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Compared with a dense soil terrain, a loose soil terrain has better characteristics of energy storage and dissipation.
Soil models with and without consideration of plastic failure are introduced to capture the behavior of loose and dense soil terrain.
Numerous investigators have examined ways in which digital elevation data can be used to define landform-based units that act as basic spatial and structural entities for soil, terrain or ecological maps.
The hypothesized explanatory variables are common economic and demographic drivers and bio-physical factors such as soil, terrain constraints, and neighborhood land-use structures that are often neglected in many large-scale land degradation assessments.
We investigated the influences of soil, terrain, and crop on soil moisture variation in an agricultural landscape at four spatial scales (entire farm of 19.5 ha, landform unit of 0.3 5.1 ha, plot size of 10 × 10 m, and slope transect of 40 × 2 m), in three depths (0.1, 0.4, and 0.8 m), and during two seasons (crop growing vs. non-growing seasons).
Sherbinin [ 24] also uses agricultural constraints like soil, terrain and climate constrains.
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This exploration assesses the capabilities and limitations of the state-of-the-art in tracked vehicle dynamics modeling and simulation over soft-soil terrain.
The combined soil-terrain method outperformed classical stratification schemes in estimating soil moisture time-series over a 4-year period.
The data structure for the description of the land resources was established according to the Soil and Terrain Digital Database (SOTER) manual (Global and National Soils and Terrain Digital Databases (SOTER).
In soil-mantled terrain, models for soil transport and production predict that hillslope adjustment timescales vary nonlinearly with hillslope length; the adjustment timescale for typical settings should vary from 10 000 to 500 000 years, similar to the timescale for glacial interglacial and other climate fluctuations.
The crop yield in extensive agriculture depends primarily on the natural fertility of the soil, the terrain, the climate, and the availability of water.
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