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52 Cards in this Set

  • Front
  • Back

Oscillate

Vibrate

Periodic motion

When each vibration takes the same amount of time

Equilibrium position

The spring's natural resting position (when it's not compressed or stretched)

Hooke's Law

F = -kx


Where F = restoring force; k = spring constant; x = displacement from equilibrium position

Amplitude

Maximum displacement from equilibrium position

Cycle

A complete compress and stretch "lap"

Period

T - Time for one oscillation (s)

Frequency

f - the number of complete cycles per second (Hz)

Frequency formulas

f = 1/T; T = 1/f;

Simple Harmonic Motion (SHM)

Any vibrating system for which the restoring force is directly proportional to the negative of the displacement (see Hooke's law)

Simple Harmonic Oscillation (SHO)

Any vibrating system for which the restoring force is directly proportional to the negative of the displacement (see Hooke's law)

Total Energy of SHO

E = 1/2 mv^2 + 1/2 kx

Velocity in SHO

V = +- V(max) sq(1-(x^2 / A^2))

Period of SHM

T = 2pi sq(m/k)

Frequency of SHM

f = 1/T = 1/2pi sq(k/m)

Displacement as a function of time

x = A cos ((2pi t) / T)

Sinusoidal Motion

The motion looks like sine (or cosine) function when graphed

Restoring Force of Pendulum

F = -mg sin (angle)

Period for Simple Pendulum

T = 2pi sq(L/g)

Frequency for Simple Pendulum

f = 1/2pi sq(g/L)

Damped Harmonic Motion

Dispruption in the Sinusoidal motion

Underdamp

Makes several swings before coming to rest;


Wiggly graph

Overdamp

The damping is so large it takes a long time to reach equilibrium position;


No wiggle;

Critical Damp

Equilibrium position is reached in the shortest amount of time;


Just the right amount og wiggle;

Forced Vibration

When a system with a particular frequency has an exernal force applied

Natural Frequency

The frequency at which a system tends to oscillate in the absence of any driving or damping external force

Resonance

When the external frequency is the same as the natural frequency

Mechanical waves

Requires a medium to travel in; Are local oscillations of matter;

Waves

Are moving oscillations that are not carrying matter

Pulse

1/2 oscillation

Periodic Wave

Continuous oscillations

Wavelenght

λ; The distance between two succesive identical points/crests;

Crest

Maximum amplitude

Trough

Minimum amplitude

Wave velocity

The velocity at which wave crests, or any other part of the wave, move

Wave Velocity Formula (for Sinusoidal Waves)

V = λf

Speed of Wave on a Chord

V = sq(Ft / (m/L))

Tranverse Wave

The wave direction and particle direction are perpendicular (like a hopprep)

Longitudal Wave

The wave direction and particle direction are the same (like a dragspel)

Energy Transported by Waves

The energy transported by wave is proportional to the square of the amplitude

Intensity

I = (E/t) / area = P / area

Wave Front

All the points along the wave forming the wave crest

Ray

A line drawn in the direction of wave motion; Perpendicular to wave front

Law of Reflection

The angle of reflection equals the angle of incidence

The Angle of Incidence

The angle the incident ray makes with the surface

Interference

Refers to what happens when two waves pass through the same region of space at the same time

Principle of Superposition

The algebraic sum of the waves' displacements

Destructive Interference

Two pulses have opposite displacement so they add up to zero

Constructive Interference

Two pulses add up to have a greater displacement

Partly Destructive Interference

When two pulses interactand don't grow larger but don't add up to zero

Phase

The relative position of two waves' crests

Standing Waves!!

!!