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Their motion from the location of discharge to a site on the crystal occurs by surface diffusion.
Furthermore, phase transition of the type II crystal occurs at 180°C a temperature at which the type III crystal is formed.
It has been shown that fracture in NiAl single crystal occurs by development of microcracks on slip bands and their subsequent instability.
When the photonic crystal is filled with ethanol vapor, the capillary condensation within the mesoporous layers (pore size of some nanometers) of the photonic crystal occurs and changes the refractive index contrast thereby shifting the central wavelength to a higher wavelength (red shift).
The simulations predict that (i) nucleation of martensite in a perfect crystal occurs collectively to accommodate the coherency strain, e.g. the critical nuclei are formed by two internally twinned orientation variants; (ii) the ultimate structure consists of plate-like martensite and retaining parent phase.
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By increasing the molecular weight of P3HT, the growth of single crystal occurred slowly in the a-direction.
WAXD pattern of POBAi-2.5 revealed that α β transition of crystal occurred during recovery process.
It was also demonstrated that a reverse transition (mesophase to crystal) occurred at slightly lower temperature which was attributed to slow nucleation and crystal growth kinetics.
As the crystallization temperature decreases, strong changes in the width-to-length ratio and, consequently in the characteristic angles of the single crystal occur.
A boundary value problem in the case of the second order axi-symmetric Young Laplace differential equation (some of whose solutions describe the static meniscus free surface, i.e. the static liquid bridge free surface between the shaper and the crystal, occurring in single crystal rod growth) is analyzed.
Scanning electron microscopy (SEM) observation showed that well-crystallized crystals occurred in the specimens with 50 70 wt% funnel glass additions, whereas the specimens with 40 wt% and 80 wt% glass additions exhibited a relative low crystallization degree.
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