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  2. 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 ] .

  3. Soil mechanics - Wikipedia

    en.wikipedia.org/wiki/Soil_mechanics

    A phase diagram of soil indicating the masses and volumes of air, solid, water, and voids. ... Consolidation is a process by which soils decrease in volume.

  4. Terzaghi's principle - Wikipedia

    en.wikipedia.org/wiki/Terzaghi's_Principle

    Terzaghi's principle applies well to porous materials whose solid constituents are incompressible - soil, for example, is composed of grains of incompressible silica so that the volume change in soil during consolidation is due solely to the rearrangement of these constituents with respect to one another.

  5. Soil compaction - Wikipedia

    en.wikipedia.org/wiki/Soil_compaction

    In geotechnical engineering, soil compaction is the process in which stress applied to a soil causes densification as air is displaced from the pores between the soil grains. When stress is applied that causes densification due to water (or other liquid) being displaced from between the soil grains, then consolidation, not compaction, has occurred.

  6. Lateral earth pressure - Wikipedia

    en.wikipedia.org/wiki/Lateral_earth_pressure

    An example of lateral earth pressure overturning a retaining wall. The lateral earth pressure is the pressure that soil exerts in the horizontal direction. It is important because it affects the consolidation behavior and strength of the soil and because it is considered in the design of geotechnical engineering structures such as retaining walls, basements, tunnels, deep foundations and ...

  7. Critical state soil mechanics - Wikipedia

    en.wikipedia.org/wiki/Critical_state_soil_mechanics

    where is the equivalent stress, is the pressure, is the pre-consolidation pressure, and is the slope of the critical state line in space. The pre-consolidation pressure evolves as the void ratio ( e {\displaystyle e} ) (and therefore the specific volume v {\displaystyle v} ) of the soil changes.

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  9. Dynamic compaction - Wikipedia

    en.wikipedia.org/wiki/Dynamic_compaction

    Dynamic compaction is a method that is used to increase the density of soils when certain subsurface constraints make other methods of soil compaction inappropriate. The process involves dropping a heavy weight repeatedly on the ground at regularly spaced points, usually laid out in a systematic fashion such as a grid.