![Strong and safe communities Strong and safe communities](/web/20061103051902im_/http://www.gsc.nrcan.gc.ca/esst_images/2002iscom_e.jpeg) Natural Resources Canada > Earth Sciences Sector > Priorities > Strong and safe communities > Radiation Geophysics
Radiation Geophysics Environmental applications
The Section maintains the data acquisition system in a state of readiness,
for use in locating and mapping radiation spills from nuclear accidents
and for use in studies of nuclear waste disposal areas.
In January 1978, the USSR's nuclear-powered Cosmos 954 satellite [1]
fell to earth [2] and scattered radioactive debris across the Northwest
Territories near Yellowknife in northern Canada [3]. During the 3 month
search & cleanup operation, the Section's innovative full-spectrum
system was re-tuned to detect radiation from man-made sources
[4] (Bristow, 1978)
and was successful in locating 500 pieces of radioactive debris [5]
for subsequent disposal [6].
Operation Morning Light was documented in an illustrated non-technical report
(NTIS, 1978)
prepared by the US National Technical Information Service.
An illustrated report from the Atomic Energy Control Board of Canada
(Gummer et al, 1980) is equally readable,
but with more details of the recovered debris.
A personal account of the operation by Q. Bristow
also makes for interesting reading.
[1]
[2]
[3]
[4]
[5]
[6]
The Radiation Geophysics Section also provides
assistance to geologists and geophysicists from other countries in
analyzing and processing their airborne gamma-ray survey data. The
Section processed a data set flown over a nuclear reactor spill in
Eastern Europe
(Rangelov et al, 1993).
The extent of the contamination from reactor products is evident
in the Cobalt-60 map [7] and in the Exposure Rate map
(superimposed on a high-resolution
SPOT
satellite image) [8].
Both maps clearly show the reactor and the path of the spill down two drainage
ditches/canals (1993, GSC Open File 2573).
[7]
[8]
Radon is a colourless, odourless radioactive gas that occurs naturally
in our environment. It is produced by the natural breakdown (radioactive decay)
of uranium. Radon can be found in high concentrations where soils and rocks
contain uranium, granite, shale or phosphate. Radon may also be found in
soils contaminated with certain types of industrial waste, such as the
by-products of uranium or phosphate mining.
Nuclear reactors & power plants |
These are maps of the exposure rate at ground level of gamma radiation emitted
by nuclear reactors:
Argon-41 (Ar41) is produced by the activation of Argon-40
(Ar40) present in the air circulating through the reactor. In the
most radioactive part of the plume, the calculated exposure rate at ground
level was found to be about three times the average natural background
radiation in Canada, but no higher than the natural level in many parts of
Canada (Grasty, 1983).
![Port Hope map](/web/20061103051902im_/http://www.gsc.nrcan.gc.ca/gamma/images/hope_.gif) |
Uranium map derived from airborne gamma-ray
spectrometry measurements over the town of Port Hope, Ontario, showing
low level radioactivity from storage areas and contaminated fill from the
refinery at Eldorado Resources Ltd. |
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