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Comments on
- ii NIAGARA MOHAWK POWER C(BIPANY E N',
First Supplement to
[j jj Preliminary Hazards Summary Report Nine Mile Point Nuclear Station RECEIVED dated August 1964 ADVISORY COMMITTEE h
ON REAC R FEGUARDS i
Prepared by OCT 141984
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AM fi pg gavironmental Meteorological Research Branch 7,8,9,1011l2,1,2,3,4,5 6 ~
i Office of Meteorological Research 1
U. S. Weather Bureau k
.4 October 6, 1964 These _ comments are directed toward the meteorological aspects of the original Preliminary Hazards Summary Report as amended by this supplement. Our comments on the original report are dated May 20, 19',4.
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.t As stated in our previous comments the meteorological analysis is very compre-j hensive and is particularly useful in estimating atmospheric dilution rates in g
a wide variety of realistic meteorological conditions.
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As was suggested in our earlier comments the subdivision of sector D in the analysis of long' term concentrations resulted in an increase in the concentra-tions in sector DI. This was primarily due to the higher frequencies of wind i
direction in sector D1 as compared to D2, Considering all esctors the highest-
- monthly concentrations occur in the month of June in sector D1 and are about a factor of two higher than previously computed according to Tables A-8.4.1 and
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A-10.4.1 as compared to A-8.4 and A-10.4.
Thus for the nearest off-site l
population at about 3 km from the reactor tge highest monthly average concentra-(~ j 250-ftemissionheightwouldbe7.3x10"{curiespercubicmeterforaunit tion for a ground source would be 1.6 x 1 curies per cubic meters and for a source strength of I curie /sec.
It should be pointed out that the actual physical mode by which the effluent f
is diluted by the atmosphere may differ from the uncomplicated ground or
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elevated source. It may well be that the mode is by means of a fumigation I
situation where an elevated plume, which is initially affected by stable air from over the lake, is subsequently brought rather rapidly to the surface because of the heating from the land. This phenomenon could lead to relatively high peak concentrations over a small area. However, it is unlikely that these concentrations would consistently occur at the same azimuth and radial distance over a month. One, therefore, can consider the monthly values for the ground and elevated source as an upper and lower boundary of expected concentrations.
At"4S GTICE COPY DO NOT REO.2
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