Numerical simulations were carried out using a 3-dimensional computational fluid dynamics (CFD) to predict the outlet water and absorber plate temperatures using the experimental values of solar insolation, ambient temperature and inlet water temperature within one hour interval.
The penetration depth for molecular diffusion calculated using the Flory–Huggins theory was consistent with that estimated using the experimental values of the radius of gyration and bond strength.
Therefore, we could calculate the values of Δα (Å3) for Fe3O4 nanoparticle using the experimental values of Δn(I) and the following equations (SI): ϵ = n 2 I − k 2 I = 1 + χ Δχ = Δα Å 3 ⋅ 10 30 ⋅ N m − 3 (5).
The deterministic values of the coefficients of Eq. 7 are determined using the experimental values available in [14].
Protein identification was checked manually and further evaluated by comparison with their calculated mass and pI values, using the experimental values obtained from 2-DE.
The current on Figure 8 is normalized to 1 when membrane potential equals 0. In order to approximate the current, we only used the experimental values obtained under the membrane depolarized conditions, and this experimental data is approximated by equation (36).
MALDI-TOF PMF candidates with a cumulative MASCOT score > 83 or nanoLC-ESI-LIT-MS/MS candidates with more than 2 assigned unique peptides with an individual MASCOT score > 25, both corresponding to p < 0.05 for a significant identification, were further evaluated by the comparison with their calculated mass and pI values, using the experimental values obtained from 2-DE.
Candidates with more than 2 assigned peptides with an individual MASCOT score >25, corresponding to p < 0.05 for a significant identification, were further evaluated by the comparison with their calculated mass and pI values, using the experimental values obtained from 2-DE.
For the values of the K C and C C interplane distances as well as for the in-plane lattice constants, we used the experimental values given in Table 4 of ref (14); i.e., a = 1.42 Å for the bond-length, d = 3.35 Å for the interplane distance in graphite, and dM = 5.41 Å for the distance between the intercalated layers.
