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Except for Se, the maximum concentrations of all selected COCs (Hg, B, Mo, As, Ba, Cd, Cr, Pb, Sb, Co, and Tl) under all tested leaching conditions were lower than the toxicity levels.
The values of Cs2− and κ under aerobic conditions were lower than those under anaerobic conditions, and the pH values increased from O2- to air- to N2-saturated culture solutions.
Under the typical operating conditions that exist in a CLC system, with particle sizes lower than 0.3mm, 40wt% of metal oxide content, and overall conversion times lower than 30s, the increases of temperature with respect to the bulk conditions were lower than 15K for any reaction of any oxygen carrier.
The findings for our experimental participants under all conditions were lower than those for the control group (Fig. 2c).
[Tsuji et al. (2006]) reported that the levels of inorganic N and N mineralization after summer cropping in no-till conditions were lower when the aboveground residue was removed, which explained why yields of winter crop were lower under residue removal conditions.
The average GFP brightness value of this dominant complex under these conditions were lower than that in cycling cells; this decrease was statistically significant at the 95% level for high salt conditions relative to wt (p��= 0.05) but not at the 95% confidence limit for α-factor treated cells (p = 0.11).
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Coke amount at different reaction conditions was lower than 0.7%.
These temperature and pressure conditions are lower than those for typical shales of current interest.
Because metamorphic fluids (dominantly composed of water and carbon dioxide) are less dense than rocks, the fluid pressure at these conditions is lower than the lithostatic pressure.
As the period decreases, reaction rates fall off indicating that time-average rates under transient conditions are lower than those acheived at quasi-steady state.
The comparison of the RTD curves between the isothermal and non-isothermal conditions presents that the extent of mixing in the tundish in nonisothermal conditions is lower than the mixing extent in isothermal conditions.
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