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Foreground samples are defined as the skeleton regions of confident reconstruction segments.
Background samples are defined as the non-skeleton regions surrounding the confident reconstruction segments.
In this algorithm, using measured current samples, some specific characteristics for the samples are defined for the fault classification.
The samples are defined with notations S1, S2, S3, and S4, where higher numbers refer to higher Si excess in the SiN x matrix (see Table 1).
Group B samples are defined as those taken at elevations above Group A and are located between 2.0 and 4.0 m amsl at Shikinejima (sites S1, S2, S3, and S6) and Kouzushima (sites K1, K3, and K4); they yield ages of AD 975 1872.
If we denote the time-domain signal for a single OFDM symbol as a vector x = { x - β - N CP, …, x N - 1 + β }, the OFDM-symbol time-domain samples are defined by vector y= {y k }, which results from the multiplication of the vector x = {x k } by the window shape w = {w k }, namely: Figure 1 Windowed OFDM symbols; red lines denote the preceding and the following OFDM symbol.
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The transition of the samples is defined through the construction of a sequence of intermediate distributions.
The lattice parameters of tin(IV) oxide samples were defined, the bandgap of samples were calculated.
A square area around r with W ×× W samples is defined to be the searching area Ω.
Phase composition of samples was defined using X-ray diffractometer Rigaku Ultima IV in monochromatic Кα-radiation of Cu-anode.
The overall difference for all samples is defined as Eg = 1 N ∑ i = 1 N ∥ S i − S i ∗ ∥.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com