Learning Labs:   Radon

 

 


Radon in the Environment

Unit Outline Radon Lab

Measurement of alpha particle radiation using CR-39

Alpha particle radiation is the major source of natural radiation in our environment. It is derived from the radioactive decay of the colorless, tasteless, inert gas, radon (222Rn) and is second only to smoking as the leading cause of lung cancer in the US.

ScienceWorks Radiation Learning Lab

Radon is an important environmental hazard due to its release of alpha particle radiation. Our curricular unit emphasizes the principles behind measurement of alpha particles and fluctuations of radon levels within our homes and schools. The biological consequences of ionizing radiation are also discussed.

Measurement of alpha particle radiation using CR-39 is a curricular unit performed in the ScienceWorks lab that demonstrates some of the important physical characteristics of alpha particles. To do this, we utilize CR-39 plastic and a smoke detector.
 

Origin of radon

From Radon in Water and Air: Health Risks and Control Measures, a publication of the University of Maine

The most abundant sources of natural background radiation are 238U (Uranium-238, half life 4.5 billion years) and 232Th (Thorium-232, half life 14 billion years) in sedimentary rock. Both of these elements decay to a radon gas, but Thorium decays to 220Rn (commonly called "thoron") which has a half life of only 55 seconds whereas Uranium decays to 222Rn (commonly called "radon") which has a half life of 3.8 days. Because of the difference in half-life, radon can diffuse from the soil, where it is produced, into living spaces, whereas thoron decays before it can move very far from where it was created. Thus, most background alpha particle radiation of importance to humans is derived from radon gas (222Rn).

Movement of radon in soil is complex governed by diffusion, convection, and flow. It is not possible to predict what the radon concentration in the atmosphere is likely to be strictly by the nature of the sedimentary rock in an area. This is compounded by the nature of gas flow in buildings. In general, where more 238U is found, more radon is expected. However, radon measurements are necessary to assess exposure in a given building because the actual concentration of radon in a structure is not predictable until measurements are made.


Alpha Particles

diagram of Am-241 decay

In the ScienceWorks lab we will use Americium-241(Am-241) as an active source of alpha particles to study their properties and demonstrate how to record their presence. An alpha particle is released from a single Am-241 atom with a known energy of 5.6 MeV. Because an alpha particle is relatively big in nuclear terms, it is very likely to interact with any matter it encounters. When it does so, it dislodges electrons from the shells of these atoms and produces a positive ion. It takes approximately 35 eV to ionize an atom. Thus, one Am-241 emitted alpha particle will produce 150,000 ions. These ions allow a current to flow in the smoke detector's ionization chamber.

Origin of Americium-241

Open smoke detector showing ionization chamber

Open smoke detector showing ionization chamber 

Americium (pronounced, "am-uh-RISH-ium" and named after America) was the first man-made element. Glenn Seaborg and colleagues produced it by neutron bombardment of Plutonium in 1944 while working on the Manhattan Project at the University of Chicago. It is a shiny, malleable metal, all isotopes of which are unstable. It has atomic number 95. Currently, Americium-241 is produced by beta decay of spent Plutonium-241 in nuclear reactors. It has a half-life of 432 years. The US Atomic Energy Commission in 1962 first offered americium dioxide for sale for $1500 per gram, and this price has remained essentially unchanged. Its major use is as a source of alpha particles in the ionization chambers of common smoke detectors, and one gram supplies enough Americium-241 for 5000 smoke detectors. Americium-241 is a potentially dangerous isotope if it is taken into the body in soluble form as it can concentrate in the skeleton and is both an alpha and a gamma emitter- potentially causing DNA mutations. However, the dioxide in smoke detectors is insoluble and even if ingested would pass harmlessly through the gastrointestinal tract without delivering a significant dose of radiation.


CR-39

CR-39 viewed at 20X

CR-39 viewed @ 20 X showing "alpha tracks"

Photo courtesy of Track Analysis Systems Ltd. (TASL)

CR-39 is an allyl glycol carbonate plastic that has the unique properties of being inert to light, X-ray, and gamma and beta radiation, but reactive with alpha particles. When an alpha particle strikes the plastic's surface it produces a path of damage to a depth of approximately 40 nm. If the plastic is then submerged in 6.25 N NaOH at 98º C for 45 minutes, a track will be etched in the plastic that is visible under a microscope at 10x -20x power. This allows individual alpha particle impacts to be counted. As each alpha particle arises from the disintegration of an individual radon atom, the gas concentration can be derived. Thus, in a high school lab, radon concentration measurements from the local environment can be accurately made. However, such measurements require weeks of exposure and are more suited to experiments performed locally as part of a school project. Thus, in the ScienceWorks lab, we use a more active source of alpha particles, Americium-241. This metal is utilized in the ionization chambers of smoke detectors.


Facts used to generate hypotheses for CR-39 experiments

Because alpha particles interact so readily with other atoms, they do not penetrate matter (even air) very deeply. 

"Tracks" produced in CR-39 plastic are the product of a single alpha particle striking the surface. The number of tracks is proportional to the number of atoms disintegrating per unit time.

Interesting Links to sources of information about radon, alpha particles, and natural radiation

The Environmental Protection Agency's online publication: RADON: A Physician's Guide - a readable and thorough presentation of the biologic effects of radon as well as how to deal with it as a health threat

The EPA's "Radon Publications" page - free publications you can order about radon in the home

The Geology of Radon - online publication from the US Geological Survey about how radon gas arises from soil

The Teacher's Corner of RadWaste.org - an excellent source of online links about all things radioactive and nuclear

Natural Radioactivity - University of Michigan's excellent overview of natural radiation sources

Alpha Trak - Craig Gabler's website - a source of CR-39 for high school laboratories

Radon in Water and Air: Health Risks and Control Measures - an informative question and answer page from the University of Maine about the health effects of radon and methods to reduce radon exposure


 

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