Abstract
Abstract The amounts of D on the graphite and beryllium divertor tiles used in JET campaigns during 1994–1995 have been measured and compared. Deposits primarily of carbon containing very high D concentrations were present in the cold shadowed areason both sets of tiles. Plasma-surface interactions involving chemical erosion of carbon and D diffusion into Be are evident.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
