4.6.1.5 Waves for Detection and Exploration (physics only) (HT only) Flashcards

1
Q

How can ultrasound be used to determine distance?

A

use equation s = v x t

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2
Q

Ultrasound:

A

ultrasound is sound waves with a frequency higher that the upper limit of human hearing (so at least 20,000 Hz)

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3
Q

Uses of ultrasound + explanation:

A

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
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4
Q

Why is ultrasound safer than X-rays?

A

ultrasound safer than X-rays as it does not cause mutations and so doesn’t increase the rick of cancer

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5
Q

Seismic waves:

A

waves produced by an earthquake

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6
Q

Internal structure of the earth:

A
  • 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
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7
Q

How can scientists observe the interior of the Earth?

A
  • 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
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8
Q

Why does an earthquake happen?

A

an earthquake happens due to sudden movement between the tectonic plates on the Earth’s crust

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9
Q

What is the path of seismic waves and how does it allow scientists to learn about the structure of the interior of the Earth?

A
  • 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
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10
Q

How have scientists used seismic waves to determine the thickness of the different parts of the Earth’s interior?

A
  • scientist have measured seismic waves from 1000s of earthquakes
  • used these to work out the thickness of the crust, mantel, outer and inner cores
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11
Q

2 main types of seismic waves:

A
  • P - Waves (primary waves)
  • S - Waves (secondary waves)
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12
Q

What type of waves are P-waves?

A

longitudinal waves

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13
Q

What states of matter can P-waves pass through?

A

can pass through solid and liquids

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14
Q

How fast do P-waves travel?

A
  • P-waves travels faster than S-waves
  • P-waves travel at different speeds in solids and liquids
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15
Q

What parts of Earths interior can P-waves travel through?

A
  • crust
  • mantel
  • outer core
  • inner core
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16
Q

What type of waves are S - waves?

A

transverse waves

17
Q

What states of matter can S - waves pass through?

A

solid

18
Q

What parts of Earths interior can S-waves travel through?

A
  • crust
  • mantel
19
Q

Echo sounding:

A

using high frequency sound waves - echo sounding is used to detect objects in deep water and measure water depth

20
Q

What parts of the Earths interior can S-waves not travel through?

A

cannot travel through outer core as it is liquid and S-waves cannot travel through a liquid