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In the past, modelling has focused on Darcy flow of soil gas (driven by indoor outdoor pressure differences) and combined diffusive and advective transport of radon.
Modeling soil-tillage interaction is a complex process due to dynamic soil-implement interaction which includes a high rate of plastic deformation and soil failure, characterized by the flow of soil particles.
Mass flow of soil air compensated for the wind-driven pressure gradients, and increases in CO2 fluxes exceeding a factor of 2 were observed in response to wind events even under a dense forest canopy.
Particular attention is given to small pressure gradients between the chamber headspace and the external environment that may induce mass flow of soil air, leading to overestimation of soil respiration.
Wind induces a ground-surface pressure field around a building that can substantially affect the flow of soil gas and thereby the entry of radon and other soil-gas contaminants into the building.
So that, flow of soil water through the soil section increases the calcium and carbonate content of the percolated water.
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This material moves in a semifluid condition and is manifested by lobelike and sheetlike flows of soil on slopes.
Many external effects of land use change are based on modifications of lateral flows of soil, water, air, fire or organisms.
The adsorption can decrease the 137Cs content (including 137Cs bound to water-soluble organic substances) in the solution phase, resulting in little transfer of 137Cs along the mass flow of the soil water in mineral soils.
This study was designed to assess the effect of different management practices on the water flow behavior of soil.
We thus analysed the variations in the pedological, herbicide sorption and flow properties of soil materials along a 2D cross-section of an intermittently flooded ditch in the Roujan catchment of southern France.
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