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Two soils were used.
Rill erosion differed between the two soils.
For the other two soils, varying degrees of leaching were observed (Table 4).
These figures illustrate clearly the intrinsic differences in the compression response between the two soils.
The method isolated 76 positive iPSB strains within 72 h from two soils with three replicates.
In the CULS experiment, the normalisation was undertaken separately for the two soils.
Measurements and computational procedures were performed on two soils with varied water contents.
After oxalate or H2O2 treatment, the difference in crack patterns between the two soils became smaller.
Of particular interest is the fact that the indigenous communities of the two soils behaved differently.
Under aerobic conditions, microorganisms in two soils mineralized 58 82% of the added [14C]pyrene.
The two soils amended with nitrate were seen to have enhanced aerobic mineralization rates.
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