Systematic studies of SiGe ∕ Si islands nucleated via separate in situ or ex situ Ga + focused ion beam-guided growth techniques
In this study, we use 25 keV in situ and 30 keV ex situ Ga + focused ion beams (FIBs) to locally modify the substrate before deposition and determine their effects on nucleation of molecular beam epitaxy grown Ge ∕ Si islands. FIB processing may alter island formation in at least five ways: the surf...
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Veröffentlicht in: | Journal of Vacuum Science and Technology. A, International Journal Devoted to Vacuum, Surfaces, and Films International Journal Devoted to Vacuum, Surfaces, and Films, 2006-03, Vol.24 (2), p.375-381 |
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Zusammenfassung: | In this study, we use 25 keV in situ and 30 keV ex situ
Ga
+
focused ion beams (FIBs) to locally modify the substrate before deposition and determine their effects on nucleation of molecular beam epitaxy grown
Ge
∕
Si
islands. FIB processing may alter island formation in at least five ways: the surfactant effect of
Ga
+
, doping effects of subsurface
Ga
+
, local strains, crystalline damage, and surface roughening. To explore these possibilities, we milled square regions of increasing
Ga
+
doses and used atomic force microscopy to monitor islanding in and around these regions. For in situ experiments, doses ranged from
∼
10
13
to
5
×
10
17
ions
∕
cm
2
(0.04–400 ML). We began to observe changes in island topology at doses as low as
∼
10
14
ions
∕
cm
2
. For doses of
∼
10
15
to
∼
8
×
10
16
ions
∕
cm
2
(2–160 ML), implanted areas were surrounded by denuded zones that grew from
∼
0.5
to
6
μ
m
with increasing dose. Immediately inside the implanted area, island size and concentration appeared to peak. At doses above
∼
6
×
10
16
ions
∕
cm
2
(120 ML),
Ga
+
produced noticeable surface depressions, which were often surrounded by enhanced island densities, rather than a denuded zone. For ex situ FIB patterning, samples underwent both pregrowth cleaning and growth of a thin capping layer (0–100 nm). Doses ranging from
7.5
×
10
13
to
∼
10
17
ions
∕
cm
2
(0.15–200 ML) were used in concert with varied capping layer thicknesses to study their combined affect on island nucleation. The results correspond well with in situ experiments for thin capping layers. Increased capping layer thickness resulted in muted modifications to island formation for low
Ga
+
doses, while for higher doses trends similar to those obtained in situ are seen. |
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ISSN: | 0734-2101 1553-1813 1520-8559 |
DOI: | 10.1116/1.2172952 |