ORNL-4191 - the Molten Salt Energy Technologies Web Site
ORNL-4191 - the Molten Salt Energy Technologies Web Site
ORNL-4191 - the Molten Salt Energy Technologies Web Site
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188<br />
Fig. 15.8. Inner Surface of Core Shell in Contact with Graphite Core of In-Pile Loop 2. 250~.<br />
These equations permit <strong>the</strong> calculation of activity<br />
if flux is given, or of flux if activity has been<br />
measured.<br />
The Ys F term is <strong>the</strong> chain production rate at a<br />
given flux or power density for <strong>the</strong> quantity of<br />
material under consideration. It was useful to<br />
treat <strong>the</strong> Y. F term in <strong>the</strong> case of fissioning as a<br />
product of fission yield Y, a standard fission<br />
rate F" per gram of uranium (at a given flux), a<br />
uranium inventory for <strong>the</strong> interval j (from salt<br />
inventory actually under irradiation, w ., times<br />
I<br />
uranium concentration U .), and <strong>the</strong> irradiation<br />
I<br />
intensity factors, p. and q., relative to full re-<br />
1 1<br />
actor power and fully inserted position. Thus for<br />
any set of intervals, for example,<br />
-A, * t -A .t<br />
- (1-e 'j). (e ' dj)<br />
A similar expression can be written for <strong>the</strong><br />
daughter isotope (such as <strong>the</strong> 35-day 5Nb daughter<br />
of 65-day "Zr).<br />
The term on <strong>the</strong> right may be computed for any<br />
given isotope from a knowledge of decay rate,<br />
irradiation, and inventory history. The term on<br />
<strong>the</strong> left represents <strong>the</strong> count to be expected,<br />
divided by <strong>the</strong> saturation value from 1 g of uranium<br />
at full power.<br />
In practice, <strong>the</strong> total loop inventory was corrected<br />
for <strong>the</strong> amount of salt not under irradiation,<br />
at <strong>the</strong> time, in sample lines and <strong>the</strong> purge tank.<br />
The activity withdrawn with each removal and that<br />
remaining in <strong>the</strong> loop were calculated. The total<br />
activity (at reference time) of a given isotope<br />
produced during <strong>the</strong> experiment was thus estimated.<br />
As mentioned in an earlier section, it appears<br />
reasonable to use <strong>the</strong> activities of certain fission<br />
products in <strong>the</strong> salt samples, in particular 37Cs,<br />
'44Ce, and "Zr, as internal standards to estimate<br />
<strong>the</strong> flux. A mean flux to <strong>the</strong> salt of 0.88 x<br />
10' was thus estimated from activities measured