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9.2 Sources of Intrinsic Stress


In the first phase of the SiGe deposition process, islands with varying crystal orientation are formed and grow isotropically. These individual islands which first form on a substrate usually exhibit compressive stress [136]. In the course of further deposition these islands start to coalescence, which forces the islands to grow in the height instead of in a direction parallel to the substrate surface. The islands are subsequently transformed from an island shape to a grain-like shape. The orientation of the crystal structure in a single grain (e.g. perpendicular to the substrate surface) is independent of the neighboring grains, since due to the amorphous substrate, it is not possible to evolve a perfect crystal structure in the first atom layers [137].

For the stress aspect the deposition process plays a key role. At first it should be noted that the deposition takes place at elevated temperatures. When the temperature is decreased, the volumes of the grains shrink and the stresses in the material increase. Furthermore, the stress gradient and the average stress in the SiGe film depend on the Si-Ge ratio which can be controlled by the silane (SiH$ _4$) and germane (GeH$ _4$) flow, the substrate temperature, and the deposition technique which is usually LPCVD (low pressure chemical vapor deposition) or PECVD (plasma enhanced chemical vapor deposition). It was observed that the average stress becomes more compressive, if the Ge concentration decreases [138]. Thus it is expected that a film with higher Ge concentration has a higher degree of crystallinity and larger grains, which leads to higher film density and to higher tensile stress.

The intrinsic stress observed in thin films has generally the following main sources [133]:


next up previous contents
Next: 9.3 Modeling of the Up: 9. Intrinsic Stress Effects Previous: 9.1 Cantilever Deflection Problem

Ch. Hollauer: Modeling of Thermal Oxidation and Stress Effects