro - HRSBSTAFF Home Page
Friction Intro - HRSBSTAFF Home Page

5.1 Circular Motion - leo physics website
5.1 Circular Motion - leo physics website

how science works
how science works

... Scientific reports are similar to the lab write-ups you do in school. And just as a lab write-up is reviewed (marked) by your teacher, reports in scientific journals undergo peer review before they’re published. The report is sent out to peers — other scientists that are experts in the same area. Th ...
Seismic strike-slip faults on a major boundary transverse to the
Seismic strike-slip faults on a major boundary transverse to the

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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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