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Little information is available concerning the small-scale vertical and horizontal distributions of P and important variables for P binding at the soil profile scale.
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Trees on steep slopes often prevent landslides by binding the soil with the roots, anchoring it to the bedrock and reducing the amount of water it contains.
Take a look at the soil.
Soil compaction can basically be distinguished as (i) soil crusting (formation of a seal at the soil surface) and (ii) subsurface compaction (the formation of a dense soil layer some distance below the soil surface).
Shoots were separated from roots at the soil surface.
Afterwards, each plant was cut at the soil surface.
The binding capacities are pH-dependent, with maximum binding at pH near the protein isoelectric point.
They may then linger in the soil by binding to clay and other minerals.
P soil indicates the soil at Potiguar Basin, and Np soil indicates the non-petroliferous soil.
Has a toxin accumulated in the soil at the center?
In contrast to the others, the soil at Site 2 is a sandy soil.
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