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Dmytry
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well ok then I am rather surprised how badly written is the software in question must have been. I am a software developer. This kinda glitch you'd usually test for.PietKuip said:I gave my name, and a link to my work pages. Teaching gamma spectrometry to physics students is one of the things I do. I know a bit about the errors that can be made.
http://www.tepco.co.jp/en/press/corp-com/release/11042008-e.html confirms what I said about the database. Their software came with a nuclide library. Short-lived Te-129 had not been listed there as a daughter nuclide of the metastable isomer.
In the re-evalution of their spectra, they looked for the main peaks of Cl-38, and did not see any. See http://www.tepco.co.jp/en/press/corp-com/release/betu11_e/images/110420e11.pdf for the reasons for change.
Don't you have to also print out the error range btw? Or the software is so crap it won't give margin of error? When i was studying we had to propagate errors through calculations.
edit: wait, its weird, the data you linked. Note the La-140 at 3.0E2 . They don't think La-140 was a fluke, even though they re-evaluated it, while they do think that Cl-38 was a fluke. even though with compensation for 10 half lifes, Cl-38 must have been at 1.5 E3 which is 5x more than La-140 . I don't know if for some reason one is entirely different part of spectrum from another though.
edit: nope. According to wolframalpha, Cl-38 decays by 4.9MeV beta, while La-140 decays by 3.76 MeV beta. Why is Cl-38 below threshold and La-140 is not?
Also, speaking of criticality detection. They should of simply checked for cs-136 vs cs-137 ratio in SFP4 water, then we could of known for sure if SFP4 was critical or not.
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