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RE: skyshine from radiography sources, Tokaimura criticalityacci dent
Title: Re: skyshine from radiography sources, Tokaimura criticality accident
Jason,
Actually, it is not that unusual for a criticality
accident to continue operating for a while. The fatal accident in Russia
involving a metal assembly (1997?) operated for about 3 days or so before
disassembled by a simple robot. It is not unusual for the initial pulse to
not release enough energy to physically disrupt the system adequately for
complete shutdown. Furthermore, solution systems may achieve thermal
equilibrium at temperatures below the boiling point of the solution, depending
on the heat transfer from the system.
Also,
the release of shortlived noble gases needs to be considered, especially for
solution systems. In models I developed a while back, in a room with
8 room changes per hour the shortlived nobles contributed over 95% of the plume
dose at 100 meters. In a surprise to me, I found that at 100 meters, if
one ignores shielding (which is often missing anyway), the doses from plume
passage for an accident like Tokaimura were essentially equal to the
direct doses from the assembly. In my simulations, they were about 1 - 2
rem each. At Tokaimura the nearest residences were only 80
meters away.
If
interested, I'd be happy to trade info with you off the
list.
Doug
Minnema, PhD, CHP
National Nuclear Security
Administration
what
few thoughts i have are truly my own ...
The Tokaimura criticality
accident was very unique in that the criticality continued for approximately
20 hours before the water blanket around the tank could be drained and the
system allowed to reach a subcritical state. Usually a criticality
accident is a pulse or burst type prompt criticality event. The energy
released during the pulse is usually sufficient to change the geometry
(through container deformation) or moderation (through boiling off of the
water moderator) of the system sufficient to make further criticality
pulses impossible or at least less powerful. Of all known
criticality accidents world wide (Ref. LA-13638), this accident's duration far
exceeded previous accidents. Because some residents were not evacuated
until 3.5 to 4 hours after the reaction started and were within a few hundred
meters of the source, the doses received by a handful of the nearest members
of the public were due primarily to the direct radiation and not sky
shine.
The Criticality Slide Rule (Ref.
NUREG/CR-6504, Vol. 2 or ORNL/TM-13322/V2) indicates that for the type of
accident at Tokaimura, at 30 meters, the skyshine dose is approximately 1/10
the total dose and at 300 meters the skyshine dose is 1/2 the total
dose.
I
have two separate reports generated soon after the accident that discuss
radiological exposures, measurements taken, emergency response, and the steps
taken to halt the ongoing criticality. One report was prepared by
Valerie Putnam on behalf of the American Nuclear Society and one prepared by
the IAEA. Both reports are in PDF format and easily transmitted. I
am not aware if they are available on the internet or
not.
I'm not sure if this answers Mr.
Franta's question, but I hope it helps.
Jason Bolling
Nuclear Criticality Safety Manager
Portsmouth Gaseous Diffusion
Plant