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The model has considered the heat transfer between the fuel cell body, gas channels, and cooling water, calculating the condensation and evaporation and modelling the water content, dragged water through membrane, water at the cathode.
This thesis acquires the diffusion coefficient of CO2 in the saline water under different conditions by means of laboratory experiments and analysis of the results, analyzing the influence that the factors such as temperature, injection pressure, salinity have on the diffusion coefficient of CO2 in saline water, calculating different diffusion coefficient of CO2.
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Figure 11 shows the oil displacement by water calculated by Buckley Leverett frontal displacement theory.
Figure 10a, b shows the mineral saturation indices (SI) of water calculated by PHREEQC model.
Figure 4 Map of soil available water calculated from SSURGO soils databases.
The density of water calculated through molecular dynamic simulations using different water models and rigid/flexible carbon nanotubes is studied.
For full LWA saturation the total volume fraction of LWA necessary calculated by Eq. (2) was used with the amount of entrained water calculated by Eq. (1).
The diffusion coefficients of oxygen in water calculated from the two measurements were almost identical: 2.00 × 10−9 m2 s−1 which is in good agreement with the literature.
Figure 5 shows the root mean square of speed relative to water calculated for foot element 1 (most proximal) and 6 (most distal).
More importantly, no statistically significant differences exist between the constant volume heat capacities of water calculated using exactly canonical MD NVT and approximately canonical REMS, both of which are in good agreement with the experimentally measured values (Fig. 3) [48].
The extracellular volume status was assessed by examining the ratio of extracellular water measured by BIA (ECWBIA) to the total body water calculated using the Watson formula (TBWWatson).
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