Momentum of flow in soils assessed with TDR-moisture readings
Momentum dissipation due to viscosity during flow in soils is assessed with TDR-measurements during and shortly after infiltration. One field example demonstrates that about 30% of the momentum applied to the soil surface during infiltration is used to drive flow along presumed macropores to the 0.3...
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Veröffentlicht in: | Geoderma 1997-10, Vol.80 (1), p.153-168 |
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