WHAT IS URANIUM?

The Navajo have another
name: Leetso, or "yellow monster."
- Uranium is a very heavy (dense)
extremely toxic and carcinogenic metal which can be used as an abundant source of concentrated energy.
- It occurs in most rocks in
concentrations of 2 to 4 parts per million and is as common in the
earth's crust as tin, tungsten and molybdenum. It occurs in
seawater, and could be recovered from the oceans if prices rose
significantly.
- It was discovered in 1789 by
Martin Klaproth, a German chemist, in the mineral called
pitchblende. It was named after the planet Uranus, which had been
discovered eight years earlier.
- Uranium was apparently
formed in
super novae about 6.6 billion years ago. While it is not common
in the solar system, today its radioactive decay provides the main source of heat inside the earth, causing convection and
continental drift.
- The high density
of uranium
means that it also finds uses in the keels of yachts and as
counterweights for aircraft control surfaces (rudders and
elevators), as well as for radiation shielding.
- Its melting point is 1132°C. The
chemical symbol for uranium is U.
The Uranium Atom
On a scale arranged according to the
increasing mass of their nuclei, uranium is the heaviest of all the
naturally-occurring elements (Hydrogen is the lightest). Uranium is 18.7
times as dense as water.
Like other elements, uranium occurs in
slightly differing forms known as 'isotopes'. These isotopes (16 in the
case of uranium) differ from each other in the number of particles
(neutrons) in the nucleus. 'Natural' uranium as found in the earth's
crust is a mixture largely of two isotopes: uranium-238 (U-238),
accounting for 99.3% and U-235 about 0.7%.
The isotope U-235 is important because under certain conditions it can
readily be split, yielding a lot of energy. It is therefore said to be
'fissile' and we use the expression 'nuclear fission'
Meanwhile, like all radioactive isotopes,
it decays. U-238 decays very slowly, its half-life being the same as the
age of the earth (4500 million years). This means that it is barely
radioactive, less so than many other isotopes in rocks and sand.
Nevertheless it generates 0.1 watts/tonne and this is enough to warm the
earth's core.
Energy from the uranium atom
The nucleus of the U-235 atom comprises 92 protons and 143 neutrons (92
+ 143 = 235). When the nucleus of a U-235 atom captures a neutron it
splits in two (fissions) and releases some energy in the form of heat,
also two or three additional neutrons are thrown off. If enough of these
expelled neutrons cause the nuclei of other U-235 atoms to split,
releasing further neutrons, a fission chain reactionı can be achieved.
When this happens over and over again, many millions of times, a very
large amount of heat is produced from a relatively small amount of
uranium.
It is this process, in effect "burning"
uranium, which occurs in a nuclear reactor. The heat is used to make
steam to produce electricity.
Inside the reactor
In a nuclear reactor the uranium fuel
is assembled in such a way that a controlled fission chain reaction can
be achieved. The heat created by splitting the U-235 atoms is then used
to make steam which spins a turbine to drive a generator, producing
electricity.
Nuclear power stations and fossil-fuelled
power stations of similar capacity have many features in common. Both
require heat to produce steam to drive turbines and generators. In a
nuclear power station, however, the fissioning of uranium atoms replaces
the burning of coal or gas .
The chain reaction that takes place in
the core of a nuclear reactor is controlled by rods which absorb
neutrons and which can be inserted or withdrawn to set the reactor at
the required power level.
The fuel elements are surrounded by a
substance called a moderator to slow the speed of the emitted neutrons
and thus enable the chain reaction to continue. Water, graphite and
heavy water are used as moderators in different types of reactors.
Because of the kind of fuel used (ie the
concentration of U-235, see below), if there is a major uncorrected
malfunction in a reactor the fuel may melt, but it cannot explode like a
bomb.
A typical 1000 megawatt (MWe) reactor can
provide enough electricity for a modern city of close to one million
people. About 35 such nuclear reactors could provide Australia's total
electricity needs.
Uranium and Plutonium
Whereas the U-235 atom is 'fissile', the U-238 atom is said to be
'fertile'. This means that it can capture one of the neutrons which are
flying about in the core of the reactor and become (indirectly)
plutonium-239, which is fissile. Pu-239 is very much like U-235, in that
it fissions when hit by a neutron and this also yields a lot of energy.
Because there is so much U-238 in a
reactor core (most of the fuel), these reactions occur frequently, and
in fact about one third of the energy yield comes from "burning" Pu-239.
But sometimes a Pu-239 atom simply
captures a neutron without splitting, and it becomes Pu-240. Because the
Pu-239 is either progressively "burned" or becomes Pu-240, the longer
the fuel stays in the reactor the more Pu-240 is in it.*
* The significance of this is that when
the spent fuel is removed after about three years, the plutonium in it
is not suitable for making weapons but can be recycled as fuel.
From uranium ore to reactor fuel
Uranium ore can be mined by underground
or open-cut methods, depending on its depth. After mining, the ore is
crushed and ground up. Then it is treated with acid to dissolve the
uranium, which is then recovered from solution.
Uranium may also be mined by in situ
leaching (ISL), where it is dissolved from the orebody in situ and
pumped to the surface.
The end product of the mining and milling
stages, or of ISL, is uranium oxide concentrate (U3O8).
This is the form in which uranium is sold.
Before it can be used in a reactor for
electricity generation, however, it must undergo a series of processes
to produce a useable fuel.
For most of the world's reactors, the
next step in making a useable fuel is to convert the uranium oxide into
a gas, uranium hexafluoride (UF6), which enables it to be
enriched. Enrichment increases the proportion of the uranium-235 isotope
from its natural level of 0.7% to 3 - 4%. This enables greater technical
efficiency in reactor design and operation, particularly in larger
reactors, and allows the use of ordinary water as a moderator.
After enrichment, the UF6 gas
is converted to uranium dioxide (UO2) which is formed into
fuel pellets. These fuel pellets are placed inside thin metal tubes
which are assembled in bundles to become the fuel elements for the core
of the reactor.
For reactors which use natural uranium as
their fuel (and hence which require graphite or heavy water as a
moderator) the U3O8 concentrate simply needs to be
refined and converted directly to uranium dioxide.
Spent reactor fuel is removed, stored,
and then either reprocessed or disposed of underground.
Who uses nuclear power?
Over 16% of the world's electricity is
generated from uranium in nuclear reactors. This amounts to about 2400
billion kWh each year, as much as from all sources of electricity
worldwide in 1960. In a current perspective, it is twelve times
Australia's or South Africa's total electricity production, five times
India's, twice China's and 500 times Kenya's total.
It comes from over 430 nuclear reactors
with a total output capacity of more than 350 000 megawatts (MWe)
operating in 31 countries. A further thirty reactors are under
construction, and another 70 are on the drawing board.

Belgium, Bulgaria, Finland, France,
Germany, Hungary, Japan, South Korea, Lithuania, Slovakia, Slovenia,
Sweden, Switzerland and Ukraine all get 30% or more of their electricity
from nuclear reactors. The USA has over 100 reactors operating, with
capacity of almost three times Australiaıs total, and supplying 20% of
its electricity. The UK gets almost a quarter of its electricity from
uranium.
Other uses of nuclear energy
Many people, when talking about nuclear
energy, have only nuclear reactors (or perhaps nuclear weapons) in mind.
Few people realise the extent to which the use of radioisotopes has
changed our lives over the last few decades.
Using relatively small special-purpose
nuclear reactors it has become possible to make a wide range of
radioactive materials (radioisotopes) at low cost. For this reason the
use of artificially produced radioisotopes has become widespread since
the early 1950s, and there are now some 270 "research" reactors in 59
countries producing them.
Radioisotopes
In our daily life we need food, water and good health. Today,
radioactive isotopes play an important part in the technologies that
provide us with all three. They are produced by bombarding small amounts
of particular elements with neutrons.
In medicine, radioisotopes are
widely used for diagnosis and research. Radioactive chemical tracers
emit gamma radiation which provides diagnostic information about a
person's anatomy and the functioning of specific organs. Radiotherapy
also employs radioisotopes in the treatment of some illnesses, such as
cancer. More powerful gamma sources are used to sterilise syringes,
bandages and other medical equipment. About one in two Australians is
likely to experience the benefits of nuclear medicine in their lifetime,
and gamma sterilisation of equipment is almost universal.
In the preservation of food,
radioisotopes are used to inhibit the sprouting of root crops after
harvesting, to kill parasites and pests, and to control the ripening of
stored fruit and vegetables. Irradiated foodstuffs are accepted by world
and national health authorities for human consumption in an increasing
number of countries. They include potatoes, onions, dried and fresh
fruits, grain and grain products, poultry and some fish. Some prepacked
foods can also be irradiated.
In the growing crops and breeding
livestock, radioisotopes also play an important role. They are
used to produce high yielding, disease and weather resistant varieties
of crops, to study how fertilisers and insecticides work, and to improve
the productivity and health of domestic animals.
Industrially, and in mining, they
are used to examine welds, to detect leaks, to study the rate of wear of
metals, and for on-stream analysis of a wide range of minerals and
fuels.
There are many other uses. A radioisotope
derived from the plutonium formed in nuclear reactors is used in most
household smoke detectors.
Radioisotopes are used by police to fight
crime, in detecting and analysing pollutants in the environment, to
study the movement of surface water and to measure water runoffs from
rain and snow, as well as the flow rates of streams and rivers.
Other reactors
There are also other uses for reactors. Over 200 small nuclear reactors
power some 150 ships, mostly submarines, but ranging from icebreakers to
aircraft carriers. These can stay at sea for long periods without having
to make refuelling stops. The worldıs first nuclear powered container
ship was built in Russia.
The heat produced by nuclear reactors can
also be used directly rather than for generating electricity. In Sweden
and Russia, for example, it is used to heat buildings and to provide
heat for a variety of industrial processes such as water desalination.
Military weapons
Both uranium and plutonium were used to make bombs before they became
important for making electricity and radioisotopes. But the type of
uranium and plutonium for bombs is different from that in a nuclear
power plant. Bomb-grade uranium is highly-enriched (>90% U-235, instead
of about 3.5%); bomb-grade plutonium is fairly pure (>90%) Pu-239 and is
made in special reactors.
Today, due to disarmament, a lot of
military uranium is becoming available for electricity production. The
military uranium is diluted about 25:1 with depleted uranium (mostly
U-238) from the enrichment process before being used.