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The greater thermal stability of the AgGO sample may also be due to the existence of AgNP. Figure 6 TGA of GO and AgGO.
It is worth noting that improved nonlinear properties of the CCTO/Au1 sample may also be related to modification of microstructure.
A larger sample may also be needed to estimate burden than to estimate prevalence, because burden is not distributed equally among cases: most of it is accounted for by a minority of those with the disorder.
Sample X3 has a sulfate band at 978 cm−1, and also a chromate band at 846 cm−1, also consistent with a PbCr1−xSxO4 formulation (this, in addition to the presence of barium sulfate in the sample, may also account for a larger peak in the µFT-IR spectra at ~1050 cm−1; see Additional file 4: Table S4).
If the mineralogy examination looks promising, then the sample may also be fed to the Sample Analysis at Mars instrument suite, which will use a mass spectrometer (one of three instruments in its arsenal) to look at elemental abundances.
The ZDHS sample may also be biased due to differential non-response in the survey and/or exclusion of population groups that do not live in households.
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The redshift in our Fe-doped ZnO samples may also due to this reason.
Methods combining image-derived IF and later blood sampling may also help minimize spillover effects [26, 27].
This decrease is more pronounced in septic than in nonseptic patients [4], at least in part because of their inflammatory response; more frequent blood sampling may also contribute.
The timing of the plasma sampling may also falsely underestimate the association between HBP and markers of permeability, as discussed below.
The absence of peak broadening of Ti 2p3/2 signals (FWHM was about 1.4 eV for all samples) may also indicate the presence of Ti4+ species only [32], and good crystallization for all samples [33].
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