Irradiation of Au and ph foils with Xe ions at temperatures between 30
and 450 K has been monitored using in situ transmission electron micr
oscopy. Single ion impacts give rise to surface craters on the irradia
ted surface with sizes as large as 12 nm. Approximately 2%-5% of impin
ging ions produce craters on Au while only about 0.6% produce craters
on Pb. Larger craters on Au frequently have expelled material associat
ed with them. Temporal details of crater formation and annihilation ha
s been recorded on video with a time-resolution of 33 ms. Craters anni
hilate in discrete steps due to subsequent ion impacts or anneal in a
continuous manner due to surface diffusion. Craters production (those
persisting for one or more video-frames) as a function of temperature
indicates that the surface diffusion process responsible for thermal a
nnealing of craters has an activation energy of 0.76 eV in Au. Crater
creation results from plastic flaw associated with near surface cascad
es. Crater annihilation in discrete steps results from plastic flow in
duced by subsequent ion impacts, including those that do not themselve
s produce a crater. Crown Copyright (C) 1998 Published by Elsevier Sci
ence S.A.