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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.
The clay is usually a combination of native clays that are suspended in the fluid while drilling, or specific types of clay processed and sold as additives for the WBM system. The most common type is bentonite, called "gel" in the oilfield. The name likely refers to the fluid viscosity as very thin and free-flowing (like chocolate milk) while ...
Phoslock is the commercial name for a bentonite clay in which the sodium and/or calcium ions are exchanged for lanthanum. The lanthanum contained within Phoslock reacts with phosphate to form an inert mineral known as rhabdophane ( LaPO 4 ⋅ n H 2 O {\displaystyle {\ce {LaPO4.{\mathit {n}}H2O}}} ).
The English name reflects the historical use of the material for fulling (cleaning and shrinking) wool, by textile workers known as fullers. [1] [2] [3] In past centuries, fullers kneaded fuller's earth and water into woollen cloth to absorb lanolin, oils, and other greasy impurities as part of the cloth finishing process.
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Mountain soap has the same properties as one of its main varieties: bentonite or montmorillonite. This is a typical clay mineral belonging to the subclass of layered silicates, due to its structure it has the ability to swell strongly. In addition, mountain soap has pronounced sorption properties.
The amount of certain clay minerals that are present, such as montmorillonite and smectite, directly affects the shrink-swell capacity of soil. [2] This ability to drastically change volume can cause damage to existing structures, such as cracks in foundations or the walls of swimming pools.
In sandy soils, the top unfrozen layer becomes waterlogged during thaws, but does not form viscous mud. On the Great Plains, a particular type of clay (bentonite clay, or aluminum phyllosilicate) turns into a sticky mess called gumbo [1] during snowmelt and spring rains. Mud season can be expensive for towns due to the damage done to dirt roads.
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