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
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
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
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
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
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
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
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
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)
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
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