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DOE, General Matter team up for new fuel mission at Hanford
The Department of Energy's Office of Environmental Management (EM) on Tuesday announced a partnership with California-based nuclear fuel company General Matter for the potential use of the long-idle Fuels and Materials Examination Facility (FMEF) at the Hanford Site in Washington state.
According to the announcement, the DOE and General Matter have signed a lease to explore the FMEF's potential to be used for advanced nuclear fuel cycle technologies and materials, in part to help satisfy the predicted future requirements of artificial intelligence.
J. K. Dickens, F. G. Perey
Nuclear Science and Engineering | Volume 36 | Number 3 | June 1969 | Pages 280-290
Technical Paper | doi.org/10.13182/NSE69-A18725
Articles are hosted by Taylor and Francis Online.
We have obtained gamma-ray spectra for the reactions 14N(n, n′γ)14N, 14N(n,þγ)14C, and 14N(n, αγ)11B for incident mean neutron energies En = 5.8, 6.4, 6.8, 7.4, 8.0, and 8.6 MeV. The gamma rays were detected using a coaxial Ge(Li) detector of 30 cm3 active volume. The detector was placed at 55 and 90° with respect to the incident neutron direction, and was 77 cm from the sample; time-of-flight was used with the gamma-ray detector to discriminate against pulses due to neutrons and background gamma radiation. The sample was 100 g of Be3N2 in the form of a right circular cylinder. Data were also obtained using a 75-g Be sample to provide an estimate of the background. The incident neutron beam was produced by bombarding a deuterium-filled gas cell with the pulsed deuteron beam of appropriate energy from the ORNL 6-MV Van de Graaff. The resulting neutron beam was monitored using a scintillation counter; a time-of-flight spectrum from this detector was recorded simultaneously with the gamma-ray data. These data have been studied to obtain absolute cross sections for production of gamma rays from 14N for the incident neutron energies quoted above. The cross sections have been compared, where possible, with previously measured values with good agreement. However, there are several important differences with previous data and these are discussed. In particular, summing the partial cross sections yields a value for the total nonelastic cross section that is approximately half of the total nonelastic cross section obtained from the difference between the total cross section and the total elastic cross section.