The relationship between gross and net erosion of beryllium at elevated temperature

Abstract Surface temperature is a critical variable governing plasma–material interactions. PISCES-B injects controllable amounts of Be impurities into the plasma to balance, or exceed, the erosion rate of beryllium from samples in un-seeded plasma exposures. At low temperature, an order of magnitude more beryllium, than the beryllium mass loss measured in un-seeded discharges, needs to be seeded into the plasma to achieve no mass loss from a sample. At elevated temperature, no mass loss is achieved when the beryllium-seeding rate equals the mass loss rate in un-seeded discharges. Molecular dynamics simulations show that below 500 K, Be adatoms have difficulty surmounting the Ehrlich–Schwoebel barrier at the edge of a terrace. Above this temperature, an Arrhenius behavior is observed with an activation energy of 0.32 eV. Qualitatively, this indicates that at low surface temperature the deposited atoms may be more easily re-eroded, accounting for the increased seeding needed to balance the erosion.