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  2. Soil erosion - Wikipedia

    en.wikipedia.org/wiki/Soil_erosion

    [34] [35] There is growing evidence that tillage erosion is a major soil erosion process in agricultural lands, surpassing water and wind erosion in many fields all around the world, especially on sloping and hilly lands [36] [37] [38] A signature spatial pattern of soil erosion shown in many water erosion handbooks and pamphlets, the eroded ...

  3. Denudation - Wikipedia

    en.wikipedia.org/wiki/Denudation

    Techniques for measuring erosion and denudation include stream load measurement, cosmogenic exposure and burial dating, erosion tracking, topographic measurements, surveying the deposition in reservoirs, landslide mapping, chemical fingerprinting, thermochronology, and analysis of sedimentary records in deposition areas. [26]

  4. Sheet erosion - Wikipedia

    en.wikipedia.org/wiki/Sheet_Erosion

    Sheet erosion or sheet wash is the even erosion of substrate along a wide area. [1] It occurs in a wide range of settings such as coastal plains, hill slopes, floodplains, beaches, [2] savanna plains [3] and semi-arid plains. [4] Water moving fairly uniformly with a similar thickness over a surface is called sheet flow, and is the cause of ...

  5. Erosion - Wikipedia

    en.wikipedia.org/wiki/Erosion

    Splash erosion is generally seen as the first and least severe stage in the soil erosion process, which is followed by sheet erosion, then rill erosion and finally gully erosion (the most severe of the four). [10]: 60–61 [13] In splash erosion, the impact of a falling raindrop creates a small crater in the soil, [14] ejecting soil particles. [4]

  6. Gully - Wikipedia

    en.wikipedia.org/wiki/Gully

    The erosion processes include incision and bank erosion by water flow, mass movement of saturated or unsaturated bank or wall material, groundwater seepage - sapping the overlying material, collapse of soil pipes or tunnels in dispersive soils, or a combination of these to a greater or lesser degree.

  7. Soil structure - Wikipedia

    en.wikipedia.org/wiki/Soil_structure

    Soil mineral particles are both separated and bridged by organic matter breakdown products, and soil biota exudates, making the soil easy to work. Cultivation, earthworms, frost action and rodents mix the soil and decrease the size of the peds. This structure allows for good porosity and easy movement of air and water.

  8. Universal Soil Loss Equation - Wikipedia

    en.wikipedia.org/wiki/Universal_Soil_Loss_Equation

    The Universal Soil Loss Equation (USLE) is a widely used mathematical model that describes soil erosion processes. [1]Erosion models play critical roles in soil and water resource conservation and nonpoint source pollution assessments, including: sediment load assessment and inventory, conservation planning and design for sediment control, and for the advancement of scientific understanding.

  9. Soil mechanics - Wikipedia

    en.wikipedia.org/wiki/Soil_mechanics

    The Leaning Tower of Pisa – an example of a problem due to deformation of soil Slope instability issues for a temporary flood control levee in North Dakota, 2009 Earthwork in Germany Fox Glacier, New Zealand: Soil produced and transported by intense weathering and erosion. Soil mechanics is a branch of soil physics and applied mechanics that ...