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In this model, both labeled data samples (with values for both two types of variables) and unlabeled data samples (with values only for routinely recorded variables) can be effectively used.
Samples with values >1, suggest an excess of (Ca2+ + Mg2+) were derived from a reverse ion exchange (Prasanna et al. 2011).
Where necessary, blank subtraction was used for areas of the chromatogram where interference occurred in samples with values were close to limits of detection.
For the samples with values of M IRM ≥ 1 × 10−11 Am2, there was no clear correlation between the M IRM and 100 × M IRM-LTD/M IRM (correlation coefficient approximately −0.22).
The highest fixed carbon content of 51.57% was recorded in the Shankodi-Jangwa coal sample, followed by Garin Maiganga and Tai coal samples with values of 34.75% and 24.11%, respectively.
The concentration of Cr is generally low (only higher than Co) in all the samples with values ranging from 4.50 to 33.50 ppm, which suggests oxic suboxic depositional conditions for the organic materials.
Accordingly, all samples with values above the cut-off were considered positive while samples with values below the cut-off were considered negative.
Samples with values greater than the last dilution were diluted further and retested.
All samples with values below detection limit were given half of these threshold values.
High concentrations of MMP7 were diluted with calibrator, to produce samples with values within the dynamic range of the assay.
Similarly, all samples with values above the level of detection (OOR>) were assigned a value of twice the largest value recorded in that assay.
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