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2026 Nuclear Energy Conference & Expo (NECX)
August 24–27, 2026
Dallas, TX|Hilton Anatole
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Front-end nuclear fuel supply cooperation: Turning allied interdependence into strategic advantage
The global nuclear revival, which is fueled by unprecedented demand for firm, affordable, dispatchable power for artificial intelligence and data center build-out, energy security imperatives, and climate commitments, has exposed a structural reality of the Western fuel cycle: No single allied nation currently possesses the full suite of front-end capabilities. From mining through conversion, enrichment, fabrication, and the emerging deconversion and metallization steps required for reactor fuels, capability is distributed across Canada, France, Japan, the United Kingdom, and the United States (collectively, the “Sapporo Five”), as well as a small group of close partners.
David J. Diamond, Sidney Yip
Nuclear Science and Engineering | Volume 40 | Number 3 | June 1970 | Pages 460-471
Technical Paper | doi.org/10.13182/NSE70-A20197
Articles are hosted by Taylor and Francis Online.
Analysis of space- and time-dependent slowing down is carried out using diffusion, P1, and B1 approximations for hydrogen and nonhydrogenous moderators. The scattering cross section is assumed to be constant, but the cross section at source neutron energy is allowed to have a different value. The calculations are primarily concerned with the first and second time moments of the flux distribution (r, v, t). The results are used to interpret the spatial variation of slowing down times. The characteristic behavior in the case of water is shown to arise from the considerably longer mean-free-path at the source energy (MeV). Time moments are also used to show that the transport approximation in P1 and B1 calculations for hydrogen can lead to a nonphysical result. Given the time moments, a simple procedure is proposed for obtaining (r, v, t). This approximation is found to be quite accurate when tested using diffusion theory moments. Comparison of theory and experiment is discussed in terms of recent measurements and Monte Carlo studies on water. So far as agreement with the available data is concerned, time-dependent diffusion theory calculations are found to be quite adequate.