Trikliniske

Trikliniske, also known as triclinic crystals, are one of the seven crystal systems in crystallography. They are characterized by having three axes of unequal lengths that are inclined at arbitrary angles to each other. This means that the angles between the axes are not necessarily 90 degrees, and they can vary widely. The unit cell of a triclinic crystal is defined by three vectors of different lengths and three angles between them, all of which are not necessarily 90 degrees.

Triclinic crystals are the most general and least symmetric of the seven crystal systems. This lack of symmetry results in a high degree of anisotropy, meaning that physical properties such as thermal expansion, electrical conductivity, and optical properties can vary significantly with direction. Due to their complex structure, triclinic crystals often exhibit unique and interesting physical behaviors.

Examples of minerals that crystallize in the triclinic system include turquoise, azurite, and some forms of quartz. The triclinic crystal system is also important in materials science, where it is used to describe the structure of certain polymers and other materials.

In summary, triclinic crystals are defined by their three unequal axes that are inclined at arbitrary angles to each other. They are the least symmetric of the seven crystal systems, resulting in a high degree of anisotropy. Examples of triclinic minerals include turquoise and azurite, and the system is also important in materials science.