Sentence examples for time scale process from inspiring English sources

Depending on the values of both, their coupling can result to enhancing the interface height overshot or increasing the global time scale process.

During passivation the electrode surface was dominated by short time scale process (D3), and during trans-passivation by medium (D4) followed by short time scale process (D2) with range of scale between 0.8 and 0.4 s, 1.6 and 0.8 s and 0.4 and 0.2 s, respectively.

It has been found that during active dissolution the electrode surface is dominated by long time scale process and the change of the position of the maximum relative energy from D7 to D8 could be an indication of future passivation.

However, a quick look at the long trajectory of any slow time scale process would indicate that proteins spend a significant amount of simulation time fluctuating within the basins associated with long-lived metastable states and a rare thermal fluctuation leads to the barrier-crossing event.

The interplay between different time scale processes is shown.

Long time scale processes were observed to result in cation exchange properties accompanied by a substantial decrease in redox activity and/or CV currents of the polypyrrole electrode.

The reduction is based on a certain number of considerations about time scales process dynamics, simplification of biomass dynamics, utilization of available on-line measurements.

Initially, a result is derived that provides necessary and sufficient conditions for the existence and the explicit form of an ε-independent coordinate change that transforms the two-time-scale process into a standard singularly perturbed form.

Whenever these conditions are not satisfied, it is established that an ε-dependent coordinate change, singular at ε=0, has to be employed to obtain a standard singularly perturbed representation of the original two-time-scale process, and the construction of such a transformation is addressed.

Even so, because of the hovering motion of the exit point, we suggest that the ionospheric source movement can be altered by small-scale processes with a time scale varying between 20 and 50 min. Consequently, chorus emission generation and their propagation might be also dependent on short time-scale processes.

We also note that often, long time-scale processes are long simply because they are composed of many "steps" or molecular events that each might occur in short time scales and therefore can be efficiently described using MD.