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Nuclear Energy Conference & Expo (NECX)
September 8–11, 2025
Atlanta, GA|Atlanta Marriott Marquis
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Fusion Science and Technology
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Deep geologic repository progress—2025 Update
Editor's note: This article has was originally published in November 2023. It has been updated with new information as of June 2025.
Outside my office, there is a display case filled with rock samples from all over the world. It contains a disk of translucent, orange salt from the Waste Isolation Pilot Plant near Carlsbad, N.M.; a core of white-and-bronze gneiss from the site of the future deep geologic repository in Eurajoki, Finland; several angular chunks of fine-grained, gray claystone from the underground research laboratory at Bure, France; and a piece of coarse-grained granite from the underground research tunnel in Daejeon, South Korea.
P.O. Biney, S. Lomperski, M.L. Corradini
Fusion Science and Technology | Volume 19 | Number 3 | May 1991 | Pages 1355-1361
Result of Large Experiment and Plasma Engineering | doi.org/10.13182/FST91-A29531
Articles are hosted by Taylor and Francis Online.
A review and discussion of the conditions leading to liquid metal ignition including experimental determination of an ignition envelope for liquid lithium are presented. A simple lumped model is used to investigate the necessary conditions (liquid metal and water temperatures) for liquid metal ignition to be imminent. Both the experimental and model results indicate that as the liquid metal temperature is increased, the water temperature required for interaction to proceed to a vapor phase reaction decreases. A rate equation for the reaction of lithium-lead alloy (Li17Pb83) is determined using a mass transport reaction model. The results indicate that the reaction of this lithium-lead alloy with water can be represented by a parabolic rate law.
