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Nuclear Energy Conference & Expo (NECX)
September 8–11, 2025
Atlanta, GA|Atlanta Marriott Marquis
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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.
J.P. Qian, Z.Y. Xu, X. Liu, Z.X. Xiao, J.B. Cheng, C.J. Pan, L.H. Sun
Fusion Science and Technology | Volume 19 | Number 3 | May 1991 | Pages 1814-1818
Impurity Control and Plasma-Facing Component | Proceedings of the Ninth Topical Meeting on the Technology of Fusion Energy (Oak Brook, Illinois, October 7-11, 1990) | doi.org/10.13182/FST91-A29607
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Physical sputtering of Mo bombarded by Ar+, blistering and flaking of Mo implanted by He+ ions are described in the present paper. The sputtering yield of Mo was approximately constant in the energy range of 10–20 Kev while the sputtering yield vs. incident angle rose with increasing incident angle in the experiment. Blistering and flaking was observed in the ion fluence range of 7 × 1017 — 1 × 1019 ions/cm2 but only surface protrusions become important when the ion incident angle was near 60°. It means that the sputtering became the dominant process comparing with blistering in this case. The “trackrace effect” of blistering has been found at room temperature and even inside the ion beam spot.