What are clay minerals?
clay minerals are found in several different types of land. They are considered part of the Phyllosilicates family. There are four different categories of clay minerals. These categories include kaolinities, illites, Smectites and vermiculites.
Minerals of soil clay alumina may impress the sandy appearance and feeling. One of the properties of clay minerals, silicate, is present in most beach sand. It gives sand its granulated and smooth softness. The color of the most silicate, such as the soil, tends to be light brown, gray or white, while some silicates accept a pinkish shade.
Phyllosilicates tends to contain a large amount of water. This is one of the reasons why the beach sand begins to feel damp and cold when it is dug. In fact, the water is contained in the baptismal leaves that form the structure of the clay. The clay mine is usually not isolated in the natural environment. It will usually be mixed with some other form of clay or crystal such as a form or quartz. OneThese groups are called kaolinity. These minerals consist of silicate and aluminum or hydroxide oxide. They are usually used in print papers, plastics and colors as a fill.
The second group of minerals is called Illites. Silicate and potassium are combined in a unique composition to create illusions. The clay minerals that fall into this group are used as fillers.
Smektities are a group that consists of layers of silicates and gibbsites. More well -known minerals in this group include ointment and saponite. They are used as fillings, in personal hygiene powders and porcelain.
The largest family Clay minerals are vermiculits or chlorites. Many minerals in this group are not commonly known as the name. The silicate is usually combined with iron, aluminum, magnesium or zinc. This group of minerals is usually not used to produce commercial materials.
are also katEgorized according to two different ratios. Minerals can be classified as one to one to one or two ratio to one. These conditions apply to types of silicate layers that exist in the structure of minerals called tetrahedral and octahedral. The ratio of one to one indicates that the structure is formed by one of each layer type, while the ratio of two to one indicates only one octahedral and two tetrahedral layers.