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A considerable difference in the rock permeability can be found for sample 17.1 with an eightfold decrease from 23 to ~ 2.9 mD within 1100 min.
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In general, they reveal the same tendencies as seen for A1 to C1 except that the thickness oscillations do not occur and that only a single GaAs-related peak is found for sample c2.
Inconclusive results were found for sample from tunnels 4 and 5 where neither increase in MN frequencies nor high concentration of particles was found.
No significant differences between treatment conditions were found for sample characteristics, or dropout rates χ 2 's (1, N = 34) ≤ 3.03, p's ≥ .22.22
A main effect was found for Sample 2, with mean cortical thickness biased toward slightly thinner estimates without an interaction with diagnostic group.
Unacknowledged discrepancies between protocols and publications were found for sample size calculations (18/34 trials), methods of handling protocol deviations (19/43) and missing data (39/49), primary outcome analyses (25/42), subgroup analyses (25/25), and adjusted analyses (23/28).
A similar case was found for sample DAF141 with an average coverage of 360 but a calculated coverage of 114 suggesting a length of three plasmids inserted into the genome.
Greater initial modulus was found for samples of r = 0.1.
High data variability was found for samples collected furthest from the dye injection point.
The best arrangement of nanopores was found for samples anodized at 40 V.
The highest magnetorheological effect has been found for samples with 6 9 μm carbonyl-iron powder.
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