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Variations of refractive indexes of samples calculated by Swanepoel method in the range of 500 to 2,000 nm wavelength of electromagnetic wave are shown in Figure 9. Extracted magnitudes for n between 2.06 and 2.28 confirm that deposited films on substrates are uniform.
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m is the index of samples.
One reason for the variation of the refractive index of samples creates bonds is polarized.
The M-index of samples in the wall rock area ranged from 0.06 to 0.27.
The fabric strengths (M-index) of samples are listed in Table 1.
The refractive index of samples n are computed from the obtained reflection and transmission spectrum.
The flexural toughness index of samples with 12 mm PVA fiber is higher than that of the control sample by over 1300%.
Open image in new window Fig. 2 The real part of refractive index Open image in new window Fig. 3 The imaginary part of refractive index of samples.
Open image in new window Fig. 5 Refractive index of samples Open image in new window Fig. 6 Extinction coefficient of samples.
The M-index of samples in the mylonite zone was much lower than that in the wall rocks, meaning a weaker LPO in the mylonite.
Given indices of samples with actual positive assigned labels (A_{j}^) for the (j -th class label and corresponding set of indices with predicted positive labels (Y_{j -thfor a total of (M) samples, we define performanclasstrics using Eqs.
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