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The data presented here demonstrate that land degradation (in the form of soil erosion) can be minimized significantly if appropriate and large scale soil and water conservation interventions are carried out, which are tailored to the biophysical setting.
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As direct measurements of solute transport are not practical at large scales, soil susceptibility to preferential flow and transport has to be estimated using proxy variables.
At a larger scale, soil fauna affects leaching and the release of particulate organic matter (POM), which in turn affect microbial activity in soil.
Alternatively, governments or the African Union could fund large-scale soil map to accelerate precision farming.
However, large-scale soil erosion model-factor parameterization and quantification is difficult due to the costs, labor and time involved.
However, Ks data are often lacking at large-scale soil database due to difficulties in direct measurement that is often labour intensive, time consuming and cost inefficient.
Large-scale soil disturbances due to surface mining for coal have removed nearly one million hectares of native forests in the eastern deciduous forests of North America.
Effects of earthworms on soil abiotic properties are well documented from several decades of laboratory and mesocosm experiments, and they are supposed to affect large-scale soil ecosystem functioning.
The encouraging results of our analysis suggest that time stability analysis may be an effective way to assess large-scale soil water storage in arid and semi-arid regions.
The changing nature of human interference, potentially as a response to underlying climatic transitions, is evident through large-scale soil depletion resulting from grazing and land clearance during the early LIA and stabilization of arable lands during the late and post-LIA eras.
This study is a first step in the implementation of large-scale soil moisture validation using existing networks such as the Soil Climate Analysis Network (SCAN) and several Agricultural Research Service watersheds as a basis for calibrating satellite soil moisture products, for networks design, and designing field experiments.
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