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The RNA integrity number values for all samples were at least 7.5.
Salt levels in some samples were at impossibly high levels, showing that they had been tampered with.
The last 2 samples were at concentrations above the recommended limit of 2000 μg/kg.
While three samples were at relatively low levels, tests on the cold water tap in one bathroom discovered the presence of legionella bacteria at seven times the safety level.
Pigs with culture positive fecal samples were at increased odds of being detected positive for each of the slaughter-collected samples examined, namely distal colonic content (OR = 30.5), ileocolic lymph nodes (OR = 12.9) and cecal content (OR = 23.2).
A south to north sample transect from coast to continental interior yielded ZFT ages between 116.6 ± 4.7 Ma and 87.3 ± 4.0, indicating that by the Late Cretaceous samples were at depths of 5 6 km in the upper crust.
Of 80 groundwater samples collected from the pilot-PRB, 11 samples exceeded 0.50 mg As L− 1; 62 samples had concentrations of arsenic at or below 0.50 mg L− 1; and, 24 samples were at or below the maximum contaminant level (MCL) for arsenic of 0.01 mg L− 1.
However, the decayed soft tissue values of the soil samples were at the threshold level.
The measurements were carried out in situ while the samples were at the temperatures and pressures of interest.
According to Wilcox diagram, 78 % of samples were at the C3-S1 and 21.5 % were at C2-S1 classes.
Pereira et al. (2014) indicated that 47.17 % of analyzed samples were at detectable concentration whereas Han et al. (2015) found 12%% at levels lower than MRL.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com