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| DOE-STD-1027-92
ATTACHMENT 1
The NRC then stated that "for all materials of greatest interest for fuel cycle and other
radioactive material licensees, the dose from the inhalation pathway H I will dominate the
dose" and dismissed the other contributors. Simplifying assumptions for Gaussian
dispersion and particle deposition were then used to calculate inhalation doses.
In modifying the NRC results, DOE has restated the equation above as
Q=
(1 rem)/(RF*SA*X/Q*(CEDE*RR + CSDE))
where
Q=
Quantity of material used as threshold (grams)
Airborne release fraction of material averaged over an entire facility
RF =
(unitless)
Specific activity of radionuclide released (Ci/gm)
SA=
Expression accounting for dilution of release at a point under given
X/Q=
meteorological conditions (sec/m 3)
CEDE= Committed effective dose equivalent for a given radionuclide
(rem/Ci)
RR=
Respiration rate, which is assumed equal to the standard value
used for an active man (3.5 E-4 m3/sec)
CSDE= Cloud shine dose equivalent (rem*m3/Ci*sec)
Specific modifications to forms of the equation are discussed in distinct sections below.
Exposure Pathways
As can be seen from the modified equation, DOE concurred with the NRC's dismissal of the
ground contamination exposure pathway. In general, DOE concurred with the dismissal of
cloudshine exposure as well because this path accounted for, on average, slightly less than
2% of dose for all radionuclides but the noble gases. Although, for the types of material that
DOE handles, it is expected that the values for noble gases will be included in the mixed
fission product threshold, DOE decided to retain this exposure pathway in the calculation for
Meteorological Conditions
DOE chose to modify the NRC meteorological assumptions used for hazard categorization
purposes. NRC used F stability at 1 m/sec meteorological conditions whereas DOE used D
stability at 4.5 m/sec for the following reasons:
A-6
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