After calculating the cross-section area and hence the bending strength of different samples, the values of ca. 210 ± 20 MPa for micro-monolithic anodes were found to be comparable with that for the single-channel geometry.
This theorem implies that for large samples the values of prior probabilities don't matter much.
For all the prepared samples, the values of m are found to be close to the value for the bulk.
The Sr/Ba values of mudstone clasts and muddy coatings are less than 0.4, excluding some exceptional samples; the values of muddy-debris-flow mudstones are also low.
The smallest Vfb is -0.53 V for the 773 K annealed thin film, and for the as-deposited and 573 K and 973 K annealed samples, the values of Vfb are - 1.01, - 0.71, and - 0.62, respectively.
Despite the lack of statistical differences in the estimated archaeal OTU richness between the samples, the values of the estimated Shannon diversity index presented some significant differences (Table 3).
