Nuclear Decay Flashcards

Pronounce it properly

1
Q

Background Radiation

A
  • Radioactive gasses are emitted from the ground, can be trapped in buildings and rise to dangerous levels
  • Radioactive elements in earths crust release gamma radiation
  • cosmic rays from outer space produce showers of particles when they hit the atmosphere and release gamma rays
  • 85% of background radiation is from these and naturally occurring isotopes, 15% is artificial
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2
Q

Safety

A
  • keep > 30cm away to stop alpha particles
  • do not touch the source
  • keep sources in lead boxes when not in use
  • keep sources pointed away from you at all times
  • limit time using sources
  • wash hands after use
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3
Q

Alpha, Beta, Gamma

A
  • Alpha = a helium nucleus, positive charge, range of 5 cm in air, highly ionising due to mass
  • Beta = an electron, negative charge, range of a few metres in air, less ionising
  • Gamma = a neutral photon, very long range, weakly ionising
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4
Q

Detection

A
  • alpha radiation can be seen with a spark chamber, as it ionises strongly in a small radius
  • beta radiation can be detected with a GM tube
  • Gamma radiation is hard to detect as it is neutral and weakly ionising
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5
Q

Decay processes

A
  • Alpha emission = Rn-204 -> Po-200 + Alpha-4
  • Beta emission = Be-10 (IV) -> B-10 (V) + Beta (-I)
  • Gama emission = released from an excited nucleus along with alpha and beta
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6
Q

Critical Mass

A
  • A specific surface area to volume ratio of radioactive material that causes a rapid release of energy
  • nuclear explosives rely on mechanisms that cause critical mass to be suddenly achieved
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7
Q

Instability

A
  • either caused by a nucleus too big that the strong nuclear force won’t act over that radius so it decays into a stable nucleus
  • imbalance between protons and neutrons in nucleus causes decay
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8
Q

Nature of decay

A
  • Spontaneous decay = don’t know which nucleus will decay next
  • Random decay = don’t know when the next nucleus will decay
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9
Q

Decay equations

A
  • rate of decay = decay constant*Number of radioactive nuclei = - change in nuclei/change in time
  • Activity (Bq) = decay constant*number of radioactive nuclei
  • half life = ln2/decay constant
  • lnA = -decay constant*time + lnA(original)
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10
Q

C-14 dating

A
  • living plants have equal ratios of C-12 to C-14 as they gain and lose it through life processes, when they die the C-14 decays away
  • using the half life of C-14 you can estimate the age of the plant matter
  • unsuitable for anything over 60 000 years old, anything over that requires K-40
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11
Q

Nuclear Medicine

A
  • radioactive tracers need long enough half-lives to not be harmful, but also short enough to give patients a minimum dosage, Technetium is a good choice
  • cancerous cells are very vulnerable to radiation damage
  • meta-stable technetium-99m is most common medical tracer formed from Molybdenum by dissolving it in saline solution and flushing it out gradually
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