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The seismic profiles presented here do not traverse through the seamount complex.
Hydration profiles presented in this paper use data up to and including the 504 h, but not after that time.
The seismic profiles presented here clearly image the lateral variations of the EMF throughout the basin (Figs. 4, 5, 6).
The vertical profiles presented in Figure 7b indicate that the two mentioned contradictory effects seem to globally balance.
The structural profiles presented demonstrate that the Kristineberg ore is situated in the northern limb of a local synformal structure.
The SEM profiles presented a three-dimensional MWNTs interwoven network surface structure with a large accessible surface area.
These effects are caused by the approximations of the TEW scatter correction method, which can be visualized when considering the shapes of the profiles presented in Fig. 5.
Subsequently, data was collected for the averaging time t a to reach converged statistics for the profiles presented in the following.
At this period, the concentration profiles presented a similar pattern of flat line in the activated carbon, biofilm, and diffusion layer.
Thus, we hypothesize that the transcriptional profiles presented here may reflect intrinsic biological properties predictive of 131I and 211At absorbed dose levels at various time points.
The profiles presented in this study can serve as a test against which future chemical and process models may be validated.
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