Atmospheric Pressure Spatial Atomic Layer Deposition of Silicon Oxide Using DIPAS and Ozone

dc.contributor.authorDurgamahanti, Poojitha
dc.contributor.authorSaha, Soumyadeep
dc.contributor.authorDelumeau, Louis-Vincent
dc.contributor.authorGrovu, Tristan
dc.contributor.authorWheaton, Craig A.
dc.contributor.authorSamedov, Kerim
dc.contributor.authorMusselman, Kevin P.
dc.date.accessioned2025-02-26T18:09:10Z
dc.date.available2025-02-26T18:09:10Z
dc.date.issued2025
dc.descriptionThis document is the Accepted Manuscript version of a Published Work that appeared in final form in Journal of Physical Chemistry C, copyright © American Chemical Society after peer review and technical editing by publisher. To access the final edited and published work see https://doi.org/10.1021/acs.jpcc.4c08359.
dc.description.abstractSilicon oxide (SiOx) is a highly versatile material used in different applications. However, its conventional growth and deposition methods often require very high temperature or the use of plasma. In this work, we present a plasma-free, low-temperature process for depositing high-quality SiOx thin films using atmospheric-pressure spatial atomic layer deposition (AP-SALD). An aminodisilane precursor, diisopropylaminosilane (SiH3N(C3H7)2, DIPAS), was synthesized and tested with different oxidants such as ozone and 30% hydrogen peroxide aqueous solution. Initial attempts with hydrogen peroxide solution resulted in precursor condensation and the formation of nano crystallite SiOx contaminated with organic molecules, indicating that the deposition process is oxidant limited. In contrast, using ozone as the oxidant facilitated the deposition of high-quality amorphous SiOx films. The microstructure was highly dependent on the deposition temperature, transitioning from nano crystallites at lower temperatures to amorphous films at temperatures of 70°C to 100°C. X-ray photoelectron spectroscopy (XPS) confirmed the deposition of SiOx films at 70°C or above using ozone, and the growth per cycle was ~1 Å/cycle, consistent with ALD of SiOx. This work shows that high-quality SiOx films can be produced by AP-SALD using DIPAS and ozone, without the aid of plasma or any surface functionalization, at low growth temperatures (T >= 70°C).
dc.description.sponsorshipNSERC I2I program (#I2IPJ #570986-22) || Waterloo Institute for Nanotechnology (WIN) Nanofellowship || CFREF-TQT || CFI || ISED || Ontario Ministry of Research & Innovation || Mike & Ophelia Lazaridis.
dc.identifier.urihttps://doi.org/10.1021/acs.jpcc.4c08359
dc.identifier.urihttps://hdl.handle.net/10012/21490
dc.language.isoen
dc.publisherAmerican Chemical Society
dc.relation.ispartofseriesJournal of Physical Chemistry C; 129(6)
dc.subjectatmospheric-pressure spatial atomic layer deposition
dc.subjectsilicon oxide
dc.subjectozone
dc.subjectDIPAS
dc.subjectthin films
dc.titleAtmospheric Pressure Spatial Atomic Layer Deposition of Silicon Oxide Using DIPAS and Ozone
dc.typeArticle
dcterms.bibliographicCitationDurgamahanti, P., Saha, S., Delumeau, L.-V., Grovu, T., Wheaton, C. A., Samedov, K., & Musselman, K. P. (2025). Atmospheric pressure spatial atomic layer deposition of silicon oxide using DIPAS and ozone. The Journal of Physical Chemistry C, 129(6), 3328–3335. https://doi.org/10.1021/acs.jpcc.4c08359
uws.contributor.affiliation1Faculty of Engineering
uws.contributor.affiliation2Mechanical and Mechatronics Engineering
uws.peerReviewStatusReviewed
uws.scholarLevelFaculty
uws.typeOfResourceTexten

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