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RE: skyshine from radiography sources, Tokaimura criticalityacci dent
Mike,
There is some radio-iodine, but it is part of the remaining 5% of the dose.
Check out DOE's release fractions handbook (sorry, I don't have the
reference with me now). It has a section on criticality accidents that
lists the isotopes that you should assume get released, and a second list
for the fractional releases depending on the type of criticality accident
(metal, solutions, finely divided powders, etc.).
If you are interested, I can send you an example of the calculations when I
get back to the office next Tuesday. Please send me a message off-list and
I'll get back to you.
Doug
-----Original Message-----
From: Michael McNaughton [mailto:mcnaught@lanl.gov]
Sent: Thursday, March 13, 2003 10:09 AM
To: Minnema, Douglas; 'Bolling, Jason E'; 'Radsafe (E-mail)'
Subject: RE: skyshine from radiography sources, Tokaimura criticality
acci dent
At 12:10 AM 03/13/2003 -0500, Minnema, Douglas wrote:
>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.
Doug: is it only nobles? For example, is there a contribution from
radio-iodine?
mike
Mike McNaughton
Los Alamos National Lab.
email: mcnaught@LANL.gov or mcnaughton@LANL.gov
phone: 505-667-6130
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