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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.
Rikard Malmbeck, Gunnar Skarnemark
Nuclear Technology | Volume 120 | Number 1 | October 1997 | Pages 48-56
Technical Paper | Material | doi.org/10.13182/NT97-A35430
Articles are hosted by Taylor and Francis Online.
Characterization of iodine on-line using mixersettlers has been performed in reactor water, reactor water cleanup (RWCU) effluent, and condensate at the three boiling water reactor (BWR) nuclear power plants (F1, F2, and F3) at Forsmark, Sweden. Characterization of reactor water iodine has also been performed following reactor shutdown at F3. The dominating species in reactor water and condensate was iodide; the rest being essentially iodate. In RWCU effluent, the major species was iodate. Iodine isotopic ratios showed that iodate was delayed when passing the RWCU system. Formation of organic iodides in the RWCU system was not significant. No changes in the iodine species composition in the reactor water could be observed directly following reactor shutdown; however, iodide was with time slowly converted to iodate by radiation-induced oxidation. In reactor water <1% and in condensate and RWCU effluent up to 3% of the total iodine existed in the organic form. Organic iodides in the condensate were older than other iodine species.