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Colin Judge: Testing structural materials in Idaho’s newest hot cell facility
Idaho National Laboratory’s newest facility—the Sample Preparation Laboratory (SPL)—sits across the road from the Hot Fuel Examination Facility (HFEF), which started operating in 1975. SPL will host the first new hot cells at INL’s Materials and Fuels Complex (MFC) in 50 years, giving INL researchers and partners new flexibility to test the structural properties of irradiated materials fresh from the Advanced Test Reactor (ATR) or from a partner’s facility.
Materials meant to withstand extreme conditions in fission or fusion power plants must be tested under similar conditions and pushed past their breaking points so performance and limitations can be understood and improved. Once irradiated, materials samples can be cut down to size in SPL and packaged for testing in other facilities at INL or other national laboratories, commercial labs, or universities. But they can also be subjected to extreme thermal or corrosive conditions and mechanical testing right in SPL, explains Colin Judge, who, as INL’s division director for nuclear materials performance, oversees SPL and other facilities at the MFC.
SPL won’t go “hot” until January 2026, but Judge spoke with NN staff writer Susan Gallier about its capabilities as his team was moving instruments into the new facility.
N. Baglan, G. Alanic
Fusion Science and Technology | Volume 60 | Number 3 | October 2011 | Pages 948-951
Measurement, Monitoring, and Accountancy | Proceedings of the Ninth International Conference on Tritium Science and Technology | doi.org/10.13182/FST11-A12572
Articles are hosted by Taylor and Francis Online.
Tritium exists in environmental samples as: (i) Tissue Free Water Tritium (TFWT) and associated with the organic matter (OBT) under two forms; (ii) bound to oxygen and nitrogen atoms into the material (E-OBT); (iii) bound to carbon atoms into the material (NE-OBT). The analysis of the NE-OBT fraction requires the elimination of E-OBT prior measurement. This operation is generally performed through labile exchange supposing that only isotopic exchange occurs. Most of the time, the recovered exchange water are coloured indicating that other mechanisms arise.To identify and to understand these mechanisms, the combination of two analytical tools, a CHNS-O elemental analyser and a spectrophotometer was used. NE-OBT analyses are performed on numerous environmental samples. In this work aliquots of those samples, under their solid form, were taken before and after labile exchange for elemental analysis purposes. In the same time the exchange waters were stored until spectrophotometric measurements. Solid analysis show that an evolution of the elemental composition could occur during the labile exchange with potential analytical impact. Moreover, it gives first ideas on which molecule could be solubilised. This trend is confirmed through spectrophotometric analysis where bands are observed for wavelength characteristics of proteins, amino acids, nucleic acids. Those preliminary results obtained using both techniques are promising but needs confirmation in the near future to determine to which extent an analytical impact could occur and to complete the identification of soluble molecules.