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The poration within the PEG microspheres was examined through the use of a confocal fluorescence microscope by taking slices of the collected fluorescence through the depth of the sphere.
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In the absence of explicit depth information the sphere is perceived to alternately rotate in either of two directions: with the leftward moving surface in front and the rightward moving surface in the back, or vice versa.
They showed that sputtering has a maximum as a function of sphere size when the ion penetration depth is of the order of the sphere radius; these results corroborate the earlier findings of Järvi et al. [12, 13].
The melt spheres and the fluid matrix could be probed quantitatively with the confocal micro-Raman system because with the ~ 1 μm diameter laser beam the sampling depth is within the range of the sphere diameter or less.
We note that the depth of the Poisson wavelet under the Bjerhammar sphere, computed as ( d = R - left| varvec{y} right| ), is the key point to determining its property in the frequency domain (Wittwer 2009).
If all of Earth's crustal surface was at the same elevation as a smooth sphere, the depth of the resulting world ocean would be 2.7 to 2.8 km.
Figure 2 shows the algorithm steps: depth equalization on the sphere, flattening, interpolation, and reconstruction.
If EB and the roots are built mainly of the ices, then the isostasy requires: (2 where h is the height above the reference sphere, w is depth of the roots and Δρ = ρav — ρice is 143 kg m−3.
diameter of the sphere.
Right panel, A schematic of the sphere culture system and a representative sphere after culture.
Test the strength of the sphere.
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