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The results indicated that significant difference in pharmacokinetic parameters of the analytes was observed between two groups, while absorptions of these analytes in insomnic group were all significantly higher than those in normal group.
The Man-Whitney U test was applied for comparisons between two groups, while, one-way analysis of variance (ANOVA) was used to compare more than two groups.
The Mann–Whitney U rank sum test was performed to analyse the difference between two groups, while for individual comparisons among the three groups the Kruskal Wallis test, followed by the Scheffe test was performed.
However, the peaks in biomarkers and tree pattern were not the same, which could be explained by the fact that biomarkers had been identified as a single peak which showed the highest discrepancy between two groups, while the patterns stressed synergistic effects of peaks in-group.
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So Kruskal Wallis was used for comparison between four groups while, Mann Whitney was used for comparison between two groups.
The lipid panel between two groups was similar while both the urine mAlb/Cr at index visit (12.12 ± 49.70 versus 3.65 ± 18.74, p = 0.011) and GFR (73.52 ± 25.48 versus 71.55 ± 23.33, p = 0.049) at the follow-up visit were significantly higher in the progression group.
Entering the variance components in statistical power equations showed that for most metrics, a total of 80 100 subjects will be required to detect a 20% difference between two groups with sufficient power, while this difference can typically be detected in repeated-measures (paired) designs using 25 subjects.
A general linear model was used to compare outcome scores between the two groups while controlling for possible confounders.
The difference between the two groups while comparing episodes of hypoglycemia was significant (p = 0.0026).
Additionally, we found that several emotions were rated significantly different between the two groups, while most were not.
First, to investigate differences in precipitable water between the two groups, while positive anomalies were shown in the western North Pacific, negative anomalies were shown in regions ranging from the central region of China, passing through the East China Sea to the east waters of Japan (Fig. 6a).
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