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Steep mountain regions can weather faster and produce soil more quickly than previously thought.
Using this approach to produce soil burn severity maps became operational for USDA Forest Service BAER teams on large wildfires in 2002.
The model was applied using two approaches: logistic-BRT as an indirect approach and multiclass-BRT as a direct approach to produce soil class maps.
In Mediterranean Europe climatic variability and human pressure combine to produce soil sealing, erosion, salinisation, fire risk, and landscape fragmentation, all regarded as important factors to start LD.
In this article, we use a multi-scale model for combining all data sources, despite varying resolutions and accuracies, to produce soil maps.
This can be used to produce soil amendments, whose management can be further improved by pelletization that, against technological and environmental advantages, has the disadvantage of requiring a quite high energy input.
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Dark-coloured ferromagnesian (iron- and magnesium-containing) rocks, for example, can produce soils with a high content of iron compounds and of clay minerals in the kaolin or smectite groups, whereas light-coloured siliceous (silica-containing) rocks tend to produce soils that are low in iron compounds and that contain clay minerals in the illite or vermiculite groups.
It produces soil.
Above all, the loess produces soil of extraordinary fertility.
Irrigation by floods or canals permits some cultivation, although intensive irrigation often produces soil salinization.
Excessive grazing and other practices that destroy the grass cover have also produced soil loss.
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