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  2. Soil mechanics - Wikipedia

    en.wikipedia.org/wiki/Soil_mechanics

    A variety of sieve sizes are available. The boundary between sand and silt is arbitrary. According to the Unified Soil Classification System, a #4 sieve (4 openings per inch) having 4.75 mm opening size separates sand from gravel and a #200 sieve with an 0.075 mm opening separates sand from silt and clay. According to the British standard, 0. ...

  3. Internal erosion - Wikipedia

    en.wikipedia.org/wiki/Internal_erosion

    Internal erosion is the formation of voids within a soil caused by the removal of material by seepage. [1] It is the second most common cause of failure in levees and one of the leading causes of failures in earth dams, [2] responsible for about half of embankment dam failures.

  4. Soil consolidation - Wikipedia

    en.wikipedia.org/wiki/Soil_consolidation

    Soil consolidation refers to the mechanical process by which soil changes volume gradually in response to a change in pressure. This happens because soil is a three-phase material, comprising soil grains and pore fluid, usually groundwater [ clarification needed ] .

  5. Coastal hydrogeology - Wikipedia

    en.wikipedia.org/wiki/Coastal_hydrogeology

    This aquifer system is similar to an unconfined continental coastal aquifer. There is a seepage zone in this case. Seepage would shift the interface towards the sea. The seawater within the seepage zone may have a slightly different chemical composition compared with seawater away from seepage zone. Unconfined Circular Island Aquifer

  6. Seep (hydrology) - Wikipedia

    en.wikipedia.org/wiki/Seep_(hydrology)

    Seep is often used in environmental sciences to define an exfiltration zone (seepage zone) where contaminated water, e.g., from waste dumps, leaves a waste system area. Seeps are often important smaller wildlife water sources, and indicated by lower riparian vegetation.

  7. Soil chemistry - Wikipedia

    en.wikipedia.org/wiki/Soil_chemistry

    Soil chemistry is the study of the chemical characteristics of soil.Soil chemistry is affected by mineral composition, organic matter and environmental factors. In the early 1870s a consulting chemist to the Royal Agricultural Society in England, named J. Thomas Way, performed many experiments on how soils exchange ions, and is considered the father of soil chemistry. [1]

  8. Dispersion (geology) - Wikipedia

    en.wikipedia.org/wiki/Dispersion_(geology)

    The best management approach to these soils is simply to avoid their disturbance. Maintaining vegetation cover of the soil is also important to minimize soil dispersion. [5] In agricultural systems, this may mean making an effort to prevent surface soil loss and/or damage, as the surface soil and ground cover form a protective barrier.

  9. Leachate - Wikipedia

    en.wikipedia.org/wiki/Leachate

    The filter layer is used above the drainage layer in leachate collection. Two types of filters are typically used in engineering practices: granular and geotextile. Granular filters consist of one or more soil layers or multiple layers having a coarser gradation in the direction of the seepage than the soil to be protected.