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In this framework, a constitutive model that gathers the main basic features of soil behaviour was developed.
The profile features of soil moisture (e.g. profile gradient and profile variability) are influenced by different environmental factors.
Ephemeral gullies are important features of soil erosion, yielding large amounts of sediment and dissecting the landscape.
The mean soil moisture is related to both the profile and dynamics features of soil moisture and is controlled by both land use and topography (e.g. aspect, position, slope and relative elevation).
In this study, the coupled ecosystem soil biogeochemistry model GUESS ROMUL is used to explore how the specific features of soil organic matter decomposition and vegetation dynamics account for an observed difference between the soils formed under contrasting moisture conditions.
A real application of the assimilation scheme with satellite-retrieved skin temperature exhibited noticeable positive impacts on the modeling simulation and weather forecast; the model obviously captured meso-scale features of soil moistures as well as the skin temperatures.
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This study developed an accelerated aging method that incorporates features of soiling and weathering.
For the investigation of many geometrical features of soils, computer-assisted image analysis has become a method of choice over the last few decades.
Régnier et al. (2013) defined the parameter fNL to reveal another feature of soil nonlinearity, that is, the shift of the predominant frequency toward lower values.
Based on the definitions of DNL, ADNL, and PNL, all parameters characterize one feature of soil nonlinearity, that is, the reduction in the site response amplitude at high frequency.
Most of the parameters to be identified in the YHyM/BTOPMC are related to physical basin features of land cover and soil.
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