Uploaded by vergasgran

Mineral Occurrence of Kaolinite

advertisement
Mineral Occurrence
Kaolinite clay occurs in abundance in soils that have formed from the chemical weathering of
rocks in hot, moist climates—for example in tropical rainforest areas.
Kaolinite is one of the most common minerals; it is mined, as kaolin,
in Malaysia, Pakistan, Vietnam, Brazil, Bulgaria, Bangladesh, France, the United Kingdom, Iran, Germany,
India, Australia, Korea, the People’s Republic of China, the Czech Republic, Spain, South Africa, and the
United States.
Formation
Formed by repeating layers of stacks of 1 silica sheet (tetrahedral) and 1 alumina silica sheet
(gibbsite). It is joined by hydrogen bonds. Since hydrogen bonds is very strong, it prevents hydration. As a
result, layers can stack up to make large crystals, up to 70 to 100 layers thick.
Kaolinite is formed by chemical weathering or hydrothermal alteration of aluminosilicate
minerals. Thus, rock rich in feldspar commonly weather to kaolinite. In order to form, ions like Na, K, Ca,
Mg, and Fe must first be leached away by the weathering alteration process. Tis leaching is favored by
acidic conditions (low pH). Granitic rocks, because they are rich in feldspar, are common source for
kaolinite.
Crystallography
Crystal system : Triclinic
Class (H-M): 1-Pedial
Space Group: P1
Cell Parameters:
a = 5.13 A, b = 8.89 A, c = 7.25 A
apha, 91.8°,: beta, 104.5°; gamma, 90.016°
Crystal Structure (pictures)
Differences (descriptions)
Kaolinite also includes dickite and nacrite; formed by the decomposition of orthoclase feldspar
(e.g. in granite); kaolin is the principal constituent in china clay.
Smectites or Montmorillonites also includes bentonite and vermiculite; formed by the alteration of
mafic igneous rocks rich in
Illite also includes glauconite (a green clay sand) and are the commonest clay minerals; formed
by the decomposition of some micas and feldspar; predominant in marine clays and shales.
Note: Kaolinite, illite and smectite pictures, kindly search nalang. Thanks
Physical Properties
Uses
1. China, Porcelain and Tableware
Kaolinite is the main, raw material used in traditional pottery ceramics. The powder is
mixed with clay and other materials in order to make it malleable.
2. Paper Industry
It serves as a paper coating which improves appearance by contributing to brightness,
smoothness and gloss.
It used as a filler, it makes the paper whiter and smoother to print sharper image on.
3. Toothpaste
Kaolin particles are used as a sort of polishing sand to smooth your teeth and ship away
plaque.
4. Pharmaceutical
Used in many pharmaceutical applications as excipient or active ingredient because it
exhibits excellent physical, chemical and surface physiochemical properties
5. Rubber
The composition of the weight percent range of clay (5-35%) to rubber latex (100%) was
feasible to produce durable rubber-clay composite sheets product.
Good mechanical reinforcement.
Low moisture pickup.
6. Paints
Color Performance- improve pigment efficiency, it consequently improves color,
strength, and thus influences color hue
Glass Performance- gloss is the function of filling rate and fineness of kaolin.
Opacity Performance- fine hydrous grades improve pigment efficiency in enamels while
calcined grades increase porosity in architectural paints.
Gel strength- improves in-can stability and avoid settling of pigment or coarse mineral
filler.
Low shear viscosity- provides excellent applicability properties such as brushers and
rollers
7. Adhesive, Sealants and Caulks
Use as economic and functional extender in an acrylic emulsion improving cohesive
strength
Facts






Kaolinite is a clay mineral. It is part of the group industrial minerals
𝐴𝑙2 𝑆𝑖2 𝑂5 (𝑂𝐻)4
Kaolinite is a common 1:1 dioctahedral phyllosilicate (clay) mineral found in soils across
the world
Being a 1:1 clay mineral, each kaolinite layer has one silica tetrahedral sheet and one
alumina octahedral sheet
Mined as kaolin
Origin: Gaoling Mine (Kauling Mine), Gaoling village, Ehu town, Fuliang Co., Jingdezhen,
Jiangxi, China
References
Adam, E. (2019). Minerals Education Coalition-Kaolinite.
Retrieved from:
https://mineralseducationcoalition.org/minerals-database/kaolinite/. Retrieved last April 9,
2019
Amethyst G. (2009). KAOLINITE (Aluminum Silicate Hydroxide).
http://www.galleries.com/Kaolinite. Retrieved last April 9, 2019
Retrieved
from:
Murray,
H.
(1960).
Industrial
Applications
of
Kaolin.
Retrieved
from:
https://pdfs.semanticscholar.org/1ac6/5687f6ac7014cd44dc1fc5ee359242c349f7.
Retrieved
last April 8, 2019.
Barthelmy, D. (2014). Kaolinite Mineral Data, Clays and Clay Miner. Retrieved from:
http://webmineral.com/data/Kaolinite.shtml#.XMXWnhnmhAh. Retrieved last April 9, 2019.
Barak, P. (2005). The Virtual Museum of Minerals and Molecules. Retrieved from: https://virtualmuseum.soils.wisc.edu/display/kaolinite/. Retrieved last April 9, 2019.
Download