1999
DOI: 10.1016/s0039-6028(99)00183-1
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The roughening transition of the Si{113} and Si{110} surfaces – an in situ, real time observation

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Cited by 31 publications
(26 citation statements)
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“…Since F͑͒ can be viewed as the radius of curvature of the equilibrium crystal surface, L is therefore the radius of curvature of the facet planes, and R is that of the corners of the equilibrium crystal, all made dimensionless by H. 21 As the sharpness of corners on an equilibrium crystal depends on temperature, [28][29][30] R can be used to study the effect of temperature. This periodic function has spikes centered at = i ͑ i are the orientations of facet planes on the equilibrium crystal͒.…”
Section: A Surface-energy Anisotropymentioning
confidence: 99%
“…Since F͑͒ can be viewed as the radius of curvature of the equilibrium crystal surface, L is therefore the radius of curvature of the facet planes, and R is that of the corners of the equilibrium crystal, all made dimensionless by H. 21 As the sharpness of corners on an equilibrium crystal depends on temperature, [28][29][30] R can be used to study the effect of temperature. This periodic function has spikes centered at = i ͑ i are the orientations of facet planes on the equilibrium crystal͒.…”
Section: A Surface-energy Anisotropymentioning
confidence: 99%
“…The simultaneous use of these three experimental data leads to the experimental determination of the absolute surface free energy c i . From the experimental point of view one has just to be able to perform true equilibrium experiments that means (at last at high temperature) to be able to compensate the desorbing flux by an impinging one as described by Heyraud et al [28].…”
Section: Experimental Determination Of Surface Energy: the Principlementioning
confidence: 99%
“…The procedure is thus quite general and can be applied each time (i) the 2D and 3D equilibrium shapes (with all orientations present) are available, (ii) the geometrical properties of the 2D and 3D equilibrium shapes as well as the thermal fluctuations of an isolated step can be measured with a sufficient accuracy, (iii) the flat surface is characterised by an isotropic stress so that the 2D equilibrium shape is not modified by surface stress (as clearly shown in [36] for Ge(0 0 1) surface). It is the case of Si(1 1 1) surface above the (7 · 7) $ (1 · 1) transition, for which (1) the recovered threefold symmetry provides an isotropic surface stress and (2) all data are available from previous studies [16,17,28,34].…”
Section: Partial Conclusionmentioning
confidence: 99%
“…On Si͑113͒, Si͑110͒, and Si͑001͒ at TϾ1100°C, the 2D-island nucleation can be easily observed. 14,15 These surfaces exhibit a roughening transition at about 1340°C ͑Ref. 14͒, 1370°C ͑Ref.…”
Section: Island Diffusion On Si"111…mentioning
confidence: 99%