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The three soils were dried at 70°C overnight.
210Pb exhibits very dissimilar distribution patterns in all three soils.
The calibrated model was validated using the soil disturbance characteristics measured in those three soils.
Three soils of similar pH and organic matter but with different N availability were used.
The degradation of (RS -ABA was enantioselective foRS -ABAhree soils tested.
Transfer of Pb was small in the three soils and under both hypotheses.
As water content increased, bulk density decreased in all the three soils with increasing levels of peat and FYM.
The distribution pattern of the three soils thus reflects a complex history involving at least three stages of landscape evolution.
Both bulk density and penetration resistance decreased with increasing levels of peat in all the three soils.
The addition of M caused the highest increase in all microbial properties in the three soils, followed by PS.
All three soils showed reasonable agreement with the model, across the range of flow rates and temperatures studied.
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