Review of Molten Salt Reactor Physics Calculations [Disc 2]
Review of Molten Salt Reactor Physics Calculations [Disc 2]
Review of Molten Salt Reactor Physics Calculations [Disc 2]
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8<br />
2. QF RESULTS AND FECOMMEIPDATIONS<br />
- V<br />
Lid<br />
B<br />
Suxnary <strong>of</strong> Results<br />
The most significant difference between the results <strong>of</strong> our calcula-<br />
tions and previous ones was in the reactivity <strong>of</strong> the reference design.<br />
Using the reference composition we obtained a kefl <strong>of</strong> 0.95. An additional<br />
14s 23% was required to achieve criticality, holding all other concen-<br />
trations constant.<br />
values used for thorium resonance integral.<br />
integral for the geometry <strong>of</strong> the reference design and obtained 36.5 barns.<br />
In the OPTIMEW calculations it had been found convenient to use the 6me<br />
resonance integral for dl geometries being considered; the value assigxied<br />
wa6 30.1 barns.<br />
The discrepancy in keM. is entirely traceable to the<br />
We calculated the resonance<br />
Our calculations agreed w ith the previous ones to within 0.01in<br />
breeding ratio as shown in Tables 2.1 and 2.2. :Huwever, there were a<br />
number <strong>of</strong> individual differences <strong>of</strong> 0.001to 0,005 In the neuhon balance.<br />
An analysis <strong>of</strong> sane <strong>of</strong> these is as follows: ,<br />
Table 2.1 MSBR Performance Carnparison<br />
I<br />
c<br />
Present<br />
<strong>Calculations</strong><br />
Previous<br />
<strong>Calculations</strong><br />
Nuclear breeding ratio 1.062 1.054<br />
Neutron production per fissile<br />
absorption (q€) 2 -228 2.221<br />
Meas .q <strong>of</strong> 233u 2.221 2.219<br />
Mean 7 <strong>of</strong> 235,<br />
Parer factor, core, pedmean<br />
1971<br />
1958<br />
Radial 2.18 2.22<br />
Axial 1.51 1-37<br />
Total 3 -29 3.04<br />
1. The avera&'q <strong>of</strong> 233U in our calculations was 2.221 while it<br />
was 2.219 previously. We used a 2200 dsec q that was 0.003 higher but<br />
obtained a less thermal spectrum because <strong>of</strong> our higher fissile concentration.<br />
However, the previous calculations used only a single thermal<br />
F<br />
,-