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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.
John Mandrekas, W. M. Stacey, Jr.
Fusion Science and Technology | Volume 19 | Number 1 | January 1991 | Pages 57-77
Technical Paper | Plasma Engineering | doi.org/10.13182/FST91-A29316
Articles are hosted by Taylor and Francis Online.
A zero-dimensional, time-dependent, particle and power balance code was developed and used to evaluate the effectiveness of different burn control methods for the stabilization of unstable ignited and subignited operating points of the International Thermonuclear Experimental Reactor (ITER) physics phase machine. Based on the results of our calculations, we conclude that the operation of ITER at thermally unstable operating points is physically and technologically feasible. Control with auxiliary power modulation seems to be the method of choice for the control of subignited unstable points, while other methods such as modulation of the fueling rate and high-Z impurity injection can also be used, especially for the control of unstable ignited points where auxiliary power modulation cannot be used.