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Two types of buckling mode are observed, and are denoted as a cosine mode and a dent mode.
Two types of buckling mode are observed, which are denoted as a cosine mode and a dent mode.
Capacitance maxima in the strong inversion mode are observed in an intermediate case, i.e., between the low-frequency and high-frequency behavior.
The absorption peaks of imines-stretching mode are observed at 1,654 and 1,638 cm−1 while the multiple peaks at 1,596 and 1,570 cm−1 are assigned to the N = Q = N, quinonoid ring, skeletal vibrations.
Dispersions of approximately ±100 ps/nm/km over a 4200-nm bandwidth for the quasi-TE mode and of approximately ±120 ps/nm/km over a 2350-nm bandwidth for the quasi-TM mode are observed.
Similar controlled blue shifts of the longitudinal mode are observed, indicating thickening of the Al2O3 layer.
Similar(54)
A different transition mode is observed in oxides, silicates, and other types of ionic compounds that comprise most rock-forming minerals.
The plate failure mode was observed on the inverted cone.
No other mode related to defect-induced local vibration mode is observed.
At low overstress, the hexagonal mode is observed in the experiments not the square mode.
At 620 cm−1, the metal oxygen (Ni O and/or Al O) stretching mode was observed.
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