| Radiographers and others who use sealed
radioactive sources must periodically "wipe" the sources to detect
the leakage of radioactive material from them. Sometimes the origin of
the radioactive contamination may not be the source that is wiped and
the identification of the radioactive material is required. This
article is a simplified attempt to tell how that is done. Maybe it is
magic!
Frank Iddings
Tutorial Projects Editor
|
Figure 1-2
Introduction
When the periodic wipe tests are done on sealed
radioactive sources, such as in isotope radio-graphy, a wipe may show
more than 185 Bq (5 x 10-9 Ci) of contamination. Removable
contamination above that level generally means the welded seal on the
source is open and radioactive material is being released from the
source. But that may not be the case; the sealed source may have been
contaminated from contact with radioactive material left in the guide
tube from a different source or wear in the metal tube inside of the
exposure device shield that allows the sealed source to rub against
the U-238 (depleted uranium) radiation shield. Most radiation exposure
devices for radiography use depleted uranium for radiation shielding
because of its weight and durability advantages over lead.
Sometimes removable radioactive material is
found on the guide tubes and collimators used with the radiographic
sources. The question then becomes what radioisotope is it? The answer
helps pin down what the source of the contamination is and what
corrective action must be taken.
With modern gamma spectrometry, identification
usually takes only a minute or so.
Some years ago, the question was asked in one of
my radiation safety classes for radiographers, "How do you identify
gamma emitting radioisotopes?" My answer began with, "It's magic!"
- a factitious answer to gain attention, but couched in some truth.
Before the availability of equipment for gamma spectrometry, such
identification was really tough and time consuming. With modern gamma
spectrometry, identification usually takes only a minute or so. The
following is a brief, simplistic description of gamma spectrometry for
gamma emitting radioisotope identification.
Gamma Spectrometry
Gamma rays (and sometimes X-rays) are emitted by
the radioisotopes used in industrial radiography. These gamma rays
(and the few X-ray emitting radioisotopes used in industry) have
unique energies. For example: Cs-137 emits a single gamma ray at an
energy of 0.662 MeV, Co-60 emits two gamma rays at 1.17 and 1.33 MeV
and Ir-192 emits several gamma rays with energies from 0.14 to 1.2
(average about 0.34) MeV. Other less common radioactive materials used
in radiography, as well as the very common U-238 shielding, all emit
specific, identifiable gamma rays.
One of the earliest efforts at identification
involved measuring the amount of gamma radiation penetrating different
thicknesses of lead so that a half value layer or half thickness for
the radiation was determined. This was slow, tedious work with
sometimes unsatisfactory results.
The development of scintillation detectors, such
as NaI(Tl) - thallium doped sodium iodide - connected to single
channel analyzers was a step forward, but still slow and tedious. With
the availability of multichannel analyzers, gamma spectra - and hence
radioisotope identification - could be obtained relatively quickly.
Briefly, the scintillation detector and
multichannel analyzer work by the conversion of the gamma ray into a
flash of light in the scintillation crystal, conversion of the light
flashes into proportional numbers of photoelectrons in the
photocathode of a photomultiplier tube and multiplication of the
photoelectrons into electrical pulses exiting from the photomultiplier
tube. The multichannel analyzer sorts out the pulses into a plot of
number versus size of the pulses (size or amplitude of the pulses is
proportional to the original gamma energy released to the crystal.)
This plot is a gamma spectrum that can be compared to tables of
similar spectra or used to obtain the energy of the gamma rays
detected (Heath, 1957).
Two advances have been made since the "magic"
of the gamma spectrometer made identification of gamma emitters
relatively quick and easy. One is the improvement of the multichannel
analyzer into a small device (some are now available that fit into a
shirt pocket) that can operate off batteries rather than a system that
occupied most of the top of a normal desk and demanded considerable
electrical power. The other improvement is the development of
semiconductor detectors, such as Ge(Li) - lithium drifted germanium
- intrinsic germanium and cadmium-tellurium, that provide much better
resolution than NaI(Tl) for the gamma spectra. Better resolution
translates into narrower peaks in the gamma spectra. See Figure 1 for
a comparison of a NaI(Tl) and a germanium detector (ASNT, 2002).
Some computer driven multichannel analyzers -
often just a card in a desktop or laptop computer - can give you the
identity of the radioisotopes producing the spectrum accumulated.
Under the proper conditions, the quantity of the radioisotopes is
calculated. All of this is within a few minutes and at a fraction of
the cost required before.
To give you an idea of the simplicity of
identification from the gamma spectra of the radioisotopes, see Figure
2, showing the gamma spectra of Co-60, Cs-137 and Ir-192 (ASNT, 2002).
The "magic" of identification of gamma
emitters is now revealed - in part. There is still plenty of
"magic" in the instruments and their use. You can identify a
radioisotope now if it is Co-60, Cs-137 or Ir-192. Just like any
magician, with more practice, you'll be able to do more magic.
References
ASNT, Nondestructive Testing Handbook, third
edition: Volume 4, Radiographic Testing, Columbus, Ohio, ASNT, 2002.
Heath, R.L., Scintillation Spectrometry
Gamma-ray Spectrum Catalogue, AEC Research and Development Report
IDO-16408, Washington DC, US Atomic Energy Commission, Office of
Technical Services, US Department of Commerce, 1957.
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