topic 4 - radioactivity Flashcards
how has the model of the atom changed (Thomson, Rutherford, Bohr
in 1897, Thomson discovered that electrons could be removed from atoms so atoms must consist of smaller components - he proposed the plum pudding model (positive pudding and negative currants)
in 1909, Rutherford’s gold foil experiment demonstrated that most of the mass of an atom was concentrated in a positively charged nucleus and that most of the atom is empty space
Bohr changed this idea slightly a few years later, proposing that electrons were arranged in fixed orbits at set distances from the nucleus (electrons can only exist in these shells)
subatomic particles
neutrons
protons
electrons
neutrons (relative mass and charge)
mass: 1
charge: 0
protons (relative mass and charge)
mass: 1
charge: +1
electrons (relative mass and charge)
mass: 0
charge: -1
electrons moving levels (up)
if an electron absorbs enough EM radiation with the right amount of energy, it can move up to another energy level
if an outer electron absorbs enough radiation, it can move so far that it leaves the atom to become a free electron - ionising the atom
electrons moving levels (down)
electrons quickly move bac to their original position and emit the amount of energy that was absorbed
what can be observed when electrons move levels
visible light is often emitted when electrons move shells
within the nucleus itself, high frequency gamma rays are emitted
isotopes
different forms of the same element
atoms with the same number of protons but a different number of neutrons
radioactive decay
when unstable isotopes decay into other elements and give out radiation as they try to become more stable
it is impossible to predict which unstable nucleus will decay next because the process is completely random
ionising radiation
any radiation that can knock electrons from atoms
3 types of radioactive decay
alpha decay
beta decay (beta-minus and positron)
gamma rays
alpha radiation
when an alpha particle (α) is emitted from the nucleus
an α particle is 2 neutrons and 2 protons (like a helium nucleus)
features of alpha radiation (4)
don’t penetrate far and are stopped quickly
travel a few cm in air
blocked by a thin sheet of paper
strongly ionising due to their size
beta particles
can be electrons ( ß- particle) or positrons (ß+ particle)
beta-minus (ß- particle)
fast moving electron released by nucleus
virtually no mass
relative charge of -1
beta-plus (ß+ particle)
fast moving positron
positron is the antiparticle of the electron
virtually no mass
relative charge of +1
beta particle decay features (4)
absorbed by a thin sheet of aluminium
moderately ionising
ß- travel a few metres in air
ß+ has a smaller range due to when they hit an electron, the two destroy each other and produce gamma rays (this is ANNIHILATION)
gamma rays
once a nucleus has decayed, it undergoes nuclear rearrangement and releases some energy
gamma rays are EM waves with a short wavelength and high frequency
gamma rays features (4)
penetrate far into materials
travel a long distance in air
weakly ionising
absorbed by thick sheets of lead or metres of concrete
background radiation
the low level radiation around us all of the time
sources of background radiation
radioactivity comes from naturally occurring unstable isotopes around us
found in air, some foods, building materials and some rocks
cosmic radiation
radiation due to human activity
cosmic radiation
radiation comes from space in the form of cosmic rays, from the sun
the atmosphere protects us mostly from cosmic radiation
radiation due to human activity
there is radiation due to human activity but this is only a tiny proportion of background radiation (eg. fallout from nuclear explosion/ nuclear waste)