This procedure holds for a stationary system and a dilute solution where the spatial correlation length of concentration fluctuations is much smaller than the detection volume, which is clearly the case for our study.
The length-scale of fluctuations within the electrolyte is larger than the characteristic distance between ionic aggregates, and we argue that at low hydration level it has a negative impact on the percolation and connectivity of the aqueous phase.
Figure 2 Schematic drawing of the density of states in the lead for the reduced model, in situations (a) L c ≪ L K ≪ L, (b) L c ≪ L ≪ L K, and (c) L ≪ L c ≪ L K, where L is the size of the AB ring, L c is the screening length of charge fluctuation, and L K is that of spin fluctuation, i.e., size of Kondo screening cloud.
We introduce L c = ℏ v F ∕ | ε ̃ 0 |, which corresponds to the screening length of charge fluctuation.
In this paper, we will focus on coherence lengths of pressure fluctuations underneath a turbulent boundary layer on an actual aircraft measured during a flight test.
Coherence lengths of pressure fluctuations have already been measured in the past and various models have been set up in order to predict the values.
This observation is explained by the fact that for high Mw blends the correlation length of the concentration fluctuations ξ is always large (ξ>Rg), implying that these blends remain microscopically inhomogeneous at all temperatures studied in this work.
From (2) it is straightforward to see that we have considered a receiving aperture smaller than the correlation length of the irradiance fluctuations, i.e., the aperture behaves essentially as a point detector [1] and ignores intersymbol interference, then the receiver detects signal light only when an 'on' state is transmitted.
The former is the screening length of the charge fluctuation and the latter is that of the spin fluctuation, i.e., size of Kondo screening cloud.
