CTBTO Detects Radioactivity Consistent with Nuclear Test
CTBTO Detects Radioactivity Consistent with 12 February Announced North Korean Nuclear Test
Vienna, 23 April 2013
The
CTBTO’s radionuclide network has made a significant
detection of radioactive noble gases that could be
attributed to the nuclear
test announced by the Democratic People’s Republic of
Korea (DPRK) on 12 February 2013.
The detection
was made at the radionuclide
station in Takasaki, Japan, located at around 1,000
kilometres, or 620 miles, from the DPRK test site. Lower
levels were picked up at another station in Ussuriysk,
Russia. Two radioactive isotopes of the noble gas xenon were
identified, xenon-131m and xenon-133, which provide reliable
information on the nuclear nature of the
source.
The ratio of the detected xenon isotopes is
consistent with a nuclear fission event occurring more than
50 days before the detection (nuclear fission can occur in
both nuclear explosions and nuclear energy production). This
coincides very well with announced nuclear test by the DPRK
that occurred on 12 February 2013, 55 days before the
measurement.
Using Atmospheric Transport Modelling
(ATM), which calculates the three-dimensional travel path of
airborne radioactivity on the basis of weather data, the
DPRK test site was identified as a possible source for the
emission. Watch
the video
here.
CTBTO
radionuclide expert Mika Nikkinen said: “We are in the
process of eliminating other possible sources that could
explain the observations; the radionuclides could have come
from a nuclear reactor or other nuclear activity under
certain specific conditions, but so far we do not have
information on such a release.”
On 12 February,
the DPRK event was detected
immediately, reliably and precisely by 94 seismic
stations and two infrasound stations of the CTBTO’s
International Monitoring System. The first data were
made available to CTBTO Member States in little more than
one hour, and before the DPRK announced that it had
conducted a nuclear test.
The event recorded at
02.57.51 (UTC) was found to have a magnitude of 4.9 using
the CTBTO International Data Centre’s magnitude scale. The
location was in the vicinity of the two previous nuclear
tests (Lat.: 41.313 degrees north; long.: 129.101 degrees
east).
The radionuclide
technology is the only one of the four monitoring
technologies employed by the CTBTO that can provide clear
evidence of the nuclear nature of an explosion. After an
underground nuclear explosion, radioactive noble gases can
seep through layers of rock and sediment until they escape
into the air. Alternatively, the radioactivity may also be
released by man-made activities at the test
site.
Exposed to prevailing winds, the noble gases
are dispersed in the atmosphere and may, after a certain
period of time, be detected thousands of kilometres away
from the explosion site. The CTBTO currently has 66
radionuclide stations in operation across the globe, of
which 30 are able to detect noble gases.
The CTBTO
is the international organization responsible for ensuring
that no nuclear explosion goes undetected. It uses four
complementary verification
technologies: seismic, hydroacoustic, infrasound and
radionuclide monitoring. Traces of the radionuclide noble
gas xenon 133 were registered after the 2006
DPRK nuclear test, but there were no detections
following the 2009
DPRK test. In total, over 87 percent of the CTBTO’s
337 monitoring facilities are now up and running; see
interactive map.
The
DPRK’s action had been strongly condemned by Tibor Tóth,
the Executive Secretary of the CTBTO, and by Jan Petersen,
Chairperson of the CTBTO’s executive body.
For further information on the detection, see Q&A sheet [here].
Broadcasters – see CTBTO Newsroom for broadcast quality video and audio available, free of rights, for broadcasters to download. The package includes animation, sound bites and b-roll including from the CTBTO’s Takasaki radionuclide and noble gas monitoring station in Japan.
For further information
on the CTBTO, please see www.ctbto.org –
your resource for ending nuclear
testing