- #10,956
etudiant
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rmattila said:It is very difficult to make any conclusions on the I-131 concentrations detected in different places, since the chemistry of iodine in the aqueous solutions found in different places of the Fukushima Dai-ichi complex is somewhat complicated. The pH of the containment water is affected by the materials from the instrumentation cables and the boric acid added to the injected water at at least some occasions, and then there's the salt etc.
It looks strange to see the levels of iodine with respect to Cs dropping slower than their decay ratio would suggest, but Cs tends to stick to surfaces, and there can well be chemical mechanisms that contribute to iodine migrating more rapidly. There's still plenty of I-131 left 5 months after the scram, even though it has halved every 8 days.
If you want to find signs of criticality, I think you would be better off finding anomalies in the ratios of short-to long lived nuclides of the same element (I, Cs) to be able to eliminate the effect of the chemical complications. However, it seems that the concentration of most radioactive isotopes is below the limit TEPCO is capable of detecting.
Hi rmattila,
Thank you for your cogent and insightful comments.
Between the minimalist disclosures from TEPCO and the 'sky is falling' summaries from eNews, you provide a refreshing and factual input. Would that many others would learn from your example.
Please keep participating.