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7.2.1 Seismic waves - The Berkeley Course in Applied Geophysics
7.2.1 Seismic waves - The Berkeley Course in Applied Geophysics

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PowerPoint

3.2 The Momentum Principles
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... This equation, formulated by Euler, states that the rate of change of momentum is equal to the applied force. It is called the principle of linear momentum, or balance of linear momentum. If there are no forces applied to a system, the total momentum of the system remains constant; the law in this c ...
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... Example 4.12: The hockey puck in the diagram struck by a hockey stick, is given an initial speed of 20.0 m/s on a frozen pone. The puck remains on the ice and slides 1.20 x 102 m, slowing down steadily until it comes to rest. Determine the coefficient of kinetic friction between the puck and the ice ...
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... ② put the bead at the height of h and start the experiment. Movie. When saving data is finished, select [picture-screen analysis] and analyze the saved data. Specify the datasaving path, determine the first and the last frame to analyze and the reference color of the object. Set up the reference poi ...
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PHYS_2326_012709
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... the electric force F  q0 E : it decreases as it moves in the same direction as the force acting on the charge ...
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... 67. *Simple Harmonic Motion – motion that takes place when the acceleration of an object is proportional to its displacement from its equilibrium position and is always directed toward its equilibrium position (NOTE: this motion is defined by the equation a = -ω2x) 68. Damping – involves a force tha ...
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Curriculum Map for Physics - Amherst

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CP Physics Final Exam Review 2

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Work, Energy and Power

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... Body A now exerts a force, F N on body B for a time t seconds. Body B receives an impulse J = Ft Ns By Newton’s third law, B exerts a force, -F N on A, also for time t secs Body A receives an impulse –J Ns. ...
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PHYS-104 - GENERAL PHYSICS BEHAVIORAL OBJECTIVES AND

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Viscosity and Cohesion Pressure

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... Point P will rotate about the origin in a circle of radius r Every particle on the disc undergoes circular motion about the origin, O Polar coordinates are convenient to use to represent the position of P (or any other point) P is located at (r, ) where r is the distance from the origin to P and  ...
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Simple Harmonic Motion

... Vibrating System is Constant KE + PE = constant If the maximum amplitude of the motion is x0 then the energy at any point x is given by: ½ mv2 + ½ kx2 = ½ kx02 From this we can solve for velocity: │v│= √ [(x02 –x2)(k/m)] From Hooke’s law, F = -kx and F =ma, therefore a = -(k/m) x ...
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INTRODUCTION TO PHYSICS II FORMULA

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