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RBS analysis of cortical bone samples gave a Ca P ratio of 1.37 ± 0.035, somewhat lower than that reported for cortical bone of adult human femora.
Validation of the new clay and SOM model using the 227 soil samples gave a root mean square error and mean error of 0.041 and + 0.013 Mg m− 3, respectively.
For compositions rich in PGMA (chitin ⪅ 20 wt%), it was revealed by d.s.c. and d.m.a. that the polymerized samples gave a Tg value higher than that of PGMA homopolymer, and the magnitude of lowering of their modulus E′ in the glass transition region became extremely small, compared with the corresponding E′-drop noted for PGMA alone.
Core samples gave a mean porosity value of 33.0% and a mean permeability value of 274 × 10−3 μm2.
Moreover, the enhancement of hardness can be related to the reduction in grain size, i.e., small grain size samples gave a higher measured hardness.
The SEM texture of the samples gave a clue that GO/rGO weakly bond with nonpolar EPDM but strongly with the polar NBR matrix.
The QCL-40 samples gave a mean result of 37.63, 40.19 and 36.07 μg/mL with the corresponding percentage change from freshly prepared samples of +6.31, −13.54 and +1.88% for freeze and thaw cycles 1, 2 and 3 respectively.
The QCM-200 samples gave a mean result of 208.34, 211.68 and 213.08 μg/mL with the corresponding percentage change from freshly prepared samples of −9.38, +7.93 and −7.90% for freeze and thaw cycles 1, 2 and 3 respectively.
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Spore and pollen samples gave an Oxfordian age (Late Jurassic) for the sequence.
192 (16.9%) samples gave an integer copy number call posterior probability of less than 0.8.
For measurement of between-run variation, high-signal samples gave an average CV of 19% (range 15%28%%) (Table 1).
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com