In contrast, for the 3-Hz wave (no. 6 source time function), the amplitude level variance became saturated at a distance of ~30 km, after which we observed a roughly flat data distribution at large hypocentral distances.
Water dissociation was not observed even under a strong bias (corresponding to a Pt surface charge of σ = 14 μC/cm2) although it was observed on a flat surface with less surface charge.
Then, it was observed that a flat small number is less than 15.
Plotting the log ratio of H3/input, we observed mostly a flat profile in euchromatin and heterochromatin, confirming that canonical H3 nucleosomes comprise almost all of the input in these regions, but we found that H3 is strongly depleted in the central domain.
In Fig. 3f we observe a completely flat distribution meaning the independence of x 1 and x 2. This agrees with the way x 1 and x 2 were generated, i.e. as two Gaussian independent time series.
Starting from sector I we observe a practically flat behaviour (at that of Fig. 3f) for both geomagnetic components, indicating the lack of any relation between dX and dY residuals and B y or B z. Moving to sectors III and IV, Figs. 4 and 5 show a clear dependence of dX and dY on B z, i.e. dX and dY residuals become larger and larger (in absolute value) with decreasing B z.
For Sym-H larger than about −60 nT we observe an almost flat behaviour, while for smaller values two distinct branches appear, indicating the existence of a dependence.
We also observed a sharp peak at the beginning of the S phase in SUM149PT cells (Fig. 4b), in contrast to the flat plateau observed in the S phase of MCF10A cells (Fig. 4a).
For nanocrystal-only films, we observe a broad and flat positive TA that decays slowly, giving rise to a negative TA signal at times larger than 200 ps.
A further unique feature observed here was a flat heritable area around the ramus of the mandible.
