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1 - IAEA Nuclear Data Services

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- 153 -<br />

homogeneity of the layers. Satisfactory results<br />

(probably accurate within 0.3%) are found for the<br />

comparison of direct weighing in vacuum and relative<br />

neutron measurements for layer thicknesses between<br />

2<br />

about 20 and 80 v-g/cm . These layers will be used<br />

as standards for fission cross-section measurements.<br />

Intercomparison of Fissile Layers<br />

The same equipment as used for the boron comparisons<br />

is used for the intercomparison of fissile layers.<br />

In this case the fission- and a-particle pulse-height<br />

spectra are recorded with beam-on and beam-off. The<br />

fission- and a-counting rates are deduced respectively<br />

per monitor count and per unit-time. The ratios of aand<br />

fission counting-rates can be compared. With nonhomogeneous<br />

sources they may differ.<br />

Measurements were performed on electro-sprayed uranylacetate<br />

sources and evaporated UF¿,-layers made from<br />

NBS-930 ^U-material and agreement was found within<br />

statistical errors proving their good homogeneity.<br />

Another method to compare the quality of the foils<br />

from different preparation methods is to compare the<br />

fission spectrum characteristics of foils with the<br />

same thickness in the same geometry. A particularly<br />

sensitive parameter, e.g., is the ratio Nj- / N-y of<br />

the light fragment peak counting-rate to the valley<br />

counting-rate. From these spectra also the low energy<br />

tailing can be evaluated and possible multiplication<br />

effects (at the high energy-side of the spectrum) of<br />

the surface-barrier detector used can be detected.<br />

They also enabled us to determine the limit thickness<br />

of applicability of the preparation methods to be more<br />

2<br />

than 500 ug/cm for electrosprayed and probably more<br />

than 1 mg/cm<br />

2<br />

for evaporated sources.<br />

2200 m/s Fission Cross-Sections<br />

The boron standard foils and the evaporated ^UF.-

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