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fertilizer broadcasted and incorporated in soil (field).
Soil field experiments usually consist of measurements of soil temperatures, heat fluxes and soil water contents.
Soil field capacity in 0 20 cm layer was higher than that in 20 40 cm layer (Fig. 2).
A total draught of this plough was measured at 39.5 kN on the black soil field and 29.8 kN on the brown soil field including the tractor running resistance.
The genotypes were evaluated under different soil field capacity (FC) levels (80%, 50 %, 30 and 20%and20
The soil field capacity was estimated by a water retention curve, and the humidity at this point corresponded to 24% water in the soil.
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The remaining 17 locations correspond to bare soil fields.
Within these soil fields, a single loop HGHE was modelled as discrete pipes placed in a heterogeneous soil continuum.
Ensembles of heterogeneous soil fields were generated with spatial correlation parameters derived from similar studies of heterogeneity in hydraulic parameters.
To remediate the adverse effects and chemical accumulation of active metabolites of applied insecticides in soil fields, different control methods are in use.
For most soils, field capacity was estimated at the water potential of – 10 to − 33 kPa (Brady and Weil 2008).
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