Radiation in a variety of forms is familiar
to all of us. Light is radiation we can see. Heat is radiation we can feel. Ultraviolet
and X-Ray we neither see nor feel. None of the four can be heard or smelled. All are like
light, because they do not continue after the source (bulb) is turned off or removed.
Radiation is as old as the universe. Stars are intensely
radioactive; our earth now only slightly so. Ever since his first appearance, man has been
exposed to both visible and invisible radiation from the sun. Like sunshine and rain,
thunder and lightning, radioactive substances until very recently occurred only in nature.
Radiation from radioactive material is stream of fast flying
particles or waves, which come from tiny units of matter called atoms. Atoms of a single
element often consist of different kinds which behave alike chemically, yet have slightly
different weights. These varieties are called "isotopes". The atoms of stable
isotopes are not radioactive, but those of unstable or radioactive substances give off
portions of themselves, and change into other isotopes in the process.
Shortly after the discovery of radium, man learned that for
millions of years another form of invisible radiation had been coming at him from outside
the earths atmosphere. The source of these particles, called "cosmic
rays", is still unknown. We do know, however, that they are stopped to some extent by
the earths atmosphere, and that if we were to live in Denver, Colorado, or elsewhere
at high elevation, cosmic radiation would be two or four times as intense as it is at sea
level. This is why scientists investigating cosmic rays, employ balloons and aircraft to
collect information at high altitudes.
Natural radioactive substances are widely distributed. They
exist in minute quantities in our bodies, in the water we drink, the air we breathe, the
soil we cultivate, even in the materials we use for building. Along with the cosmic
radiation from outer space, these tiny sources have been sending out invisible radioactive
signals for millions of years. It is against this background of natural radiation that man
has lived in the past and lives today. This so-called "background radiation"
varies slightly from one locality to another, and also with rain or snowfalls.
Within ten years of their discovery, practical uses were
found for both x-rays and radium. X-rays proved valuable in locating bone fractures, in
identifying diseases, and as a supplement to radium in the treatment of cancer. You
probably have had a chest x-ray recently or a picture of your teeth. If so, you have been
exposed to a relatively harmless amount of x-radiation administered by your own doctor or
dentist.
Within the past fifteen years, man has learned to take
naturally stable atoms and make them artificially radioactive. It is these radioactive
varieties, or "radioisotopes", which are proving to be among the most useful
tools in the entire history of science. Because they are radioactive, their radiation
tells where they are, even if the amount us extremely small. Their location, or movement
within the plant or animal tissues and in industrial and chemical processes, can ,
therefore be traced by sensitive recording instruments. Used in this manner, radioisotopes
are spoken of as "tracers".
Radioactive materials differ widely in the rate at which
they lose their radioactivity. The length of time they are kept in the body also varies.
Radium and Plutonium remain active for thousands of years and may be retained for long
periods in the body, while such elements as radiosodium will be quickly eliminated and
decay in a few days. Naturally, you must be careful to avoid taking even small amounts of
the more poisonous materials into your mouth or lungs. This is why eating or smoking is
forbidden in some radiation areas.
During an examination of the stomach or intestines, patients
frequently receive a series of exposures over a period of a few hours which may total 15
or 20 r. To render a person sterile the sex organs alone would have to receive a single
dose of 400-800 rem, and even more if the total amount were not given at one time.