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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.
G. Le Coq, J. Lewi, P. Raymond
Nuclear Science and Engineering | Volume 81 | Number 1 | May 1982 | Pages 1-8
Technical Paper | doi.org/10.13182/NSE82-A19590
Articles are hosted by Taylor and Francis Online.
The use of the one-dimensional two-phase flow six-equation model requires knowledge of mass, momentum, and energy transfers between the phases. These transfers can be expressed from the flow parameters and their derivatives. The first part of this paper is devoted to the formulation of the entropy production at the interface as a function of the velocity, Gibbs potential and temperature of each phase. It is assumed that each transfer can be expressed in the form where R is the reversible part and δR the irreversible part of the transfer R. The linear theory of irreversible thermodynamics allows the formulation of δR. The expression of R may include differential terms. In the second part of this paper, we show how to write interfacial transfer terms to reduce the six-equation model into a lower order model. The last part of this paper presents an original method for computing critical flow, taking into account the flow blockage phenomenon, which is observed when variations of downstream conditions do not produce any significant effect on the upstream flow, even though the fluid velocity is less than the sound velocity.