In chapter 13 we went over: Work › How work relates to force and distance Transfer and conservation of energy › Power Now we will learn: › How forces create waves › How waves transfer energy › How waves are classified
Wave: › The disturbance that transfers energy from one place to another Can transfer energy over distance without moving matter the entire distance. › Ocean waves travel kilometers without the water itself moving the same distance-the water simply moves up and down (disturbance) transferring its energy
Forces start a disturbance which sends a wave through the material: Rope waves: › If I flick the rope by applying a force upward then quickly apply the opposite force down, it sends a wave through the rope. › Both forces are required to start a wave
Water waves: › When an object is dropped into the water, the force applied causes waves to move through the water › D:\wave-interference_en.jar D:\wave-interference_en.jar Earthquake waves: › Sudden release of energy that has built up in the rock from a pushing and pulling (force) causes energy waves to be transferred through the ground
Medium: › Any substance that a wave moves through Water is the medium for ocean waves Rope is the medium for a rope wave Mechanical waves: › Waves that transfer energy through matter What is matter?
Think about an earthquake: › What type of energy is transferred during an earthquake (kinetic, potential, or mechanical) › The disturbance causes the ground to shake from side to side and up and down › As the energy is released, it travels in a wave but the ground itself does not travel with the wave › Faults and Earthquakes Faults and Earthquakes
Transverse waves: › The direction in which the wave travels is perpendicular, or at right angles, to the direction of the disturbance › “transverse” means across or crosswise › Look at the rope wave:
Longitudinal waves: › A wave that travels in the same direction as the disturbance Examples are: › Sound waves Molecules of air are set in motion which vibrate quickly causing more air molecules to vibrate › Slinky wave demo: If I pull the slinky back straight and release it, the coils move forward and backward.
When tracking and recording the height of waves in the ocean, scientists use: Mean: › The average of the recorded heights Median: › The middle value when all values are recorded from least to greatest Mode: › The value that occurs the most out of the data set
Measuring wave properties: › Crest: The highest point or peak of a wave › Trough: The lowest point or valley of a wave
Amplitude: › The distance between the middle of the crest to the middle of the trough in a transverse wave. › Indicates how much energy the wave is carrying (bigger the wave, the more energy) Wavelength: › The distance from the crest of one wave to the crest of the next wave › Can also be measured from trough to trough
Frequency: › The number of waves passing a fixed point in a certain amount of time › “frequent” means often Frequency and wavelength are related: › If the frequency increases, the wavelength shortens › If frequency decreases, the wavelength increases
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Speed = wavelength times frequency S=λf S means speed λ (Lamda) means wavelength f means frequency
Reflection: › The bouncing back of a wave after it strikes a barrier Refraction: › The bending of a wave as it enters a new medium at an angle other than 90 degrees Diffraction: › The spreading out of waves through an opening or around the edge of an obstacle
reflection and refraction reflection and refraction
› D:\wave-interference_en.jar D:\wave-interference_en.jar
Interference: › The meeting and combining of waves › They can add to or take away energy from each other Constructive interference: › The adding of two waves › Makes a larger wave out of two smaller waves › When joined perfectly, the new amplitude equals the combined amplitudes of the two original waves Waves can cancel each other out
Constructive interference Destructive interference
wave interference wave interference