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Model parameters were: Residue level, weed control, WSC, profile depth, and rainfall during fallow.
The MTSD was determined to be about mid-way in the soil profile, irrespective of total soil profile depth measured.
Leptosols are soils with a very shallow profile depth (indicating little influence of soil-forming processes), and they often contain large amounts of gravel.
Site-specific conditions (WSC and profile depth) affected water storage during fallow; soils with highest values for both parameters showed highest final AW.
The results show that the relationship between mean profile depth and friction coefficient at different test speed is not close as expected.
Profile depth functions have been used to represent the vertical distribution of soil attributes and to predict them at continuous depths.
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ECa raster maps were obtained for shallow (0 30 cm) and deep (0 90 cm) soil profile depths.
The prediction error for mean θ varied with sampling locations and soil profile depths.
A neural network model was trained to predict soil organic matter content, bulk density and soil organic matter density at different soil profile depths across Scotland.
Data for the three depths showed that infiltrated water was transported successfully to deeper profile depths in the macropore plot, until reaching a depth of 50 cm.
[14] To best approximate deposit thickness, we used the mean profile depths of the sampled Yedoma and thermokarst deposits.
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