Nuclear physics Flashcards
(46 cards)
Nucleon
particle in the nucleus
Atomic number (Z)
number of protons
N
number of neutrons
Mass number
protons and neutrons
Nuclide
a particle with a particular mass number
Isotopes
nuclides of the same element, same number of protons but different neutrons
evidence for isotopes
bainbridge mass spectrometer;charged atoms are fired at a specific velocity passed by an opposite plate and landing at different places reveals having different isotopes
Interactions in a nucleus
Coulomb interactions and nuclear interactions
Coulomb interactions
A charged particle will never enter the nucleus because as the distance to it reached 0, then the repulsion would be infinitely large.
Nuclear interactions
Where the coulomb repulsion is overcome, as on sun, but much larger gravities.
Stability of nuclei
if strong force and coulomb repulsion are balanced; if not, unstable
for it to be stable neutrons must be ≥ number of protons (because coulomb force goes further than strong force)
unified atomic mass unit
1/12 of the mass of a carbon-12 atom
Energy-mass equivalence
mass and energy are equivalent in that a change in mass can also be regarded in the same change in energy
E=mc^2
MeVc^-2
equivalent to 1 atomic mass unit
mass defect
difference in mass between mass of nucleus and the mass of separate nucleons
nuclear binding energy
energy required to separate the nucleus into different components (MeV)
E=mc^2 (binding energy= mass defect* c^2)
radioactive decay
when an unstable nucleus emits an alpa or beta particle or gamma ray photon resulting in a daughter nucleus which is more stable
characteristics of radioactive decay
random and spontaneous (with less nuclei, probability does not change and the number of decays reduce)
half-life
time taken for the initial activity of the radioactive sample to halve
radioactive decay law
the rate of decay is proportional to the number of undecayed nuclei (dN/dt=-λ(decay constant)*N(number of undecayed nuclei))
N=N0e^(-λt)
Activity (rate of decay same)
A=-dN/dt=λN=λN0e^(-λt)
Measuring the half-life of an isotope (long)
number of decays by time
mass of the sample and calculating the number of atoms N
using A=λN to calculate λ constant
using T1/2= ln2/λ
carbon-14 dating
once an organism has died, the amount of carbon-14 will fall with decay, which can be used to tell how old it is
why is C-14 dating possible
c14 is unstable, but c12(also present) is stable (proportion constant in living)
neither can be replenished after death
c14 decays