Subsurface Gamma Radiation Detection
Description
At many U.S. Department of Energy (DOE) sites, restoration planning requires characterization of radiation fields below the surface for both for contaminated soil and groundwater. Because gamma radiation is more penetrating and travels further than alpha or beta radiation, and because most radionuclides produce some gamma radiation, gamma detection is the most common form of radiation detection. The crucial component of any gamma-measuring device is the detector, which is a component producing electrical signals as a result of the interactions of the gamma radiation. The following are descriptions of the most recent innovations that DOE has demonstrated and evaluated to detect gamma radiation in the subsurface.
Limitations and Concerns
Applicability
All of the technologies described detect gamma radiation in the subsurface environment.
Technology Development Status
All of the technologies described are in the demonstration phase of development. However, there are traditional laboratory methods that can analyze subsurface samples for gamma radiation.
Web Links
http://apps.em.doe.gov/ost/pubs/itsrs/itsr2364.pdf
http://apps.em.doe.gov/ost/pubs/itsrs/itsr2118.pdf
http://www.mgls.org/95Sym/Papers/Hill/index.html
http://www.frtr.gov/site/8_2_2.html
Other Resources and Demonstrations
See the descriptions of Surface Gamma Radiation Detectors, BetaScintTM, Cone Pentrometer, SCAPS, and XRF.
See http://www.xrfcorp.com/technology/radiation_detection.html for a description of common radiation detection methods.
Radioactivity, or ionizing radiation, is the spontaneous disintegration of unstable atomic nuclei. Ionizing radiation can take the form of alpha particles, beta particles or gamma
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STATUS: The preceding technology description and links were last updated 10/2002.
If you believe any of the information is out of date,
please let us know at cpeo@cpeo.org.