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14 декабря, 2021
With respect to the transmutation of FPs, much less work has been performed in the last decades. In part this is because, compared to the transuranics, their radiotoxicity is lower and shorter lived so that, after about 250 years, most of them have decayed. Nevertheless, some FPs are very long lived and may be mobile in the environment so that, often, they are major contributors to the very long-term radiological impact of deep geological disposal. The long-lived FPs (LLFPs) that deserve most attention in this respect are 2 29I, 135Cs, 79Se, 99Tc and 126Sn (see Table 17.5).
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512 Nuclear fuel cycle science and engineering Table 17.5 Properties of the main long-lived FPs (LLFPs)
Isotope Half-life Type of Thermal Dose Fraction in (y) decay power (ingestion) irradiated fuel (W/Bq) (Sv/Bq) (g/t)*
Note: *PWR-UOX (3.5% U-235 enrichment, BU = 33 GWd/t) |
Unlike transuranics, FP transmutation does not produce supplementary neutrons as fission products are neutron consumers. LLFP transmutation therefore requires a large neutron surplus to be available. If this is expressed in terms of the fraction of a reactor fleet that would be needed to perform the LLFP transmutation, the value comes out at between 8 and 15%,23 i. e., a very large (and, very probably, unrealistic) figure.
Finally, it should be emphasized that the short-term heat production is essentially related to 90Sr and 1 37Cs, which are not candidates for transmutation because their relatively short half-life (~30 years) is such that no transmutation process can provide a comparable ‘transmutation half-life’, (evaluated as the product of the microscopic capture cross section of the isotope considered times the neutron flux). One way to handle these two isotopes could be to recover them with an appropriate chemical process, then store them and let them decay.
In summary, the transmutation of the so-called LLFPs is no longer envisioned by any major international program.