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Analysis of the extended defects in 3C-SiC.pdf - Nelson Mandela ...

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7.1 Introduction<br />

69<br />

CHAPTER SEVEN<br />

RESULTS AND DISCUSSION<br />

The follow<strong>in</strong>g chapter conta<strong>in</strong>s <strong>the</strong> results obta<strong>in</strong>ed from a TEM <strong>in</strong>vestigation <strong>of</strong> <strong>the</strong><br />

as-grown and ion bombarded <strong>3C</strong>-<strong>SiC</strong>. The results <strong>of</strong> this <strong>in</strong>vestigation are also<br />

compared with f<strong>in</strong>d<strong>in</strong>gs <strong>of</strong> o<strong>the</strong>r researchers.<br />

7.2 Extended Defects <strong>in</strong> -<strong>SiC</strong> Grown by CDV on (001) Si<br />

A cross-sectional sample <strong>of</strong> <strong>3C</strong>-<strong>SiC</strong> grown on Si by CVD was prepared us<strong>in</strong>g <strong>the</strong><br />

technique described <strong>in</strong> Section 6.5. Follow<strong>in</strong>g this an <strong>in</strong>vestigation was done by us<strong>in</strong>g<br />

transmission electron microscopy (TEM) as well as high-resolution TEM (HRTEM).<br />

From <strong>the</strong>se results <strong>the</strong> phase <strong>of</strong> <strong>the</strong> <strong>SiC</strong> was determ<strong>in</strong>ed to be <strong>the</strong> cubic (<strong>3C</strong>-<strong>SiC</strong>) z<strong>in</strong>c-<br />

blende structure with a lattice parameter <strong>of</strong> 4.35Å . The <strong>in</strong>terface between <strong>the</strong> <strong>SiC</strong> and<br />

Si was also <strong>in</strong>vestigated. It was found from diffraction data that parallel epitaxial<br />

orientation between <strong>the</strong> two materials was obta<strong>in</strong>ed dur<strong>in</strong>g growth. The consistency<br />

along <strong>the</strong> <strong>in</strong>terface was also <strong>in</strong>vestigated and it was seen to conta<strong>in</strong> a reasonable<br />

amount <strong>of</strong> <strong>in</strong>homogeneities. Examples <strong>of</strong> very th<strong>in</strong> tw<strong>in</strong>ned sections orig<strong>in</strong>at<strong>in</strong>g at <strong>the</strong><br />

<strong>in</strong>terface were also found. In <strong>the</strong> bulk <strong>of</strong> <strong>the</strong> material a large density <strong>of</strong> stack<strong>in</strong>g faults<br />

was observed ly<strong>in</strong>g on <strong>the</strong> {111} close-packed planes with bond<strong>in</strong>g partials <strong>of</strong> <strong>the</strong> 1/6<br />

type. The stack<strong>in</strong>g faults observed <strong>in</strong> an edge-on orientation showed an<br />

<strong>in</strong>terest<strong>in</strong>g feature <strong>in</strong> that <strong>the</strong>y generate satellite streaks <strong>in</strong> a diffraction pattern. This is<br />

consistent with what is normally seen <strong>in</strong> materials conta<strong>in</strong><strong>in</strong>g narrow planar<br />

precipitates. This is due to <strong>the</strong> shape <strong>of</strong> <strong>the</strong> precipitate be<strong>in</strong>g similar to that <strong>of</strong> a plate<br />

like crystal (see p.97 Hirsch et al. (1965)). Fur<strong>the</strong>rmore <strong>the</strong>se stack<strong>in</strong>g faults were<br />

<strong>in</strong>vestigated us<strong>in</strong>g HRTEM and found to be extr<strong>in</strong>sic <strong>in</strong> nature. These f<strong>in</strong>d<strong>in</strong>gs agree<br />

with that found by previous researchers (Sections 5.2-5.3).

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