4.6.1.5 Waves for Detection and Exploration (physics only) (HT only) Flashcards
How can ultrasound be used to determine distance?
use equation s = v x t
Ultrasound:
ultrasound is sound waves with a frequency higher that the upper limit of human hearing (so at least 20,000 Hz)
Uses of ultrasound + explanation:
Medical and industrial imaging
- ultrasound waves are partially reflected when they meet a boundary between 2 different media (so 2 different densities
- the time taken for the reflections to reach a detector can be used to determine how far away such a boundary is
- this means that ultrasound scanners can produce images of internal organs e.g. the kidney and heart - works for any organ not surrounded by bone
- can also be used to see image of foetus
- ultrasound can be used to detect hidden defects or problems with a weld
Why is ultrasound safer than X-rays?
ultrasound safer than X-rays as it does not cause mutations and so doesn’t increase the rick of cancer
Seismic waves:
waves produced by an earthquake
Internal structure of the earth:
- outside of the earth is the solid crust
- crust is very thin with a maximum depth of approx. 50km
- under crust is mantel
- mantel is solid
- however, parts of the upper mantel can flow very slowly but mantel is still considered a solid
- outer core is a liquid
- inner core is a solid
How can scientists observe the interior of the Earth?
- scientists cannot directly observe the interior of the Earth - even the deepest mines only go few km’s into crust
- scientists know the interior of the Earth has this structure because of earthquakes
- earthquakes cause seismic waves which carry energy away from the earthquake
- these seismic waves then pass through the earth and can be detected by seismometers in different countries
- patterns on these waves can give us information about the interior of the wave
Why does an earthquake happen?
an earthquake happens due to sudden movement between the tectonic plates on the Earth’s crust
What is the path of seismic waves and how does it allow scientists to learn about the structure of the interior of the Earth?
- seismometers on the Earth’s surface can detect seismic waves after they have passed through the Earth after an earthquake
- seismic waves travel in curved paths due to density changes in the Earth
- S-waves detected in mantel
- large parts of Earth’s interior where S-waves not detected (S-wave shadow zone)
- due to the fact that S-waves cannot pass through a liquid
- so cannot travel through outer core - shows that the outer core is liquid
- told scientists that the Earth must contain a liquid core or at least a core made partially from liquid material
- P-waves can pass through mantel, outer core and inner core
- large parts of Earth where P-waves cannot be detected (P-wave shadow zones)
- due to fact the P-wave travel faster in solids than liquids which means that the P-wave slow down as they enter the liquid outer core which causes them to refract towards the normal
- P-waves also refract when they leave outer core - indicates density of earth changed at dif depths (presence of boundaries)
- this confirms that the outer core is a liquid
- as you go deeper into mantel speed increases (rock is probably denser)
- sometimes faint P-waves can be detected in P-wave shadow zone
- used by scientists to show that the Earth also contains a solid inner core
How have scientists used seismic waves to determine the thickness of the different parts of the Earth’s interior?
- scientist have measured seismic waves from 1000s of earthquakes
- used these to work out the thickness of the crust, mantel, outer and inner cores
2 main types of seismic waves:
- P - Waves (primary waves)
- S - Waves (secondary waves)
What type of waves are P-waves?
longitudinal waves
What states of matter can P-waves pass through?
can pass through solid and liquids
How fast do P-waves travel?
- P-waves travels faster than S-waves
- P-waves travel at different speeds in solids and liquids
What parts of Earths interior can P-waves travel through?
- crust
- mantel
- outer core
- inner core