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India
Contact Person Vijay
Madhapar, Bhuj, Gujarat
Bentonite is an absorbent aluminium phyllosilicate, essentially
impure clay consisting mostly of montmorillonite. There are
different types of bentonite, each named after the respective
dominant element, such as potassium (K), sodium (Na), calcium (Ca),
and aluminium (Al). Experts debate a number of nomenclatorial
problems with the classification of bentonite clays. Bentonite
usually forms from weathering of volcanic ash, most often in the
presence of water. However, the term bentonite, as well as a
similar clay called tonstein, has been used to describe clay beds
of uncertain origin. For industrial purposes, two main classes of
bentonite exist: sodium and calcium bentonite. In stratigraphy and
tephrochronology, completely devitrified (weathered volcanic glass)
ash-fall beds are commonly referred to as K-bentonites when the
dominant clay species is illite. Other common clay species, and
sometimes dominant, are montmorillonite and kaolinite.
Kaolinite-dominated clays are commonly referred to as tonsteins and
are typically associated with coal.
Types
1. Sodium bentonite
1. Calcium bentonite
1. Potassium bentonite
Country: | India |
Model No: | API, Drilling Fluids |
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