| |
|
Many rocks contain traces
of uranium-238. This radioactive metal has a
half-life of 4.5 billion years. Once a
uranium atom decays it passes through a
number of further stages, all with much
shorter half-lives. It ends up as lead-206,
which is not radioactive. Uranium-235, with
a half-life of 0.71 billion years, ends up
as lead-207.
Geologists can measure
the concentrations of these two
isotopes of lead in rocks, and so
measure their age. This enables us to
estimate the length of time since the
Earth's crust became solid.
In the nineteenth century
scientists attempted to work out the age of
the Earth by estimating how long it would
take molten rock to cool down to its present
temperature. Lord Kelvin decided that this
was no more than 100 million years.
Unfortunately, Charles Darwin needed the
Earth to be much older than this for human
life to have evolved. Evolution is a very
slow process. The discovery of radioactivity
solved the problem - the Earth was much
older than Kelvin's estimate. Radioactive
minerals in the rocks were generating
sufficient heat to slow down the cooling.
|
|
|
The first number is the atomic
number (Z) (sometimes called the proton
number). This is the number of protons in the
nucleus. It is also the number of electrons going
round the nucleus. Each value of the atomic number
belongs to a particular element, from hydrogen at
number 1 to uranium at number 92. The chemical
behaviour of an element depends on the number of
electrons, which is Z.
The second number is the
neutron number (N). This is the number of
neutrons in the nucleus. All atoms of the same
element have the same Z, but they do not all
have the same value of N. Atoms having the
same number of protons, but different numbers of
neutrons are called isotopes. They belong to the
same element and behave the same in chemistry, but
they do differ slightly in properties such as
melting point. Isotopes can be separated, but it is
not easy*.
Most elements have more than one
isotope. You may have wondered why chlorine has an
atomic mass of 35.5. This is because it is 75%
chlorine-35 and 25% chlorine-37.
The mass number (N)
is the total number of nucleons (protons and
neutrons) in the nucleus. N = A - Z:
for example, uranium-238 has Z = 92, A
= 238 and N = 238 - 92 = 146.
A nuclide is a type of nucleus.
The symbol for a nuclide is the symbol for the
element with two numbers like this:
23892U.
The upper number is A and the lower number is
Z.
*To separate uranium-235 from
uranium-238, the uranium is turned into a gas -
uranium hexafluoride. The gas molecules containing
235U
will move slightly faster than those containing
238U.
Allow the gas to pass down a long pipe with porous
plugs in it: it will become steadily richer in
235U.
There is a big uranium separation plant at
Capenhurst, near Chester. |
|
|
There is an attractive force that
holds
nucleons together. This force is very strong,
but it only acts when the particles are very close
to one another. Neutrons act as a sort of glue
within the nucleus, by weakening the electrostatic
repulsion between protons.
The attractive force between
nucleons arises when they exchange another particle
backwards and forwards between them. This particle
is a pi-meson or pion - heavier than an
electron, but lighter than a
proton. It can carry a positive or negative
charge or be uncharged.
To build up nuclei from scratch
involves enormous pressures, to overcome the
repulsion between protons. The conditions required
only exist in the centre of
stars.
Hydrogen is the only nucleus with
no neutron. Light nuclei tend to have equal numbers
of neutrons and protons, but heavier nuclei have up
to 1.6 times more neutrons than protons. If a
nucleus has too many protons to be stable, then it
will be likely to convert one to a neutron by
emitting a
positron. If it has too many neutrons, then it
may change one into a proton by emitting an
electron.
A positive charge does not repel
neutrons, so they can easily enter and become
part of a nucleus, giving a radioactive isotope.
Physicists can be produce these to order for medical
and industrial applications.
Nuclei with more than 83 protons
are all unstable. Nuclei heavier than uranium-238
have been artificially produced, but they are very
unstable.
Plutonium-239 is the only one produced on a
large scale. Iron has the most stable nucleus,
because neither fission nor fusion causes it to lose
binding energy.
Nuclei that still exist are
either stable or have very long half-lives. For
example, the half-life of uranium-238 is perhaps a
third of the time since the Big Bang - and some
nuclides have half-lives a million or more times
longer. Some nuclei, however, (like radium) are
being produced continually by the decay of something
else.
Cosmic rays produce
carbon-14.
|
|
|
Binding energy is energy that is lost
when a nucleus is formed from protons and
neutrons. A lot of binding energy means a stable
nucleus. A similar idea exists in ordinary chemistry. When
sodium reacts with chlorine, a lot of energy is released.
The result is a very stable compound - sodium chloride.
Energy has mass. Losing energy means
losing mass. In ordinary chemistry this change is too small
to measure, but the amounts of energy involved in nuclear
processes are so great that the change in mass is quite
easily measurable.
To calculate binding energy we add
together the masses of all the protons and neutrons that go
to make up the nucleus. The total is greater than the actual
mass of the nucleus. The decrease in mass when the nucleus
is formed is the mass of the energy released. This energy
can be calculated using Einstein's formula, E = mc2,
where is the speed of light
Remember that
nuclear fission and
nuclear fusion both depend on the changing of binding
energy to heat. In nuclear fission a heavy nucleus splits
into two smaller pieces. In nuclear fusion two light nuclei
unite to make a heavier one. In each case binding energy is
released. A more stable nucleus is formed. Fusion works for
nuclei lighter than iron. Fission works for nuclei heavier
than iron. Therefore iron is the most stable
nucleus.
The binding energies holding nuclei
together are roughly a million times greater than the
binding energies holding molecules together. This is why
nuclear explosions are vastly more powerful than chemical
explosions.
|
Where do neutrons come from? Is it true that they are
unstable?
In 1920, Rutherford suggested that an
uncharged particle having about the same mass as a proton
might exist. He thought of it as being a combination of a
proton and an electron. Such a particle would explain why a
nucleus having, say, 12 times the mass of a proton only
weighed 6 times as much.
Rutherford had discovered in 1919 that
very occasionally an alpha-particle would collide with a
nitrogen nucleus and eject a proton from it. This also
occurred with alpha-particles and other nuclei, but
something strange happened with beryllium-17. Whatever was
ejected, it was not a charged particle. Originally they
thought it was a gamma-ray. Then, in 1932, Chadwick placed a
slab of paraffin wax in front of the beryllium. Wax contains
lots of protons (hydrogen nuclei). He found that protons
were knocked forward out of the wax. Whatever was hitting
them was giving all its energy to the proton. As it stopped
dead after the collision, it must have the same mass as a
proton. This was the neutron.
A convenient source of neutrons consists
of beryllium mixed with a strong source of alpha-particles.
This can be used to make other materials radioactive - it is
more convenient than using a nuclear reactor.
Fast-moving neutrons are used to treat
cancer. They are very penetrating - several feet of concrete
are needed to stop them. In a nuclear reactor, fast neutrons
are slowed down by bouncing them off
light nuclei.
Unlike protons, solitary neutrons are
unstable. They decay to give a proton, an electron and a
neutrino. Their half-life is 13 minutes. |
|
|
| |
|
What happens if, on average, at least one
of the neutrons produced by the fission of a uranium-235
nucleus goes on to be captured by another uranium-235 atom?
The process will keep going and generating heat - we have a
chain reaction.
What is needed to keep the reaction
going? The problem is that the neutrons are travelling too
fast to be captured easily. There are possible answers. One
is to use pure uranium-235, but this very expensive to
produce. The other is to slow down the neutrons so that they
are more easily captured. This is done by bouncing them off
the light atoms contained in a material known as a
moderator. Graphite is often used, and heavy water is very
effective. Ordinary water can be used as a moderator, but it
absorbs a lot of neutrons. A layer of heavy atoms reflects
escaping neutrons back into the reactor core.
How can we control the reaction? Rods
made of boron are pushed into channels in the reactor. These
rods absorb neutrons, so they damp down the reaction. The
speed of the reaction is controlled by moving these control
rods in and out. The heat produced is removed from the
reactor by a flow of liquid or gas coolant. The heat is used
to produce steam and drive turbines.
There is another metal that can be used
instead of uranium-235: plutonium. In a bomb, pure
uranium-235 or plutonium is used, and there is no moderator.
|
|
|
| |
|
They mean nuclear fission. In biology a
cell has a nucleus. The nucleus of a cell splits in two and
one cell becomes two. This is called fission. Scientists
studying atomic nuclei were reminded of what happened in
biology, so they used the same words.
Normal uranium is nearly all uranium-238,
but it does contain 0.72% uranium-235. Enriched uranium
contains several percent uranium-235. A uranium-235 nucleus
is special because it will undergo fission. This means that
it will absorb a stray neutron and then become unstable and
split into two roughly equal halves. Neutrons can enter the
nucleus because they are not charged. They are not repelled
by the positive charge on the nucleus
The reaction is not quite the same every
time. In a typical case the uranium nucleus splits into a
barium nucleus, a krypton nucleus and three neutrons. All
these particles fly apart at high speed, banging into other
atoms and making them vibrate more strongly. This increased
vibration is increased heat energy - the temperature rises.
The two halves of the uranium atom present a problem,
because they are always extremely radioactive.
Fission also happens with plutonium-239
nuclei. Plutonium rather than uranium is usually used in
bombs. It can also be used in reactors, but there are
problems because it is so poisonous.
|
|
|
| |
|
An atom bomb is a fission bomb. It
contains a sphere of
plutonium-239 about the size of a grapefruit.
Chain reactions start in this sphere whenever a stray
neutron enters a plutonium nucleus, but they rapidly fizzle
out; too few of the neutrons find other plutonium nuclei.
The sphere is surrounded by shaped explosive charges. The
sphere is suddenly compressed into a much smaller volume
when these explode. The nuclei are now closer together and
the chain reaction goes ahead. A
neutron source ensures there is a neutron there to start
the reaction. There is a terrific burst of heat energy. This
is equivalent to about 20,000 tonnes of TNT. Many of the
radioactive atoms produced are carried up into the
stratosphere. Eventually they reach the ground, all over the
world, as fallout.
Two heavy hydrogen nuclei can fuse
together to produce a
helium nucleus. This reaction can be triggered by a
fission bomb. The trigger is surrounded by a jacket
containing heavy hydrogen (deuterium). The resulting bang is
equivalent to at least a million tonnes of TNT - the biggest
was a hundred times more powerful.
Fission energy is released in a
controlled way in a reactor. Nobody has yet managed to
generate power by controlled fusion. The Sun and other
stars, however, get their energy from nuclear fusion.
|
|
|
| |
|
Alchemists dreamed of turning lead into
gold, but physicists regularly turn one element into
another. They bombard uranium-238 with
neutrons in a nuclear reactor. The uranium absorbs a
neutron to become uranium-239. Beta decay changes this to
neptunium-239. This emits another beta-particle to become
plutonium-239 - a metal that does not occur naturally.
All uranium reactors produce plutonium in
their fuel rods. Breeder reactors have a jacket of
uranium-238 to increase the amount of plutonium produced.
They produce more fuel than they consume.
The plutonium is mixed up with highly
radioactive fission products. The spent fuel rods are stored
under water for some time until the radioactivity has died
down - at first it is powerful enough to give the water a
blue glow. The rods are then dissolved in acid and the
plutonium and unused uranium are recovered. All this has to
be done by remote control because of the radiation and the
dangerous chemicals involved.
Plutonium-239 has a half-life of 24 000
years, so it is not intensely radioactive. However, even a
tiny amount inside someone's body can eventually cause
cancer, because it emits alpha-particles. There is also the
problem that terrorists might steal it, and use it to make
weapons.
Plutonium-238 is strongly radioactive,
with a half-life of 88 years. The heat that it produces can
be used to warm a thermocouple and generate electricity. It
can be used to power equipment such as heart pacemakers and
space probes, where an ordinary battery might not last long
enough. |
|
|
| |
|
The simplest atoms - hydrogen and helium
- are by far the most abundant in the Universe. As nuclei
become heavier and more complicated, there are fewer and
fewer of them. Hydrogen and helium were formed during the
early life of the Universe, when it was settling down after
the Big Bang. Almost all other nuclei were made in the
centres of stars. Protons repel one another. To make a
nucleus, you have to push them together - enormous pressures
are needed.
A star like the Sun gets its energy from
the fusion of hydrogen atoms to produce helium. Once the
hydrogen in the centre of the star runs out, it collapses
under gravity. The helium nuclei now start to fuse, giving
carbon and oxygen nuclei. Once the helium is used up, there
is a further collapse. Then, if the star weighs more than
7.5 times as much as the Sun, there is a further series of
fusion reactions involving carbon, oxygen and silicon
nuclei. These produce elements up to iron. Nuclei heavier
than iron cannot be produced by fusion. They build up very
slowly by collecting neutrons, some of which will decay into
protons.
The final stage in the life of a large
star is a massive explosion - a supernova. This explosion
scatters the elements around the galaxy, where they may
eventually become part of planets. The atoms in your body
were once part of a star.
Once you too were a star!
|
|
|
| |
|
At Los Alamos in May 1946, Louis Slotin
was carrying out an experiment using two hemispheres of
plutonium. They were mounted on a track and Slotin was
edging them closer and closer together using a screwdriver.
When the two came together they would exceed the critical
mass and a
chain reaction would begin. Slotin intended to stop just
short of this point, but his hand slipped and the
hemispheres came together. The room filled with blue light.
An atom bomb was going off. He wrenched the two halves apart
with his bare hands and the reaction ceased. There were
other people in the room and Slotin drew a diagram of their
positions on the blackboard to help work out their dose of
radiation. Nine days later he died, but the others survived.
You do not actually need the innards of
an atom bomb to produce a chain reaction. Merely stacking
too much enriched uranium in one place will do. Of course
there are stringent precautions to prevent this, but it
could happen. If it did, people would need no encouragement
to follow the arrows. This sort of chain reaction would lead
to a massive burst of radiation, but not to a full-scale
explosion. A nuclear bomb needs an inward pressure wave from
conventional explosives to hold it together long enough for
the chain reaction to develop fully.
When the Earth was
young - 3.5 billion years ago - the rocks must have
contained more than 30 times today's quantity of
uranium-235. It is not too far-fetched to suggest that chain
reactions must sometimes have begun spontaneously in rocks
containing uranium. |
|
|
| |
|
This is true - the difference lies in
where they come from and how fast they're going.
Heat a metal wire in a vacuum.
Electrons gain enough energy to leave the wire and form
a cloud around it. These electrons can be attracted by a
sheet of metal carrying a positive charge. They move towards
it, gaining speed as they go. If these electrons hit a
screen coated with a suitable chemical, they make it glow
(fluoresce). This is what happens in a television. The
voltage between the wire (cathode) and metal plate (anode)
might be 3000 V. In this case the electrons will reach about
one tenth of the speed of light.
A typical
beta-particle, however, leaves a nucleus with an energy
equivalent to being accelerated through 1 million volts.
This means that it will be travelling at close to the speed
of light. It will have so much kinetic energy that the mass
of this energy will be twice the rest mass of the electron!
Cathode rays are easily stopped by very thin sheets of
material. Beta-rays can pass through a millimetre or more of
aluminium.
Cathode rays are easily deflected by
electric and magnetic fields - as in a TV tube. Beta-rays
are also easily deflected by magnetic fields. Magnetic
deflection is important, because it tells us if a particle
is charged, and whether the charge is positive or negative.
Gamma rays and neutrons are not deflected at all. |
|
|
| |
|
They used carbon dating. Carbon-14 is a
radioactive isotope of carbon. When a neutron produced by a
cosmic ray hits the nucleus of a nitrogen atom, the neutron
turns into proton and the nitrogen-14 nucleus turns into a
carbon-14 nucleus. 14C
is radioactive. It decays by giving out a beta-particle. Its
half-life is 5700 years. More 14C
is constantly being produced to replace that which is
decaying, so the proportion in the atmosphere stays
constant.
Animals and plants contain carbon. While
they are alive the ratio of 14C
atoms to normal 12C
atoms inside them is the same as in the atmosphere. After
death, however, they no longer exchange atoms with their
surroundings. The proportion of
14C begins to decrease as the
atoms decay. When it has halved, for example, the specimen
is 5700 years old.
This method of dating can be used for any
organic material, such bone, wood or cloth. Originally it
involved taking quite a large chunk of the material (about
50g of wood or 200g of bone) and burning it to separate the
carbon. Modern techniques involve measuring the proportion
of 14C
atoms without waiting for them to decay. Much smaller
samples are required - small enough for the Pope to give his
consent for one to be taken from the Shroud.
One of the main problems with carbon
dating is knowing the actual concentration of
14C in ancient
times. Fortunately wood can also be dated by tree-ring
measurements and this provides a check on radiocarbon dates.
|
|
|
| |
|
Cosmic rays are charged particles with
very high energies that enter the Earth's atmosphere. They
consist mainly of protons, together with electrons and
nuclei. In outer space their paths are guided by the
magnetic field lines of the Earth and Sun. They contribute
to background radiation - particularly for people in
high-flying aircraft.
Primary cosmic rays do not get closer to
the ground than about 15 km. They interact with atoms high
in the atmosphere to produce
neutrons and
mesons. The mesons can penetrate deep underground.
Mesons are charged particles - heavier
than electrons, but lighter than protons. They have lives so
short that they should not be able to travel as far as they
do. However, time passes more slowly for them because they
are travelling at almost the speed of light.
Astrophysicists want to know where cosmic
rays come from. Nuclear physicists find them a cheap source
of
very high energy particles. They use rockets and
balloons to carry blocks of photographic emulsion into the
upper atmosphere, then study the tracks left when cosmic
rays interact with atoms in the emulsion.
Primary cosmic rays sometimes give rise
to a very high energy gamma-ray. This produces an
electron-positron pair. The pair have such high energies
that they produce more gamma-rays as they slow down. These
gammas themselves produce pairs, which generate more pairs,
and so on. The result is a cosmic ray shower. |
|
| |
|
Sometimes you see a vapour trail very
high up in the sky. You cannot see what is on the end of it,
but you assume it is a plane. The trail tells you where the
plane has been. In just the same way, the vapour trail in a
cloud chamber tells where a charged particle has been. In
fact, vapour trail is a misnomer - we should say
condensation trail. A cloud chamber is full of super-cooled
vapour looking for somewhere to condense. Water droplets
condense on the trail of ions left by a charged particle.
Alpha-particles produce short, thick trails, because they
produce lots of ions over a short distance. Beta-particles
produce long straggly trails.
Nowadays, bubble chambers have largely
replaced cloud chambers. If you remove the radiator cap on
your car while the engine is very hot, the release of
pressure causes the water to boil suddenly and violently. A
bubble chamber is full of liquid hydrogen, under pressure,
at a temperature above its normal boiling point (-253°C). A
sudden drop in pressure makes the hydrogen want to boil. The
bubbles of vapour, however, need centres round which to
form. Ions provide these centres, and lines of bubbles mark
the tracks of charged particles through the chamber.
Physicists hope that particles will react
with hydrogen nuclei or electrons in the chamber, and
something interesting will result. Flash photographs are
taken each time there is an expansion. Thousands of these
are analysed in the search for something significant. A
magnetic field across the chamber curves the paths of the
particles and gives away their charge. |
|
| |
|
A nucleus will only decay if it can lose
energy by doing so and become more stable. It is impossible,
however, to predict when a particular nucleus will decay. We
can predict that half of the atoms in a sample of radium-226
will decay in the next 1,620 years, but we cannot say which
half. A particular atom might decay in one second or after
3,000 years. Even if we knew exactly what was going in
inside a nucleus, we still could not predict when it was
going to decay. The decay of an atom is completely random -
it is an event without a cause.
Set up a Geiger counter and a radioactive
source. Measure the counts over a period of one minute. Do
this 100 times. Calculate the average. Repeat the
experiment. The two averages will be very close to one
another, but the individual counts will vary quite a lot.
They cannot be predicted.
In the past some scientists had reasoned
that the Universe was governed absolutely by the laws of
science. Everything that was going to happen was already
decided and we could not do anything about it. This must
include our own behaviour. Radioactive decay and similar
discoveries in atomic physics showed that this could not be
so.
Albert Einstein could not come to terms
with this idea. He said 'God does not play dice with the
world'; as a result he became increasingly cut off from
mainstream physics. |
|
| |
|
When a nucleus emits a particle it
recoils, just like a gun does when you fire it. Physicists
studying the recoil of a nucleus when it emitted a
beta-particle (electron) got a nasty shock. Some energy
and momentum seemed to have disappeared.
In 1933, Pauli suggested that another
particle might be involved. He called it a neutrino. Like a
gamma-ray it had momentum and energy, but no mass and no
charge. Unlike a gamma-ray, however, it seemed to pass
through matter without doing anything. If you stand near a
nuclear reactor there is a tremendous flow of neutrinos
through the shielding and straight through you.
The neutrino was finally detected in
1956. A hydrogen nucleus is a
proton. A large tank of dry-cleaning fluid contains a
lot of hydrogen atoms. Very occasionally a neutrino will
join up with a proton to give a neutron and a positive
electron or positron. Eventually a neutron and a positron
were detected at the same instant, coming from somewhere in
the tank. This confirmed the existence of neutrinos.
Today we have neutrino astronomy.
Neutrinos were detected from the supernova that appeared in
the Greater Magellanic Cloud in 1987. A supernova is the
sudden spectacular collapse of a star that has finally run
out of
fusion fuel. Neutrinos can be detected from deep inside
the Sun. Unfortunately the number does not agree with
theories of how the Sun works. |
|
|
| |
|
Basically it is energy that comes out,
but in 3 different forms - alpha, beta and gamma rays. When
they were discovered, nobody knew what they were. They just
knew there were three sorts, so they called them alpha,
beta, gamma; (they could have just said a,b,c - but they
wanted people to know that they had studied Greek at
school).
Alpha rays are actually heavy,
fast-moving particles with a positive charge. They only
travel a few centimetres in air and are stopped by a sheet
of paper. They are very good at making air conduct
electricity. They turn out to be the nuclei of
helium atoms.
Beta rays are also particles, but
very much lighter and faster moving than alpha-paricles.
They can travel through a metre or so of air, but are
stopped by a few millimetres of aluminium. They have a
negative charge and turn out to be
electrons. They are not nearly as good as alpha
particles at making air conduct electricity.
Gamma rays are waves - they are
part of the electromagnetic spectrum like light waves and
radio waves. They have a very short wavelength - smaller
than an atom. They are similar to X rays, but with shorter
wavelengths and more energy. They can pass through thick
sheets of lead. They make air conduct electricity, but much
less than alphas or betas do.
All three come from the
nucleus of the atom. Some radioactive atoms give
alphas and some betas. In some cases an atom will
emit a gamma ray when it is settling down after
emitting an alpha or a beta - a sort of nuclear
burp. |
|
|
|
| |
|
It is true that there is always very weak
radiation around us. Scientists call it background
radiation. It even makes a tiny number of people ill. Only a
very small fraction of this radiation is due to the
nuclear industry.
The main radioactive elements are uranium
and thorium, but there are others. For example, potassium
contains a trace of radioactive potassium-40. All living
things contain a small proportion of radioactive
carbon-14. In the 19th century, craftsmen used uranium
to give glass a nice yellow colour. They didn't know about
radioactivity. Luminous paint is radioactive. Workers at an
American plant producing luminous dials put their brushes in
their mouths. They developed jaw cancer.
When above-ground
nuclear bomb tests were common, traces of radioactive
fallout were everywhere. Strontium-90 was found in
children's bones. The accident at Chernobyl has made parts
of the surrounding area uninhabitable, but it also had an
effect as far away as Wales. The mutton from sheep eating
radioactive grass could not be sold.
Becquerel discovered radioactivity in
1896. An activity of 1 becquerel (Bq) means that one nucleus
decays every second.
| EXAMPLE |
ACTIVITY IN Bq |
| Loaf of bread |
70
|
| Adult person |
3,000
|
| 1kg of granite form Cornwall |
1,200
|
| 1kg of coffee |
1,000
|
| 1kg phosphate fertiliser |
5,000
|
| 1kg ash from a coal-fired power station |
2,000
|
| 1kg uranium |
10,000,000
|
|
|
|
| |
|
Gamma rays are like X-rays, but they come from the
nuclei of atoms. X-rays are produced when fast-moving
electrons hit heavy metal atoms. There is an overlap between
the gamma-ray and X-ray regions of the spectrum, but some
gamma rays are far more energetic than X-rays - they will
pass through much thicker lead shields.
X-rays can be used to photograph the
bones inside your body or the bomb in your suitcase because
they are stopped by dense materials. Finding a dangerous
hole or crack inside a metal casting, or a faulty weld,
needs a more penetrating form of radiation. Gamma rays will
do this job.
Gamma rays kill living cells, but they
kill cancer cells more easily than they kill healthy cells.
Therefore they can be used to treat tumours. Strong doses of
gamma rays can be used to sterilise surgical dressings and
instruments. They can be sealed in containers and lowered
into the water tanks where used nuclear
fuel rods are waiting to be processed. This gives them
an ample dose of radiation. Food items - such as
strawberries - can be sealed into airtight wrapping and then
dosed with gamma rays. This kills most of the fungi and
bacteria, so the fruit stays fresh for a long time. This
does not make the strawberries radioactive, and they are
quite safe to eat. People, however, are very suspicious of
anything that has been treated in this way.
|
|
|
| |
|
Helium is a very light gas, so it is soon
lost into space from the Earth's atmosphere. The very tiny
amount in the air has to come from underground. Experiments
show that when
alpha-particles finally come to a stop; they steal 2
electrons from other atoms and become atoms of helium. These
atoms go around by themselves, so a molecule of helium is
just one atom. When atoms in rocks emit alpha-particles, the
gas gets trapped in the rocks. It can be released by
grinding up and heating the rocks. A kilogram of uranium
produces about a mugful of helium in 3 million years. This
makes helium expensive, but it is used in balloons because
it does not burn like hydrogen. Divers breathe a mixture of
oxygen and helium to avoid getting the bends.
When a nucleus emits an alpha-particle,
it loses 2 protons and 2 neutrons. Its
mass number goes down by 4 and becomes an atom of the
element two places down in the table - for example,
radium-226 (element 88) becomes radon-222 (element 86).
When a
beta-particle is emitted, a neutron becomes a proton and
the atom moves one step down the table - for example
carbon-14 (element 6) becomes nitrogen-14 (element-7).
|
|
|
| |
|
Radiation affects people's bodies in a number of ways.
To begin with, a very heavy dose of radiation bronzes your
skin like a suntan, and it can burn you like the sun. It
also makes your hair fall out, and knocks out your body's
immune system. You would be unlikely to live for long. Heavy
doses have been used to try to stop people rejecting
transplants, but this is a very extreme form of treatment.
They have to be isolated from any possible infection for a
long time afterwards.
Radiation may cause more damage if it is
emitted from a source inside your body. This is particularly
true of alpha-rays. If a particle strikes the nucleus of a
cell, then it can break up the chains of DNA. These then
come back together, but in a different arrangement. If it is
an egg or sperm cell that is affected, then any baby will be
formed according to a new set of instructions. Usually the
result will be a failure, but very occasionally the change
may be for the better. Mutations caused by background
radiation have probably helped to speed up
evolution.
Damage to other cells may lead to them
multiplying uncontrollably and forming a tumour. This may
not until years later, when it is too late to track down the
cause. Gamma-rays, however, kill cancer cells more readily
than they kill normal cells - so they can actually be used
to treat
cancer. |
|
|
| |
|
Modern houses are snug and draughtproof,
but in some parts of the country - such as Cornwall - this
can actually make them dangerous to live in.
Ordinary uranium-238 decays through
several stages to become radium-226. Radium decays to become
a radioactive gas called radon-222, with a half-life of 4
days.Thorium also produces a form of radon.
In places where rocks like granite
contain uranium, the radon produced seeps up through the
ground and into houses through their foundations. If the
house is draughtproof, the amount of radon in the air can be
quite dangerous. The risk of dying from radon if you live in
Cornwall is about 1 in 3,200.
When radon-222 decays, it emits an
alpha-particle. It also continues to decay through a
series of
nuclides until it reaches lead-206, which is not
radioactive. These decay products are all solids. The danger
is that one of these atoms will lodge in someone's lung and
emit an alpha-particle. Alphas cannot penetrate the skin,
but if they are emitted inside the body they are very
dangerous. They can eventually cause lung cancer. It is
believed that quite a number of people die each year because
of radon, though actual cases are difficult to pin down.
You can get rid of radon either by
installing a sheet of material under the house to stop the
radon getting through, or by installing fans to blow it
away.
|
|
|
| |
|
Firstly remember that your eyes are
particularly sensitive to radiation, and that your
reproductive organs need protection for the sake of any
children you may have.
Don't eat, drink or breathe in anything
that might be radioactive - radiation does far more harm
inside your body. Smoking makes things worse. People did not
always realise the dangers - at one time radioactive drinks
and radioactive toothpaste were advertised as being good for
you!
If there is radioactive dust around, you
must wear overalls, hat and overshoes and - if things are
really bad - a special suit and breathing set.
There are three basic ways of protecting
yourself from external radiation. They involve time,
distance and shielding.
- Stay in the area for the shortest
time possible.
- Keep as far away from radioactive
sources as you can. Use long-handled tools to pick them
up. The radiation is 100 times stronger 10 cm from a
gamma-ray source than it is 1 metre away, and 10,000
times stronger at 1 cm from the source
- Put a barrier between yourself and
the source. Barriers of the same size and mass offer
about the same degree of protection. The denser the
material, the thinner the barrier can be. Lead makes a
thin barrier, but it is expensive. Steel barriers are
thicker, but stronger and cheaper than lead. Thick
layers of earth, concrete or even water are often used.
Where radiation is very strong, humans
cannot function at all, and robot arms and TV cameras have
to be used. |
|
|
| |
|
If you make some of
the atoms in a material radioactive, you can find out what
happens to the material even when it has become very spread
out. In the case of the mud some powdered radioactive glass
was mixed with it. Some radioactive solution might be mixed
with the water flowing through a pipe. If there is a leak in
the pipe some of the radioactivity will leak into the ground
around the pipe. This can be detected by someone above
ground following the line of the pipe.
A piston can be made radioactive by passing it through a
nuclear reactor. It is then fitted into a car engine. After
the car has run for some time, the engine oil is checked for
radioactivity. This shows how much of the piston has worn
away.
If a factory manager wants to know if materials are being
mixed thoroughly, he can make one material radioactive. Then
he checks if the activity is spread uniformly after mixing.
Radioactive chemicals can be injected into living things to
see where they end up. For example, a plant can be watered
with a solution containing radioactive phosphorus. When the
plant has taken up the solution, a leaf can be pressed
against X-ray film. A picture of the leaf is produced
showing where the phosphorus is concentrated. They are also
used in medicine. Iodine 131 is used in the detection of
thyroid cancer.
The radioactive materials used as tracers need to have a
short half-life, so that they soon disappear. |
|
|
| |
|
All matter - and not just people - is
mainly empty space. People began to realise this when they
saw how easily particles like alphas and
betas would pass through matter. They knew that there
are no real gaps between atoms in solids, so the particles
must actually be passing through the middle of the atoms.
Very occasionally, however, a particle bounces back from
something very small and very heavy in the centre of an
atom. This is the
nucleus.
To give you an idea of scale. If the atom
were the size of a large room, its nucleus would be the size
of a pinhead. The
electrons round the nucleus would be like mosquitoes
buzzing round the room. The rest would be empty space.
Solids exist because atoms attract one
another and cling together. If one atom tries to get too
close to another, however, attraction turns to increasingly
strong repulsion. This repulsion is so strong that it is
almost impossible to squash liquids or solids into a smaller
volume. However, a metal ball can be squashed to about half
its size for an instant, using specially shaped charges of
high explosive. This is what happens to the sphere of
plutonium at the centre of a
nuclear bomb.
In stars that have collapsed at the end
of their lives the pressures can be so high that the atoms
collapse completely. The density becomes unbelievably high -
a piece the size of a pinhead might weigh a million tonnes
or more. |
|
|
| |
|
The word atom comes from the Greek
for 'not cut': originally the idea was that you could not
split it: now we know better.
There is a tiny core at the centre of an
atom, called the nucleus. It consists of particles
called protons and neutrons. Protons and
neutrons have about the same mass. Protons have a positive
charge. Neutrons have no charge.
A hydrogen nucleus is just a single
proton. All the other nuclei contain protons and neutrons.
The nucleus gets bigger and heavier as we move down the list
of elements, until we come to element 92 - uranium. This has
92 protons and 146 neutrons.
Surrounding
the nucleus there is a cloud of electrons. Electrons
have a negative charge. This charge will just cancel out the
positive charge on a proton. The number of electrons in an
atom is equal to the number of protons. This atomic
number decides which element the atom belongs to, and
how it will behave chemically.
It would take about 2,000 electrons to
weigh as much as a proton, so nearly all the mass of an atom
is in the nucleus.
How big are atoms? Look at 1 millimetre
on a ruler. Imagine that millimetre magnified so that it was
as big as the diameter of the Earth. The atoms in the ruler
would then be about 1 millimetre across. |
|
|
| |
|
Uranium fuel rods can be handled before
they go into a reactor, but once in use they become so
radioactive that nobody can go near them. After a few years
each rod has to be removed from the reactor and stored under
water while the radioactivity dies down enough for it to be
processed to extract plutonium and unused uranium. The
radiation is so strong that the water glows with blue light.
This intense radioactivity is mainly due to the nuclei
produced by fission, though other materials can be made
radioactive by absorbing the neutrons that are flying round
inside a reactor.
The shorter the half-life of a
radioactive substance, the more intense the radiation from
it. This is why the radioactivity dies down rapidly at
first. The solution left after fuel rods have been processed
is so intensely radioactive that it has to be refrigerated
to prevent it from boiling. This makes it very difficult to
store safely, particularly as the time involved is maybe
20,000 years. In the long-term the idea is to turn the
liquid into a glass and bury it underground. The problem
then is to make sure that the rocks are stable and not
subject to earthquakes - no material can be allowed to get
into the water that is underground.
Apart from the wate from reactors, there
is also less radioactive waste from nuclear plants and
hospitals. This is also a problem, because there is far more
of it. |
|
|
| |
|
A molecule of ordinary water (H2O)
contains two hydrogen atoms and one oxygen atom. In heavy
water (D2O)
the hydrogen atoms are replaced by atoms of deuterium.
Deuterium is an isotope of hydrogen.
An ordinary hydrogen atom has a nucleus
consisting of a single proton. A deuterium atom has a
nucleus consisting of a proton and a neutron, so it is twice
as heavy as an ordinary hydrogen atom. This means that a
molecule of heavy water has a mass of 20 units while an
ordinary water molecule has a mass of 18 units. Pure heavy
water is 10% denser than ordinary water; it freezes at 3.8°C
and boils at 101.4°C. It is not radioactive.
Heavy water does not have to be produced:
it is present as a tiny fraction of ordinary water. It can
be separated by passing an electric current through water to
split it into hydrogen and oxygen. The deuterium atoms move
more slowly because they are heavier. They get left behind
in the liquid. Nearly 30 000 litres of water have to be
electrolysed to give one litre of almost pure heavy water.
This takes a vast amount of electrical energy, which is why
the plant being raided was in Norway. Hydroelectric power
was plentiful there.
To produce a nuclear chain reaction,
neutrons that are flying about at high speed have to be
slowed down. They can then be captured by uranium-235
nuclei. This is done by bouncing them off light nuclei, such
as deuterium. The nuclei recoil, taking away some of the
neutron's kinetic energy. A substance used to slow down
neutrons is called a moderator. Heavy water is a very good
moderator - ordinary water absorbs too many neutrons.
At the beginning of the war it was
thought that heavy water might be an important component of
a nuclear bomb - hence the raids. This turned out not to be
so, though the Germans did try unsuccessfully to build a
nuclear reactor using heavy water as a moderator.
|
|
|
| |
|
Electricity is
produced by dynamos. The generators in a power station are
similar to bicycle dynamos, but they are about as big as a
small bus and turn much faster. One dynamo will power
millions of electric fires. These generators are turned by
turbines, which are themselves powered by steam. The steam
can be produced either by burning a
fuel (coal, oil or gas) or by a nuclear reactor.
The chain reaction in the uranium fuel rods inside a reactor
creates heat. This heat is removed by passing a liquid or
gas through the reactor. Carbon dioxide, water and liquid
sodium are all used. This coolant is passed through heat
exchangers where it boils water to create the steam to drive
the turbines. In a nuclear submarine the turbines also drive
the propeller.
Originally it was
thought that nuclear reactors would be so efficient that
everybody would have free electricity. Now nuclear reactors
are becoming unpopular. People are worried about the small
amounts of radioactive liquids and gases that they emit.
They also create quantities of highly radioactive waste
products that are expensive and dangerous to store. There
are many problems with nuclear power, and there are many
benefits, such as low carbon dioxide emissions. The debate
for and against nuclear power is still very much in the
headlines. |
|
|
| |
|
Marie Curie is often portrayed as a sort
of scientific saint - the Florence Nightingale of physics.
In reality, like Florence, she was as tough as old boots and
an able administrator. She was a left-wing atheist. At one
point there was a terrific scandal when she was accused of
breaking up another physicist's marriage. There was even a
duel.
Marya Sklodowska was the daughter of a
Polish science teacher. She came to Paris to study physics
and chemistry, where she married a physics professor, Pierre
Curie. In 1897, Marie decided to study radioactivity for her
doctorate. To begin with, she worked through all the
elements and found that uranium and thorium were
radioactive. She then tried minerals and discovered that
uranium ore was far more radioactive than it should be for
the uranium that it contained.
Marie suggested that the ore might
contain an unknown element in such a small concentration as
to be invisible. This element would have to be extremely
radioactive. They had little money. She and Pierre were
forced to work in an old shed that had been a mortuary. It
took them 4 years to extract a tiny quantity of radium from
several tonnes of ore. Now they were famous, but Pierre was
soon run over and killed when he slipped on a wet pavement.
One of their daughters, Irene, and her husband Fred
Joliot-Curie discovered that it was possible to make things
radioactive using
neutrons. |
|
|
| |
|
How did people go to the Moon without being harmed by the
radiation coming from the Sun?
There is an
idea out there that the Americans never got to the Moon
because of the radiation in space that would fry astronauts.
There are a number of reasons why this argument is flawed.
Below is a basic outline:
The Van Allen Belts around the Earth trap particles from
the Sun and concentrate them. This affords the Earth some
protection from solar radiation, but the concentration of
particles in the belts is much higher than that below or
above the belts. Thus astronauts get a brief period of
intense exposure as you pass through the belt. The radiation
in question is particulate and occurs during bursts of
intense solar activity such as flares. Solar flares liberate
tremendous quantities of energy at many frequencies from
X-rays and gamma rays to long-wavelength radio waves. They
also emit high-energy particles called solar cosmic rays
(protons, electrons and atomic nuclei).
Flare X-rays and ultraviolet radiation disrupt radio
communication and the high-energy particle clouds, which are
lethal to unprotected astronauts, reach the Earth in 30
minutes; clouds of low-energy particles and disturbances in
the solar wind take 6 to 24 hours to reach to Earth.
Solar cosmic rays are formed when solar flares accelerate
atomic particles leaving the Sun. A blast wave propagates
through the solar wind at 1500 km/s. Protons, electrons and
atomic nuclei are accelerated to high energies. Most of the
particles are protons with alpha particles being second most
abundant. Solar-particle energies range from keV to about 20
GeV. Solar flare particles are perhaps a million times more
energetic than the ambient particles.
However, low energy particles (in the keV range) have
little effect as they can be stopped easily by a spacecraft
hull, space suit, camera case, etc. And high energy
particles (in the GeV) range have so much energy they can
actually pass straight through you without interacting with
body cells at all. The most dangerous level of radiation is
in the 1 MeV range. Someone in a low Earth orbit for 90 days
would receive a radiation dose from the Van Allen belts
twice that recommended for radiation workers. Astronauts on
a mission to the Moon only pass through the high
concentration of the belts briefly and then travel through
space to the Moon - a total journey time of about one week.
The radiation dose from a typical journey would thus be much
less than that from a 90 day low-orbit mission.
The issue here, however, is the effects of a flare. In
April 1981 the astronauts on the Space Shuttle Columbia
would have been in serious danger had they been outside
their craft as a large flare erupted while they were in
orbit. They were also in a low-earth orbit so relatively
safe.
However, flares don’t send particles out in all
directions. The magnetic field from the flare determines the
direction of the particle flow. So a flare may occur on one
side of the Sun and thus not affect us.
Finally, although a high dose of any form of radiation is
dangerous, being exposed to say one or two year’s worth of
dose in a short period of time as some of the Apollo
astronauts might have been during a flare, doesn’t
necessarily imply that you’ll develop cancer. Being exposed
to radiation increases the risk of developing cancer just as
smoking does but it doesn’t necessarily mean that cancer is
developed.
So in summary, high energy solar cosmic rays that occur
during flares may well provide a high enough dose of
radiation to be lethal. However, flares of this kind are few
and far between and when they do occur, need to send out
particles in the astronauts’ direction in order to affect
them.
As for photographic film being fogged, again the same
arguments apply. High energy particles will pass straight
through the film without affecting it, while low energy ones
will be stopped by the camera case.
NASA monitored solar flares during the Apollo missions
using three satellites (whose names escape me!). Now they
use earth based telescopes (radio and optical). The
government doesn't really have a policy towards radiation in
space as it's down to NASA to decide whether to launch or
not. NASA are aware of the problem and have brought missions
down early or delayed launches. However, because astronauts
get some protection from their vehicles, they can launch
most missions. |
|
|
| |
|
When an atom decays, it does not
disappear. It becomes an atom of another element. If an
electron (beta-particle)
is emitted, it eventually slows down and gets captured by an
atom that is short of an electron. An alpha-particle will
slow down, capture two electrons, and become a
helium atom. The time taken for half the atoms to decay
is called the half-life. The strength of the radioactivity
also halves in one half-life. After two half-lives the
activity will have dropped to one quarter, after three to
one ninth and so on.
Substances with a very short half-life
are very radioactive, but only for a short time. A longer
half-life means that the activity is weaker, but it lasts a
lot longer. In 10 half-lives the activity will drop to less
than one thousandth of its initial value
In practice it is more complicated.
Firstly a material like nuclear waste will be a mixture of
substances with different half-lives. Secondly the new atoms
produced are also likely to be unstable, and will decay in
their turn.
Only half the atoms in a piece of
uranium-238 will have decayed after 4.5 billion years. Just
one gram of uranium, however, contains so many atoms that
more than 12,000 will decay every second.
|
|
|
| |
|
Radiation ionises air - it makes it
conduct electricity. This can be useful in getting rid of
static electricity. Static attracts dust, can cause
dangerous sparks and makes some sheet materials difficult to
handle. Antistatic cleaning brushes for vinyl LPs used to be
made with radioactive bristles.
Beta and gamma rays are useful for measuring the
thickness of materials such as tinplate and paper that are
produced in a continuous sheet. A source is placed one side
and a detector on the other. The thinner the sheet, the more
radiation gets through. The measurements are then fed back
to the system controlling the pressure on the rollers.
Radiation can also be used to check whether sealed
containers on a production line have been filled properly.
If beta-rays are directed at a sheet of
something, some of them bounce back. This is called
back-scattering. The number of betas bouncing back increases
as the material gets thicker. Back-scattering is very useful
as means of checking the thickness of paint . It can also be
used to check if there is corrosion on the inside of a pipe
or sealed container.
|
|
|
| |
Who developed
carbon-dating and where?
A man called Willard F. Libby
born in 1908 pioneered the technique of carbon dating around 1946.
|
|
| |
Will Thermonuclear fusion become a reality in the 21st Century?
Your guess is as good as ours.
As you probably know Europe has a research facility based in
Oxfordshire called JET (Joint European Torus) which is trying to
create nuclear fusion. The Torus in the name refers to the large
donut shaped vessel inside which the scientists hope to create the
conditions for fusion. Because nuclear fusion reactions generate
very high temperatures it couldn't be contained by any metal as it
would melt it, so instead the scientists contain the high energy
plasma (inside which the reaction takes place) with a magnetic
field. This magnetic field has to constantly change to contain the
fusion reaction, and this is one of the major stumbling blocks. No
computer can currently keep up with the fluctuations in the plasma
and so it is impossible to contain the reaction, so it cannot be
sustained for any period of time. Once they can contain the reaction
for a sustained period they should be able to generate power. In
theory. But as to when? Well, as we said at the start, your guess is
as good as ours... |
|
| |
|
|
| |
How do solar
neutrino detectors work?
Solar neutrinos are very
un-reactive particles made in the Sun. They can pass through
the Earth without reacting with anything. In fact there are
thousands of neutrinos passing through your body right now.
Neutrino detectors are large containers filled with
dry-cleaning fluid and buried underground. Dry-cleaning
fluid is, strangely enough, one of the few things neutrinos
actually react with. The chlorine atoms in the fluid
occasionally react with the neutrinos causing a flash of
light. This flash of light is then detected by cameras
around the container.
|
|
|
| |
How good are various materials at shielding you from radiation?
Well it depends on the thickness of your shielding and
the type of radiation. Alpha particles are absorbed in the
dead surface layers of the skin for example, while gamma
rays are much more energetic and can penetrate quite deep
layers of shielding. As a rule of thumb the heavier the
atoms of the shielding material the more effective it is.
(This is because of the principle of conservation of
momentum). This means that lead is the most effective form
of shielding because it has heavy atoms and is very easy to
manufacture. Concrete is a useful form of shielding because
it is so easy to construct very thick layers of it. The
Ukrainians want to enclose Chernoble in a concrete
sarcophagus for instance.
|
|
| |
What was the
biggest nuclear explosion? The
biggest nuclear bomb ever, was a test carried out in the USSR in
1961... it was 50 Megatons! Compare this with the military ones used
at Hiroshima and Nagasaki which were 1-1.5 kilotons, with city-sized
devastation...and the biggest civil nuclear explosion was the
accident at Chernobyl.
|
|
| |
What do all the different units of radioactivity
mean?
1 becquerel is the activity of a quantity of
radioactive material in which 1 nucleus decays per second (this is
the unit that everyone is supposed to use these days). 1 becquerel =
2.7 E-11 Curies. One sievert is the unit of radiation dose delivered
in 1 hour at a distance of 1 centimeter from a point source of 1
milligram of radium element enclosed in platinum 0.5 mm thick.
|
|
| |
What stops an atomic
bomb going off?
For an atom bomb to go off, the mass of nuclear
material must exceed a quantity called the critical mass. This is
the amount of plutonium or other radioactive material needed to
sustain a chain reaction that causes the explosion. To stop a bomb
from going off the nuclear material is kept separate, making two
masses which do not exceed the critical mass by themselves. To
detonate the bomb, these two masses are brought together. There
joint mass is greater than the critical mass and B A N G.
|
|
| |
What is meant by the first ionization energy of an element?
Atoms are made up of a nucleus of protons
and neutrons surrounded by clouds of electrons. These electrons all
have certain energies and are usually described as occupying orbits
or levels. These orbits get closer and closer together, further and
further from the nucleus so that they are eventually 'touching' and
merge together. If you give an electron enough energy to reach this
point in an atom, it will leave the atom completely. This is known
as ionization - the removal of electrons from an atom. The first
ionization energy is just the energy it takes to remove the first
electron from an atom. The second ionization energy is the energy it
takes to remove the second, and so on. |
|
| |
| |
(a) Can you
turn gold into lead ?
(b) Can you use nuclear fusion to turn lead into gold ?
Elements like gold and lead are characterized by the number
of protons and neutrons in their nucleus (their atomic mass). In
a star, elements are created by adding protons and neutrons to
hydrogen atoms, making heavier and heavier elements. This is
called nucleosynthesis. By adding protons to the atom chemists
can theoretically do the same thing, turning lighter gold atoms
with 79 protons into heavier lead atoms with 82 protons.
However, in practice, converting gold into lead takes a lot of
energy and so costs more than the value of the lead actually
made. The reverse process of converting heavier lead atoms into
lighter gold atoms is also possible. In practice however,
tampering with elements at an atomic level is more likely to
produce dangerous unstable atoms of a new element, rather than
sparkling gold.
|
|
| |
Which quarks make up the proton? What holds it together?
Quarks are the fundamental building blocks of atoms. No
smaller particles are thought to exist, so everything is made up
of quarks. There are 6 different types of quarks called up,
down, charm, strange, bottom (or beauty) and top (or truth).
Atoms are made up of three different particles: protons,
neutrons and electrons. The protons and neutrons clump together
in the centre of the nucleus while the electrons whiz around the
outside. The proton itself is made up of one 'down' and two 'up'
quarks. We can imagine the quarks being held together like a
group of footballers held together by passing the football to
one another; quarks are the players and 'gluon' particles are
footballs. Each gluon has a property which is called (rather
misleadingly) 'colour' like an electron carrying a charge of
electricity. It is this constant exchange of colour that holds
the quarks together.
|
|
| |
How do you split an
atom?
Atoms are made up of a central core of particles called the
nucleus. This nucleus is made up of lots of different types of
particles stuck together - it's like a pile of marbles stuck
together by plasticine. Large atoms, such are uranium, have lots
of particles in their nucleus and this makes them unstable. By
firing an extra particle at this unstable nucleus it can be made
to break up. Usually the nucleus will break into two pieces to
make two new atoms and release energy. This collision also
produces two more particles that can go on to collide with other
atoms thus starting a chain reaction.
|
|
| |
|
|
| |
|
A Geiger counter depends on the fact that
radiation knocks electrons out of the atoms in a gas and
leaves them with an electric charge. These charged atoms (or
ions) can then carry an electric current through the gas.
A Geiger-Müller (G-M) tube consists of a
metal cylinder with a wire along its axis, sealed inside a
glass envelope. At one end there is a very thin mica window,
which allows radiation to enter the tube. The tube contains
gas at low pressure. There is a high voltage between the
wire and the cylinder. This produces a very strong electric
field close to the wire. Normally no current can cross the
gap. This means that there is no voltage across the 1 megohm
resistor.
When an alpha- or beta-particle enters
the tube, it produces some ions in the gas. These ions are
then accelerated by the strong field close to the wire. They
soon gain enough energy to ionise more atoms by bumping into
them. There is an avalanche of ions which allows a current
to flow through the gas. This current also flows through the
resistor and produces a pulse of voltage across it. These
pulses are counted by a special electronic circuit.
Sometimes they give a click in a loudspeaker.
Geiger counters are best at counting
beta-particles and those alpha-particles that have
sufficient energy to pass through the window. Gamma-rays and
X-rays will also be counted if they produce ions in the
tube, but they often just go straight through.
|
|
|
| |
Do cloud chambers really let you see alpha-particles?
Sometimes you see a vapour trail very
high up in the sky. You cannot see what is on the end of it,
but you assume it is a plane. The trail tells you where the
plane has been. In just the same way, the vapour trail in a
cloud chamber tells where a charged particle has been. In
fact, vapour trail is a misnomer - we should say
condensation trail. A cloud chamber is full of super-cooled
vapour looking for somewhere to condense. Water droplets
condense on the trail of ions left by a charged particle.
Alpha-particles produce short, thick trails, because they
produce lots of ions over a short distance. Beta-particles
produce long straggly trails.
Nowadays, bubble chambers have largely
replaced cloud chambers. If you remove the radiator cap on
your car while the engine is very hot, the release of
pressure causes the water to boil suddenly and violently. A
bubble chamber is full of liquid hydrogen, under pressure,
at a temperature above its normal boiling point (-253°C). A
sudden drop in pressure makes the hydrogen want to boil. The
bubbles of vapour, however, need centres round which to
form. Ions provide these centres, and lines of bubbles mark
the tracks of charged particles through the chamber.
Physicists hope that particles will react
with hydrogen nuclei or electrons in the chamber, and
something interesting will result. Flash photographs are
taken each time there is an expansion. Thousands of these
are analysed in the search for something significant. A
magnetic field across the chamber curves the paths of the
particles and gives away their charge. |
|
|
| |
|
Murray Gell-Mann and George Zeweig first
thought up the theory of these particles in 1964 to explain
how protons and neutrons and other similar particles
behaved.
Murray had just been reading Finnegan's
Wake by James Joyce which contains the phrase "three
quarks for Muster Mark". He decided it would be funny to
name his particles after this phrase.
Murray Gell-Mann had a strange sense of
humour! |
Antimatter is a sort of mirror image of
matter. A
gamma ray is energy. Sometimes, however, a gamma-ray
suddenly turns into an electron (matter) and a positron
(antimatter). This can happen when it passes near a nucleus.
When the positron meets an electron, however, they
annihilate one another. Two identical gamma rays are
produced, which shoot off in opposite directions. If there
were only one gamma-ray, momentum could not be conserved.
Energy has turned into matter plus antimatter; then matter
plus antimatter has turned back into energy.
When a nucleus emits an electron, one of
the neutrons actually becomes a
proton. Some atoms, however, decay by emitting a
positron. One of the protons becomes a neutron. It turns
out that every particle of matter has a corresponding
antiparticle. The antimatter version of hydrogen was
recently produced, and actually existed for an instant. It
consisted of an antiproton (negative) with a positron going
round it. Then it was annihilated by contact with matter.
We would expect the Big Bang to have
produced equal amounts of matter and antimatter, which would
have rapidly annihilated one another. We still need to
explain how enough matter got left over to produce the stars
and galaxies. |
|
|
| |
|
In 1920, Rutherford suggested that an
uncharged particle having about the same mass as a proton
might exist. He thought of it as being a combination of a
proton and an electron. Such a particle would explain why a
nucleus having, say, 12 times the mass of a proton only
weighed 6 times as much.
Rutherford had discovered in 1919 that
very occasionally an alpha-particle would collide with a
nitrogen nucleus and eject a proton from it. This also
occurred with alpha-particles and other nuclei, but
something strange happened with beryllium-17. Whatever was
ejected, it was not a charged particle. Originally they
thought it was a gamma-ray. Then, in 1932, Chadwick placed a
slab of paraffin wax in front of the beryllium. Wax contains
lots of protons (hydrogen nuclei). He found that protons
were knocked forward out of the wax. Whatever was hitting
them was giving all its energy to the proton. As it stopped
dead after the collision, it must have the same mass as a
proton. This was the neutron.
A convenient source of neutrons consists
of beryllium mixed with a strong source of alpha-particles.
This can be used to make other materials radioactive - it is
more convenient than using a nuclear reactor.
Fast-moving neutrons are used to treat
cancer. They are very penetrating - several feet of concrete
are needed to stop them. In a nuclear reactor, fast neutrons
are slowed down by bouncing them off
light nuclei.
Unlike protons, solitary neutrons are
unstable. They decay to give a proton, an electron and a
neutrino. Their half-life is 13 minutes. |
|
|
| |
|
The first number is the atomic number
(Z) (sometimes called the proton number). This is the
number of protons in the nucleus. It is also the number of
electrons going round the nucleus. Each value of the atomic
number belongs to a particular element, from hydrogen at
number 1 to uranium at number 92. The chemical behaviour of
an element depends on the number of electrons, which is Z.
The second number is the neutron
number (N). This is the number of neutrons in the
nucleus. All atoms of the same element have the same Z,
but they do not all have the same value of N. Atoms
having the same number of protons, but different numbers of
neutrons are called isotopes. They belong to the same
element and behave the same in chemistry, but they do differ
slightly in properties such as melting point. Isotopes can
be separated, but it is not easy*.
Most elements have more than one isotope.
You may have wondered why chlorine has an atomic mass of
35.5. This is because it is 75% chlorine-35 and 25%
chlorine-37.
The mass number (N) is the
total number of nucleons (protons and neutrons) in the
nucleus. N = A - Z: for example,
uranium-238 has Z = 92, A = 238 and N =
238 - 92 = 146.
A nuclide is a type of nucleus. The
symbol for a nuclide is the symbol for the element with two
numbers like this: 23892U.
The upper number is A and the lower number is Z.
*To separate uranium-235 from
uranium-238, the uranium is turned into a gas - uranium
hexafluoride. The gas molecules containing
235U will move
slightly faster than those containing
238U. Allow the
gas to pass down a long pipe with porous plugs in it: it
will become steadily richer in
235U. There is a big uranium
separation plant at Capenhurst, near Chester. |
|
|
| |
|
High energy physics involves using
electric and magnetic fields to accelerate particles - such
as protons - to enormously high energies, perhaps billions
of electron volts. The particles soon reach a speed very
close to that of light. Then, as their energy increases,
they just become heavier and heavier. These very high
energies are an attempt to get back to the sort of
conditions that existed in the Universe shortly after the
Big Bang and produce exotic particles - such as the Higgs
Boson - that no longer exist in the modern universe
The high-energy particles are made to
collide with other particles and nuclei, and the results
examined using a
bubble chamber or banks of detectors. The equipment
involved is enormous - the accelerator at CERN is in a
ring-shaped tunnel that crosses from Switzerland to France
and back again - and costs billions of pounds. Countries are
forced to co-operate because they cannot afford to go it
alone.
High-energy physics has been described
like this. You take a large watch. You then put a smaller
watch in a gun and fire it so that hits the first watch at
high speed. You take a photograph as all the bits fly apart.
You then use the photograph to try and find out how a watch
works. |
|
|
| |
|
What happens if, on average, at least one
of the neutrons produced by the fission of a uranium-235
nucleus goes on to be captured by another uranium-235 atom?
The process will keep going and generating heat - we have a
chain reaction.
What is needed to keep the reaction
going? The problem is that the neutrons are travelling too
fast to be captured easily. There are possible answers. One
is to use pure uranium-235, but this very expensive to
produce. The other is to slow down the neutrons so that they
are more easily captured. This is done by bouncing them off
the light atoms contained in a material known as a
moderator. Graphite is often used, and heavy water is very
effective. Ordinary water can be used as a moderator, but it
absorbs a lot of neutrons. A layer of heavy atoms reflects
escaping neutrons back into the reactor core.
How can we control the reaction? Rods
made of boron are pushed into channels in the reactor. These
rods absorb neutrons, so they damp down the reaction. The
speed of the reaction is controlled by moving these control
rods in and out. The heat produced is removed from the
reactor by a flow of liquid or gas coolant. The heat is used
to produce steam and drive turbines.
There is another metal that can be used
instead of uranium-235: plutonium. In a bomb, pure
uranium-235 or plutonium is used, and there is no moderator.
|
|
|
| |
|
This depends very much on what you mean
by industrially and what you'd want to do with it when you'd
produced it. Places like Cern that use antimatter in their
experiments, produces approximately 10E14 (1 with 14 zeros
after it) antiprotons a year. While this might seem like a
lot, in terms of actual 'energy content' this number would
only be enough to lift a person 10 metres into the air. In
order to power a spacecraft and get it into orbit, Cern
would need to produce antiprotons at this rate for 500,000
years. To produce enough energy for a medium sized bomb,
Cern would have to run for 20,000 times the age of the
Universe. So you can see that antiparticles don't exactly
have many applications in industry.
There aren't really any problems in
producing antiparticles except for the energy needed to
produce them. Just as it takes energy to produce matter, it
takes energy to produce antimatter and this energy is not
recouped when the antimatter is annihilated. Storage isn't a
problem. At the moment, antiparticles are stored in
containers with strong magnetic or electric fields around
them and a vacuum within. Kept in ideal conditions,
antiparticles should survive forever, but obviously
conditions aren't perfect and antiparticles will react with
matter in the non-perfect vacuum and will sometimes collide
with the sides of the container. | |