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Many agricultural activities result in the movement of soil.
The horizontal movement of soil can lead to tillage erosion.
A slight movement of soil has been observed prior to most landslides, earthquakes, and slope failures.
To prevent offsite movement of soil particles, many environmental regulatory agencies mandate the use of perimeter silt fences.
To date, tillage erosion studies have focused primarily on the movement of soil by primary and secondary tillage operations.
A key feature of the concept is the relatively price efficient design where the main cost is movement of soil.
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For example, pocket gophers and certain ground squirrels that burrow horizontal tunnels on sloping grounds seem to have significant impacts on horizontal movement of soils, whereas prairie dogs and harvester ants have more impact on vertical movement of soils.
It is now widely recognized that decomposition, mineralization, and plant-fungal mutualisms regulate the movement of soil-borne elements into the plant roots.
Furthermore, this barrier may impede the movement of soil-derived toxins (i.e., reduced metal ions) and gases (e.g. methane, CO2, and ethylene) into the roots (Armstrong 1979; Colmer 2003a; Greenway et al. 2006).
In contrast, except for instances involving uprooted trees or movement of soil-burrowing animals, AMF are generally not exposed to soil disturbances of this scale.
The interaction between vertical and lateral movements of soil constituents by tillage needs to be addressed to better understand the transfer processes of soil constituents on a hillslope.
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