The Fissioning Process and its Consequences
In order to understand nuclear technology and its impact on human health,
three atomic-level events must be understood: fissioning, activation and
ionisation. Fissioning, i.e. the splitting of the
uranium or plutonium atom, is responsible for producing radioactive fission
fragments and activation products. These in turn cause the ionisation of
normal atoms, leading to a chain of microscopic events we may eventually
observe as a cancer death or a deformed child.
Radioactive
fission products are produced in nuclear reactors. They are
variant forms of the ordinary chemicals which are the building blocks of all
material and living things. The radioactive forms of these chemicals were,
prior to 1943, present in only trace quantities in isolated places in the
environment as, for example, in South Africa where it appears that a small
nuclear fission reaction occurred spontaneously about 1700 million years ago.
When
a uranium atom is split or fissioned, it does not always split
in the same place. The two pieces, called fragments, are chemicals of
lower atomic weight than uranium. Each fragment receives part of the
nucleus and part of the electrons of the original large uranium atom. The
uranium atoms, of course, cease to exist after they are split. Instead,
more than 80 different possible fission products are formed,
each having the chemical properties usually associated with their
structure, but having the added capability of releasing ionising
radiation. X-rays, alpha particles, beta particles, gamma rays (like
X-rays) or neutrons can be released by these `created' chemicals. All
these can cause `ionisation', i.e. by knocking an electron out of its
normal orbit around the nucleus of an atom they produce two `ions',
the negatively charged electron and the rest of the atom which now
has a net positive electrical charge.
The
atomic structure of fission fragments is unstable. The atom will
at some time release the destabilizing particle and return to a natural,
low-energy, more stable form. Every such release of energy is an
explosion on the microscopic level. With each fissioning, 2 or 3
neutrons are released which can strike a nearby U235 atom causing
more fissioning in what is usually called a chain reaction.
The
violence of the chain reaction is such that it can also yield
what are called activation products, i.e. it can cause already existing
chemicals in air, water or other nearby materials to absorb energy,
change their structure slightly and become radioactive. As these
high-energy forms of natural materials eventually return to their normal
stable state, they can also release ionising radiation. About 300
different radioactive chemicals are created with each chain
reaction.[1]
It takes hundreds of
thousands of years for all the newly formed radioactive chemicals to
return to a stable state.
In
a nuclear power plant the fissioning takes place inside the
zirconium or magnesium alloy cladding which encloses the fuel rods. Most
of the fission fragments are trapped within the rods. However,
the activation products can be formed in the surrounding air, water,
pipes and containment building. The nuclear plant itself becomes
unusable with time and must eventually be dismantled and isolated as
radioactive waste.
After
fissioning, the fuel rods are said to be `spent'. They contain the
greatest concentration of radioactivity of any material on the planet
earth -- many hundreds of thousands of times the concentration in
granite or even in uranium mill tailings (waste). The spent fuel rods
contain gamma radiation emitters (which are similar to X-ray
emitters) so they must not only be isolated from the
biosphere, but they must also be shielded with water and thick lead
walls. Direct human exposure to spent fuel rods means certain death.
In
reprocessing, spent fuel rods are broken open and the outer
cladding is dissolved in nitric acid. The plutonium is separated out for
use in nuclear weapons or for fuel in a breeder or mixed oxide nuclear
reactor. The remaining highly radioactive debris is stored as liquid in
large carbon or stainless steel drums, awaiting some kind of
solidification and burial in a permanent repository. Waste of lower
radioactivity is buried in dirt trenches or -- as in Windscale
(Sellafield) in England -- piped out to sea. The spent nuclear fuel rods
and liquid reprocessing waste are called `high level radioactive
waste'. It must be kept secure for hundreds of thousands of years --
essentially forever. Lower level waste may be equally long-lived, but
it is less concentrated.
In
above-ground nuclear weapon testing, there is no attempt to
contain any of the fission or activation products. Everything is
released into the air and on to the land. Some underground tests are
also designed to release most of the radioactive particles; these are
called crater shots or shots with unstemmed holes. Even when
below-ground shots are designed to be contained, they normally lose the
radioactive gases and some particulates. The radionuclides trapped in
the ground can also migrate downwards in the earth to water
reservoirs which provide irrigation and drinking water for human
purposes, although this process is slow. Radioactive debris piped out
to sea can be washed back on shore or can contaminate fish.
In
all nuclear reactions, some radioactive material -- namely the
chemically inert or so-called `noble' gases, other gases, radioactive
carbon, water, iodine, and small particulates of plutonium and other
transuranics (i.e. chemicals of higher atomic number than uranium) --
is immediately added to the air, water and land of the biosphere. In
the far-distant future, all the long-lived radioactive material, even that
now stored and trapped, will mix with the biosphere unless each
generation repackages it. Our planet earth is designed to recycle
everything.
The
radioactive chemicals which escape to the biosphere can
combine with one another or with stable chemicals to form molecules
which may be soluble or insoluble in water; which may be solids,
liquids or gases at ordinary temperature and pressure; which may be
able to enter into biochemical reactions or be biologically inert. The
radioactive materials may be external to the body and
still give off destructive penetrating radiation. They may also be taken
into the body with air, food and water or through an open wound,
becoming even more dangerous as they release their energy in close
proximity to living cells and delicate body organs. They may remain
near the place of entry into the body or travel in the bloodstream or
lymph fluid. They can be incorporated into the tissue or bone. They
may remain in the body for minutes or hours or a lifetime. In nuclear
medicine, for example, radioactive tracer chemicals are deliberately
chosen among those quickly excreted by the body. Most of the
radioactive particles decay into other radioactive `daughter' products
which may have very different physical, chemical and radiological
properties from the parent radioactive chemical. The average number
of such radioactive daughters of fission products produced before a
stable chemical form is reached, is four.
Besides
their ability to give off ionising radiation, many of the
radioactive particles are biologically toxic for other reasons. Radioactive
lead, a daughter product of the radon gas released by
uranium mining retains the ability to cause brain damage exercised by
non-radioactive lead. Plutonium is biologically and chemically
attracted to bone as is the naturally occurring radioactive chemical
radium. However, plutonium clumps on the surface of bone, delivering
a concentrated dose of alpha radiation to surrounding
cells, whereas radium diffuses homogeneously in bone and thus has
a lesser localized cell damage effect. This makes plutonium, because
of its concentration, much more biologically toxic than a comparable amount of radium. Some allowance for this physiological
difference has been made in setting plutonium standards, but there
is evidence that there is more than twenty times more damage
caused than was suspected at the time of standard
setting.[2]
The
cellular damage caused by internally deposited radioactive
particles becomes manifest as a health effect related to the particular
organ damaged. For example, radionuclides lodged in the bones can
damage bone marrow and cause bone cancers or leukaemia, while radionuclides
lodged in the lungs can cause respiratory diseases. Generalised
whole body exposure to radiation can be expressed as a stress related
to a person's hereditary medical weakness. Individual breakdown
usually occurs at our weakest point. In this way, man-made radiation
mimics natural radiation and causes the ageing or
breakdown process to be accelerated.
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