Radioactivity
is invisible, has no smell, makes no sound - in fact it cannot be
detected by any of our senses. However, because radioactivity affects
the atoms that it passes, we can easily monitor it using a variety
of methods.
Most people
have heard of a "Geiger Counter" for measuring radioactivity.
This is actually a Geiger-Müller tube with some form of counter
attached, which usually tells us the number of particles detected
per minute ("counts per minute").
GM tubes work
using the ionising effect of radioactivity.
This means that they are best at detecting alpha particles, because
a-particles ionise strongly.
Different models
of GM tubes are available for detecting a,
b and g radiation.
How
it Works
You can see
how the tube works in the animation on the right. The tube is filled
with Argon gas, and around +400 Volts are applied to the thin wire
in the middle. When a particle enters the tube, it pulls an electron
from an Argon atom. The electron is attracted to the central wire,
and as it rushes towards the wire, the electron will knock other
electrons from Argon atoms, causing an "avalanche". Thus
one single incoming particle will cause many electrons to arrive
at the wire, creating a pulse which can be amplified and counted.
This gives us a very sensitive detector.
In 1896, Henri Becquerel,
working in Paris, discovered that Uranium compounds would darken a photographic
plate, even if the plate were wrapped up so that no light could get in.
Radioactivity
will darken ("fog") photographic film, and we can use
this effect to measure how much radiation has struck the film.
Workers in the
nuclear industry wear "film badges" which are sent to
a laboratory to be developed, just like your photographs. This allows
us to measure the dose that each worker has received (usually each
month).
The badges have
"windows" made of different materials, so that we can
see how much of the radiation was a particles,
or b particles, or g
rays.
Dry air is normally
a good insulator, thus a charged electroscope will stay that way,
as the charge cannot escape. When an electroscope is charged, the
gold leaf sticks out, because the charges on the gold repel the
charges on the metal stalk.
When a radioactive
source comes near, the air is ionised, and starts to conduct electricity.
This means that the charge can "leak" away, the electroscope
discharges and the gold leaf falls.
An early form
of detector, the Spark Counter is another instrument that uses the
ionising effect of radioactivity, and for this reason it works best
with a particles.
A high voltage
is applied between the gauze and the wire, and adjusted until it
is just below the voltage required to produce sparks.
When a radioactive
source is brought near, the air between the gauze and the wire is
ionised, and sparks jump where particles pass.
Download mpeg
video of school cloud chamber in action. Details...
There are two
types of cloud chamber: the "expansion" type and the "diffusion"
type.
In both types,
a or b particles
leave trails in the vapour in the chamber, rather like high-altitude
aircraft leave trails in the sky.
The chamber
contains a supersaturated vapour (e.g. methylated spirits), which
condenses into droplets when disturbed and ionised by the passage
of a particle (alpha particles are best for this).
You can clearly
see the direction and energy of the particles (low energy particles
only leave short trails).
Occasionally, a particle collides with an air molecule and changes
direction.
A cloud chamber also shows the randomness of radioactive emissions
clearly.
Expansion cloud
chambers use a vacuum pump to briefly produce the right conditions
for trails to form, whilst the Diffusion type uses solid Carbon
Dioxide to cool the bottom of the chamber and produce a temperature
gradient in which trails can be seen.
The Bubble Chamber
A similar idea
to an expansion cloud chamber, particles leave trails of tiny bubbles
in a liquid. This used to be the main instrument for tracking the
results of collisions in particle accelerators.
The chamber
would be surrounded by powerful magnets, so any charged particles
passing though the chamber would move in curved paths. The shapes
of the curves tell us about the charge, mass and speed of each particle,
so we can work out what they are - otherwise one line of bubbles
looks pretty much like another.
Technicians at
CERN working on a bubble chamber in 1970
Modern instruments
are much more sensitive than the others listed on this page.
"Scintillation
Detectors" work by the radiation striking a suitable material
(such as Sodium Iodide), and producing a tiny flash of light. This is
amplified by a "photomultiplier tube" which results in a burst
of electrons large enough to be detected. Scintillation detectors form
the basis of the hand-held instruments used to monitor contamination in
nuclear power stations. They can recognise the difference between a, b
and g radiation, and make different noises (such as bleeps or clicks)
accordingly.
"Solid-State
Detectors" are the most up-to-date instruments. They are used
in particle-accelerator laboratories to show the results of high-energy
collisions, with banks of them clustered around the collision site, feeding
data into huge computers. The way they work is way beyond what
we need for GCSEs, but basically they are similar to the CCD Silicon chips
used in video cameras.