Lm. Yang et Wj. Weber, Transmission electron microscopy study of ion-beam-induced amorphization of Ca2La8(SiO4)(6)O-2, PHIL MAG A, 79(1), 1999, pp. 237-253
In-situ transmission electron microscopy (TEM) and high-resolution transmis
sion electron microscopy (HRTEM) were used to study ion-beam-induced amorph
ization of Ca2La8(SiO4)(6)O-2, a silicate ceramic with the apatite structur
e. In-situ TEM was performed during irradiation with 1 MeVAr+, 1.5 MeV Krand 1.5MeV Xe+ ions over the temperature range from 20 to 773 K to determin
e the ion dose required for complete amorphization of the crystal (critical
amorphization dose D-c). D-c increased with increasing irradiation tempera
ture and decreased with increasing ion mass. Samples irradiated with Ar+, K
r+ and Xe+ ions to various doses were used in a detailed HRTEM study of the
amorphization process. The residual irradiation damage after low ion doses
appeared as nanometre scale amorphous domains. The images of these domains
are extremely sensitive to the sample thickness. Small domains of subcasca
de size were found only at the very thin edge of the sample at lower doses.
In thicker regions, amorphous domains appear after higher doses as the res
ult of the subcascade overlap in projection. At higher temperatures. the ob
served amorphous domains are smaller indicating thermally activated epitaxi
al recovery at the amorphous-crystalline interface. The amorphous domains a
re larger in size after irradiation with ions of higher mass. The results a
re consistent with the D-c-temperature curves determined by in-sills TEM an
d suggest an amorphization mechanism through direct subcascade impact or su
bcascade overlapping. Growth of the surface amorphous layer with increasing
ion dose and the effects of electron beam on damage recovery were also not
ed. In addition; cross-sectional TEM, computer simulation of damage product
ion and digital image processing have also been performed to understand bet
ter the plan-view HRTEM observations.