The interaction of thermal neutrons with
p>235p>U results in fission with a
probability of
![](htt<font color=)
p://www.sciencedirect.com/scidirimg/entities/223c.gif" alt="not, vert, similar" title="not, vert, similar" border="0">85%and in the formation of
p>236p>U (
t1/2 = 2.3 × 10
p>7p> yr) with a
probability of
![](htt<font color=)
p://www.sciencedirect.com/scidirimg/entities/223c.gif" alt="not, vert, similar" title="not, vert, similar" border="0">15%. While anthro
pogenic
p>236p>U is, therefore,
present in s
pent nuclear fuel at levels of
p>236p>U/U u
p to 10
p>−2p>, the ex
pected natural ratios in the
pre-anthro
pogenic environment range from 10
p>−14p> to 10
p>−10p>. At VERA, systematic investigations suggest a detection limit below
p>236p>U/U = 5 × 10
p>−12p> for sam
ples of 0.5 mg U, while chemistry blanks of
![](htt<font color=)
p://www.sciencedirect.com/scidirimg/entities/223c.gif" alt="not, vert, similar" title="not, vert, similar" border="0">2 × 10
p>7p> atoms
p>236p>U
per sam
ple limit the sensitivity for smaller sam
ples. We have found natural isoto
pic ratios in uranium reagents se
parated before the onset of human nuclear activities, in uranium ores from various origins and in water from a subsurface well in Bad Gastein, Austria. Anthro
pogenic contamination was clearly visible in soil and rivulet sam
ples from Salzburg, Austria, whereas river sediments from Garigliano river (Southern Italy) were close to the detection limit. Finally, our natural in-house standard Vienna-KkU was calibrated against a certified reference material (IRMM REIMEP-18 A).