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Windblown sand dunes are common, and soil distribution over bedrock is light and uneven.
In climates with significant precipitation and periods of annual warming, the soil distribution may be highly discontinuous.
Figure 11 Reclassified DEM and Soil distribution map developed.
As a result, recent studies examining the spatial representation and rice soil distribution are limited.
The results are of significance for highway engineering in cold regions with extensive saline soil distribution.
The aim is to reproduce the original map and predict soil distribution in the adherent landscape.
Pedometrics is the use of quantitative methods for the study of soil distribution and genesis.
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Medium cartographic scale maps have put more emphasis on parent material as a variable to explain soil distributions.
Moreover, the method is satisfactory for obtaining soil types from 3D spectral sensing as well as evaluating the catena development and other spatial soil distributions.
Borehole data and hydrological models indicate that these soil-distribution patterns are strongly related to groundwater occurrence and fluvial processes, both of which are generally governed by topography.
The simplified soil map and field study of soil morphology reveal a number of soil-distribution patterns associated with specific topographic settings.
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