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In Figure 10, the pixel values of the background and foreground have a high contrast.
The quantitative values of the background current on the three concentric areas are shown in the table of Figure 3.
The first approach we used to investigate the relationship between both parameters was comparing the mean values of the background and peak populations obtained for each of the three studied volcanic systems.
To perform the intra-sample normalization, we first calculated the net MFI value for each result by subtracting the MFI values of the background.
The not-found species were assigned to have the abundance values of the background intensity scaled for summing over the features based on the same condition as the identified peptides correspondingly.
The recorded fluorescence values of the background region were subtracted from the values of the tissue sample region.
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We are particularly concerned with the spatial estimates of the first two parameters of the space-time ETAS model: namely, μ-values of the background seismicity and aftershock productivity K-values.
This estimation is based on the penetration depth and the intensity value of the background noise in captured images.
We then obtained threshold values from the mean gray value of the background image without the film from each image files.
With each agent, a lesion-to-background (L/B) ratio was calculated from the value of the visually focal PET uptake and the value of the background uptake.
Once a value for the storativity ((S = 10^{ - 11},{text{Pa}}^{ - 1}) in the calculations) is assumed, a given SI requires a specific value of the background seismicity.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com