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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.
J. Abrefah, H. F. G. De Abreu, F. Tehranian, Y. S. Kim, D. R. Olander
Nuclear Technology | Volume 105 | Number 2 | February 1994 | Pages 137-144
Technical Paper | Nuclear Reactor Safety | doi.org/10.13182/NT94-A34918
Articles are hosted by Taylor and Francis Online.
The kinetics of the reaction of molecular iodine with preoxidized Type 304 stainless steel was studied by mass spectrometric and gravimetric techniques. The temperature range was 438 to 803 K, and the iodine partial pressures in the 1-atm total pressure water vapor-hydrogen gas ranged from 1.33 to 133 Pa. Examination of the reacted surface by electronic spectroscopies showed localized attack in the form of highly fractured crystalline deposits that contained significant iodine concentrations. The mass spectrometric results revealed no HI in the gas despite favorable thermodynamics for formation of this species. The gravimetric results showed an initial rapid increase in weight followed by a slow, long-term weight change that did not appear to approach saturation. The saturation iodine concentration on the surface due to the initial deposition process was greatest at 573 K. The kinetics of the initial uptake was analyzed by a first-order kinetics model. The characteristic times of attainment of saturation were on the order of 1 h and showed a very small activation energy.