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BEAMS parameterizes soil decomposition as a function of soil temperature and water content i.e. CENTURY.
Figure 6(c) shows the hydraulic conductivities as a function of soil suction.
Soil water conditions are a function of soil properties, available water from precipitation, and evapotranspiration.
The duration of phase 2 is a function of soil (type, permeability, and sensitivity) and pile (type, permeability, and size) properties.
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.
In the original MINoSGI, Rh was given as a function of soil temperature without considering carbon cycling in the soil [28].
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Next, an analytical expression of an OWT natural frequency is presented as a function of soil-monopile interaction through monopile head springs characterized by lateral stiffness KL, rotational stiffness KR and cross-coupling stiffness KLR, of which the differences are discussed.
The SCS curve number is a function of the soil's permeability, land use and antecedent soil water conditions (Arnold et al. 2012).
On the other hand, soil aggregate stability is a function of different soil management factors such as tillage frequency (Masri and Ryan 2006), intensity of grazing (de Souza et al. 2010) and land use change (Gajić et al. 2013).
The AC values decreased and increased as a function of increasing soil pH and foc, respectively.
The initial state of stress was defined as the measured swelling pressure which is a function of the soil depth.
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