Sentence examples for flow in soil from inspiring English sources

To analyze spudcan footprint interaction, the coupling of stress/fluid flow in soil should be considered.

The Forchheimer equation (Zeng and Grigg 2006) is adopted to describe nonlinear flow in soil (porous medium).

Preferential flow in soil is approached by a water-content wave, WCW, that proceeds downward from the ground surface.

Figure 13 shows water flow vectors inside stone column which indicates radial drainage of water flow in soil mass to inside the column.

A 2-D Galerkin finite element model was used to compare different approaches for describing macropore flow in soil.

A mathematical relationship between these parameters and the specific deposit was established on the basis of saturated flow in soil equations, some filtration models and experimental results.

Saturated hydraulic conductivity (Ks) is a key input parameter for modeling water flow in soils.

Experimental evidence of variably-saturated flow in soils often shows a non-equilibrium between water content and water potential.

Sophocleous (2002) indicated how the lowering of the water table and decrease in flow in soils near rivers (called the hyporheic zone) causes ecological damage to riparian vegetation.

Because of its significant impacts on ecosystem services and environmental quality, preferential flow in soils has become a crucial issue in both the scientific community and policymaking.

These processes should be considered when interpreting the release of P to overland and subsurface flow in soils of different P concentration.