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The major part of this load originates from diffuse land-based sources, e.g. arable soil leaching.
All waters used for irrigation purposes contain some amount of dissolved salt (salinity) which generally comes from weathering of soil, leaching of salts dissolved from geologic marine sediments into the soil solution or groundwater, and flushing of salts off roads, landscapes and stream banks during and after precipitation events.
These changes result primarily from increasing loss of silica and soluble metals as soil leaching extends deeper with increasing rainfall.
Weathering effects are weak in the stream, although effects of soil leaching and runoff are evident.
Irrigation water from King Abdullah Canal (KAC) was used for soil leaching.
Soil leaching is the main factor that contributes to the Cu concentration as suggested by Simeonov et al. (2003).
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Irrespective of sterilization, composts and biochar successfully remediated a saline sodic soil leached with reclaimed water.
The peat soil leached less DOC (0.37 mg g−1) than the vegetation and was less sensitive to climate.
The climatic influences are reflected in the dominance of red-yellow podzolic soils (leached lateritic soils) in the Wet Zone and of reddish brown earths (nonlateritic loamy soils) in the Dry Zone.
Thick Fe-coatings on particles and within the pores of soils leached with AMD change their micro-aggregation and so inhibit the dissolution of phyllosilicates.
Soil leaches were used as a technique to estimate the composition of the Zn pool available to the plants [ 21, 27].
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