Elastic strain relaxation in Si1-xGex layers epitaxially grown on Si substrates

被引:12
作者
Berbezier, I
Gallas, B
Derrien, J
机构
[1] Univ Aix Marseille 2, CNRS, Ctr Rech Mecanismes Croissance Cristalline, Lab Associe, F-13288 Marseille 9, France
[2] Univ Aix Marseille 3, CNRS, Ctr Rech Mecanismes Croissance Cristalline, Lab Associe, F-13288 Marseille, France
关键词
D O I
10.1142/S0218625X98000268
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
We have investigated the elastic strain relaxation in Si1-xGex layers grown by the molecular beam epitaxy (MBE) technique and in situ controlled with RHEED. Up to approximate to 0.8% critical lattice mismatch (about 20% Ge) uniform strained and flat layers were grown both on (111) and on (001) Si substrates. Calculations of the elastic constants evidenced a tetragonal distortion about 50% higher on (001) than on (111) in the same experimental conditions. At higher misfits (and/or thicknesses) a growth instability was evidenced only on (001) Si substrates. Si1-xGex layers there displayed a surface layer undulation. On the contrary, Si1-xGex layers grown on (111) Si substrates remained smooth throughout the growth up to the plastic relaxation of the layers. To determine stress fields in the Si1-xGex layers, a high spatial resolution convergent beam electron diffraction (CBED) experiment was performed with a field effect analytical microscope. The CBED technique was applied to two typical cases: totally strained layer and undulated dislocation-free layer. In the latter case, CBED patterns recorded on nanometer scale areas of an undulation crest (cross-section sample) showed a gradual elastic relaxation mainly directed along the growth axis (z). Moreover a triclinic distortion of the unit cell was pointed out. These results were confirmed on a plane view sample. In conclusion, our results show that the driving force for the undulation is not the in-plane elastic relaxation since CBED experiments proved an important elastic relaxation of the (001) Si1-xGex layers along the z axis. This was in agreement with the calculations of the elastic constants. We think that this could be at the origin of the undulation.
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页码:133 / 138
页数:6
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