Formation and stabilization of pyramidal etch hillocks on silicon {100} inanisotropic etchants: Experiments and Monte Carlo simulation

Citation
Aj. Nijdam et al., Formation and stabilization of pyramidal etch hillocks on silicon {100} inanisotropic etchants: Experiments and Monte Carlo simulation, J APPL PHYS, 89(7), 2001, pp. 4113-4123
Citations number
52
Categorie Soggetti
Apllied Physucs/Condensed Matter/Materiales Science
Journal title
JOURNAL OF APPLIED PHYSICS
ISSN journal
00218979 → ACNP
Volume
89
Issue
7
Year of publication
2001
Pages
4113 - 4123
Database
ISI
SICI code
0021-8979(20010407)89:7<4113:FASOPE>2.0.ZU;2-F
Abstract
On Si{100} surfaces etched in anisotropic etchants such as aqueous solution s KOH and TMAH, pyramidal etch hillocks are frequently found. Besides these hillocks, we have investigated hillocks that have partially disappeared us ing scanning electron microscopy (SEM). During re-etching numerous addition al pyramidal etch hillocks are formed on the exact spots where SEM pictures were made earlier. These observations suggest that semipermeable particles adhering to the surface are responsible for the development of the pyramid al etch hillocks. In order to investigate the influence of such nanometer s cale particles on the etch rate and the surface morphology, Monte Carlo sim ulations were performed of etching of Si{100} surfaces on which small semim asks are present. The presence of the microscopic semimasks is shown to cau se the formation of macroscopic hillocks, which closely resemble experiment ally observed hillocks. Removal of the semimask on top of a hillock leads t o a vanishing pyramidal etch hillock. In the Monte Carlo model, however, th e etch rate as a function of surface orientation has a maximum for {100}, w hile in reality {100} corresponds to a local minimum. This implies that for typical experimental conditions an etch hillock should not be stable despi te a semipermeable particle on top, because of underetching starting from < 110 > ridges of the hillock. This paradox can be resolved by assuming that the ridges act as sinks of tiny particles. This gives a reduction in etch rate of the ridges, next to the top, which is necessary for the hillock to remain stable. The exact nature of these masking particles is unknown, but silicate particles are a likely candidate. (C) 2001 American Institute of P hysics.