The lithosphere is not treated as an ideal layer that can support large (and large scale) non-hydrostatic load for billions of years.
While the doped or undoped ceria films showed a 3-dimensional growth mechanism typically characterized by a pronounced surface roughness, YSZ films showed an almost ideal layer-by-layer 2-dimensional growth.
The morphology of the multilayer structure was analysed by scanning electron microscopy; an algorithm for defining ideal layer conformity was established and no local thickness deficiencies of deposited SiOx layers could be observed.
This approach is numerically less demanding than solving the full set of resistive equations and has the major advantage of allowing for non-MHD theories of the non-ideal layers.
An almost ideal 2D layer-by-layer growth with cube-on-cube symmetry was observed for the STO buffer layer on MgO.
On the contrary, YSZ films showed an almost ideal 2D layer-by-layer growth along the (001) orientation, even in the presence of relatively unfavourable crystalline matching with the substrate, such as in the case of films grown on MgO.
In the ideal cases, layer-by-layer intercalation of organic moieties into PbI2 proceeds with a single exponential component with m = 0.9 1.1 (region I), strongly supporting the previous argument of unidirectional intercalation along the c-axis.
As, in this article, our main goal is to analyse the performance of MAC layer, we assume an ideal PHY layer with perfect time and frequency synchronisation and no channel or decoding errors.
It was also discovered by SEM that subsequent deposition of a PB film with submicron-crack openings on PANI yielded an ideal two-layer structure, but a non-idea bilayer that lacked an obvious boundary between PANI and PB layers was formed when PB was deposited first.
I find it ideal for layering under outerwear, and it doesn't restrict my mobility or weigh me down, and it always keeps me warm at the core.
