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Chapter 41 : Nuclear Physics and Radioactivity |
Common Mass and Energy Units | |
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Atomic Mass Units (amu) Defined so that a single carbon-12 atom has a mass of exactly 12 u
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Binding Energy : Atom of Hydrogen-1 | |
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Nuclear Binding Energy : Hydrogen-2 (deuterium) | |
Deuterium is completely stable. |
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Neutron Decay | |
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(CoE+CoM here implies existence of neutrino) |
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CoE allows the neutron to decay (and it does, with a half-life of about 610 sec, with this excess energy carried off by the neutrino and the electron) If the neutron can decay, why doesn't it decay when it's in a deuterium atom? Suppose the neutron in a deuterium nucleus becomes a proton by emitting an electron (and neutrino). What would the mass of the resulting picture be? |
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The mass of the atom is about 0.64 MeV less than the sum of its parts. It can't 'decay' this way without an addition of at least that much energy. Conservation of energy prevents the neutron inside deuterium from decaying
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The isotope this 'decay' would yield would have 2 protons and 0 neutrons, making it an isotope of helium. CoE prevents deuterium from decaying into this isotope, but it has been created artificially. It's unstable, with a half-life of less than a nanosecond and decays by spitting out one of the protons. |
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Hydrogen-3 (tritium) | |
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Helium-4 | |
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Uranium-238 | |
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Binding Energy per Nucleon | |
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In this graph, the nuclear binding energy (mass of parts MINUS mass of actual atom) is divided by the number of nucleons present.
Graph peaks (highest B.E. per nucleon) at Iron-56
Atoms heavier than this 'want' to move left if possible (radioactive decay modes, where possible) Atoms lighter than this can reach more stable configurations via fusion |
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Decay Series | |
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Often, radioactive isotopes decay into other isotopes of other atoms that themselves aren't stable, so they decay into other isotopes which themselves may decay and so on.
These 'chains' are called decay series.
The figure illustrates what happens to an atom of Thorium-232. |
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Attenuation and Shielding | |
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The various types of radiation (α β and γ) are all particles, and those particles will interact with matter (us, or preferably something in between the source and us).
Common Units Encountered
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One very effective form of shielding is distance.
As the radiation travels, it is 'spreading out' over a larger surface area
Area is proportional to the distance squared so I ∝ 1/r2 |
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Shielding : All these types of radiation can interact with matter, so another common approach is to just put something else between the source and us to absorb some/most of it.
x1/2 = ln(2) / μ
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Example : Attenuation | |
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The figure on the right illustrates gamma rays hitting a series of 1 cm thick layers of some shielding material, showing how many get absorbed in each layer. 10 percent (a factor of 0.1) are absorbed in the first 1 cm thick layer, so the linear attenuation coefficient here must be about μ = 0.1/cm = 0.1 cm-1. If the incoming γ ray intensity is: (a) What should be intensity be after passing through the 10 layers shown here?
(b) What is the half-value layer thickness for this shielding material? |
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Example : Rutherford Gold Foil Experiment | |
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Example : Air as shielding | |
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Example : Air and Distance together as shielding | |
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Suppose we have a small sample of radium emitting 1 μCi of α particles. The HVL for these α particles in air is 3.7 cm A Geiger counter is held 50 cm away from the source; the 'business end' (collector) has an area of 5 cm2 (a) How many clicks/sec would the Geiger counter read if we account for just the 1/r2 spreading? (b) How many clicks/sec would the Geiger counter read if we include the absorption in the air? |
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Example : Paper as Shielding | |
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Beta and Gamma Radiation |
Shielding against these types of radiation is very sensitive to the energy of the β and γ particles. Table below: HVL's for Beta (upper table) and Gamma (lower table) Radiation at various energy levels:
Example : gamma radiationGiven: Radioactive source emitting 0.1 μCi of 200 keV gamma rays (uniformly in all directions) (a) What is the intensity 1 meter from the source? (1/r2 effect) (b) The linear attenuation coefficient for gamma rays in air at this energy is μ=0.000159 cm-1 (earlier table) (c) What does adding 1 mm of lead shielding to our clothes do? (d) Suppose a source has the same intensity but is emitting 400 keV gamma rays? |