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Model results using an idealized porous medium under non-biofilm forming conditions indicate that while some heterogeneity is observed for flow rates, distributions of microbes and dissolved organic substrates remain relatively homogenous at the grain scale.
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In particular, three different flow regimes are observed for displacement flows in a moving pipe: a stable flow that is non-diffusive (for Re/Ro≲O(102) & Re/Fr2<35), a stable-diffusive flow (for Re/Ro≳O(102) & Re/Fr2<35) and an unstable-diffusive flow (for Re/Fr2>35).
Negatively stretched flames were observed for moderate flow rates and rich mixtures and for high flow rates, flames were positively stretched.
As observed for other flow cytometry parameters, it is usual to observe higher CV with low values (e.g., CD4 counts; [12]).
A highly similar SB release rate into two fat content fluids (2.9 and 4.2 wt%) was observed for identical flow conditions.
Partially stable flames were observed at high velocities for rich mixtures, whereas for lean mixture partially stable flames were observed for all flow rates.
At 900 °C, a mixture of oxynitride (TaON) and nitride (Ta3N5) material phases was observed for lower flow rates (i.e., 50-100 min−1n−1 NH3), whereas a higher amount of the Ta3N5 phase was observed at higher flow rates.
Figure 5a, b show that travel times are highly sensitive to the magnitude of recharge at the surface of the soil; as may be observed, for these flow situations, reducing the recharge rate by half makes the travel times to approximately increase by two times for most of the particles originating on the face OC of Fig. 2a.
The same behavior is observed for VoIP flows (Figure 4) which shows almost a similar performance gain.
Again, standard deviation values of generated streamflows were found to differ from the observed ones in a range of 0.22 % to 27.19 %—higher discrepancy values (32.31 % to 39.67 %) were observed for generated flows for some months (Table 3).
It is found that while shear breakup remains similar for all values of shear rate considered, other breakup modes observed for uniform flows are remarkably modified with increasing shear rate.
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