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BEAMS parameterizes soil decomposition as a function of soil temperature and water content i.e. CENTURY.
Soil water conditions are a function of soil properties, available water from precipitation, and evapotranspiration.
Figure 6(c) shows the hydraulic conductivities as a function of soil suction.
The infiltration rate is a core of the model and expressed as a negative exponential function of soil wetness.
This catabolic gene selection through earthworm soil bioturbation could be important in sustaining the degradation (detoxification) function of soil.
The duration of phase 2 is a function of soil (type, permeability, and sensitivity) and pile (type, permeability, and size) properties.
In the third model, the soil respiration rate is the function of soil temperature and soil water content (Saiz et al. 2006; Sheng et al. 2010).
Soil water content is a function of soil matric potential ψ under equilibrium conditions, and this relationship θ can be described by different types of water retention curves.
The characterization of both concentration and composition will contribute to a better understanding of processes in soil and function of soil WEOM in agricultural system.
In the original MINoSGI, Rh was given as a function of soil temperature without considering carbon cycling in the soil [28].
Surfactant effects on water infiltration and on percolation in soils are a function of soil type and surfactant characteristics (Kuhnt 1993).
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