Radioactivity

14.1 Types, Properties and Uses of Radioactivity

F/H  Some substances give out radiation all the time, whatever is done to them. These substances are said to be radioactive.
F/H There are three types of radiation emitted by radioactive sources:
F/H * alpha (*) radiation - which is easily absorbed by a few centimetres of air or a thin sheet of paper;
F/H * beta (*) radiation - which easily passes through air or paper but is mostly absorbed by a few millimetres of metal;
F/H * gamma (*) radiation - which is very penetrating and requires many centimetres of lead or metres of concrete to absorb most of it.
F/H  There are radioactive substances all around us, including in the ground, in the air, in building materials and in food. Radiation also reaches us from space. The radiation from all these sources is called background radiation.
F/H When radiation from radioactive materials collides with neutral atoms or molecules these may become charged (ionised).
F/H  When radiation ionises molecules in living cells it can cause damage, including cancer. The larger the dose of radiation the greater the risk of cancer.
F/H  Higher doses of radiation can kill cells; they are used to kill cancer cells and harmful micro-organisms.
F/H As radiation passes through a material it can be absorbed. The greater the thickness of a material the greater the absorption. The absorption of radiation can be used to monitor/control the thickness of materials.
H  When sources of radiation are outside the body:* beta and gamma radiation are the most dangerous because they can reach the cells of organs and may be absorbed by them;
H * alpha radiation is least dangerous because it is unlikely to reach living cells.
H When sources of radiation are inside the body:
H * alpha radiation is the most dangerous because it is so strongly absorbed by cells;
H * beta and gamma radiation are less dangerous because cells are less likely to absorb the radiation.
H  The half-life of a radioactive substance:
H * is the time it takes for the number of parent atoms in a sample to halve.
H * is the time it takes for the count rate from the original substance to fall to half its initial level.
H Candidates should be able to evaluate the appropriateness of radioactive sources for particular uses, including as tracers, in terms of
H * the types of radiation emitted;
H * their half-lives.

14.2 Atomic Structure and Nuclear Fission

F/H  Radioactivity occurs as a result of changes in the nuclei of atoms (nuclear changes).
F/H  Atoms have a small central nucleus made up of protons and neutrons around which there are electrons.
F/H Candidates should be able, when provided with appropriate information, to:
F/H * describe the "plum pudding" model of the atom which this model replaced;
F/H * explain how the scattering experiment by Rutherford's team provided evidence for their model.
F/H  The relative masses of protons, neutrons and electrons and their relative electric charges are as shown:
F/H            Mass Charge
F/H     Proton     1 +1
F/H     Neutron     1   0
F/H     Electron     negligible -1
F/H  In an atom, the number of electrons is equal to the number of protons in the nucleus. The atom as a whole has no electrical charge.
F/H  All atoms of a particular element have the same number of protons. Atoms of different elements have different numbers of protons. The total number of protons and neutrons (nucleons) in an atom is called its mass (nucleon) number.
F/H  Atoms of the same element which have different numbers of neutrons are called isotopes.
F/H  Radioactive isotopes are atoms with unstable nuclei. When an unstable nucleus splits up (disintegrates):
F/H * it emits radiation;
F/H * a different atom, with a different number of protons, is formed.
F/H The older a radioactive material, the less radiation it emits. This idea can be used to date materials.
H  Any isotope of an element which is radioactive is called a radioisotope (radionuclide).
H Alpha radiation consists of helium nuclei, particles made up of two protons and two neutrons.
H Beta radiation consists of electrons emitted from the nuclei of atoms.
H For each electron emitted, a neutron in the nucleus becomes a proton.
H Gamma radiation is very short wavelength electromagnetic radiation.
H Nuclear reactors use a process called nuclear fission. When an atom with a very large nucleus is bombarded with neutrons:
H * the nucleus splits into two smaller nuclei;
H * further neutrons are released which may cause further nuclear fission resulting in a chain reaction;
H * the new atoms which are formed are themselves radioactive.
H [Details of nuclear reactors are not required.]
H   The  energy released  by  an atom  during  radioactive  disintegration  or  nuclear  fission  is  very  large compared to the energy released when a chemical bond is made between two atoms. This idea can be used to date materials.
H Uranium isotopes, which have a very long half-life, decay via a series of relatively short-lived radioisotopes to produce stable isotopes of lead. The relative proportions of uranium and lead isotopes in a sample of igneous rock can, therefore, be used to date the rock.
H The proportions of the radioisotope potassium-40 and its stable decay product argon can also be used to date igneous rocks from which the gaseous argon has been unable to escape.
H Candidates should be able to make such calculations when provided with appropriate data.