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In addition, the evolution of the layer structure and morphology has been followed by ex situ scanning electron microscopy.
Time evolution of the layer thickness, chemical composition, and bonding characteristics of the silicon oxynitride layers were investigated by various analytical methods including X-ray photoelectron spectroscopy (XPS), spectroscopic ellipsometry and high-resolution transmission electron microscopy (HR-TEM).
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This paper provides the first analysis of the seasonal evolution of the sonic layer depth (SLD) relative to the mixed layer depth (MLD) for the Aegean, Marmara, Black, and Azov Seas.
The structural evolution of the carbon layer on the BNNF surface was carefully monitored.
The structural evolution of the carbon layer and the nucleation and growth process of SWCNTs were monitored in real time with HRTEM images recorded by a CCD camera.
Results from the run MP show excellent agreement with OMI, further demonstrating the ability of the TOMCAT CTM to reproduce the observed evolution of the ozone layer when forced by observed ODS boundary conditions and appropriate meteorology.
The experimental results are also compared to phase-field simulations of the microstructural evolution of the Cu6Sn5 layer.
The thickness, coarsening and morphology evolution of the Cu6Sn5 layer is investigated through the use of scanning electron microscopy.
The influence of model parameters on the kinetics and morphological evolution of the IMC layer was examined.
The microstructure evolution of the surface layer was investigated by X-ray diffraction and scanning and transmission electron microscopy observations.
Radiographs are recorded to compile a temporal evolution of the mixing layer and its subsequent reshock, compression, and re-growth phases.
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