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In a viscoelastic liquid, the migration direction and velocity depend on the competition among particle deformability, fluid elasticity, and fluid viscosity shear thinning (if any).
A reasonable groundwater monitoring programme that considers the migration direction and the distance of the pollutants from the groundwater movement in a non-natural flow field under the influence of a groundwater funnel during deep mining is also necessary.
Flow-induced HAEC migration was also influenced by the ridge/groove surface topographic features with significantly altered migration direction and increased migration tortuosity when flow was oriented perpendicular to the topography; this effect was also pitch-dependent.
In general, large rivers generating fluvial terraces are controlled by basement structure, with positive and negative crustal flexures driving their migration direction and thus controlling the spatial distribution of terraces, because the position of main streams is controlled by large tectonic lineaments that favor groundwater flow convergence.
Considering that both the morphological reorganization and the positional shift noted here have preferred directions, they may be predetermining the migration direction and hence, required for electrically-guided cell migration.
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Both the reversal of Es migration directions and 8-h Es occurrence periodicity in Fig. 5 suggest that atmospheric tidal winds may govern the occurrence and drifts of Es patches.
In this collection of guidelines, we identify a number of methodological and reporting issues including: measurement error and precision, migration and migration direction data, and the use of RSA as a screening technique.
Major hydrocarbon-generation depressions controlled the overall basement-rock reservoir distribution, paleo-uplifts (or paleo-salients) and paleo-slopes controlled the hydrocarbon migration directions, faults and unconformities controlled hydrocarbon-migration channel systems, and weathered-crust reservoirs of basement rocks controlled hydrocarbon enrichment.
The residual oil pattern during the high water-containing period is obtained; that is, the remaining oil controls the oil and gas migration direction due to the interlayer, abandoned channel and other impervious layers so that oil and gas can be enriched around the channel and impervious layer.
Comparing the migration barrier along each direction, we find that the [111] direction is the most favorable migration direction for both Si and Ge vacancies, as indicated by the significantly smaller migration barriers.
Time lapse geochemistry has been applied for prediction of hydrocarbon source kitchen, based on the fact that changes in oil saturation and hydrocarbon fingerprints overtime may indicate location of hydrocarbon source kitchen and migration direction of expelled hydrocarbon (Milkov et al. 2007).
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