Hostname: page-component-8448b6f56d-tj2md Total loading time: 0 Render date: 2024-04-24T06:56:52.162Z Has data issue: false hasContentIssue false

Increased Ordering in the Amorphous SiOx due to Hyperthermal Atomic Oxygen.

Published online by Cambridge University Press:  01 February 2011

Maja Kisa
Affiliation:
Materials Science and Engineering Department, 848 Benedum Hall, University of Pittsburgh, Pittsburgh, PA 15261, USA
William G. Stratton
Affiliation:
Materials Science and Engineering Department, University of Wisconsin-Madison, 1509, University Avenue, Madison, WI 53706–1595, USA
Timothy K. Minton
Affiliation:
Department of Chemistry and Biochemistry, 108 Gaines Hall, Montana State University, Bozeman, MT 59717, USA
Klaus van Benthem
Affiliation:
Condensed Matter Science Division, Oak Ridge National Laboratory, 1 Bethel Valley Road, Oak Ridge, TN 37831
Steve J. Pennycook
Affiliation:
Condensed Matter Science Division, Oak Ridge National Laboratory, 1 Bethel Valley Road, Oak Ridge, TN 37831
Paul M. Voyles
Affiliation:
Materials Science and Engineering Department, University of Wisconsin-Madison, 1509, University Avenue, Madison, WI 53706–1595, USA
Xidong Chen
Affiliation:
Department of Science and Mathematics, Cedarville University, 251 N Main St., Cedarville, OH 45314
Long Li
Affiliation:
Materials Science Division, Argonne National Laboratory, 9700 Cass Ave, Argonne, IL 60439
Judith C. Yang
Affiliation:
Materials Science Division, Argonne National Laboratory, 9700 Cass Ave, Argonne, IL 60439
Get access

Abstract

We had studied the effects of hyperthermal (5.1eV) atomic oxygen (AO) on the structural characteristics of the silica layer and Si/SiOx interface formed by the oxidation of Si-single crystal by a variety of microcharacterization techniques. A laser detonation source was used to produce atomic oxygen with 5.1eV kinetic energy. High Resolution Transmission Electron Microscopy (HRTEM) and Selected Area Electron Diffraction (SAED) demonstrated that the silica layer formed on Si(100) by atomic oxygen is thicker, more homogeneous, and less amorphous, compared to the oxide layer created by molecular oxygen (MO). High spatial resolution Electron Energy Loss Spectroscopy (EELS) study confirmed that the Si/SiOx interface created by atomic oxygen is abrupt containing no suboxides as opposed to the broad interface with transitional states formed by molecular oxygen. SAED technique was used to observe sharper diffraction rings present in the diffraction pattern of Si(100) oxidized by reactive atomic oxygen as opposed to the diffused haloes present in the diffraction pattern of Si(100) oxidized by molecular oxygen. Radial Distribution Function (RDF) analyses were performed on the SAED patterns of Si(100) oxidized in atomic and molecular oxygen, indicating that a more ordered oxide is formed by atomic oxygen. Initial Fluctuation Electron Microscopy (FEM) results confirmed an increased medium range ordering in SiOx formed by atomic oxygen when compared to the non-regular arrangement present in the amorphous oxide formed by the oxidation of Si(100) in molecular oxygen.

Type
Research Article
Copyright
Copyright © Materials Research Society 2005

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

REFERENCES

1. Minton, T. K. and Garton, D. J., Chemical Dynamics in Extreme Environments: Advanced Series in Physical Chemistry – Vol. 11, Edited by Dressler, R. (World Scientific, Singapore, 2001), 420489.Google Scholar
2. Chambers, A.R., Harris, I.L. and Roberts, G.T., Materials Letters 26, 121131 (1996).Google Scholar
3. Banks, B., Rutledge, S. and Auer, B., 119th TMS Annual Meeting and Exhibit, Anaheim, February 18–22 (1990).Google Scholar
4. Banks, B., Rutledge, S., de Groh, K. and Auer, B., NATO advanced study institute conference Pitlochry, Scotland, July 7–19 (1991).Google Scholar
5. Randjelovic, M. and Yang, J. C., Materials at High Temperatures, 20(3), 281285 (2003).Google Scholar
6. Caledonia, G.E., Krech, R.H. and Green, B.D., AIAA J, 25, 5963 (1987).Google Scholar
7. Oakes, D.B., Krech, R.H., Upschuete, B.L. and Caledonia, G.E., J. Appl. Phys. 77, 21662172 (1995).Google Scholar
8. Treacy, M.M.J. and Gibson, J.M., Acta Cryst. A, 52(2): 212220. (1996).Google Scholar
9. Kisa, M., Minton, T. K., and Yang, J. C., J. Appl. Phys., accepted to be published in January 2005.Google Scholar
10. Kisa, M., Twesten, R. D. and Yang, J. C., Mat. Res. Symp. Proc. 786, 267272 (2004).Google Scholar
11. Garvie, L.A.J. and Buseck, P.R., American Mineralogist, 84, 946964, (1999).Google Scholar
12. PCPDF filesGoogle Scholar
13. Tagawa, M., Ema, T., Kinoshita, H., Ohmae, N., Umeno, M., and Minton, T. K., Jpn. J. Appl. Phys. 37, L1455-L1457 (1998).Google Scholar
14. Elliot, S. R.Physics of Amorphous Materials”, Longman (1983).Google Scholar
15. Voyles, P.M., Gibson, J.M., and Treacy, M.M.J., J. Electron Microsc. 49, 259266. (2000).Google Scholar
16. Voyles, P.M. and Abelson, J.R., National Renewable Energy Laboratory- Final Report, October 2003.Google Scholar
17. Tagawa, M., Yokota, K., Ohmae, N. and Kinoshita, H., High Perform. Polym. 12, 5363 (2000).Google Scholar
18. Tagawa, M., Yokota, K., Ohmae, N., Kinoshita, H. and Umeno, M., Jpn. J. Appl. Phys, 40, 61526156 (2001).Google Scholar
19. Engstrom, J.R., Nelson, M.M. and Engel, T., J. Vac. Sci. Technol. A7(3), 18371840 (1989).Google Scholar
20. Engstrom, J.R. and Engel, T., Phys. Rev. B, 41(2), 10381042 (1990).Google Scholar
21. Irene, E., Appl. Phys. Lett. 51(10), 767769 (1987).Google Scholar
22. Ichimura, S., Kurokawa, A., Nakamura, K., Itoh, H., Nonaka, H. and Koike, K., Thin Solid Films, 377–378, 518524 (2000).Google Scholar
23. Itoh, H., Nakamura, K., Kurokawa, A. and Ichimura, S., Surface Science, 482–485, 114120 (2001).Google Scholar
24. Watanabe, H., Kato, K., Uda, T., Fujita, K. and Ichikawa, M., Phys. Rev. Lett, 80, 345 (1998).Google Scholar
25. Kuznetsova, A., Zhou, G., Chen, X., Yang, J., and Yates, J. T. Jr, Langmuir 17, 2146 (2001).Google Scholar