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Right column: PSDs corresponding to the voltage traces shown in (a1), (b1), and (c1).
Likewise, the time domain traces shown in the upper middle and the upper right panels of Figure 19 should be qualitatively compared with the time domain traces shown in panels I and III, respectively, of Figure 21.
We post processed the measurement traces shown in Figure 2(b) to see the impact of and and display it in Figure 9(a).
Boxed points in (a) correspond to the chromatographic traces shown in Fig. 2. All solutions were prepared using deoxygenated and distilled water (Milli-Q 18 MΩ).
The bold traces shown in the inset correspond to Zn3N2 obtained closest to Zn, and the thin ones to Zn3N2 obtained further donwstream.
To save calculation time, only vertical component seismo-grams were considered; i.e. only the reference (ZAG) and 24 other traces shown in Fig. 1(b).
The time domain I/ Qtraces shown in Figure 19 provide another useful look at how the SPART trims the outliers while maintaining the signal of interest.
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Their traces show in this melodic, richly contrapuntal, often muscular 10-movement work.
This tendency is clearly interpreted when one examines the changes in the voltage x-traces shown in Figure 6.
These spectra correspond to the 3-D ray-tracing shown in Fig. 2, indicating that the ray-tracing method properly predicted the RASS echoing region.
In this figure, the USDP-4 trace, shown in orange, corresponds to the conduit zone reported by Nakada et al. (2005).
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com