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These processes produce the characteristic soil profile. They are defined as soils containing at all depths no more than ten percent weatherable minerals , and low cation exchange capacity . Oxisols are always a red or yellowish color, due to the high concentration of iron (III) and aluminium oxides and hydroxides .
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This is a list of open-access journals by field. The list contains notable journals which have a policy of full open access. It does not include delayed open access journals, hybrid open access journals, or related collections or indexing services.
When soil is irrigated with high salinity water or sufficient water is not draining out from the irrigated soil, the soil would convert into saline soil or lose its fertility. Saline water enhance the turgor pressure or osmotic pressure requirement which impedes the off take of water and nutrients by the plant roots.
It is of use in distinguishing boundaries of horizons within a soil profile, [110] determining the origin of a soil's parent material, [111] as an indication of wetness and waterlogged conditions, [112] and as a qualitative means of measuring organic, [113] iron oxide [114] and clay contents of soils. [111]
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Field capacity is characterized by measuring water content after wetting a soil profile, covering it (to prevent evaporation), and monitoring the change soil moisture in the profile. A relatively low rate of change indicates when macropore drainage ceases, which is called Field Capacity; it is also termed drained upper limit (DUL).
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