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  2. Shrink–swell capacity - Wikipedia

    en.wikipedia.org/wiki/Shrinkswell_capacity

    The shrinkswell capacity of soils refers to the extent certain clay minerals will expand when wet and retract when dry. Soil with a high shrinkswell capacity is problematic and is known as shrinkswell soil, or expansive soil . [ 1 ]

  3. Expansive clay - Wikipedia

    en.wikipedia.org/wiki/Expansive_clay

    Soils with a high content of expansive minerals can form deep cracks in drier seasons or years; such soils are called vertisols. Soils with smectite clay minerals, including montmorillonite and bentonite, have the most dramatic shrinkswell capacity. The mineral make-up of this type of soil is responsible for the moisture retaining capabilities.

  4. Marine clay - Wikipedia

    en.wikipedia.org/wiki/Marine_clay

    These marine clays can be what are known as quick clays, which are notorious for its erosive properties. A great example of these quick clays is in the Pacific Northwest. They are known as blue goo which is a mix of clay and mélange (greenstone, basalt, chert, shale, sandstone, schists. uplifted through the accretionary wedge).

  5. Physical properties of soil - Wikipedia

    en.wikipedia.org/wiki/Physical_properties_of_soil

    A high bulk density is indicative of either soil compaction or a mixture of soil textural classes in which small particles fill the voids among coarser particles. [52] Hence the positive correlation between the fractal dimension of soil, considered as a porous medium , and its bulk density, [ 53 ] that explains the poor hydraulic conductivity ...

  6. Atterberg limits - Wikipedia

    en.wikipedia.org/wiki/Atterberg_limits

    The plasticity index is the size of the range of water contents where the soil exhibits plastic properties. The PI is the difference between the liquid and plastic limits (PI = LL-PL). Soils with a high PI tend to be clay, those with a lower PI tend to be silt, and those with a PI of 0 (non-plastic) tend to have little or no silt or clay.

  7. Soil compaction - Wikipedia

    en.wikipedia.org/wiki/Soil_compaction

    Soils with high shrinkswell capacity, such as vertisols, recover quickly from compaction where moisture conditions are variable (dry spells shrink the soil, causing it to crack). But clays such as kaolinite , which do not crack as they dry, cannot recover from compaction on their own unless they host ground-dwelling animals such as ...

  8. These 10 Products Are Most at Risk for 'Shrinkflation' - AOL

    www.aol.com/10-products-most-risk-shrinkflation...

    Let's look at some consumer survey data from Clarify Capital to see which product categories are most likely to "shrink" in 2024. Top 10 products affected by shrinkflation

  9. Bentonite - Wikipedia

    en.wikipedia.org/wiki/Bentonite

    Bentonite layers from an ancient deposit of weathered volcanic ash tuff in Wyoming Gray shale and bentonites (Benton Shale; Colorado Springs, Colorado). Bentonite (/ ˈ b ɛ n t ə n aɪ t / BEN-tə-nyte) [1] [2] is an absorbent swelling clay consisting mostly of montmorillonite (a type of smectite) which can either be Na-montmorillonite or Ca-montmorillonite.