Formation and stability of the prismatic stacking fault in wurtzite (Al,Ga,In) nitrides
Creators
Description
The formation of the {1bar 210} stacking fault, which has two atomic configurations in Wurtzite (Ga,Al,In)N, has been investigated by high resolution electron microscopy and energetic calculations. It originates from steps at the SiC surface and it can form on a flat (0001) sapphire surface. A modified Stillinger-Weber potential was used in order to investigate the relative stability of the two atomic configurations. They have comparable energy in AlN, whereas the 1/2<10bar 11>{1bar 210} configuration is more stable in GaN and InN. In GaN layers, only the 1/2<10bar 11>{1bar 210} configuration was observed. The 1/6<20bar 23> configuration was found in small areas inside the AlN buffer layer where it folded rapidly to the basal plane, and when back into the prismatic plane, it took the 1/2<10bar 11>{1bar 210} atomic configuration
Additional details
Publishing Information
- Publisher
- Materials Research Society
- Imprint Place
- Warrendale, PA (United States)
- ISBN
- 1-55899-503-X
- Imprint Title
- GaN and related alloys -- 1999. Materials Research Society symposium proceedings, Volume 595
- Imprint Pagination
- [1050 p.]
- Journal Page Range
- p. W3.55.1-W3.55.6
- ISSN
- 0272-9172
Conference
- Title
- 1999 Materials Research Society Fall Meeting
- Dates
- 28 Nov - 3 Dec 1999
- Place
- Boston, MA (United States)
INIS
- Country of Publication
- United States
- Country of Input or Organization
- United States
- INIS RN
- 31056548
- Subject category
- S36: MATERIALS SCIENCE;
- Resource subtype / Literary indicator
- Conference
- Descriptors DEI
- ALUMINIUM NITRIDES; ATOMIC MODELS; CRYSTAL DEFECTS; ELECTRON MICROSCOPY; GALLIUM NITRIDES; INDIUM NITRIDES; SAPPHIRE; SILICON CARBIDES; SUBSTRATES
- Descriptors DEC
- ALUMINIUM COMPOUNDS; CARBIDES; CARBON COMPOUNDS; CORUNDUM; CRYSTAL STRUCTURE; GALLIUM COMPOUNDS; INDIUM COMPOUNDS; MATHEMATICAL MODELS; MICROSCOPY; MINERALS; NITRIDES; NITROGEN COMPOUNDS; OXIDE MINERALS; PNICTIDES; SILICON COMPOUNDS