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In subsoil materials, PG degradation was very slow and incomplete.
Higher level of cadmium observed in subsoil is supported by values obtained for the soil texture.
Unlike other metals, the concentration of Cd is higher in subsoil in most of the farms.
We found that the amino sugars appeared to preferentially accumulate in subsoil.
Heavy metal retardation in subsoil can potentially reduce the fate to groundwater by up to 100%.
Long-term organic fertilization may control the accumulation of organic matter in subsoil.
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Nevertheless, the mechanisms controlling the turnover of SOC in subsoils are poorly understood.
Studies on factors controlling C-stability in subsoils are very scarce.
There was no significant difference (P > 0.05) in the levels of these heavy metals in subsoils and among farms.
Urban areas showed the highest spatial variability and specific carbon stocks, 90% of which was stored in subsoils.
The generally high apparent 14C age of soil organic carbon (SOC) in subsoils suggests a high stability against microbial degradation.
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