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Activity 4.2.2 Airfoils, Lift and Bernoulli`s Principle
Activity 4.2.2 Airfoils, Lift and Bernoulli`s Principle

TEKS 5 - Pearson School
TEKS 5 - Pearson School

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... A ball falls straight down through the air under the influence of gravity. There is a retarding force F on the ball with magnitude given by F = bv, where t is the speed of the ball and b is a positive constant. The magnitude of the acceleration a of the ball at any time is equal to which of the foll ...
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... end passes over a pulley and is attached to a hanging mass (the distance between the vibrator and pulley is L). When a wave is formed in the string at a frequency such that it has an antinode at the vibrator and a node at the pulley, a resonance is created. In this experiment changing the hanging ma ...
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Seismotectonic Study of the Ain Temouchent Region in North Western...

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6. Newton`s Laws of Motion.nb

... Newton's 2nd Law of Motion: When a force F is applied to an object then it accelerates and the acceleration a is proportional to the force F with the mass m as the proportionality constant. Mathematical Statement: F=ma. Comments: 1. It might appear that the 1st law is a special case of the 2nd law a ...
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... 18. (II) A window washer pulls herself upward using the bucket-pulley apparatus show in Fig. 4-42. (a) How hard must she pull downward to raise herself slowly at constant speed? (b) If she increases this force by 10 percent, what will her acceleration be? The mass of the person plus the bucket is 65 ...
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Seismology - Università degli studi di Trieste
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Ambient Noise Tomography

... seismic wave speeds in Earth’s interior in order to advance knowledge of temperature, composition, and fluid content which hold a key to the understanding of Earth processes. Recent studies based on TA data in the western US, such as that of Yang et al. (2008b), invert ambient noise and earthquake d ...
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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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