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The transition of the samples is defined through the construction of a sequence of intermediate distributions.
A square area around r with W ×× W samples is defined to be the searching area Ω.
The overall difference for all samples is defined as Eg = 1 N ∑ i = 1 N ∥ S i − S i ∗ ∥.
The transition of the samples is defined through the construction of a sequence of intermediate distributions, which are sampled through application of a resample-move scheme.
According to the classic Williamson-Hall method and its subsequent variations [19, 20], the differential strain of samples is defined as (1).
A source dataset ( {{{mathcal {D}}}^ s} doteq {mathbf {X}^{s (n)} }_{n = 1,.., N^ s} ) of N s labeled samples is defined.
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The lattice parameters of tin(IV) oxide samples were defined, the bandgap of samples were calculated.
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.
Phase composition of samples was defined using X-ray diffractometer Rigaku Ultima IV in monochromatic Кα-radiation of Cu-anode.
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