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Consequently, the deviation in the fractionated concentration of Fe can be attributed to the mobilization of colloids in the borehole.
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In the first step for all 816 triplets, a set of 13 equally fractionated concentrations, from FIC A 0.1 + FIC B 0.1 + FIC C 0.1 to FIC A 1 + FIC B 1 + FIC C 1, were tested in the model, thus yielding ∑FICs from 0.3 to 3. Of these, 360 triplets that resulted in the inhibition of growth at a ∑FIC of <1.2 were advanced for an exhaustive analysis of synergy.
The correlation between size-fractionated concentration of REEs and Al and Fe were not observed in the boreholes (Figures 5 and 8).
The size-fractionated concentration of U in unfiltered 09MI20 groundwater (16 ng/L) was slightly higher than those of 0.2 μm and 10 kDa filtered groundwaters at 14 and 11 ng/L, respectively (Figure 5a).
Thus, the variation in the size-fractionated concentration of Fe in 09MI20 can be explained by the contamination by secondary Fe-bearing colloids formed in the borehole after drilling.
Figure 7 Size-fractionated concentrations of colloid-forming elements from underground fracture seepages.
Figure 10 Size-fractionated concentrations of REEs from water-conducting fractures in excavation walls.
Figure 5 Size-fractionated concentrations of U and colloid-forming elements from the boreholes.
However, the size-fractionated concentrations of Fe in the 09MI20 borehole increased for the smaller membrane pore sizes (Figure 5a).
The size-fractionated concentrations of REEs in borehole groundwaters decreased significantly as membrane pore sizes decreased (Figure 8).
The size-fractionated concentrations of Fe in the 09MI20 borehole varied with the pore size (Figure 5).
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