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Nandal, V. & Nair, P. R. Predictive modeling of ion migration induced degradation in perovskite solar cells.
PBGUNS and SIMION were used for the modeling of ion source unit.
The moisture transfer coefficient (MTC) is an essential parameter utilized in diffusion convection modeling of ion ingress into cement-based systems, especially in marine environments with variable temperatures.
The modeling of ion transport and interactions in matter is a subject of growing interest, driven by the continuous increase of possible application fields.
This capability enables modeling of ion trajectories for realistic numbers of ions in realistic ion trap devices (defined by electrode structures and applied electrode voltages) and provides simulated mass spectral peaks as an end product.
These results suggest that rigorously considering electrochemical couplings will lead to a deeper understanding as to the origins of macroscopic experimental observations, and with future inclusion of effects such as cation exchange, to improved computer simulation-based modeling of ion transport through charged porous materials such as clay soils.
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Then, we compare our results under the purview of the present MPB equation with those predicted by point-like charge modeling of ions.
A model of ion flux in the oceans shows carbon dioxide driving ocean acidity.
We perform both a time integration analysis and spatial grid analysis for a kinetic ion, adiabatic electron model of ion acoustic waves.
In the first part a model of ion kinetics in a near-ground layer of troposphere is considered.
Correct modelling of ion diffusion does give significant though minor changes in absorption rate predictions: CO2 absorption is reduced and H2S absorption increased.
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