Deposition of silicon dioxide films using an atmospheric pressure microplasma jet
- Research Group Reactive Plasmas, Ruhr-Universitaet Bochum, 44780 Bochum (Germany)
Organic and inorganic silicon dioxide films have been deposited by means of an atmospheric pressure microplasma jet. Tetramethylsilane (TMS), oxygen, and hexamethyldisiloxane (HMDSO) are injected into argon as plasma forming gases. In the case of TMS injection, inorganic films are deposited if an admixture of oxygen is used. In the case of HMDSO injection, inorganic films can be deposited at room temperature even without any oxygen admixture: at low HMDSO flow rates [<0.1 SCCM (SCCM denotes cubic centimeters per minute at STP),<32 ppm], the SiO{sub x}H{sub z} films contain no carbon and exhibit oxygen-to-silicon ratio close to 2 according to x-ray photoelectron spectroscopy. At high HMDSO flow rates (>0.1 SCCM,>32 ppm), SiO{sub x}C{sub y}H{sub z} with up to 21% of carbon are obtained. The transition from organic to inorganic film is confirmed by Fourier transform infrared spectroscopy. The deposition of inorganic SiO{sub 2} films from HMDSO without any oxygen admixture is explained by an ion-induced polymerization scheme of HMDSO.
- OSTI ID:
- 21356099
- Journal Information:
- Journal of Applied Physics, Vol. 105, Issue 8; Other Information: DOI: 10.1063/1.3108541; (c) 2009 American Institute of Physics; ISSN 0021-8979
- Country of Publication:
- United States
- Language:
- English
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Related Subjects
ARGON
ATMOSPHERIC PRESSURE
CARBON
DEPOSITION
FLOW RATE
FOURIER TRANSFORM SPECTROMETERS
FOURIER TRANSFORMATION
INFRARED SPECTRA
ORGANIC SILICON COMPOUNDS
OXYGEN
PLASMA JETS
POLYMERIZATION
SILICON
SILICON OXIDES
TEMPERATURE RANGE 0273-0400 K
THIN FILMS
X-RAY PHOTOELECTRON SPECTROSCOPY
CHALCOGENIDES
CHEMICAL REACTIONS
ELECTRON SPECTROSCOPY
ELEMENTS
FILMS
FLUIDS
GASES
INTEGRAL TRANSFORMATIONS
MEASURING INSTRUMENTS
NONMETALS
ORGANIC COMPOUNDS
OXIDES
OXYGEN COMPOUNDS
PHOTOELECTRON SPECTROSCOPY
RARE GASES
SEMIMETALS
SILICON COMPOUNDS
SPECTRA
SPECTROMETERS
SPECTROSCOPY
TEMPERATURE RANGE
TRANSFORMATIONS